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污染场地铬迁移规律及铬对地下水源地影响的数值模拟研究

王睿 张耀斌 陈文芳 邵景力 崔亚莉 张秋兰

岩矿测试2026,Vol.45Issue(3):495-508,14.
岩矿测试2026,Vol.45Issue(3):495-508,14.DOI:10.15898/j.ykcs.202409110189

污染场地铬迁移规律及铬对地下水源地影响的数值模拟研究

Chromium Migration in a Contaminated Site and the Numerical Simulation of Its Effect on the Groundwater Source Area

王睿 1张耀斌 2陈文芳 3邵景力 1崔亚莉 1张秋兰4

作者信息

  • 1. 中国地质大学(北京),北京 100083
  • 2. 煤炭开采水资源保护与利用全国重点实验室,北京低碳清洁能源研究院,北京 102299
  • 3. 河南省地质矿产勘查开发局第一地质环境调查院,河南 郑州 471023
  • 4. 水利部地下水保护重点实验室(筹),中国地质大学(北京),北京 100083
  • 折叠

摘要

Abstract

Chromium(Cr)pollution has become one of the heavy metal pollutions in soil and groundwater.To study the migration law of Cr in the groundwater of contaminated sites and analyze and predict the time for Cr(Ⅵ)to migrate to the water source protection area,a certain Cr-contaminated site in Xinxiang City,Henan Province was taken as the research area.The grounder modeling systems(GMS)software was used to establish the numerical simulation model of groundwater flow and the solute transport model to analyze and predict the migration of Cr(Ⅵ)both without and with adsorption considered.The conclusions show that without considering adsorption,the time for Cr(Ⅵ)in the shallow phreatic aquifer to migrate to the water source protection area is 78 years,and in the deep phreatic aquifer,it is 70 years.When adsorption is considered and the Langmuir adsorption model is adopted,the time for Cr(Ⅵ)in both the shallow and deep phreatic aquifers to migrate to the water source protection area is about 4 years slower than that without considering adsorption.In addition,under the condition of considering adsorption,the scenarios of three changes in the source concentration,namely continuous release of the pollution source,disappearance of the pollution source after 10 years,and continuous attenuation of the pollution source,were simulated.The simulation results are as follows:in the early stage,the original concentration of Cr(Ⅵ)in groundwater rapidly rises to a peak and then drops rapidly;when the Cr slag pile infiltrates again after leaching in the later stage,the concentration changes of Cr(Ⅵ)under the three scenarios show differences.When the pollution source is continuously released,the concentration slowly increases;when the pollution source disappears after 10 years,the concentrations at the two observation points first slightly increase and then gradually approach 0;when the pollution source continuously attenuates,the concentration first rises and then falls and finally approaches 0.At the same time,it can be seen that shortening the distance between the pollution source and the observation point will significantly reduce the migration time of Cr(Ⅵ),while the time for it to reach the observation point is negatively correlated with the hydrodynamic conditions.This phenomenon is mainly controlled by key hydrogeological parameters such as the diffusion characteristics of the pollution plume and the permeability coefficient of the aquifer medium.The results can provide a scientific basis for the prediction,prevention,and control of Cr pollution in contaminated sites.

关键词

地下水/数值模拟/地下水模型系统/铬污染迁移/水源地

Key words

groundwater/numerical simulation/grounder modeling systems(GMS)/chromium contamination migration/water source

分类

天文与地球科学

引用本文复制引用

王睿,张耀斌,陈文芳,邵景力,崔亚莉,张秋兰..污染场地铬迁移规律及铬对地下水源地影响的数值模拟研究[J].岩矿测试,2026,45(3):495-508,14.

基金项目

地球深部探测与矿产资源勘查国家科技重大专项(2024ZD1004103) (2024ZD1004103)

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