决策支持系统/遥感/地理信息系统技术在地下水补给评估中的应用

Mohamed Saad, E. Nofal, Yehia Abdelmonem, Peter Riad
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引用次数: 0

摘要

通过确定地下水补给区(GWRZ)来管理水资源和储水对埃及的水安全至关重要。决策支持系统(DSS)、遥感和地理信息系统(GIS)技术为水资源建模提供了大量数据。埃及纳赛尔湖西部 Toshka 地区的地质、地貌、气候和水文特征由航天飞机雷达地形任务、气候研究单位网格时间序列、哨兵 2 时间序列和 Landsat-8 OLI 的数据生成。利用五种 DSS 技术对 15 幅 GIS 专题地图进行了排序和归一化处理:分析层次过程 (AHP)、模糊分析层次过程 (FAHP)、频率比 (FR)、香农熵 (SE) 和多重影响因子 (MIF)。为确保这些模型在计算上的实用性,对 GWRZ 进行了提取和比较。结果显示,AHP、FAHP、FR、SE 和 MIF 的 GWRZ 分别为 83%、87.5%、99.1%、99.1% 和 87.5%。采用接收器工作特征曲线(ROC)来评估这些模型的有效性。结果发现,SE 模型的预测准确率最高,其 ROC 准确值为 91.1%,而 FR、AHP、FAHP 和 MIF 方法的 ROC 准确值分别为 91、84.4、81.9 和 89.9%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Application of decision support system/remote sensing/GIS techniques in groundwater recharge assessment
Managing water resources and storing water through the identification of groundwater recharge zones (GWRZs) are critical to water security in Egypt. Decision-support systems (DSSs), remote sensing, and GIS techniques have yielded significant data for water resources modeling. The geologic, geomorphic, climatic, and hydrologic features of the Toshka area, Western Lake Nasser, Egypt, have been generated by data from Shuttle Radar Topography Mission, Climatic Research Unit gridded Time Series, Sentinel 2 time series, and Landsat-8 OLI. Fifteen GIS thematic maps have been ranked and normalized using five DSS techniques: Analytical Hierarchy Process (AHP), Fuzzy Analytical Hierarchy process (FAHP), Frequency Ratio (FR), Shannon Entropy (SE), and Multi-Influencing Factor (MIF). To ensure the computational usefulness of these models, GWRZs have been extracted and compared. The outcomes showed that 83, 87.5, 99.1, 99.1, and 87.5% of the existing wells are in high to extreme GWRZs for AHP, FAHP, FR, SE, and MIF, respectively. The receiver operating characteristic curve (ROC) was used to assess the effectiveness of these models. It was found that the SE model had the highest predictive performance rates, as its ROC accuracy value was 91.1%, while the FR, AHP, FAHP, and MIF approaches had values of 91, 84.4, 81.9, and 89.9%, respectively.
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