ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Other Sources  (45,640)
  • 2020-2024  (8,071)
  • 2005-2009  (35,988)
  • 1940-1944  (1,581)
Collection
Language
Years
Year
  • 1
    Publication Date: 2020-10-05
    Description: Die Bibliografische Datenbank GeoRef und die Virtuelle Fachbibliothek GEO-LEO eignen sich bei paralleler Nutzung für eine weitgehend erschöpfende Informationsrecherche im Bereich Geowissenschaften. Während GeoRef im Wesentlichen als Nachweisinstrument für Zeitschriftenartikel dient, werden bei GEO-LEO Bibliothekskataloge abgefragt und digitale Volltexte verfügbar gemacht. Der direkte Dokumentzugriff und die Verzeichnung von Webseiten, ein Instrument zur Erkundung von Wissen durch systematische Darstellung von Einzeldisziplinen und eine Publikationsplattform bei GEO-LEO ergänzen sich mit hervorragender Erschließung und großer thematischer Abdeckung bei GeoRef.
    Description: study
    Keywords: 551 ; V 200 ; Geowissenschaften ; Virtuelle Bibliothek ; Literaturdatenbank ; Vergleich ; 38.04
    Language: German
    Type: article_first
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    facet.materialart.
    Unknown
    Universitätsverlag Göttingen
    Publication Date: 2020-10-05
    Description: For about four decades marble has been used as thin veneer cladding. The durability of such thin slabs (mostly 30-40 mm) is satisfactory at most constructions. However, on numerous buildings all over the world, the long-term deformation (expansion, bowing) of some claddings is associated with structural weakening and strength loss which led to an inevitable restoration of the affected facades and to an image problem of marble used as a structural building stone. Up to now, the existing knowledge about the causes for this special kind of marble weathering is mostly restricted to research on Carrara marble and to the effect of individual parameters. This thesis presents the first study of the combined influence of extrinsic (environmental) and intrinsic (material specific) parameters on marble bowing. The respective impact of these factors on the weathering process is elucidated by damage mapping of four different marble facades. The work focuses on the influence of the microfabric on the damage dynamics of veneer marble and particularly considers moisture as an essential climatic parameter. In order to characterize and understand the weathering process, an array of different marble samples had to be studied with regard to their petrographic, rock physical and microstructural properties. Besides both fresh and artificially weathered marble samples this survey also included demounted façade panels from the investigated buildings with varying degrees of pre-deterioration...
    Description: Die seit etwa vier Jahrzehnten dauernde Verwendung von Marmor als dünnplattige Fassadenverkleidung hat weltweit an zahlreichen Gebäuden zu Problemen mit der Langzeitstabilität solcher Fassaden geführt. Das dabei oft auftretende Phänomen des Verbiegens von Marmorplatten geht mit einer Materialentfestigung einher, was langfristig die Sanierung der betroffenen Fassaden zur Folge hat und mittlerweile ein Imageproblem für den Werkstoff Marmor darstellt. Die bislang vorhandenen Kenntnisse zu den Ursachen dieser speziellen Form der Marmorverwitterung beschränken sich meist auf Untersuchungen an Carrara Marmor und auf die Wirkung einzelner Faktoren. In der vorliegenden Arbeit wurde der kombinierte Einfluss von umweltbedingten (extrinsischen) und materialspezifischen (intrinsischen) Parametern untersucht. Ihr Wirkungsgrad wird am Beispiel von vier Schadenskartierungen an Marmorfassaden aufgezeigt. Der Schwerpunkt liegt auf dem Einfluss des Mikrogefüges auf die Schadensdynamik von Fassadenmarmor unter besonderer Berücksichtigung der Feuchtigkeit als essentieller Klimafaktor. Basis für die Charakterisierung und Interpretation des Verwitterungsprozesses ist die Erfassung von petrographischen, gefügekundlichen und petrophysikalischen Eigenschaften an bruchfrischen und künstlich verwitterten Marmorproben sowie an demontierten Fassadenplatten unterschiedlicher Vorschädigung von den untersuchten Marmorfassaden...
    Description: thesis
    Keywords: 551 ; VKB 210 ; VBP 200 ; RVC 810 ; VAE 130 ; ZTI 000 ; VAH 000 ; VKA 170 ; Fassade ; Marmor ; Gefüge 〈Gesteinskunde〉 ; Petrophysik ; Physikalische Verwitterung ; Deformation 〈Geologie〉 ; 38.25 ; 56.47 ; 38.58
    Language: German
    Type: monograph , publishedVersion , monograph
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    facet.materialart.
    Unknown
    Universitätsverlag Göttingen
    Publication Date: 2020-10-05
    Description: Seit nunmehr 20 Jahren findet regelmäßig alle zwei Jahre das Symposium ‚Tektonik — Strukturgeologie — Kristallingeologie‘ (TSK) statt. Die Tagung soll insbesondere jungen Nachwuchswissenschaftlern die Möglichkeit bieten, ihre Ergebnisse zu diskutieren und einem breiten Fachpublikum vorzustellen. Dies ist natürlich besonders attraktiv, wenn auch die ‚alten Hasen‘ der Zunft eifrig dabei sind. In diesem Jahr wird schon TSK 11 — nach Tübingen, Erlangen, Graz, Frankfurt, Salzburg, Freiberg, Freiburg und Aachen nun zum zweiten Mal nach 1994 wieder in Göttingen durchgeführt. Wir freuen uns, auch dieses Mal wieder ein vielseitiges Tagungsprogramm präsentieren zu können. Die vorgestellten Arbeiten befassen sich mit Geländebeobachtungen, Laboranalysen und -experimenten bis hin zu Computermodellierungen. Im Maßstab reichen sie vom submikroskopischen Bereich bis hin zu ganzen Orogenen. Dabei werden sowohl duktile als auch spröde Deformationsprozesse beleuchtet. Regionale Geologie ist ebenso Thema wie auch eher angewandte Fragestellungen. Um die einzelnen Beiträge schnell auffinden zu können, wurden diese alphabetisch nach Erstautoren geordnet. Aus Zeitgründen konnte nur der kleinere Teil der mehr als einhundert eingegangen Beiträge in das Vortragsprogramm aufgenommen werden. Auf parallele Vortragssitzungen haben wir bewusst verzichtet. Besonderen Raum für anregende Diskussionen sollen auch die thematisch zusammengestellten Postersitzungen bieten, für die wir spezielle Zeiten eingeräumt haben. Hierzu werden Poster jeweils vorher im Plenum kurz vorgestellt. Die eingegangenen Manuskripte wurden, wie bei TSK üblich, für die Publikation keinem Gutachterverfahren unterzogen. Daher sind die jeweiligen Autoren allein für den Inhalt verantwortlich. Wir wünschen allen Teilnehmenden anregende Diskussionen und interessante Kontakte sowie einen schönen Aufenthalt in der ‚Stadt, die Wissen schafft‘!
    Description: conference
    Keywords: 551 ; VAE 000 ; VAC 100 ; Tektonik ; Strukturgeologie ; Kristallin ; Kongress ; 38.36 ; 38.37
    Language: German
    Type: anthology , publishedVersion
    Format: 273 S.
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2020-10-05
    Description: Bohrlochgeophysikalische Messungen haben seit Jahrzehnten einen festen Platz in der Hydrogeologie und in jüngster zeit auch in der Umweltgeologie. Die meisten Meßverfahren sind vor ihrer Anwendung in diesen Bereichen für die Zwecke der Erföl- und Erfdgaserschließung entwickelt worden. Die Meßeinrichtungen sind daher im Regelfall auch unter ungünstigen Bedingungen (hohe Drücke und Temperaturen, agressive Medien) einsetzbar und eignen sich auch unter den Bedingungen von Altdeponien und anderen Altlasten... Die vorliegende Schrift soll daher nur einen kurzen Überblick über die technischen Möglichkeiten der Meßverfahren geben. Der Schwerpunkt liegt bei der Erörterung der heute im Bereich Hydro- und Umweltgeologie häufig verwendeten Verfahren und ihrer Eignung in der Bearbeitung ingenieurtechnischer Fragestellungen. Hierbei ist insbesondere zu berücksichtigen, daß Planung, ingenieurtechnische Betreuung und Auswertung dieser Messungen im Regelfall nicht in der Hand von speziell geophysikalisch geschulten Fachleuten liegen, sondern von Geologen und Bauingenieuren ohne besondere Vorkenntnisse. Diesen sollen hiermit Anhaltspunkte für den praktischen Einsatz der gängigen Verfahren gegeben werden, aber auch die Grenzen dessen, was der Laie ohne Hinzuziehung eines Geophysikers veranlassen und aussagen kann, aufgezeigt werden...
    Description: manual
    Keywords: 550.28 ; 622.159 ; 550 ; TQG 000 ; VBQ 100 ; VBS 100 ; Geophysikalische Bohrlochmessung ; Methodik, Untersuchungsverfahren und Instrumente ; Methodik, Untersuchungsverfahren und Instrumente ; Bohrlochmessung ; 38.79 ; 38.03 ; 38.86
    Language: German
    Type: monograph , monograph
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    facet.materialart.
    Unknown
    Duehrkohp & Radicke, Göttingen
    Publication Date: 2021-03-29
    Description: Der pazifische Inselstaat Fiji (Fidschi) ist in den letzten 20 Jahren wiederholt von teils gewaltsamen, teils weitgehend friedlichen politischen Auseinandersetzungen, Machtwechseln und Umstürzen bestimmt worden. Dieser Beitrag diskutiert, inwieweit die ethnische Zusammensetzung aus indigenen Fijianern und indischstämmigen Bewohnern einflussreich auf die derzeitige Situation im Land ist. Nach einer Analyse der systemischen und sozialen Aspekte zur Einschätzung der Integration von Indern und Fijianern in Fiji lässt sich zusammenfassend feststellen, dass in Fiji nicht von Integration, sondern eher von Desintegration gesprochen werden muss. Es stellt sich aber die Frage, ob Integration bzw. zu welchem Grad Integration für ein gesellschaftliches Zusammenleben eine Notwendigkeit ist. Denn Integrationsbestrebungen können unterschiedliche Ziele verfolgen: Einerseits können sie zur Herstellung einer tatsächlichen gesellschaftlichen Einheit dienen, in der Unterschiede nicht länger wahrgenommen werden und dadurch Gleichberechtigung herrscht. Dann kann nach erfolgter sozialer und kultureller Integration von Zuwanderern von vollständiger Assimilation gesprochen werden. Andererseits kann Integration zur Förderung eines Multikulturalismus angestrebt werden, wenn ethnische Gruppen ihre kulturellen Eigenarten wie z.B. ihre Sprache beibehalten. Dann entwickelt sich bei fortschreitender sozialer Integration eine stärker pluralistische Gesellschaft und es kann lediglich von formeller Integration oder struktureller Assimilation gesprochen werden. Dabei dient die gegenseitige Anerkennung von Unterschieden als Voraussetzung für das Erreichen eines gemeinsamen Zieles. Der Überblick über die diskutierten Aspekte von Integration in Fiji kommt dieser Variante recht nahe.
    Description: Causes and Effects of Ethnic Conflicts in the Pacific: Social Disintegration in the Fiji Once again ethnic and political tensions in Fiji have lead to social and economic instability and to an international isolation of the country. In the year 2000, for the second time after 1987 the legitimately elected government was deposed in a coup d´état. The reasons for this were the nomination of an Indo-Fijian Prime Minister and the domination of the government parties by an Indo-Fijian majority. The elections in August 2001, however, resulted in a majority of votes in favour of the indigenous Fijians who one again dominate the present government. The current political events in Fiji reflect a society which is split into two ethnic main groups (Fijians 51%, Indo-Fijians 43%, Others 6%, FIJI ISLANDS BUREAU OF STATISTICS 2001). The social stratification and the spatial segregation of these groups have been strengthened, the economic effects are drastic and the perspectives for a multi-cultural society have been postponed indefinitely. The social disintegration of the Indo-Fijians is due to historical, economic, political and cultural factors. In order to understand the background of the conflicts and to describe the effects as well as the perspectives for the entire Fijian society, the causes are discussed with the help of the concepts of “Integration” by TALCOTT PARSONS (1976; 1980) and HARTMUT ESSER (2001).
    Description: research
    Keywords: 910 ; QGY 544 ; QG 250 ; QEA 000 ; Fidschi-Inseln {Geographie} ; Entwicklungsländer {Geographie} ; Sozialgeographie im engeren Sinn ; Soziale Integration ; Politische Geographie ; Minderheitenfrage ; Systemintegration ; 74.27 ; 74.09
    Language: German
    Type: article , publishedVersion
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2021-03-29
    Description: Die Bilder und Meldungen der letzten Wochen aus Bolivien, Ecuador und Peru vermitteln den Eindruck, dass politische Instabilität sukzessive von einem auf den anderen zentralen Andenstaat übergreift. Hauptakteure sind wütende Volksmassen und hilflose Regierungen, die sich als Konfliktparteien gegenüberstehen. Während Carlos Mesa im bolivianischen La Paz als Präsident zurücktrat und prophezeite, dass ein Scheitern des Reformprozesses die Unregierbarkeit Boliviens zur Folge hätte, zogen in Ecuador Tausende Demonstranten durch die Straßen Quitos und erzwangen die Amtsenthebung von Staatschef Lucio Gutiérrez. In Lima und Umland sinken derweil die Popularitätswerte des Präsidenten Alejandro Toledo unter zehn Prozent. Dieser Beitrag skizziert wesentliche Merkmale der politischen und zivilgesellschaftlichen Auseinandersetzung in Peru und Bolivien, unter Einbeziehung der aktuellen Entwicklungen in Ecuador.
    Description: research
    Keywords: 910 ; QFK 000 ; QFK 300 ; QFK 400 ; QEA 240 ; QEI 000 ; QGX 100 ; QGX 120 ; QGX 503 ; QGX 530 ; QGX 544 ; QGX 543 ; QGX 542 ; Entwicklungsländerforschung {Anthropogeographie} ; Entwicklungsstrategien, Entwicklungshilfe {Entwicklungsländerforschung} ; Empirische Entwicklungsländerforschung ; Sozialgeographische Gruppen {Sozialgeographie} ; Politische Geographie, Geopolitik ; Lateinamerika {Geographie} ; Kulturgeographie Lateinamerikas ; Kulturgeographie von Südamerika ; Tropische Andenländer {Geographie} ; Bolivien {Geographie} ; Peru {Geographie} ; Ecuador mit Galapagos-Inseln {Geographie} ; Bolivien ; Ecuador ; Peru ; Integration ; Regierbarkeit ; Multikulturelle Gesellschaft ; Minderheitenfrage ; Politische Geographie ; 74.26 ; 74.10 ; 74.09
    Language: German
    Type: article , publishedVersion
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    facet.materialart.
    Unknown
    Pacific News (APSA, Göttingen)
    Publication Date: 2021-03-29
    Description: Es gibt wieder Annäherung in den politischen Beziehungen zwischen Chile und Bolivien. Das ist die positive Erkenntnis, die sich aus den vergangenen Treffen zwischen Chiles Präsidentin Michelle Bachelet und ihrem bolivianischen Amtskollegen Evo Morales ableiten lässt. Dies ist bemerkenswert, da beide Staaten seit Ende der 1970er Jahre keine diplomatischen Beziehungen mehr zueinander unterhalten. Grund dafür ist der jahrzehntelange Streit um die Modalitäten eines Meereszugangs für Bolivien, das seit dem verlorenen Pazifikkrieg ein Binnenstaat ist. Während Bolivien einen souveränen Pazifikhafen auf chilenischem Territorium fordert, bietet Chile lediglich einen zollfreien Zugang zum Meer. Obwohl eine Neuverhandlung der territorialen Hoheitsrechte als unwahrscheinlich gilt, bemüht sich Bolivien unaufhörlich um die Rückkehr zum Pazifik. Um diese strikte Haltung verstehen zu können, bedarf es, so die These dieses Beitrags, der Berücksichtigung vielfältiger rationaler wie auch irrationaler Motive, die als Triebkräfte für die politischen Forderungen gegenüber Chile wirken. Nur auf Grundlage des Verstehens dieser Zusammenhänge können realistische Wege der Verständigung zwischen den beiden Nachbarstaaten ausgelotet werden.
    Description: research
    Keywords: 910 ; QGX 544 ; QGX 553 ; QGX 533 ; Bolivien {Geographie} ; Kulturgeographie Chiles ; Kulturgeographie der Tropischen Andenländer ; Bolivien ; Chile ; Politische Geographie ; Entwicklungspolitik ; Anthropogeographie ; Integration ; 74.10 ; 74.26
    Language: German
    Type: article , publishedVersion
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    facet.materialart.
    Unknown
    Duehrkohp & Radicke, Göttingen
    Publication Date: 2021-03-29
    Description: Allein in den vergangenen zehn Jahren sind eine Vielzahl an deutsch- und englischsprachigen Publikationen in der Geographie und den Nachbarwissenschaften erschienen, die sich mit den natur- und kulturräumlichen Entwicklungen in Nepal auseinandergesetzt haben. Studien zu den sozioökonomischen bzw. kulturgeographischen Auswirkungen des Trekkingtourismus auf die Gesellschaft, zu den Land-Stadt-Beziehungen, zu Nationalismus und Ethnizität sowie zu Landeskunde und historisch-geographischer Entwicklung Nepals sind dabei entstanden. Jüngst kamen einige akteursbezogene Arbeiten hinzu, die vor dem konzeptionellen Hintergrund der Politischen Ökologie (u.a. GRANER 1997; SOLIVA 2002) verschiedene Teilbereiche der nepalischen Gesellschaft, wie Forstwirtschaft und Naturschutz, behandeln. Was bislang wenig thematisiert blieb, war die Einbeziehung der äußeren Rahmenbedingungen bei der Analyse der Gesellschafts- und Wirtschaftsbereiche des Landes. Unter Verwendung des Konzeptes der Politischen Ökologie soll nachfolgend gezeigt werden, dass für die Behandlung und Bewertung eines regionalen Untersuchungsaspektes wie der Tourismusentwicklung in Nepal die Berücksichtigung der politischen Situation als Einflussfaktor von grundlegender Bedeutung ist. Nur so können Erkenntnisse gewonnen werden, die Grundlage für ein normatives Handlungskonzept sein und damit Anwendung in der politischen Praxis finden können.
    Description: research
    Keywords: 910 ; QG 250 ; QG 260 ; QGJ 000 ; QGJ 025 ; QFK 000 ; QEE 300 ; Entwicklungsländer {Geographie} ; Ehemalige Kolonialländer {Geographie} ; Südasien {Geographie} ; Kulturgeographie Südasiens ; Entwicklungsländerforschung {Anthropogeographie} ; Tourismus in Entwicklungsländern {Geographie} ; Nepal ; Fremdenverkehrsgeographie ; Konfliktforschung ; Politische Ökologie ; 74.23 ; 74.08 ; 74.09
    Language: German
    Type: article , publishedVersion
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2021-03-29
    Description: Vor mehr als fünfzig Jahren beschloss die kurz zuvor an die Macht gelangte MNR-Regierung, mit einer umfassenden Agrarreform eine Umverteilung des landwirtschaftlichen Eigentums in Bolivien zu initiieren. Unproduktive Latifundien sollten ebenso enteignet und an Bedarfsgruppen vergeben werden wie extensiv genutzte Areale. Tausende Familien sollten in der Folgezeit vom andinen Hochland ins tropische Tiefland (Oriente) geholt und in Plandörfern angesiedelt werden. Dieser als Agrarkolonisation bezeichnete Vorgang beinhaltet die Erschließung und Besiedlung von nur teilweise oder nicht genutzten Flächen zur Ausweitung der Agrarproduktion und zur Existenzsicherung der ländlichen Bevölkerung. Während die letzten staatlichen Umsiedlungsprogramme aufgrund von Finanzmangel, ihres begrenzten Erfolges und der öffentlichen Kritik an ihrer Umsetzung vor rund zwanzig Jahren eingestellt wurden, sind ihre Folgewirkungen in den Kolonisationsgebieten noch immer zu spüren. Flächenmangel und Grenzkonflikte führen ebenso zu Unmut und Protest bei betroffenen Siedlern wie die ärmlichen Lebensbedingungen und die räumliche Desintegration vieler Siedlungen. Dieser Beitrag diskutiert wesentliche Ziele und Probleme der Agrarkolonisation und fragt nach ihren regionalen Effekten für das ostbolivianische Tiefland.
    Description: research
    Keywords: 910 ; QEA 000 ; QEN 150 ; QG 250 ; QFK 300 ; QFK 400 ; QFK 520 ; QER 250 ; QEN 150 ; QGX 503 ; QGX 533 ; QGX 544 ; QFG 300 ; Sozialgeographie im engeren Sinn ; Ländlicher Raum {Siedlungsgeographie} ; Entwicklungsländer {Geographie} ; Entwicklungsstrategien, Entwicklungshilfe {Entwicklungsländerforschung} ; Empirische Entwicklungsländerforschung ; Wanderungen {Entwicklungsländerforschung} ; Agrar- und Forstgeographie {Wirtschaftsgeographie} ; Ländlicher Raum {Siedlungsgeographie} ; Kulturgeographie von Südamerika ; Kulturgeographie der Tropischen Andenländer ; Bolivien {Geographie} ; Regionalplanung ; Bolivien ; Sozialgeographie ; Agrarkolonisation ; Migration ; Ureinwohner ; Integration ; Multikulturelle Gesellschaft ; Regionalentwicklung ; 74.26 ; 74.09
    Language: German
    Type: article , publishedVersion
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    facet.materialart.
    Unknown
    Leidorf
    Publication Date: 2021-03-29
    Description: The analysis of desert soils near archaeological sites allowed new insights in the environmental and living conditions of the early inhabitants of the Wadi Howar (NW Sudan) and their interactions with their environment. It also provided us with more information about the soil genesis in arid regions. Further studies should concentrate on dating the described indicators of a more humid climate in the eastern Sahara during the Holocene.
    Description: Begleitende bodenkundliche Studien im Rahmen archäologischer Untersuchungen zur Besiedelungsgeschichte des Nordwest-Sudans im Holozän
    Description: The field work was possible within the scope of the Sonderforschungsbereich 389 ACACIA (Arid Climate Adaption and Cultural Innovation in Africa) of the University of Cologne, sub-project A2 »Wadi Howar: Siedlungsraum und Verkehrsweg am Südrand der Libyschen Wüste.« This project owes its funding to the Deutsche Forschungsgemeinschaft (DFG ).
    Description: research
    Keywords: 551 ; VP 400 ; VOA 000 ; TWC 500 ; VPO 000 ; VOI 230 ; Aride Regionen {Bodenkunde} ; Bodenuntersuchung, Bodenanalyse ; Klimaschwankungen und Klimaänderungen im Quartär ; Westafrika, Sudan und Guinealänder {Bodenkunde} ; Salzböden, Wüstenböden ; Sudan ; Archaeology ; climate change ; human impact ; Sudan 〈Nordwest〉 ; Wadi Howar ; Archäologische Stätte ; Wüstenboden ; Holozän ; Klimaänderung ; 38.61 ; 38.69 ; 38.19
    Language: English
    Type: article , publishedVersion
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 11
    Publication Date: 2021-03-29
    Description: Bolivien zeigt sich dieser Tage mal wieder gespalten. Auch wenn die Dezemberwahlen 2005 mit dem ersten indigenen Präsidenten Evo Morales einen eindeutigen Gewinner hervorbrachten, so halten etwa die Diskussionen über die staatliche Energie- und Ressourcenpolitik unvermindert an. Es geht dabei um die bereits vollzogene Verstaatlichung der nationalen Öl- und Erdgasvorkommen, die womöglich bald folgende von Forstwirtschaft und Bergbau sowie eine angekündigte Reform der agrarischen Besitzverhältnisse. Die Mehrheit der indigenen Bevölkerung sieht in diesem Politikwandel die lang ersehnte Realisierung einer gerechteren Aufteilung kollektiven Eigentums. Dagegen erkennen vor allem Mestizen und Weiße in den Verstaatlichungen den problematischen Versuch Morales’, dem Namen seiner Regierungspartei „Movimiento al Socialismo“ zur Verwirklichung verhelfen zu wollen: die „Bewegung hin zum Sozialismus“. Anliegen dieses Beitrages ist es nicht zu klären,welches Szenario den Realitäten in Bolivien näher kommt. Auch stehen nicht die schwer abschätzbaren Auswirkungen der staatlichen Ressourcenpolitik im Fokus. Vielmehr möchte dieser Beitrag die Fragmentierung der bolivianischen Gesellschaft beleuchten und anhand eines regionalen Beispiels verdeutlichen, dass interkulturelles Zusammenleben in Bolivien gelingen kann, wenn es denn ausprobiert wird.
    Description: research
    Keywords: 910 ; QFK 000 ; QFK 400 ; QFK 300 ; QEI 000 ; QGX 100 ; QGX 120 ; Entwicklungsländerforschung {Anthropogeographie} ; Empirische Entwicklungsländerforschung ; Entwicklungsstrategien, Entwicklungshilfe {Entwicklungsländerforschung} ; Politische Geographie, Geopolitik ; Lateinamerika {Geographie} ; Kulturgeographie Lateinamerikas ; Integration ; Multikulturelle Gesellschaft ; Bolivien ; Andenstaaten ; Sozialgeographie ; 74.26 ; 74.09
    Language: German
    Type: article , publishedVersion
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 12
    facet.materialart.
    Unknown
    Lateinamerika-Zentrum, Universität Münster
    Publication Date: 2021-03-29
    Description: Das östliche Tiefland von Bolivien, der so genannte Oriente, wird seit nunmehr einem halben Jahrhundert von umfangreichen Zuwanderungen aus den benachbarten Provinzen und dem Hochland heimgesucht. Dabei ist die Binnenmigration ein demographisches Phänomen, das den Oriente auf unterschiedliche Weise in seiner Regionalentwicklung beeinträchtigt. Einerseits kommt es zu einer tiefgründigen Modifikation der Landschaft durch Nutzung und Ausbeutung der natürlichen Ressourcen. Anderseits führen die Wanderungsbewegungen zu einer sukzessiven Transformation der Aufnahmegesellschaft. Intensität und Ausmaß der Gesellschaftsveränderungen hängen vom Grad der Integration der beteiligten Akteure ab. Es ist davon auszugehen, dass sowohl das gesellschaftliche als auch das ökologische Gleichgewicht davon abhängen, inwieweit eine Eingliederung der zugewanderten Individuen und Gruppen in das soziale System (soziale Integration) gelingt, – und inwieweit die verschiedenen Teilbereiche der Gesellschaft (politisches, ökonomisches, soziales und edukatives System) im Austausch miteinander stehen bzw. harmonieren. Die empirische Feldforschung im Agrarkolonisationsgebiet San Julián (Departamento de Santa Cruz) bezog sich auf den Zusammenhang zwischen der Integration von Zuwanderern und den Auswirkungen auf die regionale Kulturlandschaft.
