High-resolution aquifer analog of fluvial–aeolian sediments of the Guarani aquifer system
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  • 作者:Dominik H?yng (1)
    Fernando Mazo D’Affonseca (1) (2)
    Peter Bayer (3)
    Edson Gomes de Oliveira (4)
    José Alexandre J. Perinotto (4)
    Fábio Reis (4)
    Holger Wei? (5)
    Peter Grathwohl (1)
  • 关键词:Groundwater reservoir analog model ; Guarani aquifer ; Reservoir characterization ; Fluvial–aeolian sediments ; Pirambóia Formation
  • 刊名:Environmental Earth Sciences
  • 出版年:2014
  • 出版时间:April 2014
  • 年:2014
  • 卷:71
  • 期:7
  • 页码:3081-3094
  • 全文大小:2,804 KB
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  • 作者单位:Dominik H?yng (1)
    Fernando Mazo D’Affonseca (1) (2)
    Peter Bayer (3)
    Edson Gomes de Oliveira (4)
    José Alexandre J. Perinotto (4)
    Fábio Reis (4)
    Holger Wei? (5)
    Peter Grathwohl (1)

    1. University of Tübingen, Center for Applied Geosciences, H?lderlinstr. 12, 72074, Tübingen, Germany
    2. TIMGEO GmbH, H?lderlinstr. 29, 72074, Tübingen, Germany
    3. Geological Institute, ETH Zurich, Sonneggstr. 5, 8092, Zurich, Switzerland
    4. Instituto de Geociências e Ciências Exatas, UNESP, Univ. Estadual Paulista, Av. 24-A n° 1515 -B. Bela Vista, 13506-900, Rio Claro, SP, Brazil
    5. Helmholtz Center for Environmental Research (UFZ), Permoserstr. 15, 04318, Leipzig, Germany
  • ISSN:1866-6299
文摘
The Guarani aquifer system (GAS) represents one of the biggest aquifers in the world and is the most relevant groundwater resource in South America. For the first time, by combining field and laboratory measurements, a high-resolution aquifer analog model of fluvial–aeolian sediments of the GAS in S?o Paulo State (Brazil) is constructed. Three parallel sections of frontal outcrops, 28?m?×?5.8?m, and two parallel sections of lateral outcrops, 7?m?×?5.8?m, are recorded during open-pit mining of sandy sediments and describe in detail the three-dimensional distribution of the local lithofacies and hydrofacies. Variations of hydraulic conductivity, K, and porosity, n, are resolved on the centimeter scale, and the most permeable units of the fluvial–aeolian facies association are identified. The constructed aquifer analog model shows moderate hydraulic heterogeneity and a mean K value of 1.36?×?10??m/s, which is greater than the reported range of K values for the entire GAS in S?o Paulo State. The results suggest that the examined sedimentary unit constitutes a relevant portion of the GAS in S?o Paulo State in the context of groundwater extraction and pollution. Moreover, the constructed aquifer analog is considered an ideal basis for future numerical model experiments, aiming at in-depth understanding of the groundwater flow and contaminant transport patterns at this GAS portion or at comparable fluvial–aeolian facies associations.

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