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Integrated multi-parameter approach for delineating groundwater potential zones in a crystalline aquifer of southern India

机译:划定印度南部晶体含水层的地下水潜在区域的集成多参数方法

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摘要

Groundwater resources in the semi-arid regions of southern India are under immense pressure due to large-scale groundwater abstraction vis-a-vis meager rainfall recharge. Therefore, understanding and evaluating the spatial distribution of groundwater is essential for viable utilization of the resource. Here, we assess groundwater potential at the watershed scale, in a semi-arid environment with crystalline aquifer system without a perennial surface water source using remote sensing, geophysical, and GIS-based integrated multi-parameter approach. GIS-based weighed overlay analysis is performed with input parameters, viz., geology, geomorphology, lineament density, land use, soil, drainage density, slope, and aquifer thickness. The watershed is categorized into four zones, namely, "very good" (GWP4), "good" (GWP3), "moderate" (GWP2), and "low" (GWP1) in terms of groundwater potential. Overall, similar to 70% of the study area falls under moderate to low groundwater potential, indicating a serious threat to the future availability of the resource. Therefore, serious measures are required for maintaining aquifer resilience in this over-exploited aquifer (e.g., restricting groundwater withdrawal from GWP1 and GWP2 zones). Further, as the aquifer is under tremendous anthropogenic pressure, rainwater harvesting and artificial recharge during monsoon are advocated for sustainable aquifer management. Due to the direct dependence of crop production vis-a-vis farmer economy on groundwater, this study is an important step towards sustainable groundwater management and can be applied in diverse hydrological terrains.
机译:由于大型地下水抽象Vis-A-Vis造型降雨充值,印度南部半干旱地区的地下水资源受到巨大的压力。因此,理解和评估地下水的空间分布对于可行利用资源至关重要。在这里,我们评估流域的地下水潜力,在半干旱环境中,使用遥感,地球物理和基于GIS的集成多参数方法而没有多年生地表水源的晶体含水层系统。基于GIS的称量覆盖分析,用输入参数,Ziz,地质,地貌,坐标密度,土地利用,土壤,排水密度,坡度和含水层厚度进行。流域分为四个区域,即“非常好”(GWP4),“良好”(GWP3),“中等”(GWP2)和地下水潜力方面的“低”(GWP1)。总体而言,类似于70%的研究区域下降到中度至低地下水潜力,表明对未来资源可用性的严重威胁。因此,在这种过度开发的含水层中维持含水层的弹性需要严重措施(例如,限制GWP1和GWP2区域的地下水撤回)。此外,随着含水层在巨大的人为压力下,季风期​​间的雨水收获和人工补给被倡导可持续含水层管理。由于作物生产的直接依赖于地下水,这项研究是迈向可持续地下水管理的重要一步,可以应用于不同的水文地形。

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