    Description: Internal rural migration is a demographic phenomenon which affects the eastern Bolivian lowlands mainly in two different ways. On the one hand the migrations provoke a profound modification of the landscape by exploitation and potential degradation of the natural resources. On the other hand massive inflows of migrants cause the transformation of the local society. Intensity and dimension of those modifications depend on the level of integration of the individuals and groups which are involved. Consequently, the inclusion of the actors into the social system (social integration) as well as the relationship between the parts of the society (systemic integration) determine the societal as well as the ecological equilibrium. An empirical analysis of the integration process of migrants from the Andean highlands was realised in the colonisation area of San Julián, Dpt. of Santa Cruz, Bolivia. One main aspect of the investigation focused on the rural poverty and different standards of living of migrant and local households. Empirical data were collected through semi-structured interviews as well as standardised interviews in two villages (98 households). The results show a latent correlation between social integration and individual management of common natural resources. A high degree of personal integration about the four dimensions of social integration, which are “cultural adaptation”, “positioning”, “interaction” and “identification”, encourages the sensitivity for common socioeconomic welfare through specific livelihood strategies. The current situation in the research area is characterised by the fragile systemic integration of the colonisation area into the regional economy and society. This fact complicates not only social integration and intercultural living together between migrants from the Andean highlands and the lowland people, but also threatens the ecological balance of the region. Consequently, without the political and civil intentions to resolve the systemic disintegration there will not be a sustainable socio-economic development.
    Description: research
    Keywords: 910 ; QEA 000 ; QER 000 ; QEN 150 ; QEG 400 ; QEA 240 ; QFK 520 ; QFK 300 ; QFK 400 ; QFK 100 ; QGX 503 ; QGX 533 ; QGX 544 ; Sozialgeographie im engeren Sinn ; Wirtschaftsgeographie ; Ländlicher Raum {Siedlungsgeographie} ; Wanderung, Nomadismus {Geographie} ; Sozialgeographische Gruppen {Sozialgeographie} ; Wanderungen {Entwicklungsländerforschung} ; Entwicklungsstrategien, Entwicklungshilfe {Entwicklungsländerforschung} ; Empirische Entwicklungsländerforschung ; Theoretische Entwicklungsländerforschung ; Kulturgeographie von Südamerika ; Kulturgeographie der Tropischen Andenländer ; Bolivien {Geographie} ; Bolivien ; Wirtschaftsgeographie ; Migration ; Regionalentwicklung ; Agrarkolonisation ; Integration ; Multikulturelle Gesellschaft ; Importsubstitution ; Sozialgeographie ; 74.26 ; 74.09 ; 74.07
    Language: German
    Type: monograph , publishedVersion , monograph
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 13
    Publication Date: 2021-03-29
    Description: Wenn Unternehmen neue Märkte erschließen wollen, Produktions- und Lohnkosten zu senken versuchen und sich um die Flexibilisierung des Faktors Arbeit bemühen, dann tun sie das häufig über die Gründung von Tochterunternehmen, Niederlassungen und Filialen im Ausland. Allen drei Investitionsformen ist auf den ersten Blick ihre hochgradige Abhängigkeit vom Mutterkonzern gemein, die sich etwa in der Verpflichtung äußert, Gewinne an die Zentrale abzuführen und sich dieser in strategischen und operativen Entscheidungsfragen unterzuordnen. In Polen sind seit der politischen und ökonomischen Öffnung des Landes in den späten 1980er Jahren eine Vielzahl von ausländischen Tochterunternehmen gegründet worden. Dabei handelt es sich sowohl um Neugründungen von Standorten (greenfield investments; in 58 % der Fälle) als auch um Joint-Ventures (25 %) und Übernahmen von zur Privatisierung freigegebenen Staatsbetrieben (brownfield investments; 17 %). Mehr als 100 Mrd. US$ an ausländischen Direktinvestitionen sind seit Beginn der marktwirtschaftlichen Transformation nach Polen geflossen, ein Drittel davon in die Industrie. Eine wichtige Empfängerbranche ist die Automobilindustrie, die auf der Suche nach kostengünstigen, zu den westeuropäischen Kernmärkten benachbarten Standorten in Polen, Tschechien, der Slowakei, Ungarn und weiteren mittel- und osteuropäischen Ländern fündig geworden ist. Allein in Polen sind mit Fiat, General Motors und Volkswagen drei Automobilhersteller, die vor Ort Fahrzeuge produzieren. Hinzu kommen Motoren- und Getriebefertiger und mehrere Hundert Automobilzulieferer. Mit der angesprochenen hochgradigen Abhängigkeit von ihren Konzernzentralen sind ausländische Tochterunternehmen allerdings nur unzureichend beschrieben. Transnationale Unternehmen, so die These dieses Beitrags, lassen sich zwar über ihr hierarchisch organisiertes Netzwerk aus räumlich verstreuten Unternehmenseinheiten charakterisieren, jedoch zeigen Beispiele aus der polnischen Automobilindustrie, dass dezentral für das lokale Werksmanagement durchaus Handlungsspielräume etwa beim Einwerben von zusätzlichen Unternehmenskompetenzen bestehen.
    Description: conference
    Keywords: 910 ; QGG 200 ; QER 000 ; QER 500 ; QER 930 ; QER 100 ; QG 200 ; QGA 200 ; Polen {Geographie} ; Wirtschaftsgeographie ; Industriegeographie {Wirtschaftsgeographie} ; Internationale Wirtschaftsbeziehungen {Wirtschaftsgeographie} ; Wirtschaftsräume und wirtschaftsräumliche Gliederung {Wirtschaftsgeographie} ; Industrieländer {Geographie} ; Europäische Union {Geographie} ; Polen ; Transformationsländer ; Internationale Arbeitsteilung ; Kraftfahrzeugsindustrie ; Ausländische Tochtergesellschaft ; Upgrading ; Direktinvestitionen ; 74.19 ; 74.07
    Language: German
    Type: anthologyArticle , publishedVersion
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 14
    facet.materialart.
    Unknown
    Schweizerbart, Stuttgart
    In:  SUB Göttingen | 8 MIN I, 1220:SondBd 3
    Publication Date: 2022-03-21
    Description: Die Arbeit setzt die glazialgeologischen Untersuchun­gen des Authors in den Karnischen Alpen fort, vorgenommen in den Karawanken in den Jahren 1932 und 1933.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:554.3
    Language: German
    Type: doc-type:book
    Format: 382
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 15
    Publication Date: 2022-07-15
    Description: Der Königsberg westlich von Wolfstein in der Pfalz wird von einem rhyolithischen Lakkolith aufgebaut. Die im Rhyolith auftretenden Erzgänge waren insbesondere vom achtzehnten bis zwanzigsten Jahrhundert wiederholt Ziel bergbaulicher Aktivitäten. Die wichtigsten Wertminerale sind Quecksilbererze und Schwerspat. Außer im Eulental (Kästenteicher Tal) unmittelbar westlich von Wolfstein bestand keine nennenswerte historische Gewinnung des mineralischen Rohstoffs Rhyolith. Im Zuge einer rohstoffgeologischen Erkundung im Jahr 2001 wurde vom Geologischen Landesamt, heute Landesamt für Geologie und Bergbau Rheinland-Pfalz, das Rhyolithvorkommen übersichtsmäßig auf seine Eignung zur Herstellung von Mineralgemischen und Zuschlagstoffen für die Bauindustrie untersucht. Dabei ergaben sich vergleichsweise große Variationen der Güteeigenschaften. Die untersuchten Parameter können miteinander korreliert werden. Entlang der Erzgänge ist die Festigkeit des Rhyolithes deutlich verringert. Aufgrund dieser entfestigten Zonen sowie verschiedener naturschutzfachlicher Überplanungen und derzeit konfliktträchtiger Zufahrtsmöglichkeiten sind die Rahmenbedingungen für einen Neuaufschluss einer Gewinnungsstelle als ungünstig einzustufen.
    Description: The Königsberg near Wolfstein (Pfalz / Germany) is formed by a rhyolitic laccolith. The metalliferous veins hosted by the rhyolite have been exploited by underground mining repeatedly from the 18th to the 20th century. The most important valuable minerals are mercury ore and baryte. Except for the Eulental (Kästenteicher Tal) to the west of Wolfstein no considerable historical exploitation of the mineral raw material rhyolite existed. In the year 2001 the Geological survey of Rheinland-Pfalz enforced the exploration of the rhyolite as mineral raw material in a general standard. The aim of the exploration was to determine the suitability of the rhyolite as a solid bulk material. The results of the quality features varied in a wide range. The examined parameters can be correlated with each other. Along the vein zones the mechanical strength of the rhyolite is significantly reduced. Considering these zones as well as limitations due to existing nature reserves and a problematic situation concerning the roads for haulage the basic conditions of a new stone quarry are to be classified as unfavourable.
    Description: research
    Keywords: ddc:622.35 ; ddc:553.5
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 16
    Publication Date: 2022-07-15
    Description: Die schon in Teil I geschilderten Hinweise auf kompressive Beanspruchungen im Untersuchungsgebiet haben sich zwischenzeitlich erweitert um auffällig engständige Kluftscharen, störungsgebundene Dolinen und Horizontal-harnische in einem Muschelkalk-Steinbruch bei Eßlingen. Eine Auswertung des aktualisierten Störungsmusters führte zur Identifikation von mehreren Verbindungsstrukturen (Pull-apart-Gräben) zwischen linkstretenden sinistralen Südwest-Nordost-streichenden Blattverschiebungen. Andere, weniger gut erhaltene transtensionale Pull-apart-Strukturen verbinden Nord-Süd-orientierte rechtstretende dextrale Bewegungsbahnen. Es lassen sich zahlreiche langgestreckte Blattverschiebungen ausweisen, dextrale (dex I bis dex V) und sinistrale (sin I bis sin VII). Ihre Horizontalbewegungen dokumentieren sich in mikrotektonischen Phänomenen sowie in Versätzen an älteren Bruchlinien und an alt angelegten großen Hoch- und Tiefstrukturen, die schon in der Trias synsedimentär mobil gewesen waren. Eine isochrone Genese der beiden Typen von Blattverschiebungen ist unwahrscheinlich. Zu beiden Bewegungsmustern lassen sich im Untersuchungsgebiet und in der weiteren Umgebung Zeugnisse konjugierter Horizontalverschiebungen auffinden, mit kinematisch stimmigeren Winkelbeziehungen. Im Vergleich mit den Paläospannungsfeldern anderer Regionen (Voralpenland, Schiefergebirge, Rurtal-Riftsystem, Pariser Becken, Burgund, Kanalküste) ergibt sich folgender tektonomechanischer Werdegang. Die dextralen, rheinisch ausgerichteten Horizontalverschiebungen sind ins Oberoligozän (Chatt) zu stellen. Verschiebungsweiten von bis zu 3,5 km lassen sich rekonstruieren. Die sinistralen Blattverschiebungen versetzten die dextralen Bewegungsbahnen um einige Hundert Meter. Ihre Entstehung datiert ins Untermiozän. Als Reaktion auf das quartäre Beanspruchungsmuster lassen sich regional differenzierte Anhebungen mit entsprechender Abschiebungstektonik nachweisen. Über das bisher bekannte Hebungsgebiet der Eifel hinaus sind starke Hebungen in den (südlichen) Ardennen wahrscheinlich. Es resultierte ein starker Abdachungsgradient zur nordwestlichen Trierer Bucht. Nordwest-Südost streichende Abschiebungen sind weitere Resultate der jungen Hebungstendenzen. Sie treten im Südwest-Teil des Untersuchungsgebietes und insbesondere auch im Schiefergebirge auf (Westeifeler Vulkanfeld!). Die Uranlage dieser Bruchzonen als dextrale Blattverschiebungen könnte dem hier rekonstruierten untermiozänen Deformationsakt zuzuschreiben sein.
    Description: The already described indications for compressional stresses in the northwestern Trier Embayment (part I) could be supplemented in the meantime. In a dolomite quarry near Eßlingen swarm fissures, more or less crowded, fault-related dolines and horizontal slip striations were found. The analysis of an updated version of the fault pattern led to the identification of several pull-apart-grabens connecting NE-SW striking left-stepping left-lateral strikeslip faults. North-South trending dextral strike-slip faults are connected by less preserved right-stepping transtensional pull-apart structures. Several distinct strike-slip faults can be traced, dextral (dex I bis dex V) and sinistral ones (sin I bis sin VII). Their strike-slip motions are documented by microtectonic features and by horizontal dislocations of older fault lines and inherited large paleohighs and -lows, which have already been mobile in triassic times. A concurrent genesis of both types of strike-slip faults is less probable. Both motion patterns are completed by conjugate shearing features – with kinematically more consistent angles – which can be observed in the study area and in surrounding regions. Comparisons with paleostress fields of adjacent areas (foothills of the Alps, Rhenish Massif, Roer Valley rift system, Paris Basin, Burgundy, Channel area) lead to the reconstruction of the structural evolution. The rhenish striking dextral strike-slip faults generated during late Oligocene (Chattian). Horizontal displacements up to 3.5 km can be reconstructed. The sinistral strike-slip faults, that teared the dextral shear planes, date from lower Miocene. The quaternary stress field caused regionally differentiated uplift trends and downfaulting tectonics. Exceeding the so far known uplift area of the Eifel a noteworthy strong rise of the (southern) Ardennes took place. A remarkable downwarp resp. downthrow at the northwestern border of the Trier Embayment resulted from that. These motions also caused an activity of SE-NW striking normal faults with southwestward downthrow. They appear in the southwestern part of the study area and in the Rhenish Massif (West Eifel Vulcanic Field!). The initial traces of these fault zones could have generated as dextral strike-slip faults during the sketched lower Miocene deformation process.
    Description: Einführung in Teil II 5. Rekonstruktion von Bewegungsabläufen 5.1. Sinistrale Bewegungen 5.2. Dextrale Bewegungen 6. Zusammenfassende Ausdeutung 6.1. Überlegungen zur Chronologie der Deformationsereignisse 6.2. Alttertiäre Deformationen 6.3. Oberoligozäne Deformationen 6.4. Untermiozäne Deformationen 6.5. Pleistozäne Deformationen 7. Ausblick Schriften
    Description: research
    Keywords: ddc:551.8
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 17
    Publication Date: 2022-07-15
    Description: Das bisher gültige Strukturmodell des mesozoischen Deckgebirges der Trierer Bucht (Südeifel) hat über viele Jahre hinweg tragfähige Ergebnisse geliefert. Es war generell Dehnungstektonik angenommen worden; bislang sind denn auch ausschließlich Abschiebungen angetroffen worden. Bei der relativen Absenkung gegenüber den umgebenden paläozoischen Massiven bildeten sich drei, im devonischen Sockel vorgegebene, alt angelegte Richtungssysteme ab. Sie streichen NNESSW, Nordost-Südwest und ENE-WSW. Die weit durchhaltenden und großräumigen Hoch- und Tiefstrukturen dieser drei Richtungssysteme sind schon im Mesozoikum mobil gewesen. In den letzten 15 Jahren ist dieses tektonische Konzept durch neuere Geländeaufnahmen überwiegend bestätigt worden. Bei Flächenkartierungen im Zentral- und Nordwest-Teil der Trierer Bucht konnten schon bekannte Einzelstrukturen konkretisiert, in größerer Ausdehnung nachgewiesen oder in ihrer Position bzw. Ausprägung modifiziert werden. Im westlichen deutsch-luxemburgischen Grenzgebiet wurden zuvor nicht bekannte, relativ junge Nordwest-Südost-streichende Abschiebungen nachgewiesen. Sie entstanden bei der relativen Absenkung des Südwestens (Pariser Becken) gegenüber einem Hebungsgebiet in der Osteifel. Damit verbunden war auch die verstärkte Mobilität West-abschiebender Nord-Süd-Störungen. Allerdings fanden sich auch Hinweise auf eine gewisse kompressive Beanspruchung des Deckgebirges. Dies sind etwa (sub-)horizontale Harnischstriemungen, die im Untersuchungsgebiet – im Gegensatz zur Kylltalregion im Südosten der Trierer Bucht – vergleichsweise selten auftreten. Ferner erscheinen eng gescharte, nahezu saiger orientierte Störungsflächen, die nur geringe vertikale Versatzbeträge zeigen. Im Dünnschliff eines stark deformierten Sandsteins fanden sich spröde, korndurchsetzende Frakturierungen. Auffällig sind auch bogig begrenzte, an Pull-apart-Strukturen erinnernde kleine Grabenschollen in den geologisch-kartographisch gut erfassten Muschelkalk- und Keupergebieten bei Oberweis. Eine tektonische Ausdeutung der Gesamtbefunde (Teil II, nächster Jahresband) muss die Mehrphasigkeit der im Tertiär und Quartär angreifenden kompressiven Beanspruchungen berücksichtigen und unterschiedlich konfigurierte Deformationsprozesse differenzieren. Die diesbezüglichen, in der Literatur vorhandenen Ergebnisse aus benachbarten Regionen (Oberrheingraben, Burgund, Rheinisches Schiefergebirge, Rurgraben) liefern dazu wesentliche Hilfestellungen.
    Description: The tectonic working model concerning the mesozoic series of the Trier Embayment (Southern Eifel) had provided useful results since many years. Generally extensional downfaulting tectonics had been assumed, based on the fact that only nor mal faults have been observed. Caused by the downwarping of the Trier Depression in relation to surrounding paleozoic massifs (Ardennes, Eifel, Hunsrück) fault zones of three directional systems were activated. They were inherited from the Devonian basement and show NNE-SSW, NE-SW and ENE-WSW directions. The large and widely continued horst and graben structures of these three directional systems have even been mobile in mesozoic times. During the last 15 years this tectonic concept has been mostly confirmed. Arevisionary geologic field mapping covered the central and the northwestern parts of the Trier Embayment. As a result long since known structural elements could be specified. In other cases structural elements could be modified in length and position. In the west, at the border to Luxemburg, relatively young NW-SE striking additional normal faults were documented. They were generated during the late cenozoic uplift of the eastern Eifel region whilst the southwestern area (Paris Basin) subsided relatively. These motions also caused increased activity of westward throwing North-South striking faults. On the other hand some indications for compressional stresses could be observed. These indications comprise subhorizontal slip striations. In outcrops along the Kyll valley in the southeast these phenomena are quite abundant. In the studied area however they have been found ever since only twice.Moreover nearly vertical dipping fault planes, more or less crowded, with only minor vertical throw can be found. Athin section of a strongly tectonized sandstone proved brittle deformation. Even the quartz grains are fractured. Small arch-shaped grabens are noticeable as well, situated in the Muschelkalk and Keuper areas near Oberweis. They resemble to pull-apart structures. A reconstruction of the structural evolution (part II, next issue) has to take into account the succession of several cenozoic tectonic events. Hence, changing paleostress fields and a relative chronology of motions have to be regarded. Published results from adjacent areas (Upper Rhine Graben, Burgundy, Rhenish Massif, Roer Valley Graben) on the matter support the understanding of the successive local stress patterns.
    Description: 1. Einführung 2. Grundlegende Kenntnisse zur Tektonik der Trierer Bucht 3. Weitergehende strukturelle Ergebnisse 3.1. Neue Befunde zum bisherigen Modell 3.2. Hinweise auf kompressive Beanspruchungen 4. Zur Differenzierung von unterschiedlichen Scherbeanspruchungen Schriften
    Description: research
    Keywords: ddc:551.8
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 18
    Publication Date: 2022-09-12
    Description: In Rheinland-Pfalz gibt es seit einigen Jahren den Trend in steilen Weinbergshängen Querterrassen anzuordnen. Die parallel zu den Höhenlinien verlaufenden Terrassen sind leichter zu bewirtschaften. Für die Querterrassierung sind erdbautechnische Eingriffe, wie Anschnitte und Auffüllungen, erforderlich. Es finden Lastveränderungen statt und Einzelböschungen müssen im Vergleich zur Ausgangsneigung versteilt werden. In Abhängigkeit von den Untergrundverhältnissen bestehen geotechnische Risiken bis hin zu Hangrutschungen. Die Machbarkeit einer Querterrassierung erfordert verschiedene Voraussetzungen, wie zum Beispiel eine geeignete Hanggeometrie, eine ausreichende Mächtigkeit der Lockergesteinsdecke sowie eine entsprechende Standfestigkeit bzw. Hangstabilität. An verschiedenen Praxisbeispielen werden Schadensfälle, die im Umfeld von Querterrassierungen aufgetreten sind, beschrieben. Ein typisches Risiko ist das Auftreten höhenlinienparalleler Spalten bzw. Abrisse. Ziel ist es, aus den Erfahrungen der Schadensfälle zu lernen. Bei Querterrassierungen sind verschiedene Grundsätze zu beachten, deren jeweilige Gewichtung vom Einzelfall abhängt. Generell sollten für eine Querterrassierung vorgesehene Hänge im Vorfeld in geotechnischer Hinsicht überprüft werden. Hierzu gehört neben Standsicherheitsbetrachtungen auch die Feststellung der vorhandenen und zukünftigen ober- und unterirdischen Abflussverhältnisse anfallenden Wassers. Ein wichtiger Diskussionspunkt ist die Richtung des Quergefälles der einzelnen Terrassen (tal- oder bergseits). Es besteht ein wirtschaftliches Interesse, möglichst steile Böschungen herzustellen. Dies wird jedoch durch die Scherfestigkeit des Untergrunds eingeschränkt. Die neu entstandenen Böschungen sind möglichst schnell erosionsstabil zu befestigen. Bis sich eine Begrünung etabliert hat, können unterstützende Maßnahmen, wie Geotextilmatten, sinnvoll sein. Die Erdarbeiten sollten nur von Baufirmen mit entsprechender Erfahrung durchgeführt werden. Schon auf Grund der geringen Zahl bisher durchgeführter Querterrassierungen und der zum Teil aufgetretenen Schäden besteht ein weiterer Forschungsbedarf und die Notwendigkeit eines fachlichen Austausches.
    Description: Abstract: For some years there is a trend in Rheinland-Pfalz to change steep vineyard- slopes into lateral terraces. The cultivation is easier on terraces, which are orientated parallel to the contour lines. For building the lateral terraces earth-moving is necessary, such as excavations and back fillings. Due to the terracing, the distribution of weight in the slope changes and the inclination increases partially. So dependent on the soil properties there is a risk of geotechnical failures like landslides. The feasibility of lateral terracing requires special conditions such as a suitable slope geometry, sufficient in-situ soil thickness and an adequate shear strength and slope stability. Several cases of damages with relations to lateral terraces are presented. Typical failures are fissures respective vertical fractures parallel to the contour lines, the beginning of landsliding. Different policies for lateral terracing must be respected and adapted to the individual case. As a general rule the specific slopes should be investigated geotechnically. In addition to the determination of the slope stability, other properties like the surface run-off and the subsurface run-off should be considered. An important point of interest is the inclination of the terrace surface (downward or upward ). For economic reasons, steep embankments between the terraces are preferred. The steepness is restricted by the shear strength of the soils. Fresh made embankments have to be protected against erosion damages. Before the vegetation has grown up, support concepts like coverings with geosynthetics are useful. The earthwork should only be carried out by building companies with adequate practical knowledge. Due to low experiences with lateral terracing in Rheinland-Pfalz and to well known damages more research and an exchange of ideas are considered to be necessary.
