欢迎访问《生态学杂志》官方网站,今天是 分享到:

生态学杂志 ›› 2025, Vol. 44 ›› Issue (6): 2105-2112.doi: 10.13292/j.1000-4890.202506.032

• 技术与方法 • 上一篇    

基于改进DRASTIC模型的天津市平原区地下水脆弱性评价

吴潇1,郑丽芝1*,李军1,朱静蕾1,席雪萍2,高学飞2   

  1. 1天津师范大学地理学部, 天津 300387; 2天津市地质工程勘测设计院有限公司, 天津 300387)
  • 出版日期:2025-06-10 发布日期:2025-06-11

Assessment of groundwater vulnerability in Tianjin plain area based on improved DRASTIC model.

WU Xiao1, ZHENG Lizhi1*, LI Jun1, ZHU Jinglei1, XI Xueping2, GAO Xuefei2   

  1. (1Department of Geography of Tianjin Normal University, Tianjin 300387, China; 2Tianjin Geological Engineering Exploration and Design Institute Co., Ltd, Tianjin 300387, China).

  • Online:2025-06-10 Published:2025-06-11

摘要: 天津市平原区主要由山前平原、中部平原和滨海平原三部分组成,其地下水资源丰富。但随着人类对地下水资源的开发利用,天津市平原区地下水已处于超负载状态。本研究采用改进的DRASTIC模型,选取影响地下水脆弱性的7个指标,用层次分析法确定各指标权重,基于GIS软件空间分析功能评价了天津市平原区地下水脆弱性。结果表明:天津市平原区地下水脆弱性以中等脆弱性、较高脆弱性为主,两者占评价区域面积64.01%;天津市平原区地下水脆弱性呈现南高北低的趋势;天津市平原区地下水脆弱性低、较低区域呈现明显的带状分布,两者占评价区域总面积27.02%,主要分布在天津市平原区北部,其分布区域地下水埋深普遍较深,含水层厚度较厚;高脆弱性区域占评价区域的8.97%,主要分布在宁河区东北部、市内六区、武清区西南部以及滨海新区东南部。研究表明,天津市平原区地下水脆弱性总体较高,其地下水脆弱性受地下水埋深、含水层厚度以及包气带岩性影响较大。本文提出一种适合在沿海平原区的地下水脆弱性评价方法,通过引入含水层厚度和潜水层矿化度指标对天津市平原区地下水脆弱性评价进行优化。本研究成果可为天津市平原区地下水生态治理、地下水污染防治重点区划等工作提供科学依据。


关键词: DRASTIC, 天津市, GIS, 地下水脆弱性, 层次分析法

Abstract: The plain area of Tianjin could be classified into three parts: piedmont plain, central plain, and coastal plain, which are characterized by abundant groundwater resources. With the development of the society and the exploration of groundwater resources by human beings, groundwater in Tianjin plain has become overloaded. In this study, we used an improved DRASTIC model to evaluate groundwater vulnerability in the Tianjin plain area. Seven indices affecting groundwater vulnerability were selected, the respective weights of which were determined using the analytic hierarchy process. The evaluation was conducted based on the spatial analysis functions of GIS software. The results showed that groundwater vulnerability in the plain area of Tianjin is predominantly categorized as medium and high vulnerability, accounting for 64.01% of the evaluated area. The groundwater vulnerability exhibits a spatial pattern of higher values in the south and lower values in the north. Areas with low and relatively low groundwater vulnerability show distinct zonal distribution, accounting for 27.02% of the total area, mainly distributed in the northern part of the plain area of Tianjin. These areas are characterized by generally deep groundwater levels and thick aquifer layers. Higher vulnerability areas accounted for 8.97% of the evaluated area and are mainly distributed in the northeast of Ninghe District, the six districts of the central city, the southwest of Wuqing District, and the southeast of Binhai New Area. Our results indicate that the overall groundwater vulnerability in the plain area of Tianjin is relatively high and significantly influenced by groundwater depth, aquifer thickness, and the lithology of vadose zone. We present an evaluation method suitable for groundwater vulnerability in coastal plain area. By incorporating aquifer thickness and phreatic water salinity index, the assessment of groundwater vulnerability in the Tianjin plain was optimized. Our results provide a scientific basis for ecological management of groundwater and key zoning strategies for groundwater pollution prevention and control in Tianjin plain area.


Key words: DRASTIC, Tianjin, GIS, groundwater vulnerability, analytic hierarchy process