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  • Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie  (672)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 93.0192
    Type of Medium: Monograph available for loan
    Pages: XXIV, 828 S. : graph. Darst.
    Language: English
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  • 2
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: PIK N 300-99-0282
    Type of Medium: Monograph available for loan
    Pages: XIV, 571 S.
    Edition: 6., überarb. und erw. Aufl.
    ISBN: 3540641653
    Language: German
    Location: A 18 - must be ordered
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  • 3
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    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 93.0251/a
    In: Handbook of geochemistry
    Pages: XIV, 442 S.
    Language: English
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  • 4
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/G 5218/2/4
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
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  • 5
    Call number: MOP B 17185
    In: Lecture notes in mathematics
    Type of Medium: Monograph available for loan
    Pages: VIII, 194 S. : graph. Darst.
    ISBN: 3540046100 , 0-387-04610-0
    Series Statement: Lecture notes in mathematics 91
    Uniform Title: Metod drobnych šagov rešenija mnogomernych zadač matematičeskoj fiziki
    Language: German
    Location: MOP - must be ordered
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  • 6
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/G 5218/2/3
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
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  • 7
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 7476/1 ; 10/G 5218/1 ; 10/M 93.0251A/1
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Pages: XIV, 442 S.
    Language: English
    Location: Upper compact magazine
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  • 8
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 7476/2 ; 10/G 5218/2/1
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
    Location: Upper compact magazine
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  • 9
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/G 5218/2/2
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Language: English
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  • 10
    Call number: M 99.0257
    Type of Medium: Monograph available for loan
    Pages: x, 335 S.
    ISBN: 3540655719
    Classification:
    Photogrammetry, Remote Sensing
    Language: English
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  • 11
    Call number: MR 90.0041 ; G 5636
    Type of Medium: Monograph available for loan
    Pages: 314 S. + 2 Tafeln
    Edition: 2., erw. und umgearb. Aufl.
    Language: German
    Location: Upper compact magazine
    Location: Upper compact magazine
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  • 12
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 4/M 02.0106
    In: Lecture notes in earth sciences
    Type of Medium: Monograph available for loan
    Pages: X, 652 S.
    ISBN: 3540635033
    Series Statement: Lecture notes in earth sciences 83
    Classification:
    Geomagnetism, Geoelectromagnetism
    Language: English
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  • 13
    Call number: 4/M 02.0107
    In: Lecture notes in earth sciences
    Type of Medium: Monograph available for loan
    Pages: 111 S.
    ISBN: 3540656049
    Series Statement: Lecture notes in earth sciences 85
    Classification:
    A. 2.5.
    Language: English
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  • 14
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 99.0051
    Type of Medium: Monograph available for loan
    Pages: 335 S.
    ISBN: 3540649158
    Series Statement: European Communication Council report 1999
    Classification:
    E.4.
    Language: German
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  • 15
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: 12/M 00.0302 ; AWI A3-99-0166
    Type of Medium: Monograph available for loan
    Pages: XX, 374 S.
    ISBN: 3540636625
    Classification:
    Meteorology and Climatology
    Language: English
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  • 16
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 01.0390
    Type of Medium: Monograph available for loan
    Pages: XIII, 277 S.
    ISBN: 3540653481
    Series Statement: Springer-Lehrbuch
    Classification:
    C.4.1.
    Language: German
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  • 17
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: G 6540
    In: Verständliche Wissenschaft
    Type of Medium: Monograph available for loan
    Pages: 176 S. : Ill., graph. Darst.
    Edition: 2., verb. und erw. Aufl., 6. - 11. Tsd
    Series Statement: Verständliche Wissenschaft 42
    Language: German
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  • 18
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: G 5658
    Type of Medium: Monograph available for loan
    Pages: XXIV, 671 S. : graph. Darst
    Edition: 2., neubearb. u. erw. Aufl.
    Language: German
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  • 19
    Call number: IASS 20.93439
    Type of Medium: Monograph available for loan
    Pages: 255 Seiten , graphische Darstellungen
    ISBN: 9783946356134
    Series Statement: Wuppertal Spezial 55
    Language: German
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  • 20
    Call number: 4/M 98.0541
    In: Lecture notes in earth sciences
    Type of Medium: Monograph available for loan
    Pages: X, 191 S.
    ISBN: 3540650067
    ISSN: 0930-0317
    Series Statement: Lecture notes in earth sciences 80
    Classification:
    Geophysical Exploration, Geophysical Prospecting
    Language: English
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  • 21
    Call number: PIK M 031-01-0703
    Type of Medium: Monograph available for loan
    Pages: 524 p.
    ISBN: 3540654313
    Language: English
    Location: A 18 - must be ordered
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  • 22
    Call number: 19/M 95.0377
    Type of Medium: Monograph available for loan
    Pages: XV, 381 S. : Ill.
    Edition: 6., neubearb. und erw. Aufl.
    ISBN: 3540587535
    Series Statement: Springer-Lehrbuch
    Classification:
    C.5.1.
    Language: German
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  • 23
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 95.0378
    Type of Medium: Monograph available for loan
    Pages: XVII, 200 S.
    ISBN: 3540573801
    Uniform Title: Les montagnes sous la mer
    Classification:
    Regional Geology
    Language: English
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  • 24
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: M 96.0351
    In: Hochfrequenztechnik
    Type of Medium: Monograph available for loan
    Pages: XVII, 492 S.
    Edition: 5., neubearb. Aufl
    ISBN: 3540580700
    Classification:
    C.5.1.
    Language: German
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  • 25
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 96.0353
    Type of Medium: Monograph available for loan
    Pages: VIII, 173 S.
    ISBN: 3540579931
    Classification:
    Geophysical Exploration, Geophysical Prospecting
    Language: English
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  • 26
    Call number: 6/M 96.0289 ; 6/M 96.0298
    In: International Association of Geodesy symposia
    Type of Medium: Monograph available for loan
    Pages: VI, 236 S.
    ISBN: 3540608826
    Series Statement: International Association of Geodesy symposia 116
    Classification:
    Gravity Field
    Language: English
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  • 27
    Call number: AWI G3-99-0175 ; AWI G3-11-0026
    Description / Table of Contents: The Arctic is considered to be one of the most sensitive environmental elements on Earth, which may respond rapidly to climate change. However, our knowledge of the present and past processes of the Arctic system is still relatively sparse. Based on a multidisciplinary approach, German and Russian scientists describe in this book the natural processes behind short- and long-term changes in the Laptev Sea and its hinterland (Arctic Siberia), using modern climate data and paleorecords which were collected over the past 6 years. These marine and terrestrial datasets provide important new insights into the causes, impacts, and feedback mechanisms of this extreme environment.
    Type of Medium: Monograph available for loan
    Pages: XI, 711 S. , Ill., graph. Darst., Kt.
    ISBN: 3540656766
    Language: English