    Description: 1. Einleitung 2. Geologie und Georisiken im Weinbau von Rheinland-Pfalz 2.1. Boden-/Felsarten in Rheinland-Pfalz 2.2. Rutschungen in Weinbaugebieten von Rheinland-Pfalz 2.3. Beispiel einer Rutschung im Weinberg 3. Bauprinzipien für Querterrassen 4. Beispiele für Querterrassierungen in Rheinland-Pfalz 4.1. Flurbereinigungsverfahren Bienengarten in Koblenz-Güls 4.2. Flurbereinigungsverfahren König-Johann-Berg in Serrig 4.3. Agrarstrukturelle Entwicklungsplanung „In der Rheinhölle“ in Linz am Rhein 5. Empfehlungen für Querterrassierungen im Weinbau 5.1. Prüfung, Erkundung 5.2. Hydrogeologie, Entwässerung 5.3. Deckschichtenmächtigkeit und Felsklippen 5.4. Hang- und Böschungsneigung 5.5. Erdbau, Herstellen der Querterrassen 5.6. Erschließung 5.7. Begrünung, Erosionsschutz, Stützmaßnahmen 6. Schlussbemerkungen Schriften
    Description: research
    Keywords: ddc:631.45
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 19
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom März 2005 enthält die Themenblöcke: Geofokus: Impaktkrater auf der Erde - Spuren des kosmischen Bombardements, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 20
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom März 2004 enthält die Themenblöcke: Geofokus: Impaktkrater auf der Erde - Spuren des kosmischen Bombardements, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 21
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom März 2006 enthält die Themenblöcke: Geofokus: Gashydrate der Meeresböden: Methanspeicher im Ozean, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport (Neue Bücher, Personalia, Tagungsberichte)
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 22
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Juni 2006 enthält die Themenblöcke: Geofokus: Feinstaubexposition in urbanen Ballungsräumen - Ergebnisse der Elektronenmikroskopie, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport (Neue Bücher, Personalia, Tagungsberichte)
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 23
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Dezember 2005 enthält die Themenblöcke: Geofokus: Lagerstättengeologie im aktiven und stillgelegten Steinkohen-Berbau des Ruhrgebiets, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport
    Description: DFG, SUB Göttingen
    Description: source
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 24
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom September 2006 enthält die Themenblöcke: Geofokus: Das UNESCO-Weltnaturebe Grube Messel - einzigartieges Geopotential nun mit soziotouristischer Nutzung, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport (Neue Bücher, Neue Karten, Personalia, Tagungsberichte)
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 25
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Dezember 2006 enthält die Themenblöcke: Geofokus: Urgeschichte als Geowissenschaft, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport (Neue Bücher, Personalia, Tagungsberichte)
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 26
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom März 2007 enthält die Themenblöcke: Geofokus: Submarine Hysrothermalquellen - Treffpunkte von Geologie, Geochemie und Biologie, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport (Neue Bücher, Neue Karten, Personalia, Tagungsberichte)
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 27
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom September 2007 enthält die Themenblöcke: Geofokus: Das neue Museum für Naturkunde Berlin - Evolution in Aktion, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport (Neue Bücher, Personalia, Tagungsberichte)
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 28
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Juni 2007 enthält die Themenblöcke: Geofokus: Quasikristalle - von einer Kuriosität zum neuen Material , Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport (Multimedia, Neue Bücher, Neue Karten, Personalia, Tagungsberichte)
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 29
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Dezember 2007 enthält die Themenblöcke: Geofokus: Gashydrate der Meeresböden: Methanspeicher im Ozean, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport (Neue Bücher, Neue Karten, Personalia, Tagungsberichte)
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 30
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom März 2008 enthält die Themenblöcke: Geofokus: Mit Luftsäcken zum Riesenwuchs: Die Wirbelsäule sauropoder Dinosaurier, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport (Neue Bücher, Personalia, Tagungsberichte)
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 31
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom September 2008 enthält die Themenblöcke: Geofokus:Kosmogene Nuklide in den Geo- und Umweltwissenschaften, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport (Neue Bücher, Personalia, Tagungsberichte)
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 32
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom September 2005 enthält die Themenblöcke: Geofokus: Tsunami - eine unterschätzte Naturgefahr, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 33
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Dezember 2008 enthält die Themenblöcke: Geofokus: Das Magnetfeld der Erde, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport (Neue Bücher, Personalia, Tagungsberichte)
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 34
    Publication Date: 2022-09-01
    Description: Die verstärkte Nutzung geothermischer Energie ist ein wichtiger Bestandteil der zukünftigen weltweiten Energiepolitik. Aus diesem Grund steigt auch der Bedarf an Grundlagendaten zur Abschätzung der thermischen Eigenschaften von Gesteinskörpern zur Planung und Dimensionierung von geothermischen Anlagen. Zu diesen Grundlagendaten gehört die spezifische Wärmekapazität von Festgesteinen. Der vorliegende Artikel beschreibt eine einfache Methode zur Messung der spezifischen Wärmekapazität von Festgesteinskörpern nach dem Prinzip der Kalorimetrie, wie sie im Landesamt für Geologie und Bergbau Rheinland-Pfalz erprobt wurde.
    Description: Abstract: The increased use of geothermal energy is an important part of the prospective energy policy worldwide. For this reason the demand of basic data to estimate the thermal properties of bedrocks for planning and dimension of geothermal constructions rises. The specific heat capacity of hard rocks is one of the basic data. In this article a simple method of measuring the specific heat capacity of hard rocks according to the principle of calorimetry is described, as it was tested in the Landesamt für Geologie und Bergbau Rheinland-Pfalz (Geological Survey and Mining Authority of Rhineland-Palatinate) .
    Description: Inhalt 1. Einleitung und Aufgabenstellung 2. Grundlagen 3. Methodik 4. Beschreibung der Geräte 5. Versuchsaufbau und Versuchsdurchführung 5.1 Ermittlung des Wasserwertes 5.2 Ermittlung der spez. Wärmekapazität von Festgesteinen 6. Beschreibung des Probenmaterials 7. Ergebnisse 8. Fehlerbetrachtung und Diskussion 9. Ausblick Schriften Anhang
    Description: research
    Keywords: ddc:333.88
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 35
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Juni 2008 enthält die Themenblöcke: Geofokus: Versorgung mit mineralischen Rohstoffen - eine Bestandsaufnahme (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport (Neue Bücher, Personalia, Tagungsberichte)
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 36
    Publication Date: 2022-10-28
    Description: Weit verbreitete geringmächtige distale Aschenfalltuffe, die in komplex aufgebauten fluvio-lakustrinen Abfolgen des karbonisch-permischen Saar-Nahe-Beckens in Süd Westdeutschland zwischengelagert sind, liefern wichtige tephrostratigraphische Leithorizonte für Korrelationen. In der Meisenheim- Formation der mittleren Glan-Gruppe lagerten sich die vulkanischen Aschen in drei unterschiedlichen Sedimentationsbereichen ab: im offen-lakustrinen Milieu, im Prodelta- bis Deltafrontbereich sowie auf der Deltaebene. Dabei wurde die Erhaltung, die laterale Verbreitung, das Erscheinungsbild und die mineralogische Zusammensetzung der vulkanischen Aschenlagen nicht nur durch das Ablagerungsmilieu, sondern auch durch das tektonische Umfeld beeinflusst. Zudem zeigen laterale Mächtigkeitsänderungen siliziklastischer Abfolgen zwischen Tuffhorizonten Versatzbeträge an synsedimentären Störungen an. Auf angehobenen Liegendschollen bzw. Horststrukturen ist das rezente Auftreten geringmächtiger tephrostratigraphischer Leithorizonte häufig unterbrochen, wohingegen mächtigere Horizonte, die sich oft aus mehreren Aschenlagen aufbauen, meist eine durchgehende Verbreitung haben, wobei aber ihre Mächtigkeiten und Texturen variieren. Abgesenkte Hangendschollen bzw. Grabenstrukturen lieferten im Allgemeinen ein erhöhtes Erhaltungspotenzial erstens für primäre Aschenlagen, die heute noch ursprüngliche Texturen wie planare Schichtung und normale Korngrößengradierung zeigen, sowie zweitens für sekundäre Akkumulationen von Aschentuffiten und tuffitischen Turbiditen, in denen Texturen wie normale Korngrößengradierung, Rippeischrägschichtung und basale Belastungsmarken auftreten. Im Gegensatz dazu wurden Aschenablagerungen auf angehobenen Liegendschollen teilweise aufgearbeitet oder vollständig erodiert. Hier sind primäre Aschenlagen häufig nur mit reduzierter Mächtigkeit erhalten und zeigen Erosionsmarken. Andere Leithorizonte beinhalten resedimentierte tuffitische Ablagerungen mit einer hohen detritischen Beimengung. Lokal haben solche sekundären Ablagerungen die Gesamtmächtigkeit von tephrostratigraphischen Leithorizonten deutlich erhöht. Auf Hangendschollen wurden in primären Aschenlagen meist vollständige Assoziationen primär-magmatischer Schwerminerale mit allgemein idiomorphem Habitus und nur geringer Kantenrundung an Kristallen erhalten. Die Schwermineralzusammensetzung besteht hauptsächlich aus Zirkon, Biotit, Apatit und Monazit sowie geringen Anteilen von Titanit und Hornblende. Daneben finden sich in primären Fallablagerungen auch geringe Gehalte von teilweise idiomorphem Turmalin, Granat und Rutil. Diese Komponenten werden als primäre magmatische Bildungen eingestuft. In tuffitischen Turbiditen oder Aschentuffiten treten neben teils gerundeten primären Schwermineralen auch geringe Gehalte von detritischen Komponenten wie gerundete Epidote auf. Im Gegensatz dazu finden sich auf angehobenen Liegendschollen aufgrund von Aufarbeitungsprozessen normalerweise nur geringe Anteile von primären Schwermineralen mit xenomorphem, unregelmäßigem Habitus und teilweise hohem Kornrundungsgrad. Hier sind häufig detritische Komponenten wie gut gerundete Epidote und Gesteinsbruchstücke in die Aschen eingemischt. Die tephrostratigraphischen Leithorizonte in der fluvio-lakustrinen Meisenheim-Formation des Saar-Nahe-Beckens liefern ein gutes Beispiel für das Zusammenwirken von vulkanischen, sedimentären und tektonischen Prozessen bei der Ablagerung distaler vulkanischer Aschen.
    Description: Abstract: "Synsedimentary tectonic influence on occurrence, appearance, and petrography of distal ash tuffs in the Saar-Nahe Basin (SW-Germany)". Thin, but laterally widespread distal fallout ash tuff layers interbedded within complex fluvio- lacustrine successions of the Carboniferous-Permian Saar-Nahe Basin in SWGermany (Fig. 1) provide important tephrostratigraphic markers for correlations. The former volcanic ash layers of the Meisenheim Formation in the middle part of the Glan Group (Fig. 2) were deposited within three sub-environments: in an offshore lacustrine, prodelta to delta front and delta plain setting (Fig. 3). At this, the preservation, lateral distribution, appearance, and mineralogical composition of volcanic ash beds were not only influenced by the depositional environment but also by the tectonic setting. Furthermore, lateral thickness variations of sedimentary successions between specific tuff horizons indicate offset magnitudes at synsedimentary faults. The present occurrence of thin tephrostratigraphic markers is frequently interrupted on uplifted footwall blocks or hörst structures, whereas thicker markers which are frequently composed of several ash layers offen show an almost continuous distribution (Figs. 4 and 5) although their thickness and textures vary laterally. Subsided hanging-wall blocks or graben structures generally provided an enhanced preservation potential for (1) primary ash fall layers with original textures like planar bedding and normal grain-size grading, and (2) secondary accumulations of ash tuffites and tuffaceous turbidites showing textures like normal grain-size grading, ripple-cross bedding, and basal load marks (Tab. 1). In contrast, on elevated footwall blocks ash deposits were partly reworked or even entirely eroded (Fig. 6). Here, primary ash layers are offen preserved with reduced thicknesses only and show erosion marks. Other tuff horizons frequently comprise redeposited tuffaceous deposits with a high detrital contamination. Locally these secondary deposits have considerably increased the total thickness of a tephrostratigraphic marker. On subsided hanging-wall blocks, in primary ash beds frequently complete suites of primary magmatic heavy minerals with usually euhedral habitus and only minor rounding at crystal edges were preserved. This heavy mineral suite comprises mainly zircon, biotite, apatite, and monazite as well as minor contents of sphene and hornblende. In addition, in primary fall deposits also lower contents of partly euhedral tourmaline, garnet, and rutile occur (Plate 1). These components are classified as primary magmatically formed. Within tuffaceous turbidites or ash tuffites, occasionally rounded primary heavy minerals occur besides minor contents of detrital components as e.g. rounded epidotes. In contrast, on elevated footwall blocks usually only minor contents of primary heavy minerals with an anhedral, irregulär habitus and partly high degrees of grain roundness due to reworking occur (Tab. 2). Frequently, detrital components like well-rounded epidotes and rock fragments were admixed into the ash. The tephrostratigraphic marker horizons in the fluvio-lacustrine Meisenheim Formation of the Saar-Nahe Basin deliver a good example for the interaction of volcanological, sedimentary, and tectonic processes during the deposition of distal volcanic ashes.
    Description: research
    Keywords: ddc:554.3
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 37
    Publication Date: 2022-10-19
    Description: Die Konglomeratische Serie, das regionale Äquivalent der Solling- Folge (s6), greift in der westlichen Südeifel erosionsdiskordant auf den devonischen Sockel über. In dieser Beckenausweitung nach Westen zeigt sich eine Drehung der strukturell vorgegebenen Absenkungsachse aus der „diagonalen“ Südwest-Nordostin die „variszische“ WSW-ENE-Richtung. Dies geschah im Zuge des beckenweiten Bewegungsaktes der „H-Diskordanz“. Die Materialanlieferung erfolgte von einem galloardennischen Liefergebiet im Westen. Die Einstufung der Solling-Konglomerate als vom tieferen „sm“ abgetrennter „Oberer Buntsandstein“ („soc“) kann lediglich im Sinne einer „nach-H-Diskordanz-Bildung” gelten. Nach der bundesweiten Buntsandstein- Stratigraphie zählen sie noch zum Mittleren Buntsandstein. Die Konglomeratische Serie, früher als „Usch-Schichten“ in die untersten Zwischenschichten gestellt, entspricht altersmäßig dem saarländisch-lothringischen Hauptkonglomerat. Die Violette Grenzzone liegt darüber. Mit den Violettschichten, einer faziell ähnlich ausgebildeten Abfolge unter den Konglomeraten, verbindet sie lediglich eine lithogenetische Äquivalenz, nicht aber die stratigraphische Signifikanz für die Grenze Mittlerer/Oberer Buntsandstein. Die Kernbohrungen Roth und Körperich erbrachten mehrere Zehner Meter fluviatile, zyklisch gegliederte quarzitreiche Geröllsandsteine und Konglomerate, teilweise mit hohen Dolomitgehalten im Bindemittel. Sie lagern über Devon und über Erosionsresten vom Basiskonglomerat des Mittleren Buntsandstein. Die beiden Bohrprofile zeigen eine fazielle Differenzierung durch die dazwischen liegende, alt angelegte Oesling- Randflexur. Eine tektonische Kontrolle des Sedimentationsgeschehens wird deutlich.
    Description: Abstract: The coarse sediments of the „Konglomeratische Serie“ are a local equivalent of the Solling-Folge (s6) in upper Germanic Middle Buntsandstein (Lower Triassic). In the western part of the Southern Eifel these conglomerates lap on the Devonian basement. The lateral extension of the deposition area („H-discordance“) was structurally controlled. Caused by tectonic movements the direction of the basin axis rotated from SW-NE to WSW-ENE. The conglomerates do not represent a coarse base unit of the Upper Buntsandstein but correspond to the saarland-lorrainian Hauptkonglomerat. They were delivered from a western source area. The Violette Grenzzone, a famous stratigraphic marker, lies at the top. In contrast to this the facially similar Violettschichten are located below the conglomerates. The core borings Roth and Körperich yielded several ten-meters of coarse sandstones and conglomerates, showing different types of fluvial cyclothems. Correlation was difficult because the sedimentation was controlled by an old flexure zone along the southern margin of the ardennic massif („Oesling-Randflexur“). Synsedimentary tectonic movements determined the position of the fluvial streams.
    Description: 1. Einführung 2. Buntsandstein-Stratigraphie der Trierer Bucht im Überblick 3. Geographische und geologische Position der Bohrpunkte 4. Lithostratigraphie der Kernprofile Roth und Körperich 4.1. Bohrung Roth 4.2. Bohrung Körperich 5. Zusammenfassende Darlegung der Bohr- und Kartierbefunde in der Region Vianden–Roth–Körperich 6. Der „soc“: Mittlerer oder Oberer Buntsandstein? 7. Erste Hinweise zur Beckenkonfiguration der Solling-Folge in der Trierer Bucht 8. Ausblick Schriften
    Description: research
    Keywords: ddc:554.3
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 38
    Publication Date: 2022-08-02
    Description: Im Aufschluss Nußloch südlich von Heidelberg ist ein neu aufgeschlossener Lößrücken paläopedologisch aufgenommen und ein Standardprofil mit verschiedenen Methoden untersucht worden. Im Einzelnen wurden Sedimentanalysen (Korngrößen, Kohlenstoff, Kalkgehalt) und die magnetische Suszeptibilität bestimmt, biomorphologische und malakologische Untersuchungen durchgeführt sowie 27 Proben mit der IRSL-Methode datiert. Stratigraphisch umfasst der untersuchte Abschnitt das Jungpleistozän mit einem mehrgliedrigen Eem-Boden und einem ungewöhnlich mächtigen Würmlöß (ca. 18 m). Bodentypologisch wurden ein Bt-Horizont, eine Humuszone und zahlreiche Nassböden von unterschiedlicher Intensität mit und ohne Verbraunungszone nachgewiesen. Von den fünf ausgewiesenen Verbraunungszonen (WB2 - WB6) sind WB2, WB4 und WB5 aufgrund der Molluskenführung als interstadiale Bildungen anzusehen. Hinzu kommt noch eine der drei interstadialen Mosbacher Humuszonen (WB1) im stark reduzierten Altwürmabschnitt mit einem Alter von ca. 75 ka BP. Als kräftigster Interstadialboden ist der Bv-Horizont einer arktischen Braunerde erkannt worden (WB4), welcher aufgrund verschiedener Kriterien mit dem Lohner Boden bei ca. 30 ka BP parallelisiert wurde. Der im Hangenden des Lohner Bodens überlieferte Jungwürmlöß ist mit 12 m für Mitteleuropa sehr mächtig und von zahlreichen Nassböden (mindestens 10) untergliedert. Besonders aufgespaltet ist der Bereich des E2-Nassbodens, in dem auch die Böden WB5 und WB6 mit schwachen Verbraunungszonen liegen. Auch der jüngste Jungwürmlöß über dem Leithorizont des Eltviller Tuffs ist mit 4,5 m relativ mächtig und mehrgliedrig überliefert, so dass von einem E4/E5-Komplex gesprochen wird. Die paläopedologischen Befunde stimmen hervorragend mit den Veränderungen in der Molluskenfauna und der Suszeptibilitätskurve überein, so dass detaillierte stratigraphische und paläoklimatische Rekonstruktionen möglich sind. Die absoluten Altersdatierungen bestätigen dabei weitgehend die vorgenommenen Alterseinstufungen. Abschließend wird das neu bearbeitete Profil in Nußloch mit Ergebnissen von ANTOINE et al. (2001) verglichen, welche im gleichen Aufschluss an anderer Stelle erzielt worden sind.
    Description: research
    Keywords: ddc:551.7
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 39
    Publication Date: 2022-09-05
    Description: Ein Eurypteriden-Fund aus dem Unter-Siegenium von Betzdorf/Sieg wird beschrieben und abgebildet. Es handelt sich dabei um den ersten sicheren Nachweis der Familie Erieopteridae für das Siegenium des Siegerlandes. Eine Übersicht der assoziierten Fossilien wird gegeben. Darunter befinden sich Reste trigonotarbider Spinnentiere und des Myriapoden Eoarthropleura. Der erstmalige Nachweis luftatmender Trigonotarbiden und wahrscheinlich amphibisch lebender Eoarthropleuriden im Bereich des Siegener Hauptsattels ist von besonderem paläoökologischem Interesse, da hiermit die räumliche Nähe des Ablagerungsraumes zu ehemaligen Auftauchbereichen dokumentiert wird.
    Description: Abstract: A eurypterid from Early Siegenian strata near Betzdorf/Sieg is described and figured. This specimen is the first unequivocal record of the family Erieopteridae from the Siegenian of the Siegerland. The associated biota is briefly discussed and comprises trigonotarbid arachnids and the myriapod Eoarthropleura. This first record of landdwelling trigonotarbids and probably amphibious myriapods in the Siegen-Anticline is of palaeoecological significance as it documents the proximity of the depositional setting to former subaerially exposed areas.
    Description: research
    Keywords: ddc:565
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 40
    Publication Date: 2022-09-02
    Description: Bei der Erneuerung einer Gas-Pipeline (TENP) wurden in der Pfalz fossilreiche Schichten des Ober-Karbon und Unter-Perm (Rotliegend) angeschnitten. Die umfangreichen Aufschlüsse erlaubten detailreiche stratigraphischfazielle Dokumentationen. Mehrere Formationsgrenzen wurden exakter als bisher erfasst. Drei Bänke (Breitenheim-, Raumbach- und Jeckenbach-Bank) konnten lateral weiter ausgehalten werden. Durch die Überquerung des Pfälzer Sattels konnten Nord- und Südfazies gleich alter Abfolgen verglichen werden. Im Vergleich mit dem deitaisch-Iakustrm geprägten Subsidenzzentrum bei Meisenheim zeigt der Pipelinegraben deutlich stärker proximale, d. h. mehr fluviodeltaisch ausgebildete Lithofazies.
    Description: Abstract: In the year 2003, the restoration of the Trans European Natural Gas Pipeline (TENP) in the Palatinate (Southwest Germany), yielded fossiliferous sequences of Upper Carboniferous and Lower Permian (Rotliegend) age. The outcrop, 25 km long, allowed detailed lithological and palaeontological investigations. Some formation boundaries can now be fixed more precisely than before. The occurrence of the lacustrine marker horizons Breitenheim, Raumbach, and Jeckenbach bed, has been traced more to the Southwest than previously known. The northern and Southern lithofacies of time equivalent successions has been compared in detail. Generally the lithofacies of the examined sections is more fluviodeltaic formed than that of the deltaic-lacustric developed subsidence center of the Saar-Nahe-Basin near Meisenheim.
    Description: research
    Keywords: ddc:554.3
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 41
    Publication Date: 2022-08-09
    Description: Deutschland besitzt bedeutende Naturwerksteinvorkommen, die sich auf die Mittelgebirgsräume konzentrieren. Es sind aktuell ca. 150 Sorten verfügbar. Die einheimische Produktion an Fertigfabrikaten betrug im Jahr 2006 ca. 422 000 t. Die in der Naturwerksteingewinnung tätigen deutschen Produzenten sehen sich teilweise schwierigen Rahmenbedingungen bei der Genehmigung von Abbauvorhaben, einem eher stagnierenden öffentlichen Bausektor und einem erheblichen Globalisierungsdruck gegenüber. Die Chancen der einheimischen Wirtschaft liegen in der Realisierung hochwertiger Objekte im individuellen Segment, einem kundenfreundlichen Service und in einem offensiven Marketing, das auch Vorzüge des Bauens mit natürlichen Baustoffen herausstellt.
    Description: Abstract: Germany holds a wide variety of natural stone deposits, which are concentrated in the low mountain range. Currently about 150 kinds of stones are available. The domestic output of finished products comes to 422 000 tons in 2006. The German producers are facing difficult governmental requirements in the authorizing procedure of new open pits, a stagnating public building sector and a considerable pressure of globalisation. The chances of the domestic economy are the realization of high grade objects in the individual segment, a friendly customer advisory service and an offensive marketing, promoting the benefits of building with natural construction materials.
    Description: 1. Vorbemerkung 2. Deutsche Naturwerksteinvorkommen 3. Allgemeine Lage der Naturwerksteinindustrie 4. Nationale Situation 5. Probleme der Globalisierung 6. Schlussfolgerungen Schriften
    Description: report
    Keywords: ddc:338.2
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 42
    Publication Date: 2022-07-29
    Description: Infolge eines Schadensereignisses wurde in einem Hangabschnitt im Mittelrheintal oberhalb der Bundesstraße B 9 bei Trechtingshausen eine erhebliche Steinschlaggefahr festgestellt. Um den Verkehr möglichst wenig zu beeinträchtigen, sind die notwendigen Sicherungsmaßnahmen in getrennten Schritten durchgeführt worden. Als Sofortmaßnahme wurden zunächst die akut absturzgefährdeten Felskörper im Schutz verschiedener provisorischer Sicherungsmaßnahmen beräumt. Teile dieser Maßnahmen wurden danach als Temporärsicherungen im Hang belassen, bis der Streckenabschnitt letztendlich mit Hilfe von Systemfangzäunen langfristig gesichert werden konnte.
    Description: Abstract: After an incident, a considerable rockfall hazard was determined for a section of the Bundesstraße B 9 near Trechtingshausen (rhine-valley). To impair traffic as little as possible, the necessary safety measures were carried out in different steps. As an emergency precaution all obviously instable rocks were cleared away first. Therefore installed safety fences were left in the slope as temporary precautions until special rockfall barriers were set up for long term protection.
    Description: report
    Keywords: ddc:620
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 43
    Publication Date: 2022-07-29
    Description: Nahe der Ortschaft Hainau (Taunus; Rhein-Lahn-Kreis) konnte eine umfangreiche fossile Fauna aus dem Unterems (Unterdevon) aufgesammelt werden. Diese lieferte unter anderem zahlreiche Reste der homalonoten Trilobiten Arduennella maillieuxi (ASSELBERGHS 1923), Digonus ornatus linguatus WENNDORF 1990 und Wenndorfia mutabilis (KOCH 1880). Zu diesen werden die speziellen Befunde vom Fundort vorgestellt.
    Description: Abstract: Near Hainau (Taunus, Rhenish Massif; Rhein-Lahn-Kreis, Germany) a fauna of Lower Emsian age (Lower Devonian) was collected which is rich in remains of the homalonotid trilobites Arduennella maillieuxi (ASSELBERGHS 1923), Digonus ornatus linguatus WENNDORF 1990 and Wenndorfia mutabilis (KOCH 1880). For these species specific statements from this site are presented.
    Description: research
    Keywords: ddc:562
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 44
    Publication Date: 2022-07-29
    Description: Eine Wenndorfia mutabilis (Koch 1880) mit offensichtlicher Erhaltung des Verdauungstrakts und des Hypostoms in situ wird beschrieben. Für die Art wird eine wahrscheinlich räuberische Lebensweise hergeleitet. Die besondere Erhaltung des Fundes wird auf eine rasche Einbettung im Sediment zurückgeführt.
    Description: Abstract: A Wenndorfia mutabilis (Koch 1880) is described which apparently shows a preservation of its alimentary system and its hypostome in situ. A predatory feeding habit is considered probable for this species. The specimens exceptional preservation is traced back to a quick embedding.
    Description: research
    Keywords: ddc:562
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 45
    facet.materialart.
