Abstract
Barind Tract, located north western part of Bangladesh, is one of the most diversified physiographic units of the country. The surface water supply in this part is particularly limited, so the irrigation is almost entirely depends on groundwater. However, over exploitation indicates falling groundwater heads in this area. The objective of present study is to examine the nature of the aquifer system Barind Tract of Bangladesh in order to assess the sustainability of groundwater yield. Borehole lithology data were collected, processed and analyzed for this purpose. Representative panel diagram, 3-D stratigraphic and cross-sectional views were also prepared for necessary assessment of the variation of individual subsurface stratum in different locations. The study identified three subsurface geologic formations namely, a top clay layer, sand layer of different grain size and at the bottom an impermeable clay zone. Maps of formation thickness and index revealed that aquifer thickness is low in the north-western corner and in some places of middle of south-western corner. The thickness of sand formation in other places is recorded above 20 m. It is expect that the finding of the study will help groundwater resources development, planning and management in the area.
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The authors are grateful to the Barind Multiple Development Authority (BMDA), Rajshahi, for their assistance during this work.
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Hasan, M.A.F.M.R., Keramat, M.M., Shahid, S. et al. Evaluation of Subsurface Lithologic Units for Groundwater Exploration in the Barind Tract of Bangladesh. Geotech Geol Eng 34, 1395–1411 (2016). https://doi.org/10.1007/s10706-016-0050-6
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DOI: https://doi.org/10.1007/s10706-016-0050-6