    Note: Table of Contents: SECTION A: MODERN OCEAN AND SEA-ICE PROCESSES. - Features of Seasonal and Interannual Variability of the Sea Level and Water Circulation in the Laptev Sea / V. K. Pavlov and P. V. Pavlov. - Numerical Modelling of Storm Surges in the Laptev Sea Based on the Finite Element Method / I. Ashik and A. Novakov. - Large-Scale Variations of Sea Level in the Laptev Sea / G. N. Voinov and E. A. Zakharchuk. - Extreme Oscillations of the Sea Level in the Laptev Sea / I. Ashik, Y. Dvorkin and Y. Vanda. - Internal Waves in the Laptev Sea / E. A. Zakharchuk. - The Composition of the Coarse Fraction of Aerosols in the Marine Boundary Layer over the Laptev, Kara and Barents Seas / V. P. Shevchenko, A. P. Lisitzin, R. Stein, V. V. Serova, A. B. Isaeva and N. V. Politova. - New Data on Sea-Ice Albedo in the Laptev and Barents Seas / B. V. Ivanov. - Possible Causes of Radioactive Contamination in the Laptev Sea / V. K. Pavlov, V. V. Stanovoy and A. I. Nikitin. - Oceanographic Causes for Transarctic Ice Transport of River Discharge / I. Dmitrenko, P. Golovin, V. Gribanov and H. Kassens. - Step-Like Vertical Structure Formation Due to Turbulent Mixing of Initially Continuous Density Gradients / A. Zatsepin, S. Dikarev, S. Poyarkov, N. Sheremet, I. Dmitrenko, P. Golovin and H. Kassens. - Dissolved and Paniculate Major and Trace Elements in Newly Formed Ice from the Laptev Sea (Transdrift III, October 1995) / J. A. Hölemann, M. Schirmacher and A. Prange. - Particle Entrainment into Newly Forming Sea Ice - Freeze-Up Studies in October 1995 / F. Lindemann, J. A. Holemann, A. Korablev and A. Zachek. - Frazil Ice Formation during the Spring Flood and its Role in Transport of Sediments to the Ice Cover / P. Golovin, I. Dmitrenko, H. Kassens and J. A. Hölemann. - SECTION B: THE MARINE ECOSYSTEM. - Pelagic-Benthic Coupling in the Laptev Sea Affected by Ice Cover / C. Grahl, A. Boetius and E.-M. Nöthig. - Chlorophyll a Distribution in Water Column and Sea Ice during the Laptev Sea Freeze-Up Study in Autumn 1995 / K. v. Juterzenka and K. Knickmeier. - Composition, Abundance and Population Structure of Spring-Time Zooplankton in the Shelf-Zone of Laptev Sea / E. N. Abramova. - Macrobenthos Distribution in the Laptev Sea in Relation to Hydrology / V. V. Petryashov, B. I. Sirenko, A. A. Golikov, A. V. Novozhilov, E. Rachor, D. Piepenburg and M. K. Schmid. - Carepoctus solidus sp.n., a New Species of Liparid Fish (Scorpaeniformes, Liparidae) from the Lower Bathyal of the Polar Basin / N. V. Chernova. - Spring Stopover of Birds on the Laptev Sea Polynya / D. V. Solovieva. - SECTION C: LAND-OCEAN INTERACTIONS AND PATHWAYS. - Major, Trace and Rare Earth Element Geochemistry of Suspended Particulate Material of East Siberian Rivers Draining to the Arctic Ocean / V. Rachold. - Carbon Isotope Composition of Particulate Organic Material in East Siberian Rivers / V. Rachold and H.-W. Hubberten. - Distribution of River Water and Suspended Sediment Loads in the Deltas of Rivers in the Basins of The Laptev and East-Siberian Seas / V. V. Ivanov and A. A. Piskun. - Dissolved Oxygen, Silicon, Phosphorous and Suspended Matter Concentrations During the Spring Breakup of The Lena River / S. V. Pivovarov, J. A. Hölemann, H. Kassens, M. Antonow and I. Dmitrenko. - Distribution Patterns of Heavy Minerals in Siberian Rivers, the Laptev Sea and the eastern Arctic Ocean: An Approach to Identify Sources, Transport and Pathways of Terrigenous Matter / M. Behrends, E. Hoops and B. Peregovich. - The Role of Coastal Retreat for Sedimentation in the Laptev Sea / F. E. Are. - SECTION D: TERRESTRIAL ENVIRONMENT - PAST AND PRESENT. - Seasonal Changes in Hydrology, Energy Balance and Chemistry in the Active Layers of Arctic Tundra Soils in Taymyr Peninsula, Russia / J. Boike and P. P. Overduin. - The Landscape and Geobotanical Characteristics of the Levinson-Lessing Lake Basin, Byrranga Mountains, Central Taimyr / M. A. Anisimov and I. N. Pospelov. - Studies of Methane Production and Emission in Relation to the Microrelief of a Polygonal Tundra in Northern Siberia / V. A. Samarkin, A. Gundelwein and E.-M. Pfeiffer. - Carbon Dioxide and Methane Emmissions at Arctic Tundra Sites in North Siberia / M. Sommerkom, A. Gundelwein, E.-M. Pfeiffer and M. Bolter. - The Features of the Hydrological Regime of the Lake-River Systems of the Byrranga Mountains (by the Example of the Levinson-Lessing Lake) / V. P. Zimichev, D. Yu. Bolschyanov, V. G. Mesheryakov and D. Gintz. - Lead-210 Dating and Heavy Metal Concentration in Recent Sediments of Lama Lake (Norilsk Area, Siberia) / B. Hagedorn, S. Harwart, M. M. R. van der Loeff and M. Melles. - Late Weichselian to Holocene Diatom Succession in a Sediment Core from Lama Lake, Siberia and Presumed Ecological Implications / U. Kienel. - Climate and Vegetation History of the Taymyr Peninsula since Middle Weichselian Time - Palynological Evidence from Lake Sediments / J. Hahne and M. Melles. - Laminated Sediments from Levinson-Lessing Lake, Northern Central Siberia - A 30,000 Year Record of Environmental History? / T. Ebel, M. Melles and F. Niessen. - High-Resolution Seismic Stratigraphy of Lake Sediments on the Taymyr Peninsula, Central Siberia / F. Niessen, T. Ebel, C. Kopsch and G. B. Fedorov. - Archaeological Survey in Central Taymyr / V. V. Pitul'ko. - Marine Pleistocene Deposits of the Taymyr Peninsula and their Age from ESR Dating / D. Bolshiyanov and A. Molodkov. - Paleoclimatic Indicators from Permafrost Sequences in the Eastern Taymyr Lowland / C. Siegert, A. Yu. Derevyagin, G.N. Shilova, W.-D. Hermichen and A. Hiller. - SECTION E: MARINE DEPOSITIONAL ENVIRONMENT - PAST AND PRESENT. - Stable Oxygen Isotope Ratios in Benthic Carbonate Shells of Ostracoda, Foraminifera, and Bivalvia from Surface Sediments of the Laptev Sea, Summer 1993 and 1994 / H. Erlenkeuser and U. von Grafenstein. - Determination of Depositional Beryllium-10 Fluxes in the Area of the Laptev Sea and Beryllium-10 Concentrations in Water Samples of High Northern Latitudes / C. Strobl, V. Schulz, S. Vogler, S. Baumann, H. Kassens, P. W. Kubik, M. Suter and A. Mangini. - Spatial Distribution of Diatom Surface Sediment Assemblages on the Laptev Sea Shelf (Russian Arctic) / H. Cremer. - Diatoms from Surface Sediments of the Saint Anna Trough (Kara Sea) / R. N. Djinoridze, G. I. Ivanov, E. N. Djinoridze, and R. F. Spielhagen. - Distribution of Aquatic Palynomorphs in Surface Sediments from the Laptev Sea, Eastern Arctic Ocean / M. Kunz-Pirrung. - Distribution of Pollen and Spores in Surface Sediments of the Laptev Sea / O. D. Naidina and H. A. Bauch. - Clay Mineral Distribution in Surface Sediments of the Laptev Sea: Indicator for Sediment Provinces, Dynamics and Sources / B. T. Rossak, H. Kassens, H. Lange and J. Thiede. - Planktic Foraminifera in Holocene Sediments from the Laptev Sea and the Central Arctic Ocean: Species Distribution and Paleobiogeographical Implication / H. A. Bauch. - Holocene Diatom Stratigraphy and Paleoceanography of the Eurasian Arctic Seas / Y. Polyakova. - Late Quaternary Organic Carbon and Biomarker Records from the Laptev Sea Continental Margin (Arctic Ocean): Implications for Organic Carbon Flux and Composition / R. Stein, K. Fahl, F. Niessen and M. Siebold. - Late Pleistocene Paleoriver Channels on the Laptev Sea Shelf - Implications from Sub-Bottom Profiling / H. P. Kleiber and F. Niessen. - Main Structural Elements of Eastern Russian Arctic Continental Margin Derived from Satellite Gravity and Multichannel Seismic Reflection Data / S. S. Drachev, G. L. Johnson, S. W. Laxon, D. C. McAdoo and H. Kassens. - High Resolution Seismic Studies in the Laptev Sea Shelf: First Results and Future Needs / B. Kim, G. Grikurov and V. Soloviev. - SECTION F: SUMMARY. - Dynamics and History of the Laptev Sea and its Continental Hinterland: A Summary / J. Thiede, L. Timokhov, H. A. Bauch, D. Bolshiyanov, I. Dmitrenko
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  • 28
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: AWI A8-99-0052
    Description / Table of Contents: In diesem Buch wird einerseits die spannende Entdeckung der Stratosphäre selbst und verschiedener unerwarteter Phänomene in der Stratosphäre beschrieben: ein bemannter Ballonflug im Jahr 1901 bis in 11 km Höhe; eine Expedition zum Victoriasee im Jahr 1908; die Entdeckung der Ozonschicht um 1930, des "Berliner Phänomens" im Jahr 1952, des Einflusses von Vulkaneruptionen im Jahr 1982, des Ozonlochs im Jahr 1985 und des Einflusses der Sonnenaktivität im Jahr 1987. Andererseits wird gezeigt, wie diese Erscheinungen miteinander verknüpft sind und wie sie anthropogene und natürliche Schwankungen in unserem Klimasystem verursachen. Am Beispiel der Stratosphäre soll das Buch zum Verständnis komplizierter Zusammenhänge in der Natur beitragen.
    Type of Medium: Monograph available for loan
    Pages: XI, 177 Seiten , Illustrationen
    ISBN: 3540650008
    Language: German
    Note: Inhaltsverzeichnis 1 Berlin: Die Wiege der Stratosphärenforschung 1.1 Erste meteorologische Beobachtungen 1.2 Die Erforschung der Freien Atmosphäre 1.2.1 Bemannte Freiballonfahrten 1.2.2 Unbemannte Registrierballone 1.3 Die Entdeckung der Stratosphäre 1.4 Das Observatorium Lindenberg 1.4.1 Die Entdeckung der BERSON-Westwinde am Äquator 1.5 Das Institut für Meteorologie der FU Berlin 1.5.1 Die Entdeckung des Berliner Phänomens 1.5.2 Eine erste Klimatologie 1.5.3 Erste tägliche Wetterkarten von der Stratosphäre 1.5.4 Die Entdeckung des Einflusses der Sonne Literatur 2 Kurzbeschreibung der Klimatologie 2.1 Was für Daten haben wir heute? 2.2 Der mittlere Zustand der Stratosphäre 2.2.1 Die Temperatur von Pol zu Pol 2.2.2 Der Wind von Pol zu Pol 2.2.3 Die Zirkulation von Pol zu Pol 2.2.4 Monatsmittelkarten über der Nordhemisphäre 2.2.5 Monatsmittelkarten über der Südhemisphäre 2.3 Variabilität und Trends 2.3.1 Variabilität der Temperatur von Jahr zu Jahr 2.3.2 Temperaturtrends in der Stratosphäre Literatur 3 Warme und kalte Winter in der Stratosphäre 3.1 Einleitung 3.2 Major Midwinter Warming 3.2.1 Einteilung der Stratosphärenerwärmungen 3.2.2 Das "Major Midwinter Warming" im Winter 1990/91 3.2.3 Schema einer Stratosphärenerwärmung 3.3 Zusammenhänge 3.3.1 Die Southern Oscillation (SO) 3.3.2 Die Quasi-Biennial Oscillation (QBO) 3.3.3 Das solare Signal im Nordwinter 3.3.4 Vulkane und kalte Winter in der arktischen Stratosphäre 3.4 Vergleich zwischen Arktis und Antarktis 3.5 Modellexperimente Literatur 4 Die Quasi-Biennial Oscillation 4.1 Frühe Beobachtungen 4.2 Die Entdeckung der QBO 4.3 Heutiger Kenntnisstand 4.4 Zusammenhang mit den hohen Breiten Literatur 5 Die Ozonschicht und ihre Probleme 5.1 Einleitung 5.2 Frühe Beobachtungen 5.2.1 Dobsons frühes Meßnetz 5.2.2 Der Ozongehalt über Tromsö 5.3 Die natürliche Verteilung des Gesamtozons 5.4 Anthropogene Ozonabnahme in der Stratosphäre 5.4.1 Katalytische Ozonzerstörung 5.4.2 "Ozonloch" über der Antarktis 5.4.3 Trends im stratosphärischen Ozongehalt 5.4.4 Maßnahmen zur Reduktion des Chlorgehalts Literatur 6 Der 11jährige Sonnenfleckenzyklus 6.1 Einleitung 6.2 Das solare Signal im Lauf des Jahres 6.2.1 Nordhemisphäre 6.2.2 Südhemisphäre 6.2.3 Globale Korrelationen 6.3 Eine Verbindung zur tropischen Troposphäre? 6.4 Gesamtozongehalt und der Sonnenfleckenzyklus 6.5 Suche nach dem Mechanismus . Literatur 7 Schlußbetrachtungen 7.1 Zusammenfassung des bisher Gesagten 7.2 Relevanz der Stratosphäre 7.3 Unerwartetes! Inhaltsverzeichnis Glossar Sachverzeichnis
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  • 29
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 95.0152
    Type of Medium: Monograph available for loan
    Pages: 1790 S. in getr. Zählung. : Ill., zahlr. graph. Darst.
    Edition: 18. Aufl.