    Unknown
    Publication Date: 2022-07-29
    Description: Der rheinland-pfälzische Teil des Oberrheingrabens ist im bundesweiten Vergleich als Standort tiefengeothermischer Projekte besonders gut geeignet. Die Grabenstruktur verursacht ein regionales Wärmehoch mit hohem geothermischen Gradienten. Eine Nutzung dieser geothermischen Anomalie ermöglicht die Verstromung und Bereitstellung von Wärme in Wärmenetzen. Konvektiver Wärmetransport durch aufsteigende Tiefenwässer und Wasserhöffigkeit in ausreichender Tiefe machen das Gebiet der Vorderpfalz für eine hydrothermale Nutzung besonders interessant. In dieser Region kommen triassische Gesteine, Rotliegend-Sedimente sowie Kristallines Grundgebirge aufgrund der Tiefenlage, der ausgebildeten Klüftigkeit und der Existenz tiefgreifender Störungsstrukturen für eine hydrothermale Erschließung in Betracht. Außerhalb des Oberrheingrabens sind die geothermischen Verhältnisse in Rheinland- Pfalz als durchschnittlich anzusehen. In Rheinland-Pfalz werden Thermalwässer schon seit Jahrhunderten vorrangig zu balneologischen Zwecken genutzt. Erst die Verabschiedung des „Erneuerbaren-Energien- Gesetzes“ (EEG) im Jahr 2000 rückte die Nutzung tiefer geothermischer Ressourcen in den Bereich einer wirtschaftlichen Rendite. Zwischenzeitlich wurde in der Vorderpfalz zwischen der französischen Landesgrenze und Speyer mit dem Bau von vier geothermischen Kraftwerken und der Planung weiterer Projekte begonnen. Bei einem planmäßigen Projektverlauf wird Ende 2007 in Landau das erste Geothermiekraftwerk in Rheinland- Pfalz seinen Betrieb aufnehmen. Die Erschließung petrothermaler Lagerstätten wird in Rheinland-Pfalz noch nicht betrieben. Um das Hot-Dry-Rock-Verfahren (HDR) als technische Anwendung zu etablieren muss insbesondere die hydraulische Stimulationstechnik weiter entwickelt und erprobt werden. Vielversprechend erscheint zum heutigen Zeitpunkt die Bereitstellung von Wärme mit Hilfe von tiefen Erdwärmesonden. In Rheinland- Pfalz sind zahlreiche nicht verwahrte Tiefbohrungen aus der Kohlenwasserstoff- Industrie vorhanden und könnten kostengünstig für den Sondeneinbau genutzt werden.
    Description: The Upper Rhinegraben in Rhineland-Palatine is – in a nationwide comparison – a particularly well suitable location for deep-depth geothermal projects. A regional temperature high causes enhanced geothermal gradients in this graben structure and enables geothermal electrification and provision of heat in domestic heat networks. Due to convective heat transmission caused by uprising deep-depth water and potential ground water yield in sufficient depth, this area is of special interest for geothermal utilization. Triassic rocks, Permian sediments as well as crystalline basement can – due to their depth, developed joints and the existence of deep fault systems – be considered for geothermal usage. Beyond the Upper Rhinegraben in Rhineland-Palatinate the geothermal conditions are on average level. 135 Mainzer geowiss. Mitt. 35 S. 135–158 10 Abb. 1 Tab. Mainz, Oktober 2007 In Rhineland-Palatinate thermal water has been used for balneological purposes for decades. After all, the passing of the „Erneuerbare-Energien-Gesetz“ (EEG) made the use of deep-depth geothermal resources economically profitable. In the meantime four geothermal power-plants are being built between the French border and Speyer and a few more are in the design stage. If the project proceeds as scheduled, the first geothermal power-plant in Rhineland-Palatinate will go into service in the end of 2007. The development of petrothermal deposits has not yet been done in Rhineland-Palatinate so far. To establish the Hot-Dry-Rock-Technique (HDR) as a technical employment, the hydraulic simulation technology in particular has to be advanced and tested. At the present stage the provision of heat with deep-depth bore hole heat exchangers seems to be more promising. In Rhineland-Palatinate there are numerous unused deep wells from the hydrocarbon industry existing which could be used cost-efficiently for the installation of bore hole heat exchangers.
    Description: 1. Einleitung 2. Grundlagen der Nutzung tiefer geothermischer Ressourcen 3. Tiefengeothermische Bedingungen in Rheinland-Pfalz 3.1. Thermische Verhältnisse in der Vorderpfalz 3.2. Hydrogeologische Verhältnisse in der Vorderpfalz 3.3. Hydrothermale Zielhorizonte in der Vorderpfalz 3.4. Petrothermale Lagerstätten 4. Nutzung tiefer geothermischer Ressourcen in Rheinland-Pfalz 5. Ausblick Schriften
    Description: research
    Keywords: ddc:333.88 ; ddc:554.3
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 46
    Publication Date: 2022-07-22
    Description: An Bohrkernen aus dem Zechstein und Unteren Buntsandstein des Nordrandes der Pfälzer Mulde wurden in Triaxialzellen Versuche zur Bestimmung der vertikalen hydraulischen Leitfähigkeiten durchgeführt. Die Versuche dienten der Ergänzung und Verbesserung der bislang wenigen verfügbaren Daten zu geohydraulischen Kennwerten für diesen hydrogeologischen Teilraum. Die Versuchsanordnung wird erläutert; auf Probleme bei der Versuchsdurchführung wird hingewiesen. Die Ergebnisse werden diskutiert und bisher ermittelten Werten gegenüber gestellt. Der ermittelte Wertebereich der vertikalen hydraulischen Leitfähigkeiten liegt zwischen etwa 3 x 10–6 m/s bis 2 x 10–9 m/s (Medianwerte). Er gilt für den durch die Gesteinsmatrix bedingten Anteil der Gebirgsdurchlässigkeit. Das Verhältnis von vertikaler zu horizontaler hydraulischer Leitfähigkeit kann in den Größenordnungen von etwa 1:101 bis 1:103 angesetzt werden. Die Ergebnisse lassen vermuten, dass die räumliche Verteilung der Permeabilitäten im Untersuchungsgebiet bereits sehr kleinmaßstäblich durch sedimentäre und diagenetische Faziesvariationen beeinflusst wird.
    Description: Abstract: At drill cores from the Upper Permian (Zechstein) and the Lower Bunter of the northern Palatinate Syncline experiments were accomplished in triaxial cells to determine the vertical hydraulic conductivity. The experiments served for the addition and improvement of the past data set of geohydraulic parameters. The experimental assembly is described and it is referred to problems during the investigational procedure. The results are discussed and compared with so far published data. The range of the determined values of vertical hydraulic conductivity lies between approximately 3 x 10–6 m/s to 2 x 10–9 m/s (median values). It applies to the portion of the rock permeability due to the rock matrix. The ratio of vertical to horizontal hydraulic conductivity can be set in the orders of magnitude from approximately 1:101 to 1:103. The results let assume that the spatial distribution of the permeability in the area of interest is affected already by very small scale sedimentary and diagenetic facies variations.
    Description: research
    Keywords: ddc:551.49
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 47
    Publication Date: 2023-01-05
    Description: Nachdem sich Herzog Georg von Sachsen mit den Problemen des Bergbaus auf dem Aldenberg und Geising auseinandergesetzt hatte, erlies er am 11. November 1489 eine Ordnung für die dortigen Bergwerke. In den acht Artikeln dieser Ordnung wurden die Entlohnung der Bergleute sowie die Pflichten der Hutleute, Mühlmeister, Schmelzer und die Strafen bei Zuwiderhandlung festgelegt. Weiterhin wurde eine Vereidigung der Hutleute, Mühlenmeister und Schmelzer befohlen.
    Description: source
    Keywords: Herzog Georg von Sachsen ; Herzog Albrecht von Sachsen ; Hans von Bärenstein zu Ottendorf ; Altenberg ; Geising ; Zinnbergbau ; Sachsen ; Bergordnung
    Language: German
    Type: doc-type:book , updatedVersion
    Format: 6
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 48
    Publication Date: 2023-01-02
    Description: Diese Bergordnung wurde am 26. Juli 1449 für die Bergwerke in Schwaz von Herzog Siegmund von Österreich, Steiermark und Kärnten sowie Herr zu Krain und Pfirt, Graf zu Tirol und Kyburg, Landgraf zu Elsaß und Markgraf zu Burgau erlassen. Grundlage war ein 38 Paragrafen umfassendes Gutachten das von Herzog Siegmund mit einer zwölf Paragrafen umfassenden Bestätigung als Bergordnung in Kraft gesetzt wurde. Erklärt wurden das Gerichtswesen, die Holzrechte, die Entlohnung und Versorgung der im Bergbau Beschäftigten sowie die Rechte und Pflichten der Markscheider.
    Description: source
    Keywords: Herzog Siegmund von Österreich ; Österreich ; Steiermark ; Kärnten ; Tirol ; Elsaß ; Gossensaß ; Meran ; Schwaz ; Freundsberg, Burg ; Arlberg ; Brenner ; Silberbergbau ; Bergordnung
    Language: German
    Type: doc-type:book , updatedVersion
    Format: 13
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 49
    Publication Date: 2023-01-12
    Description: Transient magnetic reconnection plays an important role in energetic particle acceleration in planetary magnetospheres. Jupiter's magnetosphere provides a unique natural laboratory to study processes of energy transport and transformation. Strong electric fields in spatially confined structures such as plasmoids can be responsible for ion acceleration to high energies. In this study we focus on the effectiveness of ion energization and acceleration in plasmoids. Therefore, we present a statistical study of plasmoid structures in the predawn magnetotail, which were identified in the magnetometer data of the Juno spacecraft from 2016 to 2018. We additionally use the energetic particle observations from the Jupiter Energetic Particle Detector Instrument which discriminates between different ion species. We are particularly interested in the analysis of the acceleration and energization of oxygen, sulfur, helium, and hydrogen ions. We investigate how the event properties, such as the radial distance and the local time of the observed plasmoids in the magnetotail, affect the ion intensities close to the current sheet center. Furthermore, we analyze if ion acceleration is influenced by magnetic field turbulence inside the plasmoids. We find significant heavy ion acceleration in plasmoids close to the current sheet center which is in line with the previous statistical results based on Galileo observations conducted by Kronberg et al. (2019, https://doi.org/10.1029/2019JA026553). The observed effectiveness of the acceleration is dependent on the position of Juno in the magnetotail during the plasmoid event observation. Our results show no correlation between magnetic field turbulence and nonadiabatic acceleration for heavy ions during plasmoids.
    Description: Key Points: Intensity of heavy ions is strongly increased during plasmoids close to the current sheet center. Significant increase of heavy ion intensities is observed in plasmoids with larger wave power. Acceleration of heavy and light ions in plasmoids due to resonant interaction with the magnetic field fluctuations could not be observed.
    Description: Volkswagen Foundation (VolkswagenStiftung) http://dx.doi.org/10.13039/501100001663
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: NASA
    Description: https://pds-ppi.igpp.ucla.edu/
    Keywords: ddc:523 ; plasmoids ; Juno ; JEDI ; ion acceleration
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 50
    Publication Date: 2023-01-12
    Description: Hydrological extreme events are generated by different sequences of hydrometeorological drivers, the importance of which may vary within the sample of drought events. Here, we investigate how the importance of different hydrometeorological driver sequences varies by event magnitude using a large sample of catchments in Europe. To do so, we develop an automated classification scheme for streamflow drought events. The classification scheme standardizes a previous qualitative drought typology and assigns events to one of eight drought event types—each characterized by a set of single or compounding drivers—using information about seasonality, precipitation deficits, and snow availability. The objective event classification reveals how drought drivers vary not just in space and by season, but also with event magnitude. Specifically, we show that (a) rainfall deficit droughts and cold snow season droughts are the dominant drought event type in Western Europe and Eastern and Northern Europe, respectively; (b) rainfall deficit and cold snow season droughts are important from autumn to spring while snowmelt and wet‐to‐dry season droughts are important in summer; and (c) moderate droughts are mainly driven by rainfall deficits while severe events are mainly driven by snowmelt deficits in colder climates and by streamflow deficits transitioning from the wet to the dry season in warmer climates. These differences in sequences of drought generation mechanisms for severe and moderate events suggest that future changes in hydrometeorological drivers may affect moderate and severe events differently.
    Description: Key Points: We develop a standardized and objective classification scheme for streamflow droughts using hydroclimatic information. The most severe drought events are governed by other processes than moderate events. Moderate droughts are dominated by rainfall deficits and severe droughts by snowmelt deficits or prolonged rainfall deficit droughts.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: EC/H2020/PRIORITY 'Excellent science'/H2020 European Research Council http://dx.doi.org/10.13039/100010663
    Description: https://www.bafg.de/GRDC/EN/02_srvcs/21_tmsrs/riverdischarge_node.html
    Description: https://doi.pangaea.de/10.1594/PANGAEA.887470
    Description: https://cds.climate.copernicus.eu/cdsapp#!/dataset/reanalysis-era5-land?tab=overview
    Description: http://www.hydroshare.org/resource/77114d4dfdfd4dd39e0e1d99165f27b3
    Keywords: ddc:551.6 ; drought types ; drought generation ; extremes ; typology ; classification ; streamflow
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 51
    Publication Date: 2023-01-12
    Description: Harmonic Earth tide components in well water levels have been used to estimate hydraulic and geomechanical subsurface properties. However, the robustness of various methods based on analytical solutions has not been established. First, we review the theory and examine the latest analytical solution used to relate well water levels to Earth tides. Second, we develop and verify a novel numerical model coupling hydraulics and geomechanics to Earth tide strains. Third, we assess subsurface conditions over depth for a range of realistic properties. Fourth, we simulate the well water level response to Earth tide strains within a 2D poroelastic layered aquifer system confined by a 100 m thick aquitard. We find that the non‐linear inversion of analytical solutions to match two observations (amplitudes and phases) to multiple unknown parameters is sensible to the initial guess. We reveal that undrained, confined conditions are necessary for the analytical solution to be valid. This occurs for the dominant M2 frequency at depths 〉50 m and requires specific storage at constant strain of Sϵ ≥ 10−6 m−1, hydraulic conductivity of the aquitard of kl ≤ 5 ⋅ 10−5 ms−1 and aquifer of ka ≥ 10−4 ms−1. We further illustrate that the analytical solution is valid in unconsolidated systems, whereas consolidated systems require additional consideration of the Biot modulus. Overall, a priori knowledge of the subsurface system supports interpretation of the groundwater response. Our results improve understanding of the effect of Earth tides on groundwater systems and its interpretation for subsurface properties.
    Description: Plain Language Summary: Earth tide induced strains in the subsurface lead to well water level fluctuations in groundwater monitoring wells. This groundwater response has been interpreted with analytical solutions to estimate aquifer properties. However, analytical solutions are based on simplified assumptions whose accuracy have not yet been tested. We develop a new approach to simulate the influence of Earth tides on groundwater based on fundamental physical principles. We simulate realistic conditions and compare our results to those from analytical solution to determine the hydraulic and subsurface conditions under which simplified interpretations are valid. Our results improve understanding of the effects of Earth tides on groundwater systems and interpretation of subsurface properties from well water levels.
    Description: Key Points: We develop and verify a numerical model for the well water level response to Earth tides. Subsurface property estimation requires undrained and confined conditions occurring at depths 〉50 m. Amplitudes and phases from numerical and analytical solutions systematically diverge reflecting theory simplifications.
    Description: German Research Council
    Description: https://doi.org/10.5281/zenodo.6950492
    Keywords: ddc:551 ; tidal subsurface analysis ; numerical modeling ; Earth tides
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 52
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    Publication Date: 2023-01-09
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom September 2022 enthält die Themenblöcke: GEOfokus: Klimagerechte Geowissenschaften Glaubwürdigkeit und Vorbild, GEOaktiv (Wirtschaft, Beruf, Forschung und Lehre), GEOlobby (Gesellschaften, Verbände, Institutionen), GEOreport (Geowissenschaftliche Öffentlichkeitsarbeit, Tagungsberichte, Ausstellungen, Exkursionen, Publikationen), GEOszene (Würdigungen, Nachrufe).
    Description: DFG, SUB Göttingen
    Description: journal
    Keywords: ddc:550 ; GMIT
    Language: German
    Type: doc-type:book , publishedVersion
    Format: 132
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 53
    Publication Date: 2023-01-10
    Description: manual
    Keywords: ddc:631.4 ; Rheinland-Pfalz ; Hessen ; Bodenschutz ; Raumplanung
    Language: German
    Type: doc-type:book , publishedVersion
    Format: 68
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 54
    Publication Date: 2023-01-15
    Description: A Guinier camera equipped with an imaging plate is used to investigate and eliminate the sources of instrumental errors affecting the quality of the obtained scanned Guinier data. A program with a graphical user interface is presented which converts the data of the scanned images into different standard file formats for powder X‐ray patterns containing intensities, their standard deviations and the diffraction angles. The program also allows for manual and automatic correction of the 2gθ scale against a known reference material. It is shown using LaB6 that the exported X‐ray diffraction patterns provide a 2gθ scale reproducible enough to allow for averaging diffractograms obtained from different exposures of the imaging plate for the same sample. As shown on a mixture of NaCl and sodalite, the quality of the produced data is sufficient for Rietveld refinement. The software including source code is made available under a free software license.
    Description: A program for the digitization of Guinier powder diffraction images is described, which works with images from both optical and laser scanners. Thus, processing of data from storage‐phosphor‐based imaging plates and Ag‐based photographic films is possible.
    Keywords: ddc:548 ; IPreader software ; Guinier cameras ; imaging plates (IPs) ; diffraction pattern conversion into data columns ; powder X‐ray diffraction ; data processing ; Guinier method
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 55
    Publication Date: 2023-01-15
    Description: Key knowledge about planetary composition can be recovered from the study of thermal infrared spectral range datasets. This range has a huge diagnostic potential because it contains diagnostic absorptions from a planetary surface and atmosphere. The main goal of this study is to process and interpret the dataset from the Thermal Infrared channel (TIRVIM) which is part of the Atmospheric Chemistry Suite of the ExoMars2016 Trace Gas Orbiter mission to find and characterize dust and water ice clouds in the atmosphere. The method employed here is based on the application of principal component analysis and target transformation techniques to extract the independent variable components present in the analyzed dataset. Spectral shapes of both atmospheric dust and water ice aerosols have been recovered from the analysis of TIRVIM data. The comparison between our results with those previously obtained on Thermal Emission Spectrometer (TES) data and with previous analysis on TIRVIM data, validates the methodology here applied, showing that it allows to correctly recover the atmospheric spectral endmembers present in the TIRVIM data. Moreover, comparison with atmospheric retrievals on PFS, TES and IRIS data, allowed us to assess the temporal stability and homogeneity of dust and water ice components in the Martian atmosphere over a time period of almost 50 years.
    Description: Plain Language Summary: The analysis of thermal infrared datasets from planetary bodies is of key importance for the understanding of a planet's climate evolution and history: it contains valuable information about composition, temperature and state of the atmosphere. Moreover, surface properties and the surface‐atmosphere interaction can be studied. Here we investigated new thermal infrared data from the Thermal Infrared channel instrument of the ExoMars Trace Gas Orbiter with the main goal of carefully identifying Martian atmospheric dust and water ice clouds components. A methodology based on principal component and target transformation factor analysis techniques has been applied. Based on our results, this methodology can correctly recover both atmospheric dust and water ice aerosols spectral shapes and their abundances in the Martian atmosphere.
    Description: Key Points: First successful application of principal components and target transformation techniques to high‐resolution Thermal Infrared channel (TIRVIM) data. Spectral shapes of both atmospheric dust and water ice clouds are recognized and recovered. TIRVIM data are successfully modeled through a linear combination of the recovered water ice and dust end‐members.
    Description: Roscosmos and ESA
    Description: https://doi.org/10.5281/zenodo.7032738
    Keywords: ddc:523 ; Martian atmosphere ; TIRVIM data
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 56
    Publication Date: 2023-01-15
    Description: A limited number of gauging stations, especially for nested catchments, hampers a process understanding of the interaction between streamflow, groundwater and water usage during drought. Non‐commercial measurement devices can help overcome this lack of monitoring, but they need to be thoroughly tested. The Dreisam River in the South‐West of Germany was affected by several hydrological drought events from 2015 to 2020 during which parts of the main stream and tributaries fell dry. Therefore it provided a useful case study area for a flexible longitudinal water quality and quantity monitoring network. Among other measurements the setup employs an image‐based method with QR codes as fiducial marker. In order to assess under which conditions the QR‐code based water level loggers (WLL) deliver data according to scientific standards, we compared its performance to conventional capacitive based WLL. The results from 20 monitoring stations reveal that the riverbed was dry for 〉50% at several locations and even for 〉70% at most severely affected locations during July and August 2020, with the north western parts of the catchment being especially concerned. Highly variable longitudinal drying patterns of the stream reaches emerged from the monitoring. The image‐based method was found valuable for identification and validation of zero level occurrences. Nevertheless, a simple image processing approach (based on an automatic thresholding algorithm) did not compensate for errors due to natural conditions and technical setup. Our findings highlight that the complexity of measurement environments is a major challenge when working with image‐based methods.
    Description: We monitored zero water levels in a meso‐scale catchment with temperate climate by means of image‐based and conventional water level logging techniques. A detailed analysis of the longitudinal drying patterns enables a discussion about hydrological connectivity and the processes influencing the drying.
    Description: Badenova Fund For Innovation
    Description: https://doi.org/10.6094/UNIFR/228702
    Keywords: ddc:551.48 ; hydrological drought ; innovative sensors ; longitudinal connectivity ; stream reaches ; streamflow intermittency ; zero flow
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 57
    Publication Date: 2023-01-15
    Description: The dynamics of the Alps and surrounding regions is still not completely understood, partly because of a non‐unique interpretation of its upper‐mantle architecture. In particular, it is unclear if interpreted slabs are consistent with the observed surface deformation and topography. We derive three end‐member scenarios of lithospheric thickness and slab geometries by clustering available shear‐wave tomography models into a statistical ensemble. We use these scenarios as input for geodynamic simulations and compare modeled topography, surface velocities and mantle flow to observations. We found that a slab detached beneath the Alps, but attached beneath the Northern Apennines captures first‐order patterns in topography and vertical surface velocities and can provide a causative explanation for the observed seismicity.
    Description: Plain Language Summary: Present‐day surface deformation, including earthquakes, plate motion, and mass (re)distribution, results from processes operating at the surface and in the interior of the Earth. Understanding these processes and their coupling is of utmost importance in light of the hazard they pose to society. The Alps provide an excellent natural laboratory to understand such coupling. Here, we use seismic tomography models to constrain its upper‐mantle architecture. We further use these models to quantify forces originating from the resolved architecture and their effects on the present‐day surface deformation. The models can reproduce first‐order patterns in the observed topography and vertical surface motions. We found a causative correlation between the presence of a shallow slab attached to the overlying lithosphere in the Northern Apennines and the seismicity in the region. Our results allow us to better understand the transfer of internal forces to the surface, thereby helping to quantify the present‐day mechanical setup of the area.
    Description: Key Points: Statistical ensemble of S‐wave tomography models is used to infer the Lithosphere‐Asthenosphere Boundary configuration and slab geometries in the Alps. The 3‐D upper‐mantle architecture from the statistics reproduce first‐order patterns in observed topography and Global Navigation Satellite Systems vertical velocities. A shallow/attached slab in the Northern Apennines is consistent with the mantle depth seismicity observed in this region.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: https://doi.org/10.5880/GFZ.4.5.2019.004
    Description: https://gfzpublic.gfz-potsdam.de/pubman/item/item_238001
    Description: http://ds.iris.edu/ds/products/emc-earthmodels/
    Description: https://doi.org/10.5281/zenodo.7071571
    Description: https://doi.org/10.5281/zenodo.6538257
    Keywords: ddc:551.1 ; Alps ; Apennines ; lithospheric architecture ; slabs ; seismicity
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 58
    Publication Date: 2023-01-15
    Description: Physiological sensitivity of cold‐water corals to ocean change is far less understood than of tropical corals and very little is known about the impacts of ocean acidification and warming on degradative processes of dead coral framework. In a 13‐month laboratory experiment, we examined the interactive effects of gradually increasing temperature and pCO2 levels on survival, growth, and respiration of two prominent color morphotypes (colormorphs) of the framework‐forming cold‐water coral Lophelia pertusa, as well as bioerosion and dissolution of dead framework. Calcification rates tended to increase with warming, showing temperature optima at ~ 14°C (white colormorph) and 10–12°C (orange colormorph) and decreased with increasing pCO2. Net dissolution occurred at aragonite undersaturation (ΩAr 〈 1) at ~ 1000 μatm pCO2. Under combined warming and acidification, the negative effects of acidification on growth were initially mitigated, but at ~ 1600 μatm dissolution prevailed. Respiration rates increased with warming, more strongly in orange corals, while acidification slightly suppressed respiration. Calcification and respiration rates as well as polyp mortality were consistently higher in orange corals. Mortality increased considerably at 14–15°C in both colormorphs. Bioerosion/dissolution of dead framework was not affected by warming alone but was significantly enhanced by acidification. While live corals may cope with intermediate levels of elevated pCO2 and temperature, long‐term impacts beyond levels projected for the end of this century will likely lead to skeletal dissolution and increased mortality. Our findings further suggest that acidification causes accelerated degradation of dead framework even at aragonite saturated conditions, which will eventually compromise the structural integrity of cold‐water coral reefs.
    Description: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: Marine Research in Ireland
    Description: French National Research Agency http://dx.doi.org/10.13039/501100001665
    Keywords: ddc:577.7 ; cold-water corals ; ocean change ; laboratory experiments ; framwork dissolution ; bioerosion
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 59
    Publication Date: 2023-01-17
    Description: In this study, a spectral model for convective transport is coupled to a thermal population model on a two‐dimensional horizontal “microgrid,” covering the typical gridbox size of general circulation models. The goal is to explore new ways of representing impacts of spatial organization in cumulus cloud fields. The thermals are considered the smallest building block of convection, with thermal life cycle and movement represented through binomial functions. Thermals interact through two simple rules, reflecting pulsating growth and environmental deformation. Long‐lived thermal clusters thus form on the microgrid, exhibiting scale growth and spacing that represent simple forms of spatial organization and memory. Size distributions of cluster number are diagnosed from the microgrid through an online clustering algorithm, and provided as input to a spectral multiplume eddy‐diffusivity mass flux scheme. This yields a decentralized transport system, in that the thermal clusters acting as independent but interacting nodes that carry information about spatial structure. The main objectives of this study are (a) to seek proof of concept of this approach, and (b) to gain insight into impacts of spatial organization on convective transport. Single‐column model experiments demonstrate satisfactory skill in reproducing two observed cases of continental shallow convection. Metrics expressing self‐organization and spatial organization match well with large‐eddy simulation results. We find that in this coupled system, spatial organization impacts convective transport primarily through the scale break in the size distribution of cluster number. The rooting of saturated plumes in the subcloud mixed layer plays a key role in this process.
