利用遥感和地理信息系统(GIS)确定瓦卡瓦利流域的地下水潜力区

Sagar B. Gavit, H. Bhange, B. Ayare, S. T. Patil, P. R. Kolhe
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摘要

地下水是淡水的重要来源,它储存在地表以下的饱和带,填补了土壤和地质构造中的缝隙和空间。 地下水是一种无法直接探测的隐性自然资源,因此绘制地下水资源图是一项具有挑战性的任务。本研究综合利用遥感和地理信息系统技术,对 Ratnagiri 地区 Wakawali 流域的地下水潜力区进行了分类。 本研究使用分辨率为 30 米的 SRTM DEM 和常规数据生成专题图层,如坡度、排水密度、岩性、地貌、土壤和降雨量。采用 AHP 技术,根据各专题图层对地下水潜力的相对重要性,为其分配权重百分比。此外,还使用 Arc-GIS 软件中的 "加权和 "工具进行了整合。研究区域的地下水潜势图结果分为五个区域,即极差、差、中差、好、很好,分别占 3.18%、17.68%、30.86%、31.18% 和 17.11%。研究得出结论,遥感和地理信息系统是研究土地和水资源以及编制水资源开发计划的重要工具,可以编制出经济上可行的计划。
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Identification of Groundwater Potential Zones in Wakawali Watershed Using Remote Sensing and Geographic Information System (GIS)
Groundwater is a crucial source of fresh water that is stored below the Earth's surface in the saturated zone, filling gaps and spaces in soil and geological formations.  Groundwater is a hidden natural resource that cannot be directly detected, therefore mapping of this resource can be challenging task. In the present study, remote sensing and geographic information systems techniques were collectively used to categorize groundwater potential zones in the Wakawali watershed of Ratnagiri District.  In this study, SRTM DEM of 30 m resolution and conventional data was used to generate thematic layers such as slope, drainage density, lithology, geomorphology, soil and rainfall. Weightage percentages to each thematic layer were assigned according to their relative importance to groundwater potentiality using AHP technique. Further, integrated using “weighted sum” tool in Arc-GIS software. The outcomes of the groundwater potential map of the study area were classified into five zones viz., very poor, poor, moderately poor, good, very good contributing to 3.18%, 17.68%, 30.86%, 31.18% and 17.11% respectively. The study conclude that the remote sensing and Geographic Information System is a significant tool for land and water resource studies as well as preparation of water resources development plans, so as to prepare economically viable plans.
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