    ISBN: 3540576509
    Classification:
    C.5.2.
    Language: German
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  • 30
    Monograph available for loan
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    Call number: M 95.0301
    Type of Medium: Monograph available for loan
    Pages: 476 S.
    Edition: 2., neubearb. Aufl. / bearb. von Jörg Bechlars
    ISBN: 3540161392
    Classification:
    C.2.4.
    Language: German
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  • 31
    Call number: PIK N 071-16-89725
    Type of Medium: Monograph available for loan
    Pages: XXVI, 322 S. , graph. Darst.
    ISBN: 3540661794
    Series Statement: International and European environmental policy series
    Uniform Title: Umwelt und Sicherheit 〈engl.〉
    Language: English
    Location: A 18 - must be ordered
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  • 32
    Call number: 4/M 95.0588
    In: Lecture notes in earth sciences
    Type of Medium: Monograph available for loan
    Pages: VIII, 187 S.
    ISBN: 3540591702
    Series Statement: Lecture notes in earth sciences 57
    Classification:
    Geochemistry
    Language: English
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  • 33
    Call number: 1.10/M 95.0474
    Type of Medium: Monograph available for loan
    Pages: X, 216 S.
    ISBN: 3540586075
    Uniform Title: Interpretation of geological structures through maps
    Classification:
    Tectonics
    Language: German
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  • 34
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    Call number: M 96.0023
    Type of Medium: Monograph available for loan
    Pages: xii, 414 S.
    ISBN: 354058580X
    Classification:
    C.2.8.
    Language: German
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  • 35
    Call number: 8/M 96.0065
    In: NATO ASI Series
    Type of Medium: Monograph available for loan
    Pages: XII, 452 S.
    ISBN: 3540601856
    Series Statement: NATO ASI series : I, Global and environmental change : 2, Environment 4
    Classification:
    Seismology
    Language: English
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  • 36
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    Associated volumes
    Call number: M 95.0725
    In: Lecture notes in computer science
    Type of Medium: Monograph available for loan
    Pages: XI, 404 S.
    ISBN: 3540601597
    Series Statement: Lecture notes in computer science 951
    Classification:
    C.2.8.
    Language: English
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  • 37
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    Call number: 4/M 96.0066
    In: Lecture notes in earth sciences
    Type of Medium: Monograph available for loan
    Pages: xv, 291 S.
    ISBN: 354059051X
    Series Statement: Lecture notes in earth sciences 55
    Classification:
    Geophysical Exploration, Geophysical Prospecting
    Language: English
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  • 38
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    Call number: 16/M 96.0434
    In: Springer series in optical sciences
    Type of Medium: Monograph available for loan
    Pages: XI, 424 S.
    ISBN: 354058479X
    Series Statement: Springer series in optical sciences 71
    Classification:
    C.3.5.
    Language: English
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  • 39
    Call number: 6/M 95.0478
    In: International Association of Geodesy symposia
    Type of Medium: Monograph available for loan
    Pages: XIII, 656 S.
    ISBN: 3540592040
    Series Statement: International Association of Geodesy symposia 113
    Classification:
    A.1.1.
    Language: English
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  • 40
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    Call number: M 96.0064
    Type of Medium: Monograph available for loan
    Pages: XIV, 256 S.
    ISBN: 3540601279
    Classification:
    C.1.7.
    Language: English
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  • 41
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    Call number: 9/M 96.0096
    In: IGCP project
    Type of Medium: Monograph available for loan
    Pages: XVI, 604 S.
    ISBN: 3540554726
    Series Statement: IGCP project 233
    Classification:
    Regional Geology
    Language: English
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  • 42
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    Berlin [u.a.] : Springer
    Call number: 8/M 96.0328
    Type of Medium: Monograph available for loan
    Pages: VIII, 224 S.
    ISBN: 3540590978
    Classification:
    B.2.5.
    Language: German
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  • 43
    Monograph available for loan
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    Berlin [u.a.] : Springer
    Call number: 19/M 96.0027
    Type of Medium: Monograph available for loan
    Pages: IX, 255 S.
    Edition: 2., erw. Aufl.
    ISBN: 3540569677
    Classification:
    C.1.2.
    Language: German
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  • 44
    Call number: M 96.0284
    Type of Medium: Monograph available for loan
    Pages: viii, 272 S.
    ISBN: 354059423X
    Series Statement: Advances in spatial science
    Classification:
    E.8.
    Language: English
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  • 45
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    Associated volumes
    Call number: 6/M 95.0574 ; 6/M 95.0661
    In: International Association of Geodesy symposia
    Type of Medium: Monograph available for loan
    Pages: X, 446 S.
    ISBN: 3540594213
    Series Statement: International Association of Geodesy symposia 114
    Classification:
    A.1.1.
    Language: English
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  • 46
    Monograph available for loan
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    Berlin [u.a.] : Springer
    Call number: M 96.0210
    Type of Medium: Monograph available for loan
    Pages: XV, 298 S.
    Edition: [2nd print.]
    ISBN: 3540562206
    Classification:
    C.2.1.
    Language: English
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  • 47
    Call number: M 96.0550 ; AWI G6-96-0128
    Description / Table of Contents: A lake, as a body of water, is in continuous interaction with the rocks and soils in its drainage basin, the atmosphere, and surface and groundwaters. Human industrial and agricultural activities introduce new inputs and processes into lake systems. This volume is a selection of ten contributions dealing with diverse aspects of lake systems, including such subjects as the geological controls of lake basins and their histories, mixing and circulation patterns in lakes, gaseous exchange between the water and atmosphere, and human input to lakes through atmospheric precipitation and surficial runoff. This work was written with a dual goal in mind: to serve as a textbook and to provide professionals with in-depth expositions and discussions of the more important aspects of lake systems.
    Type of Medium: Monograph available for loan
    Pages: XVI, 334 Seiten , Illustrationen
    Edition: 2. ed.
    ISBN: 3540578919
    Classification:
    Sedimentology
    Language: English
    Note: Contents: 1 Global Distribution of Lakes / M. MEYBECK. - 1 Introduction. - 2 Background Material and Approaches to Global Lake Census. - 2.1 Data Used. - 2.2 Approaches to Global Lake Census. - 3 General Laws of Lake Distribution. - 3.1 Lake Density . - 3.2 Limnic Ratio. - 4 Distribution of Lakes of Tectonic Origin. - 5 Lakes of Glacial Origin. - 5.1 Lake Densities. - 5.2 Global Deglaciated Area. - 5.3 Total Number of Glacial Lakes. - 6 Fluvial Lakes. - 7 Global Distribution of Crater Lakes. - 8 Global Distribution of Saline Lakes. - 8.1 Coastal Lagoons. - 8.2 Salinized Lakes due to Evaporation. - 9 Global Lake Distribution. - 9.1 Extrapolation Approach. - 9.2 Lake Type Approach. - 9.3 Climatic Typology Approach. - 9.4 Lake Distribution in Endorheic Areas. - 9.5 Global Dissolved Salt Distribution in Lakes. - 10 Major Changes in Global Lake Distribution in the Geological Past. - 10.1 Lake Ages. - 10.2 Historical Changes. - 10.3 Postglacial Changes. - 11 Discussion and Conclusions. - References. - 2 Hydrological Processes and the Water Budget of Lakes / T. C. WINTER. - 1 Introduction. - 2 Hydrological System with Regard to Lakes. - 2.1 Interaction of Lakes with Atmospheric Water. - 2.2 Interaction of Lakes with Surface Water. - 2.3 Interaction of Lakes with Subsurface Water. - 2.4 Change in Lake Volume. - 3 Summary. - References. - 3 Hydrological and Thermal Response of Lakes to Climate: Description and Modeling / S. W. HOSTETLER. - 1 Introduction. - 2 Hydrological Response. - 3 The Hydrological Budget. - 4 Hydrological Models. - 5 Thermal Response. - 5.1 Energy Budget and Energy Budget Models. - 5.2 Models and Modeling. - 6 Use of Models to Link Lakes with Climate Change. - 7 Input Data Sets. - 8 Sample Applications. - 9 Summary. - References. - 4 Mixing Mechanisms in Lakes / D. M. IMBODEN and A. WÜEST. - 1 Transport and Mixing. - 2 Lakes as Physical Systems. - 3 Fluid Dynamics: Mathematical Description of Advection and Diffusion. - 3.1 Equations of Fluid Motion. - 3.2 Turbulence, Reynolds' Stress, and Eddy Diffusion. - 3.3 Vertical Momentum Equation. - 3.4 Nonlocal Diffusion and Transilient Mixing. - 4 Density and Stability of Water Column. - 4.1 Equation of State of Water. - 4.2 Potential Temperature and Local Vertical Stability. - 5 Energy Fluxes: Driving Forces Behind Transport and Mixing. - 5.1 Thermal Energy. - 5.2 Potential Energy. - 5.3 Kinetic Energy. - 5.4 Turbulent Kinetic Energy Balance in Stratified Water. - 5.5 Internal Turbulent Energy Fluxes: Turbulence Cascade. - 6 Mixing Processes in Lakes. - 6.1 Waves and Mixing. - 6.2 Mixing in the Surface Layer. - 6.3 Diapycnal Mixing. - 6.4 Boundary Mixing. - 6.5 Double Diffusion. - 6.6 Isopycnal Mixing. - 7 Mixing and Its Ecological Relevance. - 7.1 Time Scales of Mixing. - 7.2 Reactive Species and Patchiness. - 7.3 Mixing and Growth: The Search for an Ecological Steering Factor. - References. - 5 Stable Isotopes of Fresh and Saline Lakes / J. R. GAT. - 1 Introduction. - 1.1 Isotope Separatio During Evaporation. - 2 Small-Area Lakes. - 2.1 Seasonal and Annual Changes. - 2.2 Deep Freshwater Lakes. - 2.3 Transient Surface-Water Bodies. - 3 Interactive and Feedback Systems. - 3.1 Network of Surface-Water Bodies. - 3.2 Recycling of Reevaporated Moisture into the Atmosphere. - 3.3 Large Lakes. - 3.4 Large-Area Lakes with Restricted Circulation. - 4 Saline Lakes. - 4.1 Isotope Hydrology of Large Salt Lakes. - 4.2 Ephemeral Salt Lakes and Sabkhas. - 5 Isotopie Paleolimnology. - 6 Conclusions: From Lakes to Oceans. - References. - 6 