利用 GIS 和 AHP 方法绘制科尔达县地下水潜力区地图

Abinash Sahoo , Rupsa Subhadarshini, Falguni Baliarsingh
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摘要

最可靠的淡水来源是地下水。地下水供应受到城市化、工业化和人口增长等多种因素的严重威胁。影响地下水供应的数量、质量和变量受到气候多变性的严重影响。劣质地表水资源和不可靠的季风往往会加剧地下水位的下降。因此,为了补充地下水供应,必须找到并确定地下水潜力区(GPZ)。分析针对的是 Khordha 地区,该地区的地下水是农业用水的主要来源。为了确定可能的地下水区,许多因素,包括地貌、地质、海拔、坡度、降水量、土壤类型、土壤质地、排水密度 (DD)、线状密度 (LD)、土地利用/土地覆盖 (LULC) 和线状密度 (LD) 都被构建为地理信息系统 (GIS) 背景中的独立图层。利用多标准决策技术和层次分析法(AHP)对影响潜力区的标准进行配对评估,以确定不同图层的权重,然后使用 ArcGIS10.8 中的加权叠加分析(WOA)工具生成最终的地下水潜力图。指定区域的输出地图被划分为五个新等级--非常好、好、中等、差和非常差,其中 12%(325.1745 平方公里)属于 "非常低 "等级,22%(603.9765 平方公里)属于 "低 "等级,26%(700.7715 平方公里)属于 "中等 "等级,26%(694.2591 平方公里)属于 "高 "等级,14%(376.7553 平方公里)属于 "非常高 "等级。约有 1395 平方公里(占研究区域的 52%)属于 "高 "和 "极高 "类 GPZ。利用从中央地下水委员会获得的数据对生成的 GPWZ 地图进行了验证。精确度评估是通过卡帕系数误差矩阵进行的,根据总体精确度,所获得的地图与实地值的精确度为 81.538%。由于所建议的方法得出了可靠的结果,因此可以在这些地点有效地制定包含自然和人工补给措施的未来管理计划。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mapping of groundwater potential zones of Khordha District using GIS and AHP approaches

The most dependable source of fresh water is groundwater. Groundwater supplies are severely threatened by a number of factors, including urbanization, industrialization, and population growth. The amount, quality and variables affecting groundwater supplies are significantly impacted by climate variability. The fall in groundwater levels is often exacerbated by poor quality surface water resources and unreliable monsoons. Therefore, in order to supplement the groundwater supply, it is important to locate and define the groundwater potential zone (GPZ). The analysis is conducted for the Khordha district, where groundwater rather is a primary source for agricultural uses. In order to determine the possible groundwater zones, many factors, including geomorphology, geology, elevation, slope, precipitation, soil type, soil texture, drainage density (DD), lineament density (LD), Land use/Land cover (LULC), and lineament density (LD), are constructed as separate layers in the geographical information system (GIS) backdrop. The multi-criteria decision-making technique and the Analytic Hierarchy Process (AHP), which enable pairwise evaluation of criteria impacting the potential zone, were utilized to establish the weights for the different layers and after that, the weighted overlay analysis (WOA) tool in ArcGIS10.8 was used to produce the final groundwater potential map. The output map of specified region was delineated into five new classes-very good, good, moderate, poor, and very poor of which 12% (325.1745 km2) falls under ‘very low’, 22% (603.9765 km2) under ‘low’, 26% (700.7715 km2) under ‘moderate’, 26% (694.2591 km2) under ‘high’, 14% (376.7553 km2) under ‘very high’. Approximately 1395 km2 area concerning 52% of study region, falls under ‘high’ and ‘very high’ categories of GPZ. Validation of the generated GPWZ map was done with data acquired from Central groundwater board. The accuracy assessment was done by kappa coefficient error matrix, and based on overall accuracy, the obtained map was 81.538% accurate to field value. As dependable results were produced with the proposed methodology, future management plans incorporating natural and artificial recharge practices can be created in these locations with effectiveness.

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