    Description: Plain Language Summary: Recent studies have emphasized the importance of the spatial structure of convective cloud fields in Earth's climate, yet this phenomenon is not yet represented well in Earth System Models (ESMs). This study explores a new way to achieve this goal, by considering spatial organization at the scale of small bubbles of rising air called thermals that together make up convective clouds. Populations of interacting thermals are modeled in a computationally efficient way on a small two‐dimensional grid. This microgrid is then coupled to a convection scheme, which stands for the set of equations used to statistically represent the impact of convective transport at scales that remain unresolved in ESMs. The coupling makes the scheme decentralized, in that the transport becomes dependent on a population of longer‐lived convective structures that slowly develop and evolve on the microgrid. The new scheme is tested for observed conditions at a meteorological site in the Southern Great Plains area of the United States, making use of a combination of high‐resolution simulations and measurements to evaluate performance. Apart from proof of concept for the new modeling approach, the results provide new insights into how the spatial structure of convective cloud populations can affect its vertical transport.
    Description: Key Points: A multiplume spectral convection scheme is coupled to a binomial thermal population model on a horizontal microgrid. Observed diurnal cycles of continental shallow convection are reproduced, including good agreement on scale growth and spatial organization. Spatial organization impacts convective transport through the scale break in the cluster number density, with a key role played by plume rooting.
    Description: U.S. Department of Energy http://dx.doi.org/10.13039/100000015
    Description: https://doi.org/10.5281/zenodo.6044338
    Keywords: ddc:551.5 ; convective parameterization ; spatial organization ; population dynamics ; thermals ; microgrid modeling ; shallow cumulus
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 60
    Publication Date: 2023-01-17
    Description: It is generally agreed that the resolution of a regular quadrilateral mesh is the side length of quadrilateral cells. There is less agreement on the resolution of triangular meshes, exacerbated by the fact that the numbers of edges or cells on triangular meshes are approximately three or two times larger than that of vertices. However, the geometrical resolution of triangular meshes, that is, maximum wavenumbers or smallest wavelengths that can be represented on such meshes, is a well defined quantity, known from solid state physics. These wavenumbers are related to a smallest common mesh cell (primitive unit cell), and the set of mesh translations that map it into itself. They do not depend on whether discrete degrees of freedom are placed on vertices, cells or edges. For equilateral triangles the smallest wavelength equals twice the triangle height. Resolutions of quadrilateral and triangular meshes approximately agree if they have the same numbers of vertices.
    Description: Plain Language Summary: Some models used in climate studies are formulated on triangular computational meshes. We discuss how to determine the smallest scales that are resolved on such meshes. They are referred to as a mesh resolution. The notion of mesh resolution is commonly used to relate climate model results simulated on different meshes.
    Description: Key Points: Geometrical resolution of an equilateral triangular mesh is defined by the height of its triangles. Quadrilateral and triangular meshes with the same number of vertices have approximately the same resolution.
    Description: Collaborative Research Centre
    Description: German Research Foundation
    Keywords: ddc:550 ; triangular meshes ; resolved wavenumbers
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 61
    Publication Date: 2023-01-17
    Description: In this study, we investigated the phase stability of Al‐free and Al‐bearing superhydrous phase B (shy‐B) up to 55 GPa and 2500 K. In comparison with Al‐free shy‐B, the incorporation of 11.7 wt.% Al2O3 in shy‐B expands the stability by ∼400–800 K at 20–30 GPa. The determined dehydration boundary for Al‐bearing phase D indicates that it could be present even at normal mantle geotherm conditions at 30–40 GPa. Up to 23.8 mol.% Al2O3 can be dissolved into the structures of akimotoite and bridgmanite as a result of the decomposition reactions of Al‐bearing shy‐B and phase D between 20 and 40 GPa. Results of further experiments indicate that δ‐AlOOH is the stable hydrous phase coexisting with Al‐depleted bridgmanite at pressures above 52 GPa. This study shows that the incorporation of Al in dense hydrous magnesium silicates can have a profound impact on our picture of the water cycle in the deep Earth.
    Description: Plain Language Summary: Constraining the deep cycle of water has a tremendous impact on our picture of the current state of the Earth and the evolution of the Earth's interior. Dense hydrous magnesium silicates (DHMSs) are considered potential H2O carriers in the Earth's mantle. However, the DHMSs can only be present at the relatively cold conditions of subduction slabs due their limited thermal stability. We determined the phase stability of Al‐bearing DHMSs at high pressure and temperature (P‐T) conditions. Our results show that the thermal stability of Al‐bearing shy‐B extends by 400–800 K with respect to its Al‐free counterpart at 600–800 km depth. The incorporation of Al also expands the phase stability of phase D and enhances the likelihood of its occurrence at normal mantle conditions at 800–1100 km. In addition, we observe that 23.8 mol.% Al2O3 can be dissolved into the structures of akimotoite and bridgmanite as a result of the decomposition reactions of Al‐bearing shy‐B and phase D between 600 and 100 km depth. Furthermore, δ‐AlOOH is the stable hydrous phase coexisting with Al‐depleted bridgmanite in the MgO‐SiO2‐Al2O3‐H2O system at pressures above 52 GPa and 1500 K.
    Description: Key Points: In comparison with Al‐free shy‐B, the incorporation of 11.7 wt.% Al2O3 in superhydrous phase B (shy‐B) expands the stability by ∼400–800 K at 20–30 GPa. Al‐bearing phase D could be present even at normal mantle geotherm conditions at 30–40 GPa. δ‐AlOOH is the stable hydrous phase coexisting with Al‐depleted bridgmanite at pressures above 52 GPa.
    Description: Center for Molecular Water Science, CMWS
    Description: https://doi.org/10.5281/zenodo.6320835
    Keywords: ddc:549 ; Al‐bearing superhydrous phase B ; phase D ; phase stability ; high pressure and temperature ; deep Earth water cycle
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 62
    facet.materialart.
    Unknown
    Wangari, E. G. ; Mwanake, R. M. ; Kraus, D. ; [et al.]
    Publication Date: 2023-01-17
    Description: Accurate quantification of landscape soil greenhouse gas (GHG) exchange from chamber measurements is challenging due to the high spatial‐temporal variability of fluxes, which results in large uncertainties in upscaled regional and global flux estimates. We quantified landscape‐scale (6 km2 in central Germany) soil/ecosystem respiration (SR/ER‐CO2), methane (CH4), and nitrous oxide (N2O) fluxes at stratified sites with contrasting landscape characteristics using the fast‐box chamber technique. We assessed the influence of land use (forest, arable, and grassland), seasonality (spring, summer, and autumn), soil types, and slope on the fluxes. We also evaluated the number of chamber measurement locations required to estimate landscape fluxes within globally significant uncertainty thresholds. The GHG fluxes were strongly influenced by seasonality and land use rather than soil type and slope. The number of chamber measurement locations required for robust landscape‐scale flux estimates depended on the magnitude of fluxes, which varied with season, land use, and GHG type. Significant N2O‐N flux uncertainties greater than the global mean flux (0.67 kg ha−1 yr−1) occurred if landscape measurements were done at 〈4 and 〈22 chamber locations (per km2) in forest and arable ecosystems, respectively, in summer. For CO2 and CH4 fluxes, uncertainties greater than the global median CO2‐C flux (7,500 kg ha−1 yr−1) and the global mean forest CH4‐C uptake rate (2.81 kg ha−1 yr−1) occurred at 〈2 forest and 〈6 arable chamber locations. This finding suggests that more chamber measurement locations are required to assess landscape‐scale N2O fluxes than CO2 and CH4, based on these GHG‐specific uncertainty thresholds.
    Description: Plain Language Summary: Greenhouse gas emissions are subject to high spatial and temporal variability, leading to large uncertainties in regional and global estimates. We quantified fluxes of soil and ecosystem respiration (SR/ER‐CO2), methane (CH4) and nitrous oxide (N2O) at the landscape scale (6 km2 in central Germany). We determine the number of measurement chambers required to estimate landscape fluxes within globally significant uncertainty thresholds. Our results show a stronger influence of season and land use, as opposed to soil type and topography. The number of chambers required for robust landscape‐wide flux estimates depended on the size of the fluxes, which varied by season, land use and GHG type. An increase in the number of monitoring sites significantly reduced the uncertainties estimation on the whole landscape. Significant uncertainties in N2O fluxes above the global annual mean was found when landscape measurements were made at 〈4 monitoring sites in forests and 〈22 monitoring sites (per km2) in cropland ecosystems during the summer period. For SR/ER‐CO2 fluxes, as few as 〈2 was sufficient in forest ecosystems and under 〈6 in cropland ecosystems. This result implies that in general more monitoring sites are needed to assess landscape‐scale N2O fluxes than for CO2 and CH4 fluxes.
    Description: Key Points: Land use and seasonality rather than soil type and slope strongly influenced soil greenhouse gas (GHG) fluxes at a landscape‐scale. The minimum number of chamber locations required for robust landscape‐scale flux estimates depends on the season, land use, and GHG type. Chamber locations required to reduce uncertainties of landscape flux estimates declined as follows N2O 〉 CO2 〉 CH4.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: https://doi.org/10.5281/zenodo.6821111
    Keywords: ddc:631.4 ; soil respiration ; ecosystem respiration ; methane uptake ; nitrous oxide fluxes ; spatial‐temporal variability ; stratfied sampling
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 63
    Publication Date: 2023-01-17
    Description: The collision between the Indian and Eurasian plates promotes the southeastward extrusion of the Indochina Peninsula while the internal dynamics of its crustal deformation remain enigmatic. Here, we make use of seismic data from 38 stations and employ the ambient noise tomography to construct a 3‐D crustal shear‐wave velocity (Vs) model beneath the Indochina Peninsula. A low‐Vs anomaly is revealed in the mid‐lower crust of the Shan‐Thai Block and probably corresponds to the southern extension of the crustal flow from SE Tibet. Although the Khorat Plateau behaves as a rigid block, the observed low‐Vs anomalies in the lower crust and also below the Moho indicate that the crust may have been partially modified by mantle‐derived melts. The strike‐slip shearing motions of the Red River Fault may have dominantly developed crustal deformation at its western flank where a low‐Vs anomaly is observed at the upper‐middle crust.
    Description: Plain Language Summary: The Indochina Peninsula was believed to behave as a rigid block where significant southeastward extrusion and clockwise rotation have occurred in response to the collision between the Indian and Eurasian plates. Here, we employ ambient noise data to obtain the shear‐wave velocity (Vs) images and find deformations in the interior of the crust beneath the Indochina Peninsula. A low‐Vs anomaly is observed in the mid‐lower crust of the Shan‐Thai Block and represents the crustal flow from SE Tibet. The crust of the Khorat Plateau, the core of the Indochina Block, has been partially modified by mantle‐derived melts. The strike‐slip shearing motions of the Red River Fault have brought crustal deformation at its southwestern flank characterized as a low‐Vs anomaly in the upper‐middle crust.
    Description: Key Points: A 3‐D crustal shear‐wave velocity (Vs) model was constructed for the Indochina Peninsula from ambient noise tomography. Low‐Vs in the middle‐lower crust of the Shan‐Thai Block may represent the southern extension of the crustal flow from SE Tibet. The crust of the rigid Khorat Plateau has been partially modified by intrusion of mantle‐derived melts.
    Description: National Natural Science Foundation of China http://dx.doi.org/10.13039/501100001809
    Description: the State Key Laboratory of Marine Geology, Tongji University
    Description: Shanghai Sheshan National Geophysical Observatory
    Description: https://doi.org/10.5281/zenodo.5235658
    Keywords: ddc:551.1 ; Indochina Peninsula ; crustal structure ; lower‐crustal flow ; ambient noise tomography
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 64
    Publication Date: 2023-01-11
    Description: Diese Bergordnung wurde am 7. Januar 1474 für die Bergwerke in Schwaz von Herzog Siegmund von Österreich erlassen. Mit dem ab 1470 stark ansteigenden Bergbauaktivitäten kam es gleichzeitig zu zahlreichen Missständen bei der Dienstdurchführung der Hutleute sowie zu offensichtlich chaotischen Zuständen bei der Vermessung der Grubenfelder. In 16 Paragrafen wurden deshalb die Rechte der Gruben an ihren Feldern, das ordentliche Vermessen der Grubenfelder und das Verhalten bei Durchschlägen beschrieben sowie die Zuständigkeiten der Hutleute klar benannt. In einem später eingefügten Zusatz wurde das Fällen von Bäumen im gesamten Bergbaubezirk verboten.
    Description: source
    Keywords: Herzog Siegmund von Österreich ; Österreich ; Tirol ; Schwaz ; Freundsberg, Burg ; Schlitters ; Innsbruck ; Silberbergbau ; Bergordnung
    Language: German
    Type: doc-type:book , updatedVersion
    Format: 7
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 65
    Publication Date: 2023-01-14
    Description: Climate model simulations typically exhibit a bias, which can be corrected using statistical approaches. In this study, a geostatistical approach for bias correction of daily precipitation at ungauged locations is presented. The method utilizes a double quantile mapping with dry day correction for future periods. The transfer function of the bias correction for the ungauged locations is established using distribution functions estimated by ordinary kriging with anisotropic variograms. The methodology was applied to the daily precipitation simulations of the entire CORDEX‐Africa ensemble for a study region located in the West African Sudanian Savanna. This ensemble consists of 23 regional climate models (RCM) that were run for three different future scenarios (RCP 2.6, RCP 4.5, and RCP 8.5). The evaluation of the approach for a historical 50‐year period (1950–2005) showed that the method can reduce the inherent strong precipitation bias of RCM simulations, thereby reproducing the main climatological features of the observed data. Moreover, the bias correction technique preserves the climate change signal of the uncorrected RCM simulations. However, the ensemble spread is increased due to an overestimation of the rainfall probability of uncorrected RCM simulations. The application of the bias correction method to the future period (2006–2100) revealed that annual precipitation increases for most models in the near (2020–2049) and far future (2070–2099) with a mean increase of up to 165mm⋅a−1 (18%). An analysis of the monthly and daily time series showed a slightly delayed onset and intensification of the rainy season.
    Description: Adapting water management strategies to future precipitation projected by climate models is associated with high uncertainty in sparsely gauged catchments. Kriging was utilized to estimate distribution parameters for ungauged locations in a West African region to perform a bias correction of the CORDEX‐Africa ensemble. The application of the bias correction method revealed higher annual precipitation amounts and an intensifaction of the rainy season but only little change to the onset of the rainy season.
    Description: German Federal Ministry of Education and Research, Bonn (BMBF), West African Science Service Centre on Climate Change and Adapted Land Use (WASCAL)
    Keywords: ddc:551.6 ; bias correction ; climate change ; CORDEX‐Africa ; geostatistical approaches ; precipitation ; quantile mapping ; West Africa
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 66
    Publication Date: 2023-01-14
    Description: The Paris Agreement marks a significant milestone in international climate politics. With its adoption, Parties call for non‐ and sub‐state actors to contribute to the global climate agenda and close the emissions gap left by states. Such a facilitative setting embraces non‐state climate action through joint efforts, synergies, and different modes of collaboration. At the same time, non‐state actors have always played a critical and confrontational role in international climate governance. Based on a systematic literature review, we identify and critically assess the role of non‐state climate action in a facilitative post‐Paris climate governance regime. We thereby highlight three constitutive themes, namely different state‐non‐state relations, competing level of ambition, and a variety of knowledge foundations. We substantiate these themes, derived from an inductive analysis of existing literature, with illustrative examples and propose three paradigmatic non‐state actor roles in post‐Paris climate governance on a continuum between compliance and critique. We thereby highlight four particular threats of a facilitative setting, namely substitution of state action, co‐optation, tokenism, and depoliticization. Future research should not limit itself to an effective integration of NSSAs into a facilitative climate regime, but also engage with the merits of contestation. This article is categorized under: Policy and Governance 〉 Multilevel and Transnational Climate Change Governance
    Description: Three constitutive themes—different state‐non‐state relations, levels of ambition, and knowledge foundations—define the multiple roles non‐ and sub‐state actors can occupy in the post‐Paris climate governance regime. Yet, calls for voluntary, collaborative, and synergetic non‐state climate action in a facilitative post‐Paris climate governance setting run the risk to overshadow fundamental tensions when governing climate change.
    Description: Svenska Forskningsrådet Formas http://dx.doi.org/10.13039/501100001862
    Description: Deutsche Forschungsgemeinschaft (DFG)
    Keywords: ddc:341.7 ; climate change governance ; contestation ; environmental politics ; non‐state actors ; Paris Agreement ; transformation
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 67
    Publication Date: 2023-01-14
    Description: We theoretically and empirically investigate the investments of water users in a stylized local irrigation system. We model irrigation self‐management as an interdependent interaction of users in an evolutionary game and study the resilience of the irrigation system. The theoretical model implies multiple stable equilibria at different efficiency levels. Users may be trapped in a low level of collective investment or succeed by being locked in a high collective investment level, implying an irrigation system resilient against external shocks. The study seeks to empirically identify such lock‐ins in experimental interactions among Central Asian farmers. Furthermore, we inquire into whether a pre‐play cheap talk opportunity with peer‐monitoring or sanctioning treatments influence the self‐reinforcing dynamic. Our findings revealed several stable states. Among these states, there are both low and high levels of efficiency, which we measure in the size of public good. Communication among users results in higher collective investment levels. However, this does not guarantee the complete elimination of inferior conventions from best‐response play. Penalties crowded out the intrinsic motivation to cooperate as they reduced collective investment in both low‐ and high‐level equilibria. Our findings imply that institutional settings tailored to each community can improve resilience to climate‐driven perturbations in water resources.
    Description: VolkswagenStiftung (Volkswagen Foundation) http://dx.doi.org/10.13039/501100001663
    Description: Federal Ministry for Economic Cooperation (BMZ) http://dx.doi.org/10.13039/501100001663
    Keywords: ddc:333.91 ; Central Asia ; experiment ; multiple equilibria ; resilience ; water management ; Asie centrale ; expérimentation ; équilibres multiples ; résilience ; gestion de l'eau
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 68
    Publication Date: 2023-01-14
    Description: Spaceborne impact ionization mass spectrometers, such as the Cosmic Dust Analyzer on board the past Cassini spacecraft or the SUrface Dust Analyzer being built for NASA's upcoming Europa Clipper mission, are of crucial importance for the exploration of icy moons in the Solar System, such as Saturn's moon Enceladus or Jupiter's moon Europa. For the interpretation of data produced by these instruments, analogue experiments on Earth are essential. To date, thousands of laboratory mass spectra have been recorded with an analogue experiment for impact ionization mass spectrometers. Simulation of mass spectra of ice grains in space is achieved by a Laser Induced Liquid Beam Ion Desorption (LILBID) approach. The desorbed cations or anions are analyzed in a time‐of‐flight mass spectrometer. The amount of unstructured raw data is increasingly challenging to sort, process, interpret and compare with data from space. Thus far this has been achieved manually for individual mass spectra because no database containing the recorded reference spectra was available. Here we describe the development of a comprehensive, extendable database containing cation and anion mass spectra from the laboratory LILBID facility. The database is based on a Relational Database Management System with a web server interface and enables filtering of the laboratory data using a wide range of parameters. The mass spectra can be compared not only with data from past and future space missions but also mass spectral data generated by other, terrestrial, techniques. The validated and approved subset of the database is available for general public (https://lilbid-db.planet.fu-berlin.de).
    Description: Plain Language Summary: Thousands of laboratory mass spectra, each with an individual set of experimental parameters, have been recorded so far using a facility situated at Freie Universität Berlin, Germany. The mass spectra help analyze and interpret data returned from spacecraft in the vicinity of icy moons in the Solar System. The unstructured laboratory data is increasingly challenging to sort and compare to the data from space. We developed an extendable database containing the laboratory data. The database is available for general public and allows filtering the stored data for a wide range of experimental parameters and, in turn, significantly improves analysis of data not only from past space missions but also future missions in particular.
    Description: Key Points: We describe the development of a comprehensive spectral database containing laboratory analogue data for spaceborne mass spectrometers. The database is based on a Relational Database Management System with a web interface and accessible for community use. Filtering the laboratory data using a wide range of experimental parameters allows a straightforward analysis of returned flight data.
    Description: EC, Horizon 2020 Framework Programme (H2020) http://dx.doi.org/10.13039/100010661
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: https://doi.org/10.5281/zenodo.6863855
    Description: https://sbnarchive.psi.edu/pds3/cassini/cda/COCDA_0007.tar.gz
    Keywords: ddc:550 ; mass spectral database ; analogue experiments ; ice grains ; ocean worlds ; SUDA ; ENIA ; LILBID ; TOF‐MS
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 69
    Publication Date: 2023-01-14
    Description: Over the last decades, treatment of domestic wastewater promoted by environmental regulations have reduced human health risks and improved water quality. However, ecological risks caused by effluents of wastewater treatment plants (WWTPs) discharged into rivers still persist. Moreover, the evolution of these ecological risks in the future is intimately related to effects of changing climate, especially regarding streamflow in receiving rivers. Here, we present an analytical and transferable framework for assessing the ecological risks posed by WWTP‐effluents at the catchment scale. The framework combines the size‐class k of WWTPs, which is a load‐proxy, with their outflows' location in river networks, represented by stream‐order ω. We identify ecological risks by using three proxy indicators: the urban discharge fraction and the local‐scale concentrations of each total phosphorous and ammonium‐nitrogen discharged from WWTPs. About 3,200 WWTPs over three large catchments (Rhine, Elbe, and Weser) in Central Europe were analyzed by incorporating simulated streamflow for the most extreme projected climate change scenario. We found that WWTPs causing ecological risks in the future prevail in lower ω, across almost all k. Distinct patterns of ecological risks are identified in the k‐ω framework for different indicators and catchments. We show, as climate changes, intensified risks are especially expected in lower ω receiving effluents of intermediate‐k WWTPs. We discuss the implications of our findings for prioritizing WWTPs upgrading and urging updates on environmental regulations. Further discussions underline the feasibility of applying the framework to any geographical regions and highlight its potentials to help in achieving global long‐term commitments on freshwater security.
    Description: Key Points: An analytical, generic framework was developed to assess wastewater treatment plants causing ecological risks in rivers under climate change. Smaller streams will face higher ecological risks for almost all load classes of wastewater treatment plants in future climate. Of the legally regulated effluent parameters for treated wastewater, ammonium‐nitrogen concentration will pose the greatest ecological risk.
    Description: Helmholtz Association http://dx.doi.org/10.13039/501100009318
    Keywords: ddc:551.48 ; analytical assessment framework ; wastewater treatment plants emissions ; river stream‐order ; dilution ; local‐scale nutrients concentrations
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 70
    Publication Date: 2023-01-14
    Description: Specular meteor radars (SMRs) have significantly contributed to the understanding of wind dynamics in the mesosphere and lower thermosphere (MLT). We present a method to estimate horizontal correlations of vertical vorticity (Qzz) and horizontal divergence (P) in the MLT, using line‐of‐sight multistatic SMRs velocities, that consists of three steps. First, we estimate 2D, zonal, and meridional correlation functions of wind fluctuations (with periods less than 4 hr and vertical wavelengths smaller than 4 km) using the wind field correlation function inversion (WCFI) technique. Then, the WCFI's statistical estimates are converted into longitudinal and transverse components. The conversion relation is obtained by considering the rotation about the vertical direction of two velocity vectors, from an east‐north‐up system to a meteor‐pair‐dependent cylindrical system. Finally, following a procedure previously applied in the upper troposphere and lower stratosphere to airborne wind measurements, the longitudinal and transverse spatial correlations are fitted, from which Qzz, P, and their spectra are directly estimated. The method is applied to a special Spread spectrum Interferometric Multistatic meteor radar Observing Network data set, obtained over northern Germany for seven days in November 2018. The results show that in a quasi‐axisymmetric scenario, P was more than five times larger than Qzz for the horizontal wavelengths range given by ∼50–400 km, indicating a predominance of internal gravity waves over vortical modes of motion as a possible explanation for the MLT mesoscale dynamics during this campaign.
    Description: Key Points: We investigate the horizontal correlation functions of vertical vorticity and horizontal divergence for mesoscale wind fluctuations in the mesosphere and lower thermosphere. 2D zonal and meridional correlation functions and 1D longitudinal and transverse correlation functions as a function of horizontal lags are analyzed. The divergence dominated over the vorticity during November 2018 in northern Germany.
    Description: Leibniz SAW
    Description: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: French Ministry of Foreign and European
    Description: https://doi.org/10.22000/536
    Keywords: ddc:551.5 ; MLT ; vorticity ; correlation function ; meteor radar ; mesoscales ; divergence
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 71
    Publication Date: 2023-01-14
    Description: High‐resolution flight data obtained from in situ measurements in the free atmosphere aboard the High Altitude and Long Range Research Aircraft (HALO) are used to determine eddy dissipation rates along extended flights during the recent Southern Hemisphere Transport, Dynamics, and Chemistry aircraft campaign (SOUTHTRAC) in the 2019 austral winter. These data are analyzed and correlated with quantities characterizing the ambient airflow and the magnitudes of vertical energy propagation through internal gravity waves. The observed turbulence events are strongly correlated with elevated shear values, and overturning gravity waves do not appear to play a role. A highlight of the analysis is the validation of a recently implemented Clear Air Turbulence (CAT) forecast index in the European Centre for Medium‐Range Weather Forecast integrated forecast system. Here we find a slightly better correlation of the CAT prediction with the HALO research aircraft observations compared to those of commercial aircraft. The observed turbulence during SOUTHTRAC was never stronger than moderate, as EDR values remained below 0.3 m2/3 s−1. In general, light and light‐to‐moderate turbulence events were extremely rare, occurring in only about 5% of the flight time, and stronger events in less than 0.2%. These results are also reflected in the local atmospheric conditions, which were dominated by a thermally very stable airflow with low vertical shear and large Richardson numbers.
    Description: Plain Language Summary: This study analyzes high‐resolution data of velocity components in the upper troposphere and lower stratosphere collected with the German research aircraft High Altitude and Long Range Research Aircraft during the Southern Hemisphere Transport, Dynamics, and Chemistry (SOUTHTRAC) campaign in September–November 2019. Flights were conducted predominantly over the southern part of South America, the Drake Passage, and the Antarctic Peninsula. The objective of the analysis was to determine the eddy dissipation rates during the 22 flights. The cubic root of eddy dissipation rates is a common measure used to characterize turbulent regions in the atmosphere. High quality observations with a very accurately calibrated sensor are rare, especially in the remote areas of the SOUTHTRAC campaign. Observed eddy dissipation rates have been correlated with gravity wave activity, but these correlations are very small. A much stronger dependence of the eddy dissipation rates exists on the vertical shear of the horizontal wind. Thus, mechanical generation of turbulence appears to dominate in the observed cases. Overall, the observed turbulence was never stronger than moderate. Turbulence events were extremely rare, occurring in only about 5% of the flight time, and stronger events less than 0.2%. Finally, the observed eddy dissipation rates were compared with weather model forecasts, demonstrating their reliability in predicting turbulent regions.
