Department of Applied Geology, Indian School of Mines, Dhanbad, India.
Environ Monit Assess. 2010 Jun;165(1-4):179-91. doi: 10.1007/s10661-009-0937-2. Epub 2009 May 5.
A part of the Gangetic Alluvial Plain covering 2,228 km(2), in the state of Bihar, is studied for demarcating groundwater development potential zones. The area is mainly agrarian and experiencing intensive groundwater draft to the tune of 0.12 million cubic metre per square kilometres per year from the Quaternary marginal alluvial deposits, unconformably overlain northerly sloping Precambrian bedrock. Multiparametric data on groundwater comprising water level, hydraulic gradient (pre- and post-monsoon), aquifer thickness, permeability, suitability of groundwater for drinking and irrigation and groundwater resources vs. draft are spatially analysed and integrated on a Geographical Information System platform to generate thematic layers. By integrating these layers, three zones have been delineated based on groundwater development potential. It is inferred that about 48% of the area covering northern part has high development potential, while medium and low development potential category covers 41% of the area. Further increase in groundwater extraction is not recommended for an area of 173 km(2), affected by over-exploitation. The replenishable groundwater resource available for further extraction has been estimated. The development potential enhances towards north with increase in thickness of sediments. Local deviations are due to variation of-(1) cumulative thickness of aquifers, (2) deeper water level resulting from localised heavy groundwater extraction and (3) aquifer permeability.
在比哈尔邦的恒河冲积平原的一部分,面积为 2228 平方公里,正在进行研究以划定地下水开发潜力区。该地区主要是农业区,每年从第四纪边缘冲积层中抽取地下水,以 0.12 百万立方米/平方公里/年的强度抽取地下水,这些地下水来自于不整合覆盖北部倾斜前寒武纪基岩。对包括水位、水力梯度(前、后季风期)、含水层厚度、渗透率、地下水对饮用水和灌溉的适宜性以及地下水资源与开采量在内的地下水多参数数据进行了空间分析,并在地理信息系统平台上进行了综合分析,生成专题图层。通过整合这些图层,根据地下水开发潜力划定了三个区域。推断约 48%的北部地区具有较高的开发潜力,而中低开发潜力区则覆盖了 41%的地区。由于过度开采,不建议在 173 平方公里的区域进一步抽取地下水。对可进一步开采的可再生地下水资源进行了估算。随着沉积物厚度的增加,开发潜力向北部增强。局部偏差是由于(1)含水层累积厚度的变化,(2)由于局部地下水大量开采导致的水位变深,以及(3)含水层渗透率的变化。