RT - Journal Ty - Jour YR - 2016-11-08 JF - 当前世界环境Jo - Sp - Op - Vo - 35是 - 38 UL - www.cwwejournal.org/article/963/ Do - 10.12944 / CWe.11.3。09 N2 - 在本研究中，为了证明在理解本地地下水地水条件下，将水样从4个NOS收集水分，以证明使用组合同位素和盐度测绘。定义的湖泊（Kadaba，Belavatta，Pura和Nittur）;沿着湖泊的周边从浅手泵/管孔中收集地下水样品。还收集了雨水。湖水似乎在其同位素组合物中富集主要是由于该地区的蒸发。与附近的地下水盐度相比，湖水盐度较低。地下水的流动，​​在Nittur湖中充电，至少直到pura下游。在Pura-地下水和地表水之间看到地下水的盐度增加（可能是由于亚表面土壤的溶解）。发现在贝拉瓦塔上采样的地下水从局部沉淀而不是从表面体充电。 The water body (Kadaba) is getting filled mainly due to precipitation and to some extent due to runoff from the upper reach of water body. There is a strong link between lake water–groundwater (e.g. site Pura) and groundwater–lake water (e.g. Site Kadaba). Therefore, this procedure is expected to radically increase the accountability of usage and help in planning of suitable ground water supply and would provide a holistic approach to promote maximum agricultural output and industrial growth. ER -