Exchange of Chemicals Between the Atmosphere and Lakes / P. VLAHOS, D. MACKAY, S. J. EISENREICH, and KC. HORNBUCKLE. - 1 Introduction. - 2 Air-Water Partitioning Equilibria. - 3 Diffusion Between Water and Air. - 4 Volatilization and Absorption: Double-Resistance Approach. - 5 Factors Affecting Mass-Transfer Coefficients. - 6 Partitioning of Chemical to Paniculate Matter in Air and Water. - 6.1 Air. - 6.2 Water. - 7 Atmospheric Deposition Processes. - 7.1 Dry Deposition. - 7.2 Wet Deposition. - 8 Specimen Calculation. - 8.1 Step 1: Physicochemical Properties. - 8.2 Step 2: Mass-Transfer Coefficients. - 8.3 Step 3: Sorption in Air and Water. - 8.4 Step 4: Equilibrium Status. - 8.5 Step 5: Volatilization and Deposition Rates. - 9 Role of Air-Water Exchange in Lake Mass Balances. - 10 Case Studies. - 10.1 Mass Balance on Siskiwit Lake, Isle Royale. - 10.2 Mass Balance on Lake Superior. - 10.3 Air-Water Exchange in Green Bay, Lake Michigan. - 10.4 Air-Water Exchange in Lake Superior. - 11 Conclusions. - References. - 7 Atmospheric Depositions: Impact of Acids on Lakes / W. STUMM and J. SCHNOOR. - Abstract. - 1 Introduction: Anthropogenic Generation of Acidity. - 1.1 Genesis of Acid Precipitation. - 2 Acidity and Alkalinity: Neutralizing Capacities. - 2.1 Transfer of Acidity (or Alkalinity) from Pollution Through the Atmosphere to Ecosystems. - 3 Acidification of Aquatic and Terrestrial Ecosystems. - 3.1 Disturbance of H+ Balance from Temporal or Spatial Decoupling of the Production and Mineralization of the Biomass. - 3.2 In Situ H+ Ion Neutralization in Lakes. - 3.3 Krug and Frink Revisited. - 4 Brønsted Acids and Lewis Acids: Pollution by Heavy Metals, as Influenced by Acidity. - 4.1 Cycling of Metals. - 4.2 Pb in Soils. - 5 Impact of Acidity on Ecology in Watersheds. - 5.1 Soils. - 5.2 Lakes. - 5.3 Nitrogen Saturation of Forests. - 6 Critical Loads. - 6.1 Critical Load Maps. - 6.2 Models for Critical Load Evaluation. - 7 Case Studies. - 7.1 Chemical Weathering of Crystalline Rocks in the Catchment Area of Acidic Ticino Lakes, Switzerland. - 7.2 Watershed Manipulation Project at Bear Brooks, Maine. - 8 Summary. - References. - 8 Redox-Driven Cycling of Trace Elements in Lakes / J. HAMILTON-TAYLOR and W. DAVISON. - 1 Introduction. - 2 Major Biogeochemical Cycles and Pathways. - 3 Iron and Manganese. - 3.1 Transformations and Cycling. - 3.2 Iron and Manganese Compounds as Carrier Phases. - 4 Sediment-Water Interface. - 4.1 Diffusive Flux from Sediments. - 4.2 Evidence of Little or No Diffusive Efflux from Sediments. - 4.3 Transient Remobilization. - 4.4 Diffusive Flux into Sediments. - 5 Pathways Involving Redox Reactions Directly: Case Studies. - 5.1 Arsenic. - 5.2 Chromium. - 5.3 239,240Pu. - 5.4 Selenium 6 Pathways Involving Redox Reactions Indirectly: Case Studies. - 6.1 137Cs. - 6.2 Stable Pb, 210Pb, and 210Po. - 6.3 Zinc. - 7 Summary and Conclusions. - References. - 9 Comparative Geochemistry of Marine Saline Lakes / F. T. MACKENZIE, S. VINK, R. WOLLAST, and L. CHOU. - 1 Introduction. - 2 General Characteristics of Marine Saline Lakes. - 3 Comparative Sediment-Pore-Water Reactions. - 3.1 Mangrove Lake, Bermuda. - 3.2 Solar Lake, Sinai. - 4 Conclusions. - References. - 10 Organic Matter Accumulation Records in Lake Sediments / P. A. MEYERS and R. ISHIWATARI. - 1 Introduction. - 1.1 Significance of Organic Matter in Lake Sediments. - 1.2 Origins of Organic Matter to Lake Sediments. - 1.3 Alterations of Organic Matter During Deposition. - 1.4 Similarities and Differences Between Organic Matter in Sediments of Lakes and Oceans. - 1.5 Dating of Lake-Sediment Records. - 2 Indicators of Sources and Alterations of Total Organic Matter in Lake Sediments. - 2.1 Source Information Preserved in C/N Ratios of Sedimentary Organic Matter. - 2.2 Source Information from Carbon-Stable Isotopic Compositions. - 2.3 Source Information from Nitrogen-Stable Isotopic Compositions. - 3 Origin and Alterations of Humic Substances. - 4 Sources and Alterations of Lipid Biomarkers. - 4.1 Alteration of Lipids During Deposition. - 4.2 Changes in Sources vs Selective Diagenesis. - 4.3 Effects of Sediment Grain Size on Geolipid Compositions. - 4.4 Source Records of Alkanes in Lake Sediments. - 4.5 Preserv
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  • 48
    Publication Date: 2020-02-12
    Description: In summer 2017, the ICDP SUSTAIN project (Surtsey Underwater volcanic System for Thermophiles, Alteration processes and INnovative concretes), drilled three cored boreholes (Table 1) through Surtsey at sites ≤10 m from a cored hole obtained in 1979. Drilling through the still hot volcano was carried out with an Atlas Copco CS1000 drill rig, whose components were transported by helicopter to Surtsey and re-assembled on site. The first vertical borehole, SE-02a, was cored in HQ diameter to 152 meters below surface (m b.s.) during August 7-16. It was terminated due to borehole collapse. A second vertical (SE-02b) cored borehole was then drilled in HQ diameter to 192 m during August 19-26. Wireline borehole logging in SE-02b was performed August 26. The anodized NQ-sized aluminum tubing of the Surtsey Subsurface Observatory was installed in SE-02b to 181 m depth on August 27. A third borehole, SE-03, angled 35° from vertical and directed 264°, was drilled from August 28 to September 4 and reached a measured depth of 354 m (~290 m vertical depth) under the eastern crater. The core is HQ diameter to a measured depth of 213 m and NQ diameter from 213-354 m measured depth. The core traverses the deep conduit and intrusions of the volcano to a total vertical depth of 290 m b.s. Seawater drilling fluid for boreholes SE-02a and SE-02b was filtered and doubly UV-sterilized at the drill site. No mud products were employed while coring SE-02a, while small amounts of attapulgite mud were used in SE-02b and SE-03. Core samples for geochemical analyses of pore water and microbiological investigations were collected on site from all three boreholes. About 650 m of core was transported by helicopter to Heimaey, 18 km northeast of Surtsey, to a processing laboratory where the core was scanned, documented, and described. Additional core processing has taken place at the Náttúrufraedistofnun Íslands, the Icelandic Institute of Natural History in Gardabaer, where both the 1979 and 2017 cores are stored.
    Language: English
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  • 49
    Publication Date: 2020-02-12
    Description: Length: 32 min What forms the landscapes of the Earth with its mountains, rivers, soils, the places we live in? Is Earth’s surface shaped when rocks are uplifted by geologic forces, and are then destroyed by rain, ice, and wind; or do plants with their roots, animals that dig into soil and the vast number of microorganisms shape the landscapes? Watch the scientists of the German-Chilean “EarthShape” project study these questions along a fascinating landscapes in Chile, and in their home laboratories. A science movie designed and produced by Friedhelm von Blanckenburg from GFZ Potsdam, Germany, Kirstin Übernickel from Universität Tübingen, and Wolfgang Dümcke from Filmbüro Potsdam, Germany, within the DFG-funded research network “EarthShape – Earth Surface Shaping by Biota” which is coordinated by Todd Ehlers (Universität Tübingen) und Friedhelm von Blanckenburg (GFZ Potsdam).
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  • 50
    Publication Date: 2020-05-26
    Description: Deliverable D5.2 presents the experimental outcome of jetting experiments at simulated reservoir conditions. Different rock types are tested under various conditions with the use of three different types of test bench. At first jetting experiments are conducted under submerged conditions in order to derive a better understanding of the governing erosion mechanism. Therefore pitting tests are combined with PIV measurements in order to derive and explain the erosion pattern of the occurring cavitation erosion and why the rock is more like to be eroded by the stagnation pressure of the impinging jet. Second, jetting experiments under pressure controlled conditions are performed. Rate of penetrations (ROP) of up to 100 m/h can be achieved which proofs the successful application of RJD technology especially in sand stone reservoir rock types. Especially the rotating nozzle design bears the highest potential for jetting operations where the static nozzle designs tend to fail, especially when pore pressure increases. The third experimental series under application of a bi- axial stress field show that the current RJD technology, as being used by project partner WSG, is not able to penetrate harder sandstone rock types (e.g. Dortmund sandstone) when field operating conditions are applied. The induced stress in the specimen does not initiate or enhance ROP. A second experiment thereby shows that higher nozzle exit speeds can lead to massive breakouts. Fourth, experiments are performed under a tri-axial stress field in collaboration with TU DELFT. Rock cubes are tested under different and very severely stress regimes while jetting into them. Compared to tests at atmospheric conditions it can be stated that the application of a stress field does not enhance the erosion of rock. At last experiments are conducted with the project partner WSG in order to determine the jetability of the Icelandic Basalt rock type and Icelandic inter basalt sediment layer. The experiments show that already higher pump pressures result in higher jetting performance, hence making them jetable as previously not expected. Furthermore the experiments approved the feasibility of the planned field test in Iceland when the soft sediment layer is the target zone. All in all the experiments conducted with the RJD technology show different results at simulated reservoir conditions compared to those at atmospheric which are described in deliverable D5.1 (Hahn & Wittig, 2017). Therefor, further testing at conditions representing the reservoir conditions more closer are needed in order to better understand and analyze the jetting process downhole.
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  • 51
    Publication Date: 2020-05-27
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  • 52
    Publication Date: 2020-05-26
    Description: In this deliverable, the objectives of the Imperial College team are to consider jetted boreholes in the context of conventional borehole wall-rock stability analysis and to utilise an in-house advanced combined finite-discrete element code to examine the wall-rock failure process for jetted holes. The geomechanical modelling of Lateral Stability in D7.2 presented here is in addition to the main focus on modelling the water-jetting breakdown of the rock itself, reported in D7.1.
