Development of unconfined conditions in multi-aquifer flow systems: a case study in the Rajshahi Barind, Bangladesh
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  • 作者:K. R. Rushton ; M. Asaduz Zaman
  • 关键词:Groundwater hydraulics ; Aquitard ; Bangladesh ; Conceptual models ; Over ; abstraction
  • 刊名:Hydrogeology Journal
  • 出版年:2017
  • 出版时间:February 2017
  • 年:2017
  • 卷:25
  • 期:1
  • 页码:25-38
  • 全文大小:
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Hydrogeology; Hydrology/Water Resources; Geology; Water Quality/Water Pollution; Geophysics/Geodesy; Waste Water Technology / Water Pollution Control / Water Management / Aquatic Pollution;
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1435-0157
  • 卷排序:25
文摘
Identifying flow processes in multi-aquifer flow systems is a considerable challenge, especially if substantial abstraction occurs. The Rajshahi Barind groundwater flow system in Bangladesh provides an example of the manner in which flow processes can change with time. At some locations there has been a decrease with time in groundwater heads and also in the magnitude of the seasonal fluctuations. This report describes the important stages in a detailed field and modelling study at a specific location in this groundwater flow system. To understand more about the changing conditions, piezometers were constructed in 2015 at different depths but the same location; water levels in these piezometers indicate the formation of an additional water table. Conceptual models are described which show how conditions have changed between the years 2000 and 2015. Following the formation of the additional water table, the aquifer system is conceptualised as two units. A pumping test is described with data collected during both the pumping and recovery phases. Pumping test data for the Lower Unit are analysed using a computational model with estimates of the aquifer parameters; the model also provided estimates of the quantity of water moving from the ground surface, through the Upper Unit, to provide an input to the Lower Unit. The reasons for the substantial changes in the groundwater heads are identified; monitoring of the recently formed additional water table provides a means of testing whether over-abstraction is occurring.

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