Dhakate Ratnakar, Singh V S, Negi B C, Chandra Subhash, Rao V Ananda
National Geophysical Research Institute, Uppal Road, Hyderabad 500007, Andhra Pradesh, India.
J Environ Manage. 2008 Sep;88(4):1373-83. doi: 10.1016/j.jenvman.2007.07.014. Epub 2007 Aug 23.
The increasing demand for fresh water has necessitated the exploration for new sources of groundwater, particularly in hard rock terrain, where groundwater is a vital source of fresh water. A fast, cost effective and economical way of exploration is to study and analyze remote sensing data. Interpreted remote sensing data was used to select sites for carrying out surface geophysical investigations. Various geomorphologic units were demarcated and the lineaments were identified by interpretation of remote sensing satellite images. The potential for occurrence of groundwater in the watershed areas was classified as very good, good, moderate and poor by interpreting the images. Sub-surface geophysical investigations, namely vertical electrical soundings, were carried out to delineate potential water-bearing zones. Integrated studies of interpretation of geomorphologic and geophysical data were used to prepare a groundwater potential map. The studies reveal that the groundwater potential of shallow aquifers is due to geomorphologic features and the potential of deeper aquifers is determined by lineaments such as faults and joints.
对淡水需求的不断增加使得有必要探索新的地下水源,特别是在硬岩地区,在那里地下水是淡水的重要来源。一种快速、经济高效的勘探方法是研究和分析遥感数据。经解释的遥感数据被用于选择进行地面地球物理调查的地点。通过对遥感卫星图像的解释,划分了各种地貌单元并识别了线性构造。通过对图像的解释,将流域地区地下水的赋存潜力分为非常好、好、中等和差四类。进行了地下地球物理调查,即垂向电测深,以划定潜在的含水层区域。利用地貌和地球物理数据解释的综合研究来绘制地下水潜力图。研究表明,浅层含水层的地下水潜力归因于地貌特征,而深层含水层的潜力则由断层和节理等线性构造决定。