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  • 53
    Publication Date: 2020-05-26
    Description: The aim of this research is to investigate the failure mechanism for different types of rock in the context of water jet drilling and to predict the jet-ability or assess the radial jet drilling (RJD) performance prior to drilling and at the well petrophysical analysis stage. The main approach is to numerically simulate the water jet drilling for different types of rock using ICL’s in-house fluid-solid coupling codes. The rock properties, CT-scan data and jetting results obtained from D4.1 (Bakker et al., 2018) and D5.1 (Hahn et al., 2017) provide a good foundation for the related numerical results.
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  • 54
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    GFZ German Research Centre for Geosciences
    In:  Scientific Technical Report STR
    Publication Date: 2020-08-10
    Description: The GEOFON program consists of a global seismic network (GE Network), a seismological data centre (GEOFON DC) and a global earthquake monitoring system (GEOFON EQinfo). These three pillars are part of the MESI research infrastructure of the Helmholtz Centre Potsdam - GFZ German Research Centre for Geosciences aiming at facilitating scientific research. GEOFON provides real-time seismic data, access to its own and third party data from the archive facilities as well as global and rapid earthquake information. The GEOFON Seismological Software can be considered a fourth cross-cutting module of the GEOFON Program. Data, services, products and software openly distributed by GEOFON are used by hundreds of scientists and data centres worldwide. Its earthquake information service is accessed directly by tens of thousands of visitors. The SeisComP software package is the flagship software provided to the community, which is geared for seismic observatory and data centre needs and used extensively to support our internal operations. Like all other MESI (Modular Earth Science Infrastructure) modules GEOFON has the majority of users outside the GFZ as well as an external advisory committee that provides advice to the GFZ Executive Board and to the GEOFON team. This report describes the main activities carried out within the three GEOFON pillars and the software development group.
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  • 55
    facet.materialart.
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    GFZ German Research Centre for Geosciences
    Publication Date: 2020-02-12
    Description: Length: 32 min What forms the landscapes of the Earth with its mountains, rivers, soils, and the places we live in? One view holds that Earth’s surface is shaped when rocks are uplifted by geologic forces, and are then destroyed by rain, ice, and wind that carve landscapes by erosion and weathering. Another view suggests that the green layer of life between rocks below and climate above is the key player. Do plants with their roots, animals that dig into soil and the vast number of microorganisms shape the landscapes? Or do minerals, soil, and water provide the environment for them to live? Or are they both interdependent? Can they together resist the massive climate change imposed by humans today? Watch the scientists of the German-Chilean “EarthShape” project study these questions along a climate gradient in Chile, in the National Parks Pan de Azúcar, La Campana, and Nahuelbuta. Take a tour through fascinating landscapes and see the young scientists study the interactions between geology and biology, from the dry Atacama Desert to dense forests, and in their sophisticated home laboratories. See how feedbacks control Earth’s climate. A science movie designed and produced by Friedhelm von Blanckenburg from GFZ Potsdam, Germany, Kirstin Übernickel from Universität Tübingen, and Wolfgang Dümcke from Filmbüro Potsdam, Germany, within the German National Science Foundation (DFG) funded research network “EarthShape – Earth Surface Shaping by Biota” which is coordinated by Todd Ehlers (Universität Tübingen) und Friedhelm von Blanckenburg (GFZ Potsdam).
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  • 56
    facet.materialart.
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    GFZ German Research Centre for Geosciences
    In:  Scientific Technical Report - STR Data
    Publication Date: 2020-02-12
    Description: There has been growing recognition of the importance of the accurate seismic locations in quantitative seismological studies, such as seismic hazard analyses, fault zone characterization, and Earth's deformation. Accurate estimation of seismic locations is critical since a wrong estimate of the seismic source location will result in wrong interpretations in the subsequent analyses. We present SCOTER, an open-source Python program package that is designed to relocate multiple seismic events by using P- and S-wave station correction terms. The package implements static and shrinking-box source-specific station terms techniques extended to regional and teleseimic distances and adopted for probabilistic, non-linear, global-search location for large-scale multiple-event location. This program provides robust relocation results for seismic event sequences over a wide range of spatial and temporal scales by applying empirical corrections for the biasing effects of 3-D velocity structure. Written in the Python programming language, SCOTER is run as a stand-alone command-line tool (requiring no knowledge of Python) and also provides a set of sub-commands to develop inputs (dataset, configuration etc) and export results (hypocenter parameters, travel-time residuals etc) { routine but non-trivial tasks that can consume much user time. This package can be used for relocation in local, regional, and teleseimic scales. We describe SCOTER's functionality, design and technical implementation, accompanied by an overview of its use cases. As an illustration, we demonstrate the applicability of this tool through two examples based on (1) a catalogue of several hundred events in the Arctic plate boundary region using regional and teleseismic arrival times and (2) a small dataset of low-magnitude seismic events recorded by dense, local stations at the western Iberia, central Portugal. The relocated datasets highlight the future potential for applying the SCOTER relocation tool to greatly improve the relative location accuracy among nearby events.
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  • 57
    Publication Date: 2020-02-12
    Description: Length: 32 min ¿Qué forma los paisajes de la Tierra, con sus montañas, ríos, suelos, los lugares en los que vivimos? ¿Se forma la superficie de la Tierra cuando las rocas son levantadas por fuerzas geológicas, y luego destruidas por la lluvia, el hielo y el viento; o las plantas con sus raíces, los animales que excavan en el suelo y el gran número de microorganismos dan forma a los paisajes? Observe a los científicos del proyecto alemán-chileno "EarthShape" estudiar estas preguntas a lo largo de fascinantes paisajes de Chile, y en sus laboratorios. Una película científica diseñada y producida por Friedhelm von Blanckenburg de GFZ Potsdam, Alemania, Kirstin Übernickel de la Universidad de Tübingen, y Wolfgang Dümcke de Filmbüro Potsdam, Alemania, dentro del consorcio de investigación "EarthShape - Earth Surface Shaping by Biota", financiado por la DFG y coordinado por Todd Ehlers (Universität Tübingen) y Friedhelm von Blanckenburg (GFZ Potsdam).
    Language: Spanish
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  • 58
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    GFZ German Research Centre for Geosciences
    Publication Date: 2020-02-12
    Description: Length: 3 min Watch the fascinating cycle through which plants obtain the mineral nutrients that they need to grow. Plants “eat” mineral nutrients like phosphorous or potassium from the soil and rock that their roots grow in. But this natural resource is limited. To prevent running out of nutrients, hyphae (long thread-like cells of fungi that are attached to roots) recycle phosphorus from falling leaves, and return it to the trees. In dry landscapes plants take up their phosphorus directly from rock. See the fundamental difference of ecosystems in different climates. An animated science movie designed and produced by Friedhelm von Blanckenburg from GFZ Potsdam, Germany, Michaela Dippold from Universität Göttingen, Germany, and Andreas Schulz from Filmbüro Potsdam, Germany within the DFG Project ““EarthShape – Earth Surface Shaping by Biota”.
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  • 59
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    GFZ German Research Centre for Geosciences
    Publication Date: 2020-02-12
    Description: Length: 32 min Was formt die Oberfläche der Erde, auf der wir leben? Ihre Berge, ihre Flüsse, die Täler, die Böden? Ein wissenschaftliches Paradigma besagt, dass Landschaften geformt werden, wenn Gesteine durch geologische Kräfte gehoben werden. Dann werden sie mit Regen, Eis und Wind durch Erosion und Verwitterung wieder zerstört. Doch welche Rolle spielt die grüne Schicht des Lebens, die sich zwischen den nackten Felsen und dem Klima darüber ausbreitet? Gestalten etwa Pflanzen mit ihren Wurzeln und Tiere, die den Boden durchwühlen und die Vielzahl der Mikroorganismen die Landschaft? Oder bestimmen umgekehrt Minerale, Boden und Wasser die Formen des Lebens? Oder sind sie beide voneinander abhängig? Können Biosphäre und Geosphäre gemeinsam dem massiven Klimawandel widerstehen, den der Mensch heute verursacht? Erleben Sie, wie die Wissenschaftler des deutsch-chilenischen Projekts "EarthShape" diese Fragen entlang eines Klimagradienten in Chile, in den Nationalparks Pan de Azúcar, La Campana und Nahuelbuta untersuchen. Wir erleben eine Tour durch faszinierende Landschaften und erleben, wie die jungen Wissenschaftlerinnen die Wechselwirkungen zwischen Geologie und Biologie untersuchen: von der trockenen Atacama-Wüste bis hin zu dichten Regenwäldern; und in hoch-technischen Laboratorien. Sehen Sie, wie Rückkopplungen das Klima der Erde beeinflussen. Dieser Wissenschaftsfilm wurde von Friedhelm von Blanckenburg vom GFZ Potsdam, Kirstin Übernickel von der Universität Tübingen und Wolfgang Dümcke vom Filmbüro Potsdam im Rahmen des von der Deutschen Forschungsgemeinschaft (DFG) geförderten Forschungsnetzwerks "EarthShape - Earth Surface Shaping by Biota" konzipiert und produziert. Das Forschungsnetzwerk wird von Todd Ehlers (Universität Tübingen) und Friedhelm von Blanckenburg (GFZ Potsdam) koordiniert.
    Language: German
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  • 60
    Publication Date: 2020-02-12
    Description: Length: 10 min Was formt die Oberfläche der Erde, auf der wir leben: ihre Berge, ihre Flüsse, die Täler, die Böden? Wird die Erdoberfläche geformt, wenn Gesteine durch geologische Kräfte hochgehoben und dann durch Regen, Eis und Wind zerstört werden oder prägen Pflanzen mit ihren Wurzeln, Tiere, die in den Boden graben, und die große Anzahl von Mikroorganismen die Landschaft? Erleben Sie, wie die Wissenschaftler des deutsch-chilenischen Projekts "EarthShape" diese Fragen entlang einer faszinierenden Landschaft in Chile und in ihren Laboratorien zu Hause untersuchen. Ein Wissenschaftsfilm, der von Friedhelm von Blanckenburg vom GFZ Potsdam, Kirstin Übernickel von der Universität Tübingen und Wolfgang Dümcke vom Filmbüro Potsdam im Rahmen des DFG-geförderten Forschungsnetzwerks "EarthShape - Earth Surface Shaping by Biota" konzipiert und produziert wird. Das Netzwerk wird von Todd Ehlers (Universität Tübingen) und Friedhelm von Blanckenburg (GFZ Potsdam) koordiniert wurde.
