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  • Other Sources  (33)
  • 551.4  (33)
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  • 2010-2014  (33)
  • 1990-1994
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  • 2010  (33)
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  • Other Sources  (33)
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  • 2010-2014  (33)
  • 1990-1994
  • 1965-1969
  • 1930-1934
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  • 2010  (33)
  • 1991
  • 1990
  • 1967
  • 1931
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  • 1
    Publication Date: 2021-03-29
    Description: report
    Keywords: 551.4 ; 550
    Language: English
    Type: article , publishedVersion
    Format: 113 S.
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  • 2
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    IFM-Geomar, Kiel
    Publication Date: 2021-03-29
    Description: report
    Keywords: 551.4 ; 551.22 ; 550
    Language: English
    Type: article , publishedVersion
    Format: 193 S.
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  • 3
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    IFM-GEOMAR, Kiel
    Publication Date: 2021-03-29
    Description: report
    Keywords: 551.4 ; 550 ; TSZ 300 ; Pazifischer Ozean {Geophysik}
    Language: English
    Type: article , publishedVersion
    Format: 229 S.
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  • 4
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    IFM-GEOMAR, Kiel
    Publication Date: 2021-03-29
    Description: report
    Keywords: 551.4 ; 550
    Language: English
    Type: article , publishedVersion
    Format: 159 S.
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  • 5
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    Geologisches Institut 〈Freiberg〉
    Publication Date: 2021-03-29
    Description: research
    Keywords: 551.4 ; UBF 000 ; VJA 310 ; VBD 000 ; UBG 320 ; Unterirdische Gewässer insgesamt {Hydrologie} ; Statistische Auswertung {Geochemie} ; Mathematische und Statistische Geologie ; Methoden, Meßsysteme {Hydrologie, Unterirdische Gewässer} ; hydrogeology ; hydrochemistry ; hydrogeochemistry ; data analysis ; data processing ; statistical analysis ; mathematical methods
    Language: English
    Type: article , publishedVersion
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  • 6
    Publication Date: 2021-03-29
    Description: The present work deals with two challenging problems of applied geostatistics: (i) Stationarity assumptions often do not hold under real-world conditions. (ii) Geostatistical methods have to be linked with spatial databases in order to be applicable in non-stationary situations. Solutions for both problems are proposed and implemented. (i) A central assumption in geostatistics is the stationarity of the process. However the spatial variability of many natural phenomena heavily depends on the local geology, which is nonstationary in most cases. To deal with this, the concept of process stationarity is replaced by a stationarity of the governing influence relating the local semivariogram and the local geology as stored in a Geographical Information System (GIS). A construction method is used, which can meaningfully incorporate additional spatial information from GIS, e.g. smoothly varying geology in the investigated area, spatially varying anisotropy induced by mountainous morphology, or geological faults interrupting continuity. Least-squares parameter estimation is used for fitting instationary semivariogram models in typical example situations, leading to non-linear optimization problems. Furthermore, a method for semivariogram parameter estimation in the present of linear trend is proposed. (ii) Geostatistical tools that make use of the local geology need direct access to the data stored in the GIS. A link between the presented geostatistical tools and the GIS software ArcView was established. Thus, spatial data such as measured contaminant concentrations, soil properties and morphology can be incorporated in geostatistical analyses. R code that fits instationary semivariogram models and performs kriging was implemented and can be obtained from the author. It is applied to simulated datasets.
    Description: Die vorliegende Diplomarbeit befasst sich mit zwei wichtigen Problemen der angewandten Geostatistik: (i) Stationaritätsannahmen werden unter realweltlichen Bedingungen oft nicht erfüllt. (ii) Geostatistische Methoden müssen mit räumlichen Datenbanken verbunden werden, um unter nichtstationären Bedingungen anwendbar zu sein. Lösungen für beide Probleme werden vorgeschlagen und implementiert. (i) In der Geostatistik ist die Stationarität des Prozesses eine zentrale Annahme. Die räumliche Variabilität vieler Phänomene in unserer Umwelt hängt jedoch stark von lokalen geologischen Verhältnissen ab, die meist aber instationär sind. Um damit umgehen zu können, wird das Konzept der Stationarität des Prozesses ersetzt durch eine Stationarität des Einflusses der lokalen Geologie, wie sie in einem GIS gespeichert ist, auf das lokale Semivariogramm. Es wird eine Konstruktionsmethode benutzt, die auf sinnvolle Art räumliche Informationen aus dem GIS in Semivariogrammmodelle einbinden kann, etwa sich über das Untersuchungsgebiet gleichmäßig verändernde geologische Verhältnisse, sich räumlich verändernde Anisotropie im Gebirgsrelief oder geologische Störungen, die die Kontinuität unterbrechen. Kleinste-Quadrate Schätzung wird für die Anpassung instationärer Semivariogrammmodelle in typischen Beispielsituationen verwendet. Dies führt zu nichtlinearen Optimierungsproblemen. Des weiteren wird eine Methode der Schätzung von Semivariogrammparametern in Modellen mit linearem Trend vorgestellt. (ii) Geostatistische Werkzeuge, die lokalen geologischen Verh¨ältnisse berücksichtigen, benötigen einen direkten Zugang zu Daten, die in einem GIS gespeichert sind. Im Rahmen dieser Arbeit wurde eine Verbindung zwischen den vorgestellten geostatistischen Werkzeugen und dem GIS Programm ArcView erstellt. Auf diese Weise können räumliche Daten wie etwa Schadstoffkonzentrationen, Bodeneigenschaften oder die Morphologie in geostatistische Analysen einbezogen werden. R-Code, der instationäre Semivariogrammmodelle anpasst und Kriging durchführt, wurde erstellt und auf simulierte Datensätze angewandt. Der Code kann über den Author bezogen werden.