    Description: Key Points: Small eddy dissipation rates were observed in the free atmosphere along extended research flights during Southern Hemisphere Transport, Dynamics, and Chemistry in austral winter 2019. Stronger turbulence events are rare and are mostly correlated with enhanced vertical shear of the horizontal wind. EDR predictions of a 15‐member ensemble shows higher correlation with research aircraft observations than with those by commercial aircraft.
    Description: Federal Ministry for Education and Research
    Description: German Science Foundation
    Description: https://halo-db.pa.op.dlr.de/mission/116
    Description: https://halo-db.pa.op.dlr.de/dataset/8497
    Description: https://halo-db.pa.op.dlr.de/dataset/8496
    Description: https://apps.ecmwf.int/codes/grib/param-db/?id=260290
    Description: https://doi.org/10.21957/xbar-5611
    Description: https://halo-db.pa.op.dlr.de/dataset/8955
    Description: https://madis.ncep.noaa.gov/acars_variable_list.shtml
    Keywords: ddc:551.5 ; turbulence in the free atmosphere ; eddy dissipation rate ; clear‐air turbulence predictions ; ECMWF integrated forecast system
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 72
    Publication Date: 2023-01-14
    Description: Distributed models have been increasingly applied at finer spatiotemporal resolution. However, most diagnostic analyses aggregate performance measures in space or time, which might bias subsequent inferences. Accordingly, this study explores an approach for quantifying the parameter sensitivity in a spatiotemporally explicit way. We applied the Morris method to screen key parameters within four different sampling spaces in a grid‐based model (mHM‐Nitrate) for NO3‐N simulation in a mixed landuse catchment using a 1‐year moving window for each grid. The results showed that an overly wide range of aquatic denitrification rates could mask the sensitivity of the other parameters, leading to their spatial patterns only related to the proximity to outlet. With adjusted parameter space, spatial sensitivity patterns were determined by NO3‐N inputs and hydrological transport capacity, while temporal dynamics were regulated by annual wetness conditions. The relative proportion of parameter sensitivity further indicated the shifts in dominant hydrological/NO3‐N processes between wet and dry years. By identifying not only which parameter(s) is(are) influential, but where and when such influences occur, spatial sensitivity analysis can help evaluate current model parameterization. Given the marked sensitivity in agricultural areas, we suggest that the current NO3‐N parameterization scheme (land use‐dependent) could be further disentangled in these regions (e.g., into croplands with different rotation strategies) but aggregated in non‐agricultural areas; while hydrological parameterization could be resolved into a finer level (from spatially constant to land use‐dependent especially in nutrient‐rich regions). The spatiotemporal sensitivity pattern also highlights NO3‐N transport within soil layers as a focus for future model development.
    Description: Key Points: A diagnostic analysis was conducted to disentangle the parameter sensitivity for NO3‐N simulations in catchment modeling in space and time. Sensitivity differed within sampling spaces, but was controlled spatially by NO3‐N supply/water fluxes while temporally by wetness condition. Analysis suggests finer‐level parameterization needs in arable land, and prioritizes NO3‐N transport in soils for improved conceptualization.
    Description: Chinese Scholarship Council
    Description: Leverhulme Trust http://dx.doi.org/10.13039/501100000275
    Description: Einstein Stiftung Berlin http://dx.doi.org/10.13039/501100006188
    Description: Berlin University Alliance http://dx.doi.org/10.13039/501100021727
    Description: https://doi.org/10.5281/zenodo.6497225
    Description: https://fred.igb-berlin.de/data/package/629
    Keywords: ddc:551 ; spatial time‐varying sensitivity analysis ; distributed nitrate modeling
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 73
    Publication Date: 2023-01-14
    Description: Invasive alien species continue to spread and proliferate in waterways worldwide, but environmental drivers of invasion dynamics lack assessment. Knowledge gaps are pervasive in the Global South, where the frequent heavy human‐modification of rivers provides high opportunity for invasion. In southern Africa, the spatio‐temporal ecology of a widespread and high‐impact invasive alien snail, Tarebia granifera, and its management status is understudied. Here, an ecological assessment was conducted at seven sites around Nandoni Reservoir on the Luvuvhu River in South Africa. The distribution and densities of T. granifera were mapped and the potential drivers of population structure were explored. T. granifera was widespread at sites impacted to varying extents due to anthropogenic activity, with densities exceeding 500 individuals per square meter at the most impacted areas. T. granifera predominantly preferred shallow and sandy environments, being significantly associated with sediment (i.e., chlorophyll‐a, Mn, SOC, SOM) and water (i.e., pH, conductivity, TDS) variables. T. granifera seemed to exhibit two recruitment peaks in November and March, identified via size‐based stock assessment. Sediment parameters (i.e., sediment organic matter, sediment organic carbon, manganese) and water chemistry (i.e., pH, total dissolved solids, conductivity) were found to be important in structuring T. granifera populations, with overall snail densities highest during the summer season. We provide important autecological information and insights on the distribution and extent of the spread of T. granifera. This may help in the development of invasive alien snail management action plans within the region, as well as modelling efforts to predict invasion patterns elsewhere based on environmental characteristics.
    Description: Alexander von Humboldt‐Stiftung http://dx.doi.org/10.13039/100005156
    Description: National Research Foundation http://dx.doi.org/10.13039/501100001321
    Description: University of Venda http://dx.doi.org/10.13039/501100008976
    Keywords: ddc:577.6 ; aquatic non‐native invasions ; environmental gradients ; Global South ; human‐modified river ; quilted melania ; reservoir
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 74
    Publication Date: 2023-01-14
    Description: The seasonal deposition and sublimation of CO2 constitute a major element in Martian volatile cycles. We reprocess the Mars Orbiter Laser Altimeter (MOLA) data and apply co‐registration procedures to obtain spatio‐temporal variations in levels of the Seasonal North Polar Cap (SNPC). The maximum level over the Residual North Polar Cap (RNPC) is 1.3 m, approximately half of that at the south pole (2.5 m). However, the maximum level in the dune fields at Olympia Undae can be up to 3.8 m. Furthermore, off‐season decreases up to 3 m during the northern winter at Olympia Undae are observed. These are likely due to metamorphism effects accentuated by the reduced snowfall at this period. Meanwhile, off‐season increases of up to 2 m during the northern spring are noted, the cause of which remains to be explored. The volume of the SNPC peaks at the end of northern winter and is estimated to be approximately 9.6 × 1012 m3, which is 2% more than that of the Seasonal South Polar Cap. The bulk density of the SNPC can go through phased decreases in accordance with phased accumulation at northern high‐latitudes. These findings can put important constraints on the Martian volatile cycling models.
    Description: Plain Language Summary: Due to its axial tilt, seasons also exist on Mars. Up to one third of the atmosphere's CO2 is in annual exchange with the polar regions through seasonal deposition/sublimation processes. Here, we make use of previously proposed approaches of analyzing the Mars Orbiter Laser Altimeter profiles and obtain spatio‐temporal level variations of the Seasonal North Polar Cap (SNPC). Particularly, we bring attention to abnormal behavior of the SNPC in the dune fields at Olympia Undae. Maximum level there can be all the way up to 4 m which is much higher than a maximum of 1.5 m over the Residual North Polar Cap. Meanwhile, off‐season decreases during the northern winter with magnitudes up to 3 m and off‐season increases during the northern spring of magnitudes up to 2 m are observed. These could possibly be related to metamorphism of the seasonal deposits and phased snowfall. The maximum volume of the SNPC is constrained to be 9.6 × 1012 m3. The bulk density of the SNPC does not continuously increase as previously assumed but can go through phased decreases in accordance with phased snowfall at the north pole. These findings can put important constraints on the Martian climate models.
    Description: Key Points: Through co‐registration of laser altimetry profiles, spatio‐temporal level variations of the Seasonal North Polar Cap (SNPC) of Mars are obtained. Maximum level of the SNPC can be up to 3.8 m at Olympia Undae and up to 1.3 m over the Residual North Polar Cap. Northern winter decreases of up to 3 m and northern spring increases of up to 2 m are observed at Olympia Undae.
    Description: China Scholarship Council
    Description: Deutsche Forschungsgemeinschaft
    Description: Institut National des Sciences de l’Univers
    Description: Centre National de la Recherche Scientifique
    Description: Centre National d’Etudes Spatiales
    Description: https://doi.org/10.17632/x953mzxxvv.1
    Description: https://doi.org/10.17632/z59b9nd6s9.2
    Description: https://pds-geosciences.wustl.edu/missions/mgs/pedr.html
    Description: https://naif.jpl.nasa.gov/pub/naif/pds/data/mgs-m-spice-6-v1.0/mgsp_1000/data/
    Description: https://www.uahirise.org/hiwish/browse
    Keywords: ddc:523 ; Mars ; seasonal polar cap ; CO2 ice ; MOLA ; level variation ; pseudo cross‐over
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 75
    Publication Date: 2023-01-13
    Description: The thermal conductivities of mantle and core materials have a major impact on planetary evolution, but their experimental determination requires precise knowledge of sample thickness at high pressure. Despite its importance, thickness in most diamond anvil cell (DAC) experiments is not measured but inferred from equations of state, assuming isotropic contraction upon compression or assuming isotropic expansion upon decompression. Here we provide evidence that in DAC experiments both assumptions are invalid for a range of mechanically diverse materials (KCl, NaCl, Ar, MgO, silica glass, Al2O3). Upon compression, these samples are ∼30–50% thinner than expected from isotropic contraction. Most surprisingly, all the studied samples continue to thin upon decompression to 10–20 GPa. Our results partially explain some discrepancies among the highly controversial thermal conductivity values of iron at Earth's core conditions. More generally, we suggest that in situ characterization of sample geometry is essential for conductivity measurements at high pressure.
    Description: Plain Language Summary: The thermal and electrical conductivities of the materials making up Earth's core and lowermost mantle are crucial inputs for modeling Earth's interior and the geodynamo mechanism. Yet, large disagreements between published values of conductivity are common, including a factor‐of‐seven discrepancy in the thermal conductivity of iron at core‐mantle boundary conditions. One possible source of systematic uncertainty is the estimate of sample thickness during high‐pressure experiments. Here we show that common materials in compression experiments tend to thin by much more than previously assumed. Surprisingly, the thinning continues upon decompression. These thinning trends could lead to ∼30–50% systematic error, partially explaining the discrepancy in iron conductivity. In situ thickness measurements are thus crucial for accurate determination of conductivities of Earth's mantle and core.
    Description: Key Points: Samples in diamond anvil cell experiments contract and expand in a strongly non‐isotropic fashion upon compression and decompression. Experimental reports on iron conductivity at high pressure contain errors due to the assumption of isotropic contraction or expansion. Accurate in situ determination of sample geometry is necessary for thermal and electrical conductivity measurements at high pressure.
    Description: Helmholtz Association http://dx.doi.org/10.13039/501100009318
    Description: National Science Foundation http://dx.doi.org/10.13039/100000001
    Description: https://doi.org/10.17632/wnvbty8y83.4
    Keywords: ddc:551.12 ; diamond anvil cell ; thermal conductivity ; high pressure
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 76
    Publication Date: 2023-01-13
    Description: Polarities of seismic reflections at the discontinuity atop the D" region (PdP and SdS) indicate the sign of the velocity contrast across the D" reflector. Recent studies found PdP polarities matching and opposite those of P and PcP. While anisotropy could explain this behavior, we find that the ratio of the change in S wave velocity over change in P wave velocity (R‐value) can influence polarity behavior of D" reflected P waves. For R‐values exceeding 3, the P wave reverses polarity in the absence of anisotropy while S wave polarity is not influenced by the R‐value. Using sets of one million models for normal mantle and MORB with varying minerals and processes across the boundary, we carry out a statistical analysis (Linear Discriminant Analysis) finding that there is a marked difference in mantle mineralogy to explain R‐values larger and smaller than 3, respectively. Based on our results we can attribute different mineralogy to a number of cases. In particular, we find that when velocities increase across D" and polarities of PdP and SdS are opposite the post‐perovskite phase transition is still the best explanation whereas MORB is the best explanation when PdP and SdS are the same. When the velocities are decreasing, the post‐perovskite phase transition within MORB is the best explanation if PdP and SdS polarities are the same but if PdP and SdS are opposite, our results indicate that primordial material or mantle enriched in bridgmanite can explain the polarity behavior, further constraining mineralogy within the large low seismic velocity provinces.
    Description: Plain Language Summary: Polarities of seismic waves reflecting at structures in the Earth's mantle indicate seismic velocity changes there. For the lowermost mantle reflector, a velocity increase generates a polarity that is the same for the main wave and the core‐reflected wave. If, however, the percentage change of the velocity of the S wave increases at least three times as much as that of the P wave velocity (expressed as the R‐value, the ratio dVs/dVp), the polarity of the D"‐reflected PdP wave changes polarity, becoming opposite to both the main P wave and the reflection from the core‐mantle boundary below it. Here, we analyze sets of 1 million models with variable compositions of mantle material and mid‐ocean ridge basalt and use an advanced statistical method to identify those combinations of minerals that produce large positive R‐values. We distinguish four cases and find that previous explanations for three of these cases concur with our analysis. For regions where velocities decrease over the D" reflector, our analysis shows that enrichment with the lower‐mantle mineral bridgmanite is responsible for the observed polarity behavior of P and S waves. This means that for regions such as large low‐velocity anomalies in the lowermost mantle, primitive or bridgmanite‐enriched material is the preferred explanation.
    Description: Key Points: Ratio (R) of S‐ over P wave velocity changes (%) controls the polarity of P wave reflections at D" reflector. Thermochemical modeling and statistical analysis show specific minerals contributing to large R‐values. Polarity observations indicate that part of the Pacific large low seismic velocity province is due to bridgmanite enrichment.
    Description: Deutsche Forschungsgemeinschaft and Agence Nationale de la Recherche http://dx.doi.org/10.13039/501100001659
    Description: Nederlandse Organisatie voor Wetenschappelijk Onderzoek http://dx.doi.org/10.13039/501100003246
    Description: Deutscher Akademischer Austauschdienst http://dx.doi.org/10.13039/501100001655
    Description: https://doi.org/10.7914/SN/XE_2003
    Description: https://doi.org/10.7914/SN/TA
    Keywords: ddc:551.12 ; seismology ; wave polarity ; statistics ; thermochemical modeling ; D
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 77
    Publication Date: 2023-01-13
    Description: Managed aquifer recharge (MAR) refers to a suite of methods that is increasingly being applied worldwide for sustainable groundwater management to tackle drinking or irrigation water shortage or to restore and maintain groundwater ecosystems. The potential for MAR is far from being exhausted, not only due to geological and hydrogeological conditions or technical and economic feasibility but also due to its lack of acceptance by the public and policymakers. One approach to enable the safe and accepted use of MAR could be to provide comprehensive risk management, including the identification, analysis, and evaluation of potential risks related to MAR. This article reviews current MAR risk assessment methodologies and guidelines and summarizes possible hazards and related processes. It may help planners and operators select the appropriate MAR risk assessment approaches and support the risk identification process. In addition to risk assessment (and subsequent risk treatment) related to the MAR implementation phase, this review also addresses risk assessment for MAR operation. We also highlight the limitations and lessons learned from the application and development of risk assessment methodologies. Moreover, developments are recommended in the area of MAR‐related risk assessment methodologies and regulation. Depending on data availability, collected methodologies may be applicable for MAR sites worldwide. Integr Environ Assess Manag 2022;18:1513–1529. © 2022 The Authors. Integrated Environmental Assessment and Management published by Wiley Periodicals LLC on behalf of Society of Environmental Toxicology & Chemistry (SETAC).
    Description: Key Points: The past two decades have seen a marked increase in the literature on MAR‐related risk assessment, and a further increase is expected, since more attractive strategies are being used worldwide for integrated groundwater management. The development of holistic risk management plans can improve social acceptability and contribute to safer implementation and operation of MAR schemes. In connection with holistic risk management, MAR can be seen as a viable option for reaching the United Nations Sustainable Development Goal #6. Widely lacking regulations worldwide for risk assessment of MAR schemes is identified to hinder MAR implementation and safe operation worldwide.
    Description: DEEPWATER‐CE
    Description: ENeRAG
    Keywords: ddc:553.7 ; Groundwater management ; Guidelines ; Managed aquifer recharge ; Methodologies ; Risk assessment
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 78
    Publication Date: 2023-01-13
    Description: A volcanic eruption is usually preceded by seismic precursors, but their interpretation and use for forecasting the eruption onset time remain a challenge. A part of the eruptive processes in open conduits of volcanoes may be similar to those encountered in geysers. Since geysers erupt more often, they are useful sites for testing new forecasting methods. We tested the application of Permutation Entropy (PE) as a robust method to assess the complexity in seismic recordings of the Strokkur geyser, Iceland. Strokkur features several minute‐long eruptive cycles, enabling us to verify in 63 recorded cycles whether PE behaves consistently from one eruption to the next one. We performed synthetic tests to understand the effect of different parameter settings in the PE calculation. Our application to Strokkur shows a distinct, repeating PE pattern consistent with previously identified phases in the eruptive cycle. We find a systematic increase in PE within the last 15 s before the eruption, indicating that an eruption will occur. We quantified the predictive power of PE, showing that PE performs better than seismic signal strength or quiescence when it comes to forecasting eruptions.
    Description: Plain Language Summary: When a volcano shows the first sign of activity, it is challenging to determine whether and when the actual eruption will occur. Usually, researchers create earthquake lists and locate these events to assess this. However, an alternative and simpler method can be directly applied to continuous seismic data. We tested a method that assesses the complexity of signals. We first created synthetic data to find reasonable parameter settings for this method. While volcanoes do not erupt very often, frequent eruptions at geysers allow us to systematically study and compare several eruptions. We analyzed the continuous record of 63 eruptions of the Strokkur geyser, Iceland. Our results show a distinct pattern that repeats from one eruption to the next one. We also find a clear pattern that indicates about 15 s before the next eruption that an eruption will occur. We show that this method performs better in eruption forecasting than assessing the seismic noise or silence caused by the geyser.
    Description: Key Points: Permutation Entropy (PE) is a simple tool to assess the complexity of a time series. We analyzed the PE evolution for 63 eruptive cycles of Strokkur geyser and found characteristic changes in PE during recharge. PE is found to be an useful statistical predictor of the eruption times and highlights the precursor 15 s before eruptions.
    Description: Deutscher Akademischer Austauschdienst http://dx.doi.org/10.13039/501100001655
    Description: https://geofon.gfz-potsdam.de/doi/network/7L/2017
    Description: https://gitup.uni-potsdam.de/pujiastutisudibyo/permutationentropy
    Keywords: ddc:551.21 ; permutation entropy ; forecasting ; geyser ; eruption ; hydrothermal system ; volcano‐seismology
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 79
    Publication Date: 2023-01-13
    Description: Low‐level mixed‐phase clouds (MPCs) occur extensively in the Arctic, and are known to play a key role for the energy budget. While their characteristic structure is nowadays well understood, the significance of different precipitation‐formation processes, such as aggregation and riming, is still unclear. Using a 3‐year data set of vertically pointing W‐band cloud radar and K‐band Micro Rain Radar (MRR) observations from Ny‐Ålesund, Svalbard, we statistically assess the relevance of aggregation in Arctic low‐level MPCs. Combining radar observations with thermodynamic profiling, we find that larger snowflakes (mass median diameter larger than 1 mm) are predominantly produced in low‐level MPCs whose mixed‐phase layer is at temperatures between −15 and −10°C. This coincides with the temperature regime known for favoring aggregation due to growth and subsequent mechanical entanglement of dendritic crystals. Doppler velocity information confirms that these signatures are likely due to enhanced ice particle growth by aggregation. Signatures indicative of enhanced aggregation are however not distributed uniformly across the cloud deck, and only observed in limited regions, suggesting a link with dynamical effects. Low Doppler velocity values further indicate that significant riming of large particles is unlikely at temperatures colder than −5°C. Surprisingly, we find no evidence of enhanced aggregation at temperatures warmer than −5°C, as is typically observed in deeper cloud systems. Possible reasons are discussed, likely connected to the ice habits that form at temperatures warmer than −10°C, increased riming, and lack of particle populations characterized by broader size distributions precipitating from higher altitudes.
    Description: Plain Language Summary: Low‐level mixed‐phase clouds (MPCs), that is, shallow clouds containing both liquid droplets and ice crystals, form frequently in the Arctic region. Their characteristic structure—consisting of one or multiple liquid layers at sub‐zero temperatures, from which ice crystals form and precipitate—is nowadays well understood. However, the processes that lead to the growth of ice crystals into snow have been overlooked. Using a 3‐year data set of radar observations from Ny‐Ålesund, in Svalbard, Norway, we are able to identify situations when the ice particle growth is dominated by aggregation of several individual crystals. Combining radar observations with temperature information, we find that larger snowflakes are only produced in MPCs if their liquid portion is at temperatures between −15 and −10°C. This coincides with the temperature regime known for favoring aggregation due to growth and subsequent entanglement of branched crystals. Surprisingly, we find no evidence of enhanced ice aggregation at temperatures warmer than −5°C, as is typically observed in deeper cloud systems. Possible reasons are discussed, likely connected to the ice crystal shapes that develop at temperatures warmer than −10°C, increased liquid droplet production, and lack of particles precipitating from higher altitudes.
    Description: Key Points: Low‐level mixed‐phase clouds (MPCs) at Ny‐Ålesund produce large aggregates predominantly at dendritic‐growth temperatures. Enhanced aggregation due to dendritic growth occurs intermittently in limited regions of the MPC. The typically observed enhanced aggregation zone close to 0°C is absent in low‐level MPCs at the site.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Keywords: ddc:551.5 ; Arctic mixed‐phase clouds ; aggregation ; riming ; dendritic‐growth zone ; radar
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 80
    Publication Date: 2023-01-13
    Description: Massif‐type anorthosite and comagmatic associations of rutile‐bearing ilmenitite (RBI) and oxide‐apatite‐rich amphibolite (OARA) from the Chiapas Massif Complex (CMC) in southeastern Mexico display a protracted billion‐year accessory mineral record encompassing magmatic crystallization at c. 1.0 Ga to recent ductile shear deformation at c. 3.0 Ma. Multiple discrete zircon populations between these age end‐members resulted from neoformation/recrystallization during local to regional metamorphism that affected the southeastern portion of the CMC. The ubiquitous presence of relict baddeleyite (ZrO2), along with various zircon generations spatially associated with pristine to partly retrogressed Zr‐bearing igneous and metamorphic minerals (e.g., ilmenite, rutile, högbomite and garnet), suggests significant Zr diffusive re‐equilibration (exsolution) during slow cooling and mineral breakdown followed by crystallization of baddeleyite. The subsequent transformation of baddeleyite into zircon was likely driven by reaction with Si‐bearing fluids in several geochronologically identified metamorphic stages. Strikingly contrasting compositional signatures in coeval zircon from anorthosite (silicate‐dominated) and comagmatic RBI (Ti‐Fe‐oxide‐dominated) indicate a major role of fluids locally equilibrating with the rock matrix, as indicated by distinct zircon trace element and oxygen isotopic compositions. A high‐grade metamorphic event at c. 950 Ma is likely responsible for the formation of coarse‐grained rutile (~0.1–10 mm in diameter), srilankite, zircon and garnet with rutile inclusions as well as metamorphic högbomite surrounding Fe‐Mg spinel. Zr‐in‐rutile minimum temperatures suggest 〉730°C for this event, which may correlate to rutile‐forming granulite facies metamorphism in other Grenvillian‐aged basement rocks in Mexico and northern South America. A younger generation of baddeleyite exsolution occurred during post‐peak cooling of coarse‐grained rutile, reflected in rimward Zr depletion and formation of discontinuous baddeleyite coronas. Baddeleyite around rutile was then transformed into zircon possibly during subsequent metamorphism at c. 920 or 620 Ma, resulting from syn‐kinematic and contact metamorphism, respectively. Regional metamorphism at c. 450 and 250 Ma extensively overprinted the existing zircon population, especially during the Triassic event, as suggested by a significant presence of zircon with this age. Nearly pristine baddeleyite occurring interstitial to ilmenite yielded an isochron age of c. 232 Ma according to in situ U–Pb secondary ion mass spectrometry (SIMS), suggesting either formation during metamorphic peak conditions or post‐peak cooling. Zircon with ages of c. 80–100 Ma in anorthosite is identified for the first time within the CMC and coincides with cooling ages of c. 100 Ma for coarse‐grained rutile. This age is similar to those of rocks occurring ~200 km further to the east in Guatemala, which are also bounded to the Polochic fault system but overprinted by eclogite facies metamorphism. A high‐pressure event in the southern CMC after 200 Ma, however, is presently unsupported. Although the abundance of rutile and ilmenite is unusually high in the CMC anorthosite assemblage compared with common igneous rocks, the reactions documented here nonetheless stress the importance of these phases for generating Zr‐bearing accessory minerals over a wide range of metamorphic conditions.