    Language: German
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  • 61
    Publication Date: 2020-02-12
    Language: English
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  • 62
    Publication Date: 2020-02-12
    Description: Length: 32 min ¿Qué es lo que forma los paisajes de la Tierra con sus montañas, ríos, suelos, los lugares en los que vivimos? La superficie de la Tierra se forma cuando las rocas son levantadas por fuerzas geológicas, y luego son destruidas por la lluvia, el hielo y el viento que tallan los paisajes por la erosión y la meteorización. Pero hay una capa verde de vida entre las rocas de abajo y el clima de arriba. ¿Las plantas con sus raíces, los animales que excavan en el suelo y el gran número de microorganismos dan forma a los paisajes? ¿O es que los minerales, el suelo y el agua proveen el ambiente para la vida? ¿O ambos son interdependientes? ¿Pueden resistir juntos el cambio climático masivo impuesto por el ser humano hoy en día? Observe a los científicos del proyecto aleman-chileno "EarthShape" estudiando estas preguntas a lo largo de un gradiente climático en Chile, en los Parques Nacionales Pan de Azúcar, La Campana y Nahuelbuta. Recorra por paisajes fascinantes y vea a los jóvenes científicos estudiando las interacciones entre la geología y la biología, desde el desierto seco de Atacama hasta los densos bosques, y en sus sofisticados laboratorios de sus instituciones. Vea cómo las retroalimentaciones controlan el clima de la Tierra.
    Language: Spanish
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  • 63
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    GFZ German Research Centre for Geosciences
    In:  Scientific Technical Report STR - Data | GIPP Experiment- and Data Archive
    Publication Date: 2020-02-12
    Description: Glacial contribution to eustatic sea level rise is currently dominated by loss of the smaller glaciers and ice caps, about 40% of which are tidewater glaciers that lose mass through calving ice bergs. The most recent predictions of glacier contribution to sea level rise over the next century are strongly dependent upon models that are able to project individual glacier mass changes globally and through time. A relatively new promising technique for monitoring glacier calving is through the use of passive seismology. CalvingSEIS aims to produce high temporal resolution, continuous calving records for the glaciers in Kongsfjord, Svalbard, and in particular for the Kronebreen glacier laboratory through innovative, multi-disciplinary monitoring techniques combining fields of seismology and bioacoustics to detect and locate individual calving events autonomously and further to develop methods for the quantification of calving ice volumes directly from the seismic and acoustic signals.
    Language: English
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  • 64
    Publication Date: 2020-02-12
    Language: English
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  • 65
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    GFZ German Research Centre for Geosciences
    Publication Date: 2020-02-12
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  • 66
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    GFZ German Research Centre for Geosciences
    In:  Scientific Technical Report STR - Data
    Publication Date: 2020-02-12
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  • 67
    Publication Date: 2020-02-12
    Language: English
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  • 68
    Publication Date: 2020-02-12
    Description: The Collisional Orogeny in the Scandinavian Caledonides (COSC) scientific drilling project focuses on mountain building processes in a major mid‐Paleozoic orogen in western Scandinavia and its comparison with modern analogues. The project investigates a subduction‐generated complex (Seve Nappes) and how these in part under ultra‐high pressure conditions metamorphosed outer continental margin and continent‐ocean transition zones (COT) assemblages were emplaced onto the Baltoscandian platform and there influenced the underlying allochthons and the basement in a section provided by two fully cored 2.5 km deep drill holes. This operational report concerns the first drill hole, COSC‐1 (ICDP 5054‐1‐A), drilled from early May to late August 2014. It sampled a thick section of the lower part of the Seve Complex and was planned to penetrate its basal thrust zone into the underlying lower grade metamorphosed allochthon. The drill hole reached a depth of 2495.8 m and nearly 100 % core recovery was achieved. Although planning was based on existing geological mapping and new high‐resolution seismic surveys, the drilling resulted in some surprises: the Lower Seve Nappe proved to be composed of rather homogenous gneisses, with only subordinate mafic bodies and its basal thrust zone was unexpectedly thick (〉 800 m). The drill hole did not penetrate the bottom of the thrust zone. However, lower grade metasedimentary rocks were encountered in the lowermost part of the drill hole together with garnetiferous mylonites tens of metres thick. The tectonostratigraphic position is still unclear and geological and geophysical interpretations are under revision. The compact gneisses host only 8 fluid conducting zones of limited transmissivity between 300 m and total depth. Downhole measurements suggest an uncorrected average geothermal gradient of ~20°C/km. The drill core was documented on‐site and XRF scanned off site. During various stages of the drilling, the borehole was documented by comprehensive downhole logging. This operational report provides an overview over the COSC‐1 operations from drilling preparations to the sampling party and describes the available datasets and sample material.
    Language: English
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  • 69
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    GFZ German Research Centre for Geosciences
    Publication Date: 2020-02-12
    Description: Length: 4 min Imagine a planet without plants. Would a landscape on that planet differ from a landscape with plants as we know it? There are two ways to tell: we can either compare natural landscapes with each other, or use computer models. We show one model for a landscape that is covered with a dense forest and one that carries almost no vegetation. Be surprised by the large difference you see in these between these two landforms! An animated science movie designed and produced by Todd Ehlers from the University of Tübingen, Germany, Andreas Schulz from Filmbüro Potsdam, Germany, with contributions of Manuel Schmid Willi Kappler, and Friedhelm von Blanckenburg, Germany within the DFG Project ““EarthShape – Earth Surface Shaping by Biota”.
    Language: English
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  • 70
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    GFZ German Research Centre for Geosciences
    Publication Date: 2020-05-19
    Description: Based on the aviailable material we come to the conclusion that jetting has no direct influence on the surrounding area. Analysis on multiple scales: μm (porosity); cm (mechanical and acoustical properties); dm scale (elastic properties with and without a jetted hole) do not show a significant changes compared to in-tact material, nor can a significant change be detected with respect to distance to a jetted hole. Results fall within the intra-block variability, and differences between blocks can be well explained by block-to-block variation. True-triaxial elastic deformation tests have been designed and ran to test the effect of a lateral (jetted hole) on the elastic properties. The jetted hole itself was jetted with a rotating nozzle type, producing cilindrical holes. Comparing laboratory tests with a numerical model proved that the laboratory results may be well compared to a model with cylindrical hole embedded in a rock mass, much like a conventional borehole. The stress field around the jetted hole can therefore be well aproximated by the Kirsh-equations, modified for compression.
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  • 71
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    GFZ German Research Centre for Geosciences
    Publication Date: 2020-05-19
    Language: English
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  • 72
    Publication Date: 2020-05-19
    Language: English
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  • 73
    Publication Date: 2020-05-26
    Description: Work at GZB (International Geothermal Centre) had been focused on several potential, novel micro type drilling technologies. These technologies have been investigated and discussed to determine possible future options. In this report the different technologies are being presented, starting with abrasive enhanced jetting, followed by pulsation and mechanically supported drilling, ending with percussion type mechanical rock destruction and drilling. Their influence on rock disintegration and drilling efficiency have been investigated in several laboratory experiments. These were carried out to manifest a better understanding of each potential technology. The results are being presented and discussed regarding the potential increase in drilling performance versus lessons learned within WP 5.1 as well as their applicability in the field. Water jets enhanced with abrasive particles have the ability to penetrate into virtually any rock type with rather low hydraulic power. However, the (downhole) applicability in the field is commonly a challenge due to extremely fast and high wear on the pertinent material and equipment other than the rock itself, including the jetting BHA (bottom hole assembly) and nozzles. In order to partly overcome this dilemma a dedicated nozzle for abrasive mixing has been designed and patented. It may be found under patent number DE 10 2016 125 916.0. Pulsating water jets are a different approach to enhance the efficiency of rock destruction via water jet. Both techniques are based on pure high pressure jets, one adding particles to a constant jet (abrasive jetting), the other one dividing and cutting a constant jet into small, short sections to generate not constant impulses (pulsation). Various tests were carried out under reservoir type conditions inside the autoclave system “iBOGS mini”. So far the effect of pulsation seems to be low compared to the suppressed cavitation erosion mechanism under elevated pressure conditions. A very different approach is the use of micro turbines powered by the high pressure water, combined with a mechanical drill bit. The hydraulic energy of the intensified water is not directly used to penetrate the rock, but rather to generate rotation even with substantial torque via a micro turbine system. Thus, the jetting action is neglectable, as the mechanical bit does the cutting into the rock mass with rather high rotation speeds. Testing showed rather high efficiency regarding drilling speed. The technology works also independently of the rock type. All tested rock types including granite were drilled successfully with rather low hydraulic power of 10 kW (e.g. turbine differential pressures of 150 bar and flow rates of about 40 l/min). Future testing at macro and meso scale levels are being planned to verify reliability, drilling direction and more. As of now, this technology seems to be the most promising for hard rock formations in the very near future. One challenge may be their slightly larger geometrical shape and size regarding the current downhole installation scheme. But this is underway to be solved in the near future. On the final end of the possible spectrum for high pressure jet drilling from pure jetting (e.g. SURE WP 5.1 to 5.3) to transforming the intensified, high pressure water to eventually generate and gain more mechanical support over jetting are percussion engines as being known and used in so called DTH (down-the-hole) hammers. Here, the intensified water does generate medium frequency mechanical blows (“pulses”, e.g. 50 – 70 Hz) by powering a piston and drill bit for rock disintegration with very high drilling speeds. The differential pressure across such a hammer with approx. 180 bar is at the same level as for the before mentioned micro turbines and thus, much lower than for direct high pressure water jetting. Compared to the turbine, the hammer works with a highly dynamic force and low rotation, whereas the turbine is based on a very constant load or weight on bit (WOB) with rather high rotation speed (RPM), generating more of a grinding effect. However, the hammer ́s geometrical shape, namely its length, makes it much more difficult to be deployed downhole for micro drilling, while also some rotation needs to be generated. Here is more work underway as well. To summarize high pressure jet drilling, the full scale of currently possible solutions from pure high pressure jetting to mechanically enhanced or supported jet type drilling including abrasives, pulsation, micro turbines and percussion motors were considered and being looked at regarding their possible application in hard rock formations and future potential.