    Description: research
    Keywords: 551.4 ; QBD 700 ; QBK 000 ; VJA 310 ; VBD 000 ; VJA 100 ; VKB 311 ; QFC 430 ; Geoinformationssysteme {Geographie} ; Mathematische Geographie ; Statistische Auswertung {Geochemie} ; Mathematische und Statistische Geologie ; Probennahme, Probenaufbereitung {Geochemie} ; Untersuchungsmethoden und Probennahme im Gelände {Sedimentologie} ; Methoden und Techniken der Umweltforschung {Angewandte Geographie} ; geographic information systems ; geostatistics ; combination ; spatial distribution ; sampling
    Language: English
    Type: article , publishedVersion , publishedVersion
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  • 7
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    Institut für Geologie 〈Freiberg〉
    Publication Date: 2021-03-29
    Description: Deutsche Forschungsgemeinschaft
    Description: research
    Keywords: 551.4 ; VJC 000 ; VQ 600 ; VJF 000 ; Aquatische Geochemie ; Grenzgebiete. Beziehungen. Einflüsse. Wirkungen. {Lagerstättenkunde} ; Umweltgeochemie insgesamt ; uranium ; geochemistry ; hydrochemistry ; hydrogeochemistry ; physicochemical properties ; isotope fractionation ; isotope fractionation ; spectroscopy
    Language: English
    Type: article , publishedVersion
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  • 8
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    Geologisches Institut 〈Freiberg〉
    Publication Date: 2021-03-29
    Description: Lake Urema is one of the most important ecological features of the Gorongosa National Park, Central Mozambique. It is located in the Urema Rift which is a part of the East African Rift System. The understanding of the geo-ecology of the lake and its tributaries is particularly important for the conservation of its floodplain habitats. There are recent concerns that the lake has changed during the last years. A multi-temporal and multi-disciplinary approach was applied to investigate the dynamics and control mechanisms of the lake. Principal methods adopted were: remote sensing analyses of time series of Landsat and ASTER data, geomorphological interpretations of SRTM (Shuttle Radar Topography Mission) data as well as field investigations such as water and sediment analyses and vegetation mapping. The study showed that the water of Lake Urema and its in- and outflow has very low concentrations of total dissolved solids (TDS) between 20 to 100 mg/l. The pH is on average about 7, regulated by a CO2 - HCO3 —- CO3 2_ buffering system. The water transparency is very low, mostly less than half a meter. During the period of investigation no outflow of the lake was observed, but the Vunduzi River, one of the tributaries to Lake Urema, had a considerable discharge. A decrease of the lake level height was detected over a period of two months. In addition to the evaporation from the open water surface of the lake, water is probably also lost through spreading into the adjacent floodplain grasslands, through evapotranspiration as well as through infiltration. A significant enrichment of the water constituents in the dry season did obviously not occur. The widespread distribution of clayey sediments over large parts of the lake and the evidence of sandy sediments in the narrowing part of the lake towards its outflow suggest a temporally and spatially constrained pattern of transport and deposition. It is supposed that the axial part of the lake is characterized by a more energetic flow and the lateral areas by quiescent conditions. The results of the supervised classification of the satellite images from 1979 to 2000 did not indicate a trend for the variations of the lake's size. The area of Lake Urema ranged from 17.4 km² (09/1995) to 25.1 km² (08/1979). A rainfall anomaly was responsible for the outstanding lake size in May 1997. Investigations showed that alluvial fans limit the Urema Basin from all sides and make Lake Urema a kind of “reservoir lake”. Further studies should focus on the enlightenment of the water balance of the lake system. Especially the contribution of groundwater to the water balance of the lake is not yet understood.
    Description: Deutscher Akademischer Austauschdienst
    Description: research
    Keywords: 551.4 ; UBE 700 ; UD 330 ; UBO 600 ; UBE 400 ; UBE 500 ; UBE 600 ; Typologie von Seen {Hydrologie} ; Tropische und subtropische Zone {Hydrologie} ; Wasserhaushalt einzelner Regionen {Hydrologie} ; Eigenschaften des Seewassers {Hydrologie, Seen} ; Ökologie von Seen {Hydrologie} ; Morphologie und Geologie von Seen {Hydrologie} ; Mozambique ; East African Rift ; East African Lakes ; limnology ; lakes ; hydrochemistry ; ecology ; water balance
    Language: English
    Type: monograph , publishedVersion , monograph
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  • 9
    Publication Date: 2021-03-29
    Description: report
    Keywords: 551.4 ; 551 ; 550 ; VAT 300 ; VEZ 300 ; TSZ 300 ; Geologie des Meeresboden ; Pazifischer Ozean {Geologie} ; Pazifischer Ozean {Geophysik}
    Language: English
    Type: article , publishedVersion
    Format: 190 S.
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  • 10
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    Institut für Geologie 〈Freiberg〉
    Publication Date: 2021-03-29
    Description: research
    Keywords: 551.4 ; VBQ 900 ; UD 340 ; UBG 200 ; UBG 600 ; UBG 300 ; VEI 400 ; Hydrogeologie einzelner Regionen ; Aride und semiaride Zone {Hydrologie} ; Grundwasserbildung {Hydrologie, Unterirdische Gewässer} ; Grundwasserhaushalt {Hydrologie, Unterirdische Gewässer} ; Grundwassereigenschaften {Hydrologie, Unterirdische Gewässer} ; Israel, Palästina {Geologie} ; Jordan ; ground water ; recharge ; hydrogeology ; hydrogeochemistry ; PHREEQE
    Language: English
    Type: article
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