    Description: Consejo Nacional de Ciencia y Tecnología (CONACYT) http://dx.doi.org/10.13039/501100003141
    Description: Deutsche Forschungsgemeinschaft (DFG)
    Keywords: ddc:549 ; Diffusion ; SIMS ; Srilankite ; Ti‐Fe deposits ; Ti‐in‐zircon ; Zr‐in‐rutile
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 81
    Publication Date: 2023-01-13
    Description: Recent observations by the Juno spacecraft have shown that electrons contributing to Jupiter's main auroral emission appear to be frequently characterized by broadband electron distributions, but also less often mono‐energetic electron distributions are observed as well. In this work, we quantitatively derive the occurrence rates of the various electron distributions contributing to Jupiter's aurora. We perform a statistical analysis of electrons measured by the JEDI‐instrument within 30–1,200 keV from Juno's first 20 orbits. We determine the electron distributions, either pancake, field‐aligned, mono‐energetic, or broadband, through energy and pitch angles to associate various acceleration mechanisms. The statistical analysis shows that field‐aligned accelerated electrons at magnetic latitudes greater than 76° are observed in 87.6% ± 7.2% of the intervals time averaged over the dipole L‐shells according the main oval. Pancake distributions, indicating diffuse aurora, are prominent at smaller magnetic latitudes (〈76°) with an occurrence rate of 86.2% ± 9.6%. Within the field‐aligned electron distributions, we see broadband distributions 93.0% ± 3.8% of the time and a small fraction of isolated mono‐energetic distribution structures 7.0% ± 3.8% of the time. Furthermore, these occurrence statistics coincide with the findings from our energy flux statistics regarding the electron distributions. Occurrence rates thus also characterize the overall energetics of the different distribution types. This study indicates that stochastic acceleration is dominating the auroral processes in contrast to Earth where the discrete aurora is dominating.
    Description: Plain Language Summary: With the Juno spacecraft arriving in the magnetosphere of Jupiter, first flyby particle measurements have changed the knowledge about the developing process of Jupiter's intense aurora. The observations of auroral particles show a stochastic behavior rather than a preference for specific energy. Our statistical analysis of the first 20 flybys at Jupiter compares the occurrence of different particle distributions and highlights the importance of different generation theories for Jupiter's aurora. A generation via stochastic rather than mono‐energetic behavior is deduced and supports previous observations.
    Description: Key Points: We present a statistical study of Jupiter's auroral electrons within 30–1,200 keV based on Juno's first 20 perijoves. Broadband electron distributions dominates Jupiter's main auroral zone as they are observed in 93% ± 3% of the intervals studied here. Dominance of broadband distributions underlines the importance of a turbulent or stochastic acceleration process.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: Universität zu Köln http://dx.doi.org/10.13039/501100008001
    Description: https://lasp.colorado.edu/home/mop/files/2015/02/CoOrd_systems7.pdf
    Description: https://pds-ppi.igpp.ucla.edu/mission/JUNO/JNO/JEDI
    Description: https://lasp.colorado.edu/home/mop/files/2020/04/20190412_Imai_MagFootReader_UIowa_rev.pdf
    Keywords: ddc:523 ; auroral precipitation budget ; particle distribution ; Jupiter ; Juno
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 82
    Publication Date: 2023-01-13
    Description: Management of hydropower plants strongly influences streamflow dynamics and hence the interaction between surface water and groundwater. As dam operations cause variations in river stages, these can result in changes in the groundwater level at multiple temporal scales. In this work, we study the case of an Alpine aquifer, where weekly fluctuations are particularly pronounced. We consider an area with four river reaches differently impacted by reservoir operations and investigate the influence of these rivers on the common aquifer. Using continuous wavelet transform and wavelet coherence analysis, we show that weekly fluctuations in the groundwater table are particularly pronounced in dry years, in particular in the winter season, although the area of the aquifer impacted by dam operations remains almost unchanged. We thus observe that in Alpine catchments, surface water‐groundwater interaction is sensitive to the conditions determined by a specific hydrological year. We also investigate the influences of the river‐aquifer water fluxes and show that under dry conditions hydropeaking mainly affects their temporal dynamics. Our observations have significant consequences for predicting nutrient and temperature dynamics/regimes in river‐aquifer systems impacted by hydropower plant management.
    Description: Plain Language Summary: The operation of hydropower plants affects the water level in the downstream part of the river, which in turn can alter the groundwater level. In this work, we study an Alpine aquifer crossed by rivers differently impacted by hydropower production. We use statistical tools to analyze the interaction between the rivers and the groundwater, and observe that this interaction is sensitive to the conditions of the hydrological year, such as dry periods.
    Description: Key Points: Wavelet power spectrum and coherence analysis is used to study river‐aquifer interactions under dam operations in an Alpine catchment. The impact of reservoir operations on the aquifer is strongest under low flow conditions but the area impacted shows little variation. Under low flow conditions, dam operations considerably influence the frequency of the water exchange between rivers and aquifer.
    Description: Consejo Nacional de Ciencia y Tecnología http://dx.doi.org/10.13039/501100003141
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: Consejo Veracruzano de Investigación Científica y Desarrollo Tecnológico
    Description: https://doi.org/10.17632/97jchhz4s8.2
    Keywords: ddc:551 ; surface water‐groundwater interaction ; hydropower ; managed rivers ; groundwater modeling
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 83
    Publication Date: 2023-01-13
    Description: During the last 20 years some very hot and dry summers affected Europe, resulting in regionally record‐breaking high temperature or low precipitation values. Long‐term changes of such extremely hot and dry summers are of great relevance for our society, as they are connected with manifold negative impacts on human society, natural ecosystems, and diverse economic sectors. Long‐term variations in drought and five record drought summer half years are studied based on 63 stations across Europe with high‐quality precipitation and temperature time series spanning the period 1901–2018. Eight drought indices are deployed to analyse drought intensity, frequency, and duration; four of them purely precipitation‐based and four integrating potential evapotranspiration in the computation. Additionally, three heavy precipitation indices and simultaneous increases in drought and heavy precipitation are studied. The five driest summer half years over Europe are identified (1947, 2018, 2003, 1921, and 1911). They are analysed by aggregating eight drought indices into the aggregated drought evaluation index (ADE) for five subregions. The ADE shows increasing summer drought conditions over most of Europe, except for some stations in northern Europe. The increase in drought conditions during the warm part of the year is particularly pronounced for indices integrating evapotranspiration in their definition. At the same time, the intensity of heavy precipitation events shows a positive trend, as well as an increased contribution to total precipitation. Several stations in central Europe show simultaneously increasing drought conditions and increasing heavy precipitation events. This increases the risks connected with precipitation extremes.
    Description: Drought and heavy precipitation trends are studied for selected stations with long time series. Both extreme events are related to specific impacts on different economic sectors and thus society. Stations that simultaneously show increasing trends in drought and heavy precipitation mainly occur in central Europe. This indicates a probably higher exposure to these risks in central Europe as well as a demand for broader adaptation options in this region.
    Keywords: ddc:551.6 ; climate indices ; climate variability and change ; dry periods ; mRAI ; WBAI
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 84
    Publication Date: 2023-01-19
    Description: Detailed imaging of accretionary wedges reveals splay fault networks that could pose a significant tsunami hazard. However, the dynamics of multiple splay fault activation during megathrust earthquakes and the consequent effects on tsunami generation are not well understood. We use a 2‐D dynamic rupture model with complex topo‐bathymetry and six curved splay fault geometries constrained from realistic tectonic loading modeled by a geodynamic seismic cycle model with consistent initial stress and strength conditions. We find that all splay faults rupture coseismically. While the largest splay fault slips due to a complex rupture branching process from the megathrust, all other splay faults are activated either top down or bottom up by dynamic stress transfer induced by trapped seismic waves. We ascribe these differences to local non‐optimal fault orientations and variable along‐dip strength excess. Generally, rupture on splay faults is facilitated by their favorable stress orientations and low strength excess as a result of high pore‐fluid pressures. The ensuing tsunami modeled with non‐linear 1‐D shallow water equations consists of one high‐amplitude crest related to rupture on the longest splay fault and a second broader wave packet resulting from slip on the other faults. This results in two episodes of flooding and a larger run‐up distance than the single long‐wavelength (300 km) tsunami sourced by the megathrust‐only rupture. Since splay fault activation is determined by both variable stress and strength conditions and dynamic activation, considering both tectonic and earthquake processes is relevant for understanding tsunamigenesis.
    Description: Plain Language Summary: In subduction zones, where one tectonic plate moves beneath another, earthquakes can occur on many different faults. Splay faults are relatively steep faults that branch off the largest fault (the megathrust) in a subduction zone. As they are steeper than the megathrust, the same amount of movement on them could result in more vertical displacement of the seafloor. Therefore, splay faults are thought to play an important role in the generation of tsunamis. Here, we use computer simulations to study if an earthquake can break multiple splay faults at once and how this affects the resulting tsunami. We find that multiple splay faults can indeed fail during a single earthquake due to the stress changes from trapped seismic waves, which promote rupture on splay faults. Rupture on splay faults results in larger seafloor displacements with smaller wavelengths, so the ensuing tsunami is bigger and results in two main flooding episodes at the coast. Our results show that it is important to consider rupture on splay faults when assessing tsunami hazard.
    Description: Key Points: Multiple splay faults can be activated during a single earthquake by megathrust slip and dynamic stress transfer due to trapped waves. Splay fault activation is facilitated by their favorable orientation with respect to the local stress field and their closeness to failure. Long‐term geodynamic stresses and fault geometries affect dynamic splay fault rupture and the subsequent tsunami.
    Description: Volkswagen Foundation (VolkswagenStiftung) http://dx.doi.org/10.13039/501100001663
    Description: Royal Society (The Royal Society) http://dx.doi.org/10.13039/501100000288
    Description: EC | H2020 | H2020 Priority Excellent Science | H2020 European Research Council (ERC) http://dx.doi.org/10.13039/100010663
    Description: Deutsche Forschungsgemeinschaft (DFG) http://dx.doi.org/10.13039/501100001659
    Description: National Science Foundation (NSF) http://dx.doi.org/10.13039/100000001
    Description: https://github.com/TUM-I5/SWE
    Description: https://doi.org/10.5281/zenodo.6969455
    Keywords: ddc:551 ; earthquake ; tsunami ; subduction zone ; dynamic rupture ; splay fault ; numerical modeling
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 85
    Publication Date: 2023-01-19
    Description: Realistic prediction of the near‐future response of Arctic Ocean primary productivity to ongoing warming and sea ice loss requires a mechanistic understanding of the processes controlling nutrient bioavailability. To evaluate continental nutrient inputs, biological utilization, and the influence of mixing and winter processes in the Laptev Sea, the major source region of the Transpolar Drift (TPD), we compare observed with preformed concentrations of dissolved inorganic nitrogen (DIN) and phosphorus (DIP), silicic acid (DSi), and silicon isotope compositions of DSi (δ30SiDSi) obtained for two summers (2013 and 2014) and one winter (2012). In summer, preformed nutrient concentrations persisted in the surface layer of the southeastern Laptev Sea, while diatom‐dominated utilization caused intense northward drawdown and a pronounced shift in δ30SiDSi from +0.91 to +3.82‰. The modeled Si isotope fractionation suggests that DSi in the northern Laptev Sea originated from the Lena River and was supplied during the spring freshet, while riverine DSi in the southeastern Laptev Sea was continuously supplied during the summer. Primary productivity fueled by river‐borne nutrients was enhanced by admixture of DIN‐ and DIP‐rich Atlantic‐sourced waters to the surface, either by convective mixing during the previous winter or by occasional storm‐induced stratification breakdowns in late summer. Substantial enrichments of DSi (+240%) and DIP (+90%) beneath the Lena River plume were caused by sea ice‐driven redistribution and remineralization. Predicted weaker stratification on the outer Laptev Shelf will enhance DSi utilization and removal through greater vertical DIN supply, which will limit DSi export and reduce diatom‐dominated primary productivity in the TPD.
    Description: Plain Language Summary: Ongoing warming and sea ice loss in the Arctic Ocean may significantly impact biological productivity, which is mainly controlled by light and nutrient availability. To investigate nutrient inputs from land, biological utilization, and the influence of water mass mixing and winter processes on the nutrient distributions, we measured nutrient concentrations and silicon isotopes in the Laptev Sea. We found high concentrations in the southeastern Laptev Sea in agreement with nutrient inputs from the Lena River. Toward the northern Laptev Sea, nutrient concentrations decreased in the surface layer and the silicon isotope signatures shifted to heavier values, consistent with nutrient utilization by phytoplankton. In contrast to the depleted surface layer, the bottom layer beneath the Lena River plume was strongly enriched in some nutrients, which we attribute to different physical and biogeochemical processes. These observations are important for our understanding of nutrient bioavailability in the Laptev Sea and the Transpolar Drift (TPD), which is a surface current that connects the Laptev Sea with the central Arctic Ocean and the Fram Strait. The changing hydrography of the Laptev Sea will likely cause a decrease in silicic acid concentrations and thus a reduction in nutrient export and diatom‐dominated primary productivity in the TPD.
    Description: Key Points: Surface dissolved inorganic nitrogen (DIN), dissolved inorganic phosphorus (DIP), silicic acid (DSi), and Si isotope dynamics are controlled by marine and riverine inputs and uptake by phytoplankton. Strong DIP and DSi enrichments beneath the Lena River plume are due to sea ice‐driven nutrient redistribution and remineralization. Enhanced DSi utilization in the Laptev Sea will lead to a reduced diatom‐dominated primary productivity in the Transpolar Drift.
    Description: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Description: Ocean Frontier Institute http://dx.doi.org/10.13039/501100010784
    Description: Canada First Research Excellence Fund http://dx.doi.org/10.13039/501100010785
    Description: https://doi.pangaea.de/10.1594/PANGAEA.931257
    Description: https://doi.pangaea.de/10.1594/PANGAEA.931240
    Description: https://doi.pangaea.de/10.1594/PANGAEA.931209
    Description: https://doi.pangaea.de/10.1594/PANGAEA.938259
    Keywords: ddc:577.7 ; Arctic Ocean ; Laptev Sea ; transpolar drift ; nutrients ; silicon isotopes ; diatoms
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 86
    Publication Date: 2023-01-19
    Description: Climate change, pollution, and deforestation have a negative impact on global mental health. There is an environmental justice dimension to this challenge as wealthy people and high‐income countries are major contributors to climate change and pollution, while poor people and low‐income countries are heavily affected by the consequences. Using state‐of‐the art data mining, we analyzed and visualized the global research landscape on mental health, climate change, pollution and deforestation over a 15‐year period. Metadata of papers were exported from PubMed®, and both relevance and relatedness of terms in different time frames were computed using VOSviewer. Co‐occurrence graphs were used to visualize results. The development of exemplary terms over time was plotted separately. The number of research papers on mental health and environmental challenges is growing in a linear fashion. Major topics are climate change, chemical pollution, including psychiatric medication in wastewater, and neurobiological effects. Research on specific psychiatric syndromes and diseases, particularly on their ethical and social aspects is less prominent. There is a growing body of research literature on links between mental health, climate change, pollution, and deforestation. This research provides a graphic overview to mental healthcare professionals and political stakeholders. Social and ethical aspects of the climate change‐mental health link have been neglected, and more research is needed.
    Description: Plain Language Summary: Climate change, deforestation, and pollution are having a major effect on mental health all around the world. Yet there are huge disparities on how these negative consequences affect people within and between countries. We analyzed large databases of research articles using digital tools (data mining) to uncover the direction of scientific research and areas that have received less scholarly attention. While research linking climate change to mental health issues is expanding, a detailed examination of the social justice dimension of how climate change and pollution are affecting the different groups of people is still relatively scarce. We provide a graphical overview of the most important research keywords of the last 15 years.
    Description: Key Points: Climate change, pollution, and deforestation threaten global mental health and need to be addressed as a mental health issue. Data mining can help to uncover trends and gaps in research. Mental health research on climate change and pollution is growing, while research linking these to environmental injustice is less prominent.
    Description: Clinician Scientist Programme of the Medical Faculty of Ulm University
    Keywords: ddc:363.7 ; climate change ; mental health ; data mining ; medical ethics ; contamination ; environmental justice
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 87
    Publication Date: 2023-01-19
    Description: The Atmosphere and Ocean De‐Aliasing Level‐1B (AOD1B) product provides a priori information about temporal variations in the Earth's gravity field induced by non‐tidal circulation processes in atmosphere and ocean. It is routinely applied as a background model in the Gravity Recovery and Climate Experiment (GRACE)/GRACE Follow‐On (GRACE‐FO) satellite gravimetry data processing. We here present three new datasets in preparation for the upcoming release RL07 of AOD1B, that are based on either the global ERA5 reanalysis or the ECMWF operational data together with simulations from the Max‐Planck‐Institute for Meteorology general circulation model forced consistently with the fields of the same atmospheric data set. The oceanic simulations newly include an updated bathymetry around Antarctica including cavities under the ice shelves, the explicit implementation of the feedback effects of self‐attraction and loading to ocean dynamics as well as a refined harmonic tidal analysis. Comparison to the current release of AOD1B in terms of GRACE‐FO K‐band range‐acceleration pre‐fit residuals, LRI line‐of‐sight gravity differences and band‐pass filtered altimetry data reveals an overall improvement in the representation of the high‐frequency mass variability. Potential benefits of enhancing the temporal resolution remain inconclusive so that the upcoming release 07 will be sampled again every 3 hr.
    Description: Plain Language Summary: Satellite gravimetry missions such as the Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow‐On (GRACE‐FO), which play a vital role in the monitoring of the Earth's mass transports, require a priori background information on the high‐frequency mass variations which can not be resolved by the monthly gravity solutions. The Atmosphere and Ocean De‐Aliasing Level‐1B (AOD1B) data product provides the required background information for non‐tidal high‐frequency mass changes in the atmosphere and oceans. However, the accurate representation of these mass variations remains challenging and deficiencies in the background models have a significant impact on the overall gravity field errors. Thus, we here present three new datasets in preparation for an upcoming release of AOD1B (RL07). The datasets improve over previous releases by incorporating the effects of the self attraction and solid earth deformation caused by anomalous water masses (SAL), an improved representation of the bathymetry and atmospheric forcing around Antarctica, making use of the new ERA5 atmospheric reanalysis as well as an updated estimation and subtraction of atmospherically induced tidal signals. We compare the new data to the previous release of AOD1B using microwave‐ and laser‐ranging data from GRACE‐FO as well as Jason‐3 altimetry data and show a global improvement in the representation of high‐frequency mass changes.
    Description: Key Points: Atmospheric mass variability from ECMWF’s latest global reanalysis ERA5 is discussed. Ocean response from Max‐Planck‐Institute for Meteorology Ocean Model includes feedback of self‐attraction and loading. Applicable for Gravity Recovery and Climate Experiment (GRACE), GRACE Follow‐On, and legacy data from SLR satellites.
    Description: Deutsche Forschungsgemeinschaft, DFG http://dx.doi.org/10.13039/501100001659
    Description: https://doi.org/10.5880/GFZ.1.3.2022.003
    Keywords: ddc:526.7 ; AOD1B RL07 ; GRACE ; ERA5 ; self‐attraction and loading ; satellite gravimetry
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 88
    Publication Date: 2023-01-19
    Description: About 10% of Europe's surface area is prone to rapid flooding of rivers confined in valleys. The devastating potential of such floods is exacerbated by the deficits of existing gauging networks, including low station densities and recording frequencies, and lack of information beyond stage height. Here, we use seismic data of the July 2021 Ahrtal flood, Germany, to extract information to complement sparse hydrometric data, and to reconstruct the rapid evolution of this fatal event. We show that a seismic station can deliver essential flood metrics such as magnitude, propagation velocity and debris transport rate. These seismic products provide high resolution insight to the non‐linear flood behavior. We argue that an approach combining distributed low‐cost seismometers with existing seismic stations, can provide important real time data on future catastrophic floods and associated hazards in upland catchments, offering precious response time also in currently ungauged landscapes.
    Description: Plain Language Summary: Rapidly evolving floods are a major hazard for 10% of European landscapes. They are hard to adequately detect and describe by the classic gauge station scheme, but seismic sensors provide a valuable alternative to this difficulty. A seismometer can sense a flood like the devastating one that hit the Ahr valley, Germany, in July 2021 up to 1.5 km away. The seismic footprint of the flood allows to provide information on flood magnitude, velocity and trajectory at sub‐minute resolution and at near real time. We show how this new approach can be utilized for future flood protection.
    Description: Key Points: Seismic sensing of valley confined floods improves classic detection approaches. Near‐real time information on flood magnitude, trajectory, and velocity. Gate keeper seismometer networks can improve flood risk management in Europe.
    Description: GFZ German Research Centre for Geosciences
    Description: Helmholtz Centre Potsdam—GFZ German Research Centre for Geosciences http://dx.doi.org/10.13039/501100010956
    Description: German Research Foundation
    Keywords: ddc:622.1592 ; hazard ; realtime warning ; flash flood ; seismic
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 89
    Publication Date: 2023-01-19
    Description: Along ultraslow spreading ridges melt is distributed unequally, but melt focusing guides melt away from amagmatic segments toward volcanic centers. An interplay of tectonism and magmatism is thought to control melt ascent, but the detailed process of melt extraction is not yet understood. We present a detailed image of the seismic velocity structure of the Logachev volcanic center and adjacent region along the Knipovich Ridge. With travel times of P‐ and S‐waves of 3,959 earthquakes we performed a local earthquake tomography. We simultaneously inverted for source locations, velocity structure and the Vp/Vs‐ratio. An extensive low velocity anomaly coincident with high Vp/Vs‐ratios 〉1.9 lies underneath the volcanic center at depths of 10 km below sea level in an aseismic area. More shallow, tightly clustered earthquake swarms connect the anomaly to a shallow anomaly with high Vp/Vs‐ratio beneath the basaltic seafloor. We consider the deep low‐velocity anomaly to represent an area of partial melt from which melts ascent vertically to the surface and northwards into the adjacent segment. By comparing tomographic studies of the Logachev and Southwest Indian Ridge Segment‐8 volcano we conclude that volcanic centers of ultraslow spreading ridges host spatially confined, circular partial melt areas below 10 km depth, in contrast to the shallow extended melt lenses along fast spreading ridges. Lateral feeding over distances of 35 km is possible at orthogonal spreading segments, but limited at the obliquely spreading Knipovich Ridge.
    Description: Plain Language Summary: Mid‐ocean ridges mark the tectonic plate boundaries, where the plates drift apart. Fresh magma rises into the gap and builds new seafloor. The slower the plates drift apart, the less magma is present underneath the ridge. At very slow spreading ridges there is not enough magma to build new seafloor along the entire length of the ridge. Rather, melt is guided toward individual volcanic centers spaced at about 100 km, where melt accumulates and ascents. In our study we try to find melt storage areas and ascent paths of such a volcanic center. With velocities of different seismic wave types from earthquakes we map the velocity structure of the area underneath the major Logachev volcanic center. Lower velocities indicate an area partly including melt at depths of more than 10 km, far deeper than at mid‐ocean ridges with sufficient melt supply. From the deep magma reservoir, many earthquake swarms map the long ascent path of melt to the surface. The interplay of magmatic and tectonic activity is important here. In a comparison with results from another volcanic center, we find that lateral magma feeding is possible in orthogonal spreading, but limited in oblique spreading, as at the Knipovich Ridge.
    Description: Key Points: Active volcanic centers at ultraslow spreading ridges host deeper and more confined partial melt areas than faster spreading ridges. Earthquake swarms delineate melt ascent paths from the partial melt area to the surface. Lateral feeding at shallow depths into subordinate segments is prevented by ridge obliquity.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Keywords: ddc:551.22 ; ultraslow spreading ; Knipovich Ridge ; local earthquake tomography ; seismicity ; mid‐ocean ridge ; partial melt area
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 90
    Publication Date: 2023-01-19
    Description: The lithospheric architecture of passive margins is crucial for understanding the tectonic processes that caused the breakup of Gondwana. We highlight the evolution of the South Atlantic passive margins by a simple thermal lithosphere‐asthenosphere boundary (LAB) model based on onset and cessation of rifting, crustal thickness, and stretching factors. We simulate lithospheric thinning and select the LAB as the T = 1,330°C isotherm, which is calculated by 1D advection and diffusion. Stretching factors and margin geometry are adjusted to state‐of‐the‐art data sets, giving a thermal LAB model that is especially designed for the continental margins of the South Atlantic. Our LAB model shows distinct variations along the passive margins that are not imaged by global LAB models, indicating different rifting mechanisms. For example, we model up to 200 km deep lithosphere in the South American Santos Basin and shallow lithosphere less than 60 km in the Namibe Basin offshore Africa. These two conjugate basins reflect a strong asymmetry in LAB depth that resembles variations in margin width. In a Gondwana reconstruction, we discuss these patterns together with seismic velocity perturbations for the Central and Austral Segments of the margins. The shallow lithosphere in the Namibe Basin correlates with signatures of the Angola Dome, attributed to epeirogenic uplift in the Neogene, suggesting an additional component of post‐breakup lithospheric thinning.
    Description: Plain Language Summary: Passive margins mark the transition zone from a continent to the ocean without being an active boundary of tectonic plates. They are typical for all continents on the globe. In the South Atlantic, the passive margins are located adjacent to the eastern coastline of South America and the western coastline of Africa. Studying the architecture of passive margins is essential for understanding plate tectonic history of the earth because they define how the continents once fitted together and how they broke apart. Passive margin segments on opposite sides of an ocean form so called conjugate margin pairs. Most geophysical studies of passive margins focus on the first few kilometers under the surface. However, their deeper extension to the base of the rigid shell of the earth, known as lithospheric thickness, is to a large extent unknown. Based on a simple temperature model, we find that the lithospheric thickness is highly variable and shows large variations along the South Atlantic passive margins. These differences are associated with the extension of conjugate margin pairs: where one margin is narrower than the conjugate, its lithospheric thickness is greater. This asymmetry indicates that the geodynamic processes, causing the breakup of the two continents, must have been asymmetric as well. Offshore Angola, the lithosphere is modeled shallow and matches with relatively young rock signatures. This suggests additional tectonic activity on the African side after the breakup between the two continents occurred.