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  • 74
    Publication Date: 2020-05-27
    Description: Radial Jet Drilling (RJD) is a technique to stimulate wells by creating small-diameter laterals from vertical or deviated wells using hydraulic jets. The laterals, also called radials, can be up to 100 m in length. To analyze under which sub-surface conditions the radials improve the well performance most, a step-wise approach is followed in which first the performance of a single stimulated well is analyzed and in a second step, the performance of a doublet system is analyzed. Finally, case studies that are more detailed are simulated. For the single well case, a good first estimate of radial stimulation performance for different reservoir conditions can be obtained from (semi-) analytical solutions. These results show that the anisotropy in the permeability and the thickness of the reservoir influence the relative increase in productivity/injectivity most. The permeability influences in particular the absolute performance of the stimulated well. Many aspects not included in the semi-analytical solution also influence the performance of the radial stimulation: - Since the radials are open hole, stability for friable rocks or deep reservoirs is unlikely. This depends on the in-situ stress conditions. Collapsed radials probably have much lower performance or no effect at all. - The uncertainty in the radial path and diameter decreases the expected benefits from radials significantly depending on the type of reservoir. For example for a layered reservoir, the expected increase may be tens of percent lower. - Due to the small diameter (0.02-0.05 m) and rough surface of the radials and the high rates of geothermal wells, viscous pressure drop due to flow in the radials has to be taken into account for prediction of performance. For example for a radius of 0.04 m and well rate of 3600 m3/d, expected increase in performance is halved when taking into account pressure drop. - Heterogeneity in the permeability has a strong impact on the performance of the radials. Performance of individual radials depends in first approximation on the local permeability. However, this is difficult to capture in general terms. - Near well bore damage (positive skin) and prior stimulation (negative skin) have a large impact on the expected increase due to stimulation. In case the radials can be used to by-pass near well damage, performance can be much higher than predicted using the analytical equations. - Heterogeneity due to fault and/or fractures, voids, sharp transitions or layering all make potential success more uncertain and predictability lower due to potential issues with jetting. Whether increased performance for a single well can be translated to similar increased performance of a doublet depends on the doublet settings and subsurface conditions. For a fixed doublet distance or field size, an increase in rate due to improved performance of the wells will result in a reduced field life. The increased well performance can also be used to lower pumping cost at a fixed rate and thus improve performance of the doublet. It was found, that for most subsurface systems, the impact of the radials on production temperature was minor (for constant rate). Only for some fractured systems, short-circuiting can be increased due to radials. Overall, the ideal candidate for radial stimulation is a reservoir which is not too deep, in homogeneous, competent rock with a well with near well bore damage or in a not too deep anisotropic reservoir in which the main well is not drilled beneficially compared to the main direction of permeability.
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  • 75
    Publication Date: 2020-05-26
    Description: This report describes activity connected to radial jet drilling (RJD) in Iceland in WP6 – Macro Scale in the SURE project. Well HN-13, located in N-Iceland close to the town of Akureyri was selected as a candidate for RJD trials within the SURE project. It was drilled in between two prior drilled low-temperature geothermal wells, HG-10 (a.k.a. HN-10) and BO-01 (a.k.a. BN-01), that are both productive and used for district heating of Akureyri and nearby communities. Although the location was in between two producing wells, it was a poor producer only producing 5-6 liters per minute (0,1 l/s) while being air lifted. For comparison, the mean production from well HG-10 that sits 20 m NNE of HN-13, is about 25 l/s of 90°C hot water. HN-13 was therefore valued as an excellent candidate for demonstration of the stimulation technology, as any increased production after RJD will clearly be revealed. Jetting experiments in WP5 into basalt rock types sent from Iceland to Bochum were shown to be impractical as high pressure and velocities are required. Therefore, softer inter-basaltic layers were targeted. Main information on well HN-13, nearby wells, target depth as well as the RJD field testing are described in this report.
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  • 76
    Publication Date: 2020-05-28
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  • 77
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    GFZ German Research Centre for Geosciences
    In:  Scientific Technical Report STR - Data | GIPP Experiment and Data Archive
    Publication Date: 2020-05-20
    Description: This report describes the passive seismic data acquired by the TOPASE network deployed over Rittershoffen geothermal field (Alsace, France). The monitoring period extends from March 2013 to November 2014, which includes the stimulation of the first well of the doublet, the drilling of the second well and well tests. These data were acquired using 31 Earth Data Loggers PR6-24 and MARK-SERCEL L-4C-3D 1 Hz seismometers of the Geophysical Instrument Pool Potsdam (GIPP), which were provided to the KIT-AGW-Geothermal research division.
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  • 78
    Publication Date: 2020-05-19
    Description: To date, information about the wellbore integrity of high temperature and high pressure geothermal wells is scarce. Hardly any measurement data is available about the thermal and mechanical load onto the subsurface installation (casing and cemented annulus) during the operation of such wells. In order to monitor the response of the subsurface installation to changing load conditions, a fiber optic cable was installed behind casing of a geothermal well. To increase the knowledge about the wellbore integrity and to benefit from the combined application of different fiber optic sensing technologies, temperature, strain as well as acoustic noise measurements were performed during well completion and testing. These include the distributed temperature sensing (DTS) technology, based on Raman scattering, as well as the distributed strain and distributed acoustic sensing (DAS) technologies, both based on Rayleigh scattering. Here, we present information about the laboratory experiments, the cable installations and downhole measurement campaigns together with results of our analysis. It could be shown that the fiber optic measurements are well suited to monitor the well completion procedures. In addition, the technology offers a possibility to monitor well integrity throughout the lifetime of a geothermal well.
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  • 79
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    GFZ German Research Centre for Geosciences
    In:  Scientific Technical Report
    Publication Date: 2020-05-22
    Description: This study contributes to the effort of space geodesy to reach the 1mm accuracy level on a global scale. This stringent requirement is vital to realize a global reference system upon which phenomena such as sea-level rise can be reliably monitored. The study deals with two interrelated challenges: modeling geophysical loads imposed on the crust of the Earth and quantifying the atmospheric propagation delay of signals employed by space geodetic techniques, namely VLBI, SLR, GNSS, and DORIS. If not adequately modeled, both geophysical loading and propagation delay corrupt space geodetic data analysis results, thus distorting the implied reference frame and compromising the physical interpretation of other parameters. The explicit purpose of this work is to understand how these effects propagate into the parameters estimated within the geodetic adjustment, and to develop models that alleviate geodetic results from these effects. To achieve this goal, the scientific framework was divided into two contributions to be understood and enhanced: the theory governing the effects of geophysical loading and atmospheric propagation, and the space geodetic technique data analysis pipeline, largely using VLBI as a test-bed. In essence, the research conducted here includes: (i) the development of software capable of realistically simulating VLBI, SLR, GNSS, and DORIS observations within a Monte Carlo framework, (ii) the homogenization of in situ meteorological data recorded at VLBI and SLR stations, (iii) the development of ray-traced delays, mapping functions and higher-order gradients for all four space geodetic techniques, (iv) the comprehensive investigation of inter-frequency and inter-system atmospheric ties, (v) the development of models to describe the displacement induced by mass redistribution within Earth’s fluid envelope including the atmosphere, the ocean, and the continental hydrology, (vi) the development of empirical models to describe the signal propagation delay (GFZ-PT) and the non-tidal geophysical loading displacement (EGLM), and (vii) the study of the impact of the atmospheric refraction and non-tidal geophysical loading models in space geodetic data analysis on station coordinates, the terrestrial reference frame, the Earth orientation, and the integrated water vapour trends. A number of developments were carried out herein for the first time, for example, the simulation of space geodetic measurements based on ray-traced delays, the study of systematic errors on the reference frame induced by not properly accounting for the orbital altitude of the satellites in the calculation of atmospheric refraction corrections, and the assessment of the probability of successful laser ranges based on integrated cloud fraction along the ray path. It was found that microwave and optical atmospheric gradients are starkly different both spatially and temporally, and cannot be scaled to fit each other. Failing to account for non-tidal geophysical loading and atmospheric asymmetries induces a scale bias in the SLR reference frame as well as a spurious geocenter motion predominantly along the Z-axis. Employing a VLBI-tailored atmospheric refraction model to reduce DORIS observations displaces stations in the radial component thus inducing a large scale bias in the implied frame. Employing homogeneous in lieu of raw meteorological data in VLBI data analysis reduces the scatter of station coordinates and improves the baseline length repeatability. Employing the mapping functions developed herein in lieu of VMF1 yields an overall improvement in VLBI data analysis. Applying the geophysical loading models developed herein reduces the response of almost all station coordinate and baseline length series at seasonal and synoptic timescales. Based on the investigations carried out herein, differences in Earth orientation induced by the quality of the atmospheric refraction and geophysical loading models — or their very application for the latter — are not statistically significant in the framework of the modern VLBI system. Nevertheless, to fulfill the 1mm requirement, proper treatment of geophysical loading and atmospheric refraction is a necessity.
    Language: English
    Type: info:eu-repo/semantics/doctoralThesis
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  • 80
    Publication Date: 2020-05-22
    Description: The Collisional Orogeny in the Scandinavian Caledonides (COSC) project supported by the International Continental Scientific Drilling Program (ICDP) and the Swedish Scientific Drilling Program (SSDP) drilled a borehole through the Seve Nappe in Sweden to investigate mountain building processes. It recovered 2.5 km of drill core. Five core samples from the depth from 1682 to 2469 m were analyzed in this thesis. A hyperspectral imaging spectrometer (HySpex) was used to conduct the measurements. It is a two sensor system which combines a VNIR and a SWIR sensor. The measurements were taken with a resolution of 0.22 mm/ pixel. As a comparison, mineral maps based on Laser Induced Breakdown Spectroscopy (LIBS) element measurements of approximately the same resolution were used. This thesis developed a working process chain which includes 1) the adjustment of the measurement parameters of the sensors to acquire optimal data cubes, 2) the "unrolling" of a drill core to depict and analyze the whole core mantle surface and to map the distribution of minerals accurately not only over the length but also the whole surface of the core and 3) the mineral mapping based on spectral absorption features with the EnGeoMap algorithm. This can be seen as the beginning of the development of a stand-alone drill core scanner including the geological evaluation by EnGeoMap. The measurements revealed a basic approach to determine the integration time for the VNIR and the SWIR sensor based on the signal-to-noise ratio of the white reflectance standard. An approach of a step-wise rotation of the core and a translation measurement and a mosaicking based on the rectification of the core surface was developed. The stitching of several core images via key points was deployed. The duration of the unrolling amounts to 22 h/ m of core and results in an hyperspectral mosaic of the core mantle surface. Relative to the approximately 550 h needed to measure the surface area of 1 m of core with the LIBS system, 22 h seems tolerable. The feasibility of the unrolling and the mosaicking of drill cores varies. In scientific operations the accuracy is valued higher than the time-consumption, in industrial operations the time is a big factor to make a project profitable. The mineral mapping with EnGeoMap proved to be very precise in case of detecting the abundance of single minerals. When mapping multiple minerals, a bias towards a few minerals showed which were mapped with higher abundances than in reality. This is due to mineral-dependent fit value thresholds and has to be investigated further. When choosing few but distinct proxy minerals, EnGeoMap is a valuable tool to evaluate the mineral abundances and the distribution over the course of a drill core, to highlight changes and to give information about mineral assemblages.
