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Mapping groundwater potential zones using remote sensing and GIS approach in Jammu Himalaya, Jammu and Kashmir

机译:使用遥感和GIS方法在Jammu Himalaya,Jammu和Kashmir中映射地下水潜在区域

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摘要

Locating potential groundwater zones is becoming more convenient, cost-effective than invasive methods and efficient with the advent of high-resolution satellite imagery. In the present study, remote sensing and geographic information system has been integrated together for delineation of groundwater potential zones in Jammu Himalaya to generate various thematic layers using weighted overlay analysis. Various thematic layers such as (slope, Topographic Position Index, Topographic Wetness Index, geology, drainage density, lineament density and land use land cover) were integrated and appropriate weights were assigned to each class. Based on the generated groundwater potential map, about 26% of the study area falls in high category zone, 27.27% fall in moderate, 28.72% fall in low and 18% very low category zones. Furthermore, annual replenishable groundwater status for the year 2004, 2009, 2011 and 2013 was estimated as 85077 (ha m), 93133 (ha m), 130102 (ha m) and 123264 (ha m) respectively and the net groundwater availability for the year 2004, 2009, 2011 and 2013 was estimated as 76569 (ha m), 83819 (ha m), 117092 (ha m) and 110254 (ha m) respectively. The stage of groundwater development in the Jammu Himalaya was calculated 17.62% for the year 2004, 22.84% for the year 2009, 18.36% for the year 2011 and 26.26% for the year 2013 with no significant decline of water levels hence the Jammu Himalaya is categorized as 'Safe' for future groundwater development.
机译:定位潜在的地下水区变得更加方便,比侵入性方法和高分辨率卫星图像的出现效率更具成本效益。在本研究中,遥感和地理信息系统已经集成在一起,用于划分Jammu Himalaya中的地下水潜在区域,以产生使用加权覆盖分析的各种专题层。诸如(斜坡,地形位置指数,地形湿度指数,地质,排水密度,衬里密度和土地使用陆覆盖)的各种专题层被整合,并将适当的重量分配给每个班级。基于所产生的地下水潜在地图,大约26%的研究区落在高类别区,27.27%处于中等,28.72%下降,低18%的类别。此外,2004年,2009年,2011年和2013年的年度补充地下水地位估计为85077(HA M),93133(HA M),130102(HA M)和123264(HA M),净地下水可用性2004年,2009年,2011年和2013年估计为76569(HA M),83819(HA M),117092(HA M)和110254(HA M)。 2004年,Jammu Himalaya的地下水开发阶段计算了2009年的17.62%,2009年的22.84%,2011年的2013年和2013年的26.36%,因此水平没有显着下降,因此jammu喜马拉雅为未来地下水开发分类为“安全”。

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