    Description: Key Points: A simple thermal lithosphere‐asthenosphere boundary (LAB) model for the South Atlantic passive margins has been developed. The LAB model shows distinct variations along the margins that correlate with margin widths. Conjugate margin pairs reflect an asymmetry in LAB depth patterns that are locally related to post‐breakup lithospheric thinning.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: https://doi.org/10.5880/GFZ.1.3.2020.006
    Description: https://www.earthbyte.org/webdav/ftp/Data_Collections/Muller_etal_2019_Tectonics/
    Description: https://doi.org/10.5281/zenodo.7074000
    Description: https://earthbyte.org/webdav/ftp/Data_Collections/Haas_etal_2022_Tectonics/
    Keywords: ddc:551.13 ; passive margins ; South Atlantic ; thermal LAB ; rift asymmetry ; Gondwana
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 91
    Publication Date: 2023-01-19
    Description: Surface wave energy and dissipation are observed across the surf zone. Utilizing the concept of surface rollers, a new scaling is introduced to obtain the energy flux and dissipation related to rollers from Doppler velocities measured by a shore‐based X‐band marine radar. The dissipation of wave energy and hence the transformation of the incoming wave height (or energy) is derived using the coupled wave and roller energy balance equations. Results are compared to in‐situ wave measurements obtained from a wave rider buoy and two bottom mounted pressure wave gauges. A good performance in reproducing the significant wave height is found yielding an overall root‐mean‐square error of 0.22 m and a bias of −0.12 m. This is comparable to the skill of numerical wave models. In contrast to wave models, however, the radar observations of the wave and roller energy flux and dissipation neither require knowledge of the bathymetry nor the incident wave height. Along a 1.5 km long cross‐shore transect on a double‐barred, sandy beach in the southern North Sea, the highest dissipation rates are observed at the inner bar over a relatively short distance of less than 100 m. During the peak of a medium‐severe storm event with significant wave heights over 3 m, about 50% of the incident wave energy flux is dissipated at the outer bar.
    Description: Plain Language Summary: Ocean waves are carrying a large amount of mechanical energy which they have gained from the wind blowing over the ocean surface. At the coast this energy supply generates strong water motions, creates forces on coastal structures, moves sand, and can cause coastal erosion. It is therefore important to know when, where, and to what extent wave energy is reduced under different environmental conditions. The majority of the energy is removed by wave breaking. However, this process is still not completely understood which is partly due to fact that it is difficult to observe. This is particularly the case during storm conditions when it is very complicated to install and recover measurement equipment in the ocean. The present work describes a methodology to obtain such measurements using a special radar device which is installed at the beach; hence, it is not being impacted by harsh wave conditions. This approach will enable scientists to perform long‐term monitoring of wave breaking thus opening new opportunities to study beach processes and coastal changes.
    Description: Key Points: high‐resolution observations of surface wave and roller dissipation as well as the transformation of wave height across the surf zone. the concept of surface rollers is applied to shore‐based X‐band Doppler radar data. in storm conditions, 50% of the wave energy is dissipated at a submerged outer sandbar, but strongest dissipation occurs further inshore.
    Description: Helmholtz Association http://dx.doi.org/10.13039/501100009318
    Description: http://codm.hzg.de/codm
    Description: https://doi.org/10.1594/683PANGAEA.898407
    Description: https://doi.org/10.1594/PANGAEA.942014
    Description: https://doi.org/10.5281/zenodo.5787131
    Keywords: ddc:551.46 ; wave breaking ; X‐band radar ; roller concept ; close‐range remote sensing ; energy dissipation ; wave transformation
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 92
    Publication Date: 2023-01-19
    Description: Enhancing the resilience of complex social‐ecological systems (SES) to climate change requires transformative changes. Yet, there are knowledge gaps on how best to achieve transformation. In this study, we present an approach for assessing governance performance in SES and identifying leverage points to ultimately enhance climate resilience. The approach combines three different methods including a capital approach framework, fuzzy cognitive mapping, and a leverage points analysis. Using a coastal case‐study in Algoa Bay, South Africa, the performance of governance processes contributing to different forms of capital is assessed. Subsequently, leverage points ‐ where a small shift may lead to transformative changes in the system as a whole ‐ are identified based on measures of centrality and performance. Results suggest that a range of leverage points can improve governance performance and therefore climate resilience in the case‐study. Leverage points include improving (a) support from the provincial government; (b) priority given to climate change in the integrated development plan; (c) frequency of collaborations; (d) participation in the implementation of climate action plans; (e) allocation of funding to climate change actions; (f) the overall level of preparedness in terms of staff with relevant expertise; (g) public awareness and understanding of climate change. The approach can also be used to analyze and model the relations and interactions between capitals. The study advances methodological and theoretical knowledge on the identification of leverage points for enabling transformations toward climate resilience and broader sustainability goals in SES.
    Description: Plain Language Summary: Climate change has severe impacts on both people and nature. Enhancing the ability to persist and adapt to climate change requires transformative governance of social‐ecological systems. However, more knowledge is required on how to enable such transformations. In this paper, we present an approach to measure the performance of different governance processes, such as decisions and actions for climate change adaptation made by public and governmental organizations. The approach aims to identify key processes, where a small intervention may improve overall performance for climate change adaptation, and therefore transformation. We apply the approach in a real‐world example in Algoa Bay, South Africa. Results suggest that different processes in the case‐study can be changed in order to enhance the ability to persist and adapt to climate change. This includes seven actions: (a) more support from governmental organizations; (b) greater priority given to climate change in relevant policies; (c) increasing the frequency of interactions between organizations; (d) enhancing the participation in the implementation of climate action plans; (e) better allocation of funding to climate change actions; (f) training staff within organizations to enhance their climate expertise; (g) improving public awareness and understanding of climate change.
    Description: Key Points: The study presents an approach for assessing governance performance and identifying leverage points in social‐ecological systems. The approach combines three different methods: a capital approach framework, fuzzy cognitive mapping, and a leverage points analysis. The study advances methodological and theoretical knowledge on how to operationalize transformation toward climate resilience.
    Description: Helmholtz‐Zentrum Hereon
    Description: Western Indian Ocean Marine Science Association http://dx.doi.org/10.13039/501100009106
    Description: https://doi.org/10.6084/m9.figshare.20732788
    Keywords: ddc:551.6 ; social‐ecological systems ; climate change adaptation ; transformation ; leverage points ; coastal governance ; adaptive capacity
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 93
    Publication Date: 2023-01-19
    Description: Europe has been affected by record‐breaking heat waves in recent decades. Using station data and a gridded reanalysis as input, four commonly used heat wave indices, the heat wave magnitude index daily (HWMId), excess heat factor (EHF), wet‐bulb globe temperature (WBGT) and universal thermal climate index (UTCI), are computed. The extremeness of historical European heat waves between 1979 and 2019 using the four indices and different metrics is ranked. A normalisation to enable the comparison between the four indices is introduced. Additionally, a method to quantify the influence of the input parameters on heat wave magnitude is introduced. The spatio‐temporal behaviour of heat waves is assessed by spatial–temporal tracking. The areal extent, large‐scale intensity and duration are visualized using bubble plots. As expected, temperature explains the largest variance in all indices, but humidity is nearly as important in WBGT and wind speed plays a substantial role in UTCI. While the 2010 Russian heat wave is by far the most extreme event in duration and intensity in all normalized indices, the 2018 heat wave was comparable in size for EHF, WBGT and UTCI. Interestingly, the well‐known 2003 central European heat wave was only the fifth and tenth strongest in cumulative intensity in WBGT and UTCI, respectively. The June and July 2019 heat waves were very intense, but short‐lived, thus not belonging to the top heat waves in Europe when duration and areal extent are taken into account. Overall, the proposed normalized indices and the multi‐metric assessment of large‐scale heat waves allow for a more robust description of their extremeness and will be helpful to assess heat waves worldwide and in climate projections.
    Description: Europe has been affected by record‐breaking heat waves in recent decades. Using station data and a gridded reanalysis, the extremeness of European heat waves between 1979 and 2019 is ranked using four indices: heat wave magnitude index daily (HWMId), excess heat factor (EHF), wet‐bulb globe temperature (WBGT) and universal thermal climate index (UTCI). In order to assess heatwaves worldwide and in climate projections, the spatial extent, large‐scale intensity and duration of heatwaves are visualized using bubble plots.
    Description: AXA Research Fund http://dx.doi.org/10.13039/501100001961
    Description: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: Karlsruher Institut für Technologie http://dx.doi.org/10.13039/100009133
    Keywords: ddc:551.5 ; duration ; heat wave ; indices ; intensity ; large‐scale ; spatial extent
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 94
    Publication Date: 2023-01-20
    Description: Over the last decades, remote observation tools and models have been developed to improve the forecasting of ash‐rich volcanic plumes. One challenge in these forecasts is knowing the properties at the vent, including the mass eruption rate and grain size distribution (GSD). Volcanic lightning is a common feature of explosive eruptions with high mass eruption rates of fine particles. The GSD is expected to play a major role in generating lightning in the gas thrust region via triboelectrification. Here, we experimentally investigate the electrical discharges of volcanic ash as a function of varying GSD. We employ two natural materials, a phonolitic pumice and a tholeiitic basalt (TB), and one synthetic material (soda‐lime glass beads [GB]). For each of the three materials, coarse and fine grain size fractions with known GSDs are mixed, and the particle mixture is subjected to rapid decompression. The experiments are observed using a high‐speed camera to track particle‐gas dispersion dynamics during the experiments. A Faraday cage is used to count the number and measure the magnitude of electrical discharge events. Although quite different in chemical composition, TB and GB show similar vent dynamics and lightning properties. The phonolitic pumice displays significantly different ejection dynamics and a significant reduction in lightning generation. We conclude that particle‐gas coupling during an eruption, which in turn depends on the GSD and bulk density, plays a major role in defining the generation of lightning. The presence of fines, a broad GSD, and dense particles all promote lightning.
    Description: Plain Language Summary: Explosive volcanic eruptions are accompanied by volcanic lightning (VL), which are electrical discharges resulting from particles that become electrically charged during eruption. We investigated experimentally the discharge behavior of three different materials by performing shock‐tube experiments. We used different rocks and analog material. We focused on the abundance of particle sizes smaller 〈10 μm (very fine ash) by testing individual grain size fractions mixed with coarser grains. The jet behavior was recorded by a high‐speed camera. We find that the presence of very fine particles has a major influence on the probability to produce electrical discharges within the particle‐laden jet. Based on our experiments, more VL is expected when (a) fine ash is abundant, (b) there is a wide grain size distribution, and (c) the particles are dense.
    Description: Key Points: Electrical discharges are generated in experimentally decompressed volcanic ash. The presence of fines (〈10 μm), a broad grain size distribution, and dense particles promote laboratory‐generated volcanic lightning. The coupling of the particles to the jet determines whether an electrical discharge occurs within the jet.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: European Research Council
    Description: Alexander von Humboldt‐Stiftung http://dx.doi.org/10.13039/100005156
    Description: National Science Foundation http://dx.doi.org/10.13039/100000001
    Description: CIFAR Earth 4D
    Keywords: ash ; electric charge ; rapid decompression ; volcanic lightning
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 95
    Publication Date: 2023-01-20
    Description: Seasonal variations in landslide activity remain understudied compared to recent advances in landslide early warning at hourly to daily timescales. Here, we learn the seasonal pattern of monthly landslide activity in the Pacific Northwest from five heterogeneous landslide inventories with differing spatial and temporal coverage and reporting protocols combined in a Bayesian multi‐level model. We find that landslide activity is distinctly seasonal, with credible increases in landslide intensity, inter‐annual variability, and probability marking the onset of the landslide season in November. Peaks in landslide probability in January and intensity in February lag the annual peak in mean monthly precipitation and landslide activity is more variable in winter than in summer, when landslides are rare. For a given monthly rainfall, landslide intensity at the season peak in February is up to 10 times higher than at the onset in November, underlining the importance of antecedent seasonal hillslope conditions.
    Description: Plain Language Summary: Better knowing when landslides are likely over the course of the year can reduce landslide risk by improving emergency preparedness. One research challenge is that catalogs of past landslides rarely cover the same areas or time periods, and have been collected in different ways. Here, we use statistical models to estimate monthly landslide activity in the Pacific Northwest. The models are able to combine five different landslide catalogs to make best use of all available information. We find a seasonal pattern in both the average number of landslides in a month and the probability of having any landslides. The landslide season begins in November, when the average number and the probability of landslides increase. The probability of landslides peaks in January and the average number in February, lagging behind winter rainfall peaks by one to two months. While landslides are least likely in summer, their activity is more variable in winter, with some winters bringing hundreds of landslides, and some very few. At the landslide season peak in February, a comparable amount of rain leads to many more landslides than at the onset in November, likely because already wet hillslopes are more prone to failure.
    Description: Key Points: Bayesian inference learns the seasonal pattern of landslide activity in the Pacific Northwest from five combined heterogeneous inventories. Landsliding is distinctly seasonal with highest probability (intensity) in January (February), lagging the annual precipitation peak. Landslide intensity for a given monthly rainfall during peak season in February is up to 10 times higher than at the onset in November.
    Description: DFG RTG NatRiskChange
    Description: https://data.nasa.gov/Earth-Science/Global-Landslide-Catalog/h9d8-neg4
    Keywords: ddc:551.3 ; landslide ; seasonality ; Pacific Northwest ; Bayesian multi‐level models ; logistic regression ; negative binomial regression
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 96
    Publication Date: 2023-01-20
    Description: We constrain Europa's tenuous atmosphere on the subsolar hemisphere by combining two sets of observations: oxygen emissions at 1,304 and 1,356 Å from Hubble Space Telescope (HST) spectral images and Galileo magnetic field measurements from its closest encounter, the E12 flyby. We describe Europa's atmosphere with three neutral gas species: global molecular (O2) and atomic oxygen (O), and localized water (H2O) present as a near‐equatorial plume and as a stable distribution concentrated around the subsolar point on the moon's trailing hemisphere. Our combined modeling based on the ratio of OI 1,356 to OI 1,304 Å emissions from Roth (2021; https://doi.org/10.1029/2021gl094289) and on magnetic field data allows us to derive constraints on the density and location of O2 and H2O in Europa's atmosphere. We demonstrate that 50% of the O2 and between 50% and 75% of the H2O abundances from Roth (2021; https://doi.org/10.1029/2021gl094289) are required to jointly explain the HST and Galileo measurements. These values are conditioned on a column density of O close to the upper limit of 6 × 1016 m−2 derived by Roth (2021; https://doi.org/10.1029/2021gl094289), and on a strongly confined stable H2O atmosphere around the subsolar point. Our analysis yields column densities of 1.2 × 1018 m−2 for O2, and 1.5 × 1019 to 2.2 × 1019 m−2 at the subsolar point for H2O. Both column densities, however, still lie within the uncertainties of Roth (2021; https://doi.org/10.1029/2021gl094289). Our results provide additional evidence for the existence of a stable H2O atmosphere at Europa.
    Description: Key Points: We combine Hubble Space Telescope spectral images and Galileo magnetometer data to constrain the density and location of water vapor in Europa's atmosphere. We simulate the plasma interaction for the Galileo E12 flyby with a three‐component atmosphere: global O2, stable confined H2O, and a plume. Using 50% of O2 and from 50% to 75% of H2O column densities from Roth (2021) yields magnetic field signatures consistent with both observations.
    Description: European Research Council http://dx.doi.org/10.13039/100010663
    Description: http://doi.org/10.17189/1519667
    Keywords: ddc:523 ; Europa ; Jupiter ; moon‐magnetosphere interaction ; icy moons ; atmosphere
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 97
    Publication Date: 2023-01-20
    Description: Understanding the magmatic plumbing system of rift volcanoes is essential when examining the interplay between magmatic and tectonic forces. Recent seismicity, volcanic activity, magma emplacement, and volatile release make the Natron basin the ideal location to study these processes in the East African Rift System. Here, we present the first high‐resolution tomographic imaging of Oldoinyo Lengai volcano and surrounding volcanic systems using attenuation mapping. High scattering and absorption features reveal fluid‐filled fracture networks below regions of magmatic volatile release at the surface and a close spatial association between carbonatite volcanism and deeply penetrating, fluid‐filled faults. High‐absorption features appear sensitive to fluids and thermal gradients, revealing a central sill complex and connected plumbing system down to the mid‐crust, which links volcanoes and rift segments across the developing magmatic rift.
    Description: Plain Language Summary: The interplay between magmatic and tectonic forces during rifting is still debated. While they are a key component of rift development, the complex structures of rifts and melt storage systems scatter and absorb seismic waves passing through them: in turn, this deteriorates the quality of the subsurface images we obtain from them. In this study, we use the loss of energy suffered by seismic waves to image the Natron basin, which hosts extinct volcanoes and the only active natrocarbonatite volcano on Earth, Oldoinyo Lengai. The results identify areas of melt storage and fracture networks that feed volatiles and melt to this volcano. Results suggest that carbonatite melts may ascend through the crust efficiently along deep‐seated faults systems, while silicate melts in the region may be primarily sourced from a separate melt reservoir. This reservoir, which is elongate and oriented oblique to the general trend of the rift, may act as a magmatic transfer zone between two rift segments.
    Description: Key Points: First fine‐scale 3D images reveal an interconnected rift plumbing system using scattering and absorption mapping. High scattering and absorption mark fluid‐filled faults that degas magmatic fluids and act as potential conduits for carbonatite melts. A high absorption melt reservoir feeds eruptions at Oldoinyo Lengai and dike intrusions and acts as a transfer zone between rift segments.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: National Science Foundation http://dx.doi.org/10.13039/100000001
    Description: Terrestrial Magmatic Systems
    Description: https://github.com/LucaDeSiena/MuRAT
    Description: https://doi.org/10.14470/4W7564850022
    Description: http://doi.org/10.6084/m9.figshare.20101232
    Keywords: ddc:551 ; rift plumbing system ; attenuation imaging ; magma‐fault interactions ; Oldoinyo Lengai ; Natron Basin
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 98
    Publication Date: 2023-01-20
    Description: We present the first global ocean‐biogeochemistry model that uses a telescoping high resolution for an improved representation of coastal carbon dynamics: ICON‐Coast. Based on the unstructured triangular grid topology of the model, we globally apply a grid refinement in the land‐ocean transition zone to better resolve the complex circulation of shallow shelves and marginal seas as well as ocean‐shelf exchange. Moreover, we incorporate tidal currents including bottom drag effects, and extend the parameterizations of the model's biogeochemistry component to account explicitly for key shelf‐specific carbon transformation processes. These comprise sediment resuspension, temperature‐dependent remineralization in the water column and sediment, riverine matter fluxes from land including terrestrial organic carbon, and variable sinking speed of aggregated particulate matter. The combination of regional grid refinement and enhanced process representation enables for the first time a seamless incorporation of the global coastal ocean in model‐based Earth system research. In particular, ICON‐Coast encompasses all coastal areas around the globe within a single, consistent ocean‐biogeochemistry model, thus naturally accounting for two‐way coupling of ocean‐shelf feedback mechanisms at the global scale. The high quality of the model results as well as the efficiency in computational cost and storage requirements proves this strategy a pioneering approach for global high‐resolution modeling. We conclude that ICON‐Coast represents a new tool to deepen our mechanistic understanding of the role of the land‐ocean transition zone in the global carbon cycle, and to narrow related uncertainties in global future projections.
    Description: Plain Language Summary: The coastal ocean is an area hardly taken into account by current climate change assessment activities. Yet, its capacity in carbon dioxide (CO2) uptake and storage is crucial to be included in a science‐based development of sustainable climate change mitigation and adaptation strategies. Earth system models are powerful tools to investigate the marine carbon cycle of the open ocean. The coastal ocean, however, is poorly represented in global models to date, because of missing key processes controlling coastal carbon dynamics and too coarse spatial resolutions to adequately simulate coastal circulation features. Here, we introduce the first global ocean‐biogeochemistry model with a dedicated representation of the coastal ocean and associated marine carbon dynamics: ICON‐Coast. In this model, we globally apply a higher resolution in the coastal ocean and extend the accounted physical and biogeochemical processes. This approach enables for the first time a consistent, seamless incorporation of the global coastal ocean in model‐based Earth system research. In particular, ICON‐Coast represents a new tool to deepen our understanding about the role of the land‐ocean transition zone in the global climate system, and to narrow related uncertainties in possible and plausible climate futures.
    Description: Key Points: We introduce the first global ocean‐biogeochemistry model with a dedicated representation of coastal carbon dynamics. We globally apply a grid refinement in the coastal ocean to better resolve regional circulation features, including ocean‐shelf exchange. We explicitly incorporate key physical and biogeochemical processes controlling coastal carbon dynamics.
    Description: German Research Foundation, Excellence Strategy EXC 2037 (CLICCS)
    Description: European Union, Horizon2020 Research and Innovation Program (ESM2025)
    Description: German Federal Ministry of Education
    Description: https://doi.org/10.5281/zenodo.6630352
    Keywords: ddc:551 ; coastal ocean ; global modeling ; marine carbon cycle ; variable‐resolution grid ; ocean‐biogiochemistry ; high‐resolution modeling
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 99
    Publication Date: 2023-01-20
    Description: Understanding conditions in the Earth's interior requires data derived from laboratory experiments. Such experiments provide important insights into the conditions under which mineral reactions take place as well as processes that control the localization of deformation in the deep Earth. We performed Griggs‐type general shear experiments in combination with numerical models, based on continuum mechanics, to quantify the effect of evolving sample geometry of the experimental assembly. The investigated system is constituted by CaCO3 and the experimental conditions are near the calcite‐aragonite phase transition. All experimental samples show a heterogeneous distribution of the two CaCO3 polymorphs after deformation. This distribution is interpreted to result from local stress variations. These variations are in agreement with the observed phase‐transition patterns and grain‐size gradients across the experimental sample. The comparison of the mechanical models with the sample provides insights into the distribution of local mechanical parameters during deformation. Our results show that, despite the use of homogeneous sample material (here calcite), stress variations develop due to the experimental geometry. The comparison of experiments and numerical models indicates that aragonite formation is primarily controlled by the spatial distribution of mechanical parameters. Furthermore, we monitor the maximum pressure and σ1 that is experienced in every part of our model domain for a given amount of time. We document that local pressure (mean stress) values are responsible for the transformation. Therefore, if the role of stress as a thermodynamic potential is investigated in similar experiments, an accurate description of the state of stress is required.
    Description: Plain Language Summary: To understand processes in the Earth's interior, we can simulate the extreme conditions via laboratory experiments by compressing and heating millimeter‐sized samples. Such experiments provide important insights into mineral reactions and processes that control deformation in the Earth. We performed rock deformation experiments close to calcite‐aragonite phase (CaCO3) transition. Deforming the sample leads to stress variations due to the experimental geometry. These variations are documented by locally occurring phase transition and variation in the grain‐size. We performed computer simulations of the deforming sample to quantify, for the first time, the effect of sample geometry on the distribution of mechanical variables, such as stress, pressure, or deformation, inside the sample. The new findings document that any mechanical variable cannot be treated as homogeneous within the sample because the variations can be significant. Deforming the sample leads to stress concentrations. By comparing the experimental observations and simulation results, we show that locally high pressure triggers the phase transition to aragonite, the high‐pressure polymorph. This has important consequences for further thermodynamic interpretations of systems under stress, where the role of deformation, pressure, or maximum principal stress on mineral reactions is investigated.
    Description: Key Points: Heterogeneous stress distribution in deformation experiments is investigated by numerical models, locally resolving mechanical variables. Resolving the mechanical variables in experiments suggests a link between local pressure (mean stress) variations and phase transition. Thermodynamic interpretations of deformed samples require a detailed understanding of local mechanical parameters.
    Description: ETH Zürich Foundation http://dx.doi.org/10.13039/501100012652
    Description: https://doi.org/10.5281/zenodo.6974768
    Keywords: ddc:550.78 ; deformation experiments ; numerical modeling ; phase transition ; rock deformation ; localization ; stress variations
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 100
    Publication Date: 2023-01-20
    Description: River‐valley morphology preserves information on tectonic and climatic conditions that shape landscapes. Observations suggest that river discharge and valley‐wall lithology are the main controls on valley width. Yet, current models based on these observations fail to explain the full range of cross‐sectional valley shapes in nature, suggesting hitherto unquantified controls on valley width. In particular, current models cannot explain the existence of paired terrace sequences that form under cyclic climate forcing. Paired river terraces are staircases of abandoned floodplains on both valley sides, and hence preserve past valley widths. Their formation requires alternating phases of predominantly river incision and predominantly lateral planation, plus progressive valley narrowing. While cyclic Quaternary climate changes can explain shifts between incision and lateral erosion, the driving mechanism of valley narrowing is unknown. Here, we extract valley geometries from climatically formed, alluvial river‐terrace sequences and show that across our dataset, the total cumulative terrace height (here: total valley height) explains 90%–99% of the variance in valley width at the terrace sites. This finding suggests that valley height, or a parameter that scales linearly with valley height, controls valley width in addition to river discharge and lithology. To explain this valley‐width‐height relationship, we reformulate existing valley‐width models and suggest that, when adjusting to new boundary conditions, alluvial valleys evolve to a width at which sediment removal from valley walls matches lateral sediment supply from hillslope erosion. Such a hillslope‐channel coupling is not captured in current valley‐evolution models. Our model can explain the existence of paired terrace sequences under cyclic climate forcing and relates valley width to measurable field parameters. Therefore, it facilitates the reconstruction of past climatic and tectonic conditions from valley topography.
    Description: Plain Language Summary: Little is known on how valleys widen and what sets their width. Therefore, it remains difficult to model the wealth of valley geometries that occur in nature and to predict how valleys adjust to environmental changes. Paired river terraces are staircases of abandoned valley floors that preserve valley widths of the past. The formation of river‐terrace sequences requires changes between vertical river incision and lateral river erosion of valley walls. Moreover, to preserve terraces on both sides of the river, the valley has to narrow over time. While cyclic climate changes during the Quaternary can explain the alternations between vertical incision and lateral erosion, they cannot explain why those valleys narrow. Here we investigate past valley geometries in paired, climatically formed river terraces. We find a negative linear relationship between valley width and valley height. We propose that this relationship reflects a balance between sediment that is moved from hillslopes into the channel and the capacity of the river to remove this sediment. Higher valley walls contribute more sediment that protects the wall from further widening. By including this hillslope‐erosion term, valley‐formation models can reproduce paired river terraces, and allow us to work toward “reading” climatic conditions from valley geometries.
    Description: Key Points: Valley width in alluvial terraces is inversely proportional to valley height. We suggest sediment supply from river‐independent hillslope erosion limits valley width. The coupling of hillslopes and river channels demands revision of current valley‐evolution models.
    Description: EC H2020 PRIORITY “Excellent science” H2020 Marie Skłodowska‐Curie Actions http://dx.doi.org/10.13039/100010665
    Description: https://doi.org/10.5880/fidgeo.2022.021
    Keywords: ddc:551.3 ; valley width ; river terraces
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...