    Language: English
    Type: info:eu-repo/semantics/masterThesis
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  • 81
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    GFZ German Research Centre for Geosciences
    In:  Scientific Technical Report
    Publication Date: 2020-05-22
    Description: The spectral characteristics of Rare Earth Elements (REEs) have been poorly researched although the economic interest in these elements is increasing. This study investigates the detection of REEs using remote sensing data. For this purpose the spectral response of each individual REE has been studied with four spectrometers (HySpex (VNIR-1600, SWIR-320m-e), ASD Field Spec 3, Perkin Elmer LAMBDA 950, FTIR Spectrum GX) using a spectral range of 350 to 16000 nm to incorporate different techniques. The relationship between the spectral response and the REE concentration as well as the influence of other materials on the detection of REEs was examined using mixtures of calcium carbonate (the main component of REE ore rocks) and iron (III) oxide (hematite). Finally, characteristic absorption bands have been employed on an EO-1 Hyperion satellite image, covering the REE Mountain Pass mine in California and a HySpex image of a rock sample from Norway (soevite) to evaluate their potential use as REE detectors. The results show that the REEs lanthanum, neodymium, samarium, europium, terbium, dysprosium, holmium, erbium, thulium and ytterbium cause several and differing absorption features in the visible near-infrared (VNIR) and shortwave-infrared (SWIR) region. However, in wavelength ranges between 2500 and 16000 nm no absorption bands distinctive of REEs appeared. In most cases, the concentration of REEs and the absorption depth show a logarithmic relationship for different absorption features. The mixtures of neodymium and iron (III) oxide show that in presence of hematite the absorption features of neodymium are superimposed by those features caused by iron (III) oxide. In comparison to hematite, calcium carbonate has had no influence on the detection of neodymium in the VNIR. The application of characteristic absorption bands on the satellite image shows that the REE signal causes only, if any, very small absorption bands in the spectrum at higher REE concentrations. In the rock sample, however, REEs related absorption bands are detectable and can be seen clearly in the spectrum with a neodymium concentration of around 0.14%. This study shows that imaging spectroscopy serves as a helpful tool for the characterization and detection of REE concentrations in the laboratory and field environment. The detection of REEs via satellite images is limited by the low intensity of the absorption features, despite the high REEs concentration. Nevertheless, the detection of REEs by means of remote sensing is a non-invasive method that saves both money and time for sample preparation, underlining its economic value.
    Language: English
    Type: info:eu-repo/semantics/masterThesis
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  • 82
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    GFZ German Research Centre for Geosciences
    In:  Scientific Technical Report STR
    Publication Date: 2020-08-10
    Description: The GEOFON program consists of a global seismic network (GE Network), a seismological data centre (GEOFON DC) and a global earthquake monitoring system (GEOFON EQinfo). These three pillars are part of the MESI research infrastructure of the Helmholtz Centre Potsdam - GFZ German Research Centre for Geosciences aiming at facilitating scientific research. GEOFON provides real-time seismic data, access to its own and third party data from the archive facilities as well as global and rapid earthquake information. The GEOFON Seismological Software can be considered a fourth cross-cutting module of the GEOFON Program. Data, services, products and software openly distributed by GEOFON are used by hundreds of scientists and data centres worldwide. Its earthquake information service is accessed directly by tens of thousands of visitors. The SeisComP software package is the flagship software provided to the community, which is geared for seismic observatory and data centre needs and used extensively to support our internal operations. Like all other MESI (Modular Earth Science Infrastructure) modules GEOFON has the majority of users outside the GFZ as well as an external advisory committee that provides advice to the GFZ Executive Board and to the GEOFON team. This report describes the main activities carried out within the three GEOFON pillars and the software development group.
    Language: English
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  • 83
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    GFZ German Research Centre for Geosciences
    Publication Date: 2020-12-17
    Description: In geosciences 3D geomechanical-numerical models are used to estimate the in-situ stress state. In such a model each geological unit is populated with the rock properties Young’s module, Poisson ratio, and density. Usually, each unit is assigned a single set of homogeneous properties. However, variable rock properties are observed and expected within the same geological unit. Even in small volumes large variabilities may. The Python script HIPSTER (Homogeneous to Inhomogeneous rock Properties for Stress TEnsor Research) provides an algorithm to include inhomogeneities in geomechanical-numerical models that use the solver Abaqus®. The user specifies the mean values for the rock properties Young's module, Poisson ratio and density, and their variability for each geological unit. The variability of the material properties is individually defined for each of the three rock properties in each geological layer. For each unit HIPSTER generates a normal or uniform distribution for each rock property. From these distri-butions for each single element HIPSTER draws individual rock properties and writes them to a separate material file. This file defines different material properties for each element. The file is included in the geomechanical-numerical analysis solver deck and the numerical model is solved as usual.
    Language: English
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  • 84
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    GFZ German Research Centre for Geosciences
    In:  WSM Technical Report
    Publication Date: 2021-04-10
    Description: In geosciences the discretization of complex 3D model volumes into finite elements can be a time-consuming task and often needs experience with a professional software. Es-pecially outcropping or out-pinching geological units, i.e. geological layers that are rep-resented in the model volume, pose serious challenges. Changes in the geometry of a model may occur well into a project at a point, when re-meshing is not an option any-more or would involve a significant amount of additional time to invest. In order to speed up and automate the process of discretization, Apple PY (Automatic Portioning Preventing Lengthy manual Element assignment for PYthon) separates the process of mesh-generation and unit assignment. It requires an existing uniform mesh together with separate information on the depths of the interfaces between geological units (herein called horizons). These two pieces of information are combined and used to assign the individual elements to different units. The uniform mesh is created with a standard meshing software and contains no or only very few and simple structures. The mesh has to be available as an Abaqus input file. The information on the horizons depths and lateral variations in the depths is provided in a text file. Apple PY compares the ele-ment location and depth with that of the horizons in order to assign each element to a corresponding geological unit below or above a certain horizon.
    Language: English
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  • 85
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    GFZ German Research Centre for Geosciences
    In:  WSM Technical Report
    Publication Date: 2021-04-10
    Description: The distribution of data records for the maximum horizontal stress orientation SHmax in the Earth’s crust is sparse and very unequally. To analyse the stress pattern and its wavelength and to predict the mean SHmax orientation on regular grids, statistical interpolation as conducted e.g. by Coblentz and Richardson (1995), Müller et al. (2003), Heidbach and Höhne (2008), Heidbach et al. (2010) or Reiter et al. (2014) is necessary. Based on their work we wrote the Matlab® script Stress2Grid that provides several features to analyse the mean SHmax pattern. The script facilitates and speeds up this analysis and extends the functionality compared to the publications mentioned before. This script is the update of Stress2Grid v1.0 (Ziegler and Heidbach, 2017). It provides two different concepts to calculate the mean SHmax orientation on regular grids. The first is using a fixed search radius around the grid points and computes the mean SHmax orientation if sufficient data records are within the search radius. The larger the search radius the larger is the filtered wavelength of the stress pattern. The second approach is using variable search radii and determines the search radius for which the standard deviation of the mean SHmax orientation is below a given threshold. This approach delivers mean SHmax orientations with a user-defined degree of reliability. It resolves local stress perturbations and is not available in areas with conflicting information that result in a large standard deviation. Furthermore, the script can also estimate the deviation between plate motion direction and the mean SHmax orientation.
    Language: English
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  • 86
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    GFZ German Research Centre for Geosciences
    In:  Scientific Technical Report STR
    Publication Date: 2021-03-28
    Description: The MT repository contains geophysical data sets collected in field experiments from all over the world. The acronym MT stands for magnetotelluric, a geophysical method used to probe the Earth's deep interior for its electrical conductivity distribution through electromagnetic (EM) induction. MT is based on EM fields generated by natural processes in the Earth's atmosphere and magnetosphere. But the repository also contains data from Controlled Source Electromagnetic (CSEM) projects, for which man-made EM sources are used. The principle form of data in the repository are time-series of EM field components acquired with heterogeneous sets of sensors, recording instruments, and sampling rates. It is the main purpose of this archive or repository to provide the links between the data and their physical meaning by means of metadata. To achieve this, the repository is organized as a combination of data files and associated meta-data in a well defined folder (directory) structure, with the data files being sorted into subfolders. Meta-data are provided as XML (Extensible Markup Language) formatted file.
    Language: English
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  • 87
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    GFZ German Research Centre for Geosciences
    In:  WSM Technical Report
    Publication Date: 2023-01-31
    Description: In geosciences 3D geomechanical-numerical models are used to estimate the in-situ stress state. In such a model each geological unit is populated with the rock properties Young’s module, Poisson ratio, and density. Usually, each unit is assigned a single set of homogeneous properties. However, variable rock properties are observed and expected within the same geological unit. Even in small volumes large variabilities may. The Python script HIPSTER (Homogeneous to Inhomogeneous rock Properties for Stress TEnsor Research) provides an algorithm to include inhomogeneities in geomechanical-numerical models that use the solver Abaqus®. The user specifies the mean values for the rock properties Young's module, Poisson ratio and density, and their variability for each geological unit. The variability of the material properties is individually defined for each of the three rock properties in each geological layer. For each unit HIPSTER generates a normal or uniform distribution for each rock property. From these distributions for each single element HIPSTER draws individual rock properties and writes them to a separate material file. This file defines different material properties for each element. The file is included in the geomechanical-numerical analysis solver deck and the numerical model is solved as usual. The HIPSTER script files and example files are provided for download at http://github.com/MorZieg/hipster. Table 0-1 Structure of the GitHub repository gives an overview of the repository and files including a short explanation.
    Language: English
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  • 88
    Publication Date: 2018-11-19
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: Spanish
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  • 89
    Publication Date: 2018-11-19
    Keywords: ddc:380
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: German
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  • 90
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2014-08-15
    Keywords: ddc:330
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: German
    Type: contributiontoperiodical , doc-type:contributionToPeriodical
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  • 91
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:380
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 92
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: German
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  • 93
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    Chur : Rüegger | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2014-08-15
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: German
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  • 94
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:380
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: German
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  • 95
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: German
    Type: contributiontoperiodical , doc-type:contributionToPeriodical
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  • 96
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 97
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    Köln/Wuppertal : Die Grünen | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: German
    Type: report , doc-type:report
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  • 98
    Publication Date: 2018-04-18
    Keywords: ddc:330
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: German
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  • 99
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    Wuppertal : Wuppertal Institute for Climate, Environment and Energy | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
    Type: report , doc-type:report
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  • 100
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: German
    Type: contributiontoperiodical , doc-type:contributionToPeriodical
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