文章摘要
杨 美, 李云良, 邢子康, 储小东, 陈 静.基于层次分析法的鄱阳湖流域地下水潜力分区研究Journal of Water Resources and Water Engineering[J].,2025,36(2):19-28
基于层次分析法的鄱阳湖流域地下水潜力分区研究
Groundwater potential zoning for the Poyang Lake Basin using GIS and analytical hierarchical process techniques
  
DOI:10.11705/j.issn.1672-643X.2025.02.03
中文关键词: 地下水潜力分区  层次分析法  极端干旱  地理信息系统  鄱阳湖流域
英文关键词: groundwater potential zoning  analytic hierarchy process (AHP)  extreme drought  geographic information system (GIS)  the Poyang Lake Basin
基金项目:国家自然科学基金项目(42401049); 中国科学院青年创新促进会优秀会员项目(Y2023084); 江西省双千计划人才项目(jxsq2023101105); 江西省自然科学基金重点项目(20242BAB26044); 水灾害防御全国重点实验室“一带一路”水与可持续发展科技基金面上项目(2023490611); 中国科学院南京地理与湖泊研究所十四五揭榜挂帅项目(NIGLAS2022GS08); 江西省水资源基础调查项目
Author NameAffiliation
YANG Mei1,2,3, LI Yunliang1,3, XING Zikang1,3, CHU Xiaodong4, CHEN Jing5,6 (1. 中国科学院南京地理与湖泊研究所湖泊与流域水安全全国重点实验室 江苏 南京 210008 2.中国科学院大学 资源与环境学院 北京 101408 3.中国科学院南京地理与湖泊研究所鄱阳湖湖泊湿地综合研究站 江西 九江 332899 4.江西省地质调查勘察院地质环境监测所 江西 南昌 330006 5.河海大学 水文水资源与水利工程科学国家重点实验室 江苏 南京 210098 6.江西省水文监测中心 江西 南昌 330002) 
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中文摘要:
      地下水是极端干旱气候条件下的重要隐藏水源和水资源储备,近年来鄱阳湖流域极端干旱事件频发,为了从空间上探明鄱阳湖流域地下水潜力,结合地理信息系统和层次分析法,识别和绘制鄱阳湖流域地下水潜力区域。选取含水层岩性、地貌、土壤类型、土地利用/覆盖、河网密度、曲率、粗糙度、地形湿度指数、地形位置指数、年降水量、坡度共计11个影响因素作为衡量地下水潜力的指标。结果表明:含水层岩性、地貌、土壤类型和土地利用/覆盖对地下水潜力影响权重合计达0.5;鄱阳湖流域地下水潜力非常好、较好、中等、较差和非常差的区域面积分别占12.1%、26.0%、34.2%、18.7%和9.0%,地下水潜力较好和非常好的区域主要分布在鄱阳湖区洲滩以及河流周边漫滩。验证结果显示,ROC曲线的IAUC值为0.755,即预测结果良好,所得地下水潜力分区结果可靠。研究结果明晰了鄱阳湖集水区的整体地下水潜力,可为干旱时期地下水源地选择及地下水资源管理调控提供科学参考,进一步丰富了鄱阳湖流域地下水研究的理论框架与实践应用。
英文摘要:
      As a hidden water source, groundwater plays the role of important water resources reserve under extreme arid conditions. In recent years, extreme drought events have occurred frequently in the Poyang Lake Basin. To explore the potential storage of groundwater in the Poyang Lake Basin spatially, the groundwater potential area was identified and mapped by the geographic information system (GIS) and the analytic hierarchy process (AHP). A total of 11 influencing factors were selected to characterize the groundwater potential, including lithology, geomorphology, soil type, land use/land cover (LULC), drainage density, curvature, roughness, topographic wetness index, topographic position index, annual precipitation, and slope. The results showed that the combined weight of lithology, geomorphology, soil type, and LULC influencing on groundwater potential reached 0.5. The areas with excellent, good, moderate, poor, and very poor groundwater potential in the Poyang Lake Basin accounted for 12.1%, 26.0%, 34.2%, 18.7%, and 9.0%, respectively, with good and excellent groundwater potential areas mainly distributing in the bottomland of the Poyang Lake area and the river floodplain. According to the validation results, the IAUC value of the ROC curve was 0.755, indicating an excellent prediction performance and reliable potential zoning results. The results clarified the overall groundwater potential of the Poyang Lake Basin, which can provide a reference for the selection of groundwater sources and the regulation of groundwater resources in drought period. This study enriched the theoretical framework and practical application of groundwater research in the Poyang Lake Basin.
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