地球科学进展

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2014 , Vol. 29 >Issue 1: 30 - 41

DOI: https://doi.org/1001-8166(2014)01-0030-12

非均质含水层中渗流与溶质运移研究进展*

  • 覃荣高 ,
  • 曹广祝 ,
  • 仵彦卿
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  • 1.上海交通大学环境科学与工程学院, 上海 200240
    2.昆明理工大学国土资源与工程学院地球科学系, 云南 昆明 650093

覃荣高（1982-），男，广西来宾人，讲师，主要从事地下水污染物迁移模拟方面的研究. E-mail: qinronggao@126.com

收稿日期: 2013-08-05

  修回日期: 2013-11-12

  网络出版日期: 2014-01-10

基金资助

国家自然科学基金面上项目“非均质含水层中有机污染物迁移机理研究”（编号：41272261）资助.

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Review of Study on Groundwater Flow and Solute Transport in Heterogeneous Aquifer

  • Ronggao Qin ,
  • Guangzhu Cao ,
  • Yanqing Wu
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  • 1.School of Environmental Science and Engineering, Shanghai Jiao Tong University, Shanghai 200240, China
    2. Department of Earth Sciences, Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming 650093, China
仵彦卿（1957-）, 男, 陕西咸阳人, 教授, 主要从事地下水污染模拟与修复方面的研究. E-mail: wuyanqing@sjtu.edu.cn

Received date: 2013-08-05

  Revised date: 2013-11-12

  Online published: 2014-01-10

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摘要

含水层的非均质性控制着地下水渗流和溶质迁移特性, 准确定量化描述非均质含水层中的渗流和溶质迁移问题受到广泛关注, 已成为地球科学领域中的研究热点。首先从非均质含水层地下水流和溶质迁移理论模型、矩分析、多尺度进行系统综述, 指出尺度转换在目前水文地质研究中主要解决的问题以及存在的问题；其次从非均质含水层场地试验、不确定性以及速度连通性等方面分析了该方向的研究进展；最后指出地球物理反演含水层非均质性、随机理论与随机模拟软件开发、尺度转换及速度连通性的不确定性问题、非均质性与水文地质条件关系研究4个方面是该领域今后的主要研究方向。

关键词： 非均质含水层; 矩分析; 多尺度; 不确定性; 连通性

本文引用格式

覃荣高 , 曹广祝 , 仵彦卿 . 非均质含水层中渗流与溶质运移研究进展*[J]. 地球科学进展, 2014 , 29(1) : 30 -41 . DOI: 1001-8166(2014)01-0030-12

Abstract

Natural aquifer heterogeneity controls the groundwater flow and solute transport, and how to accurately quantify the flow and solute transport in heterogeneous aquifers has received wide attention by many scholars, and has become a hot research topic in earth science. Theoretically, a systematic review is given by the following aspect: flow and solute transport model, moment analysis, multiscale analysis. The resolved and remained issues for scale conversion in hydrogeology research are pointed out. Secondly, recent advances of heterogeneous field test, uncertainty and velocity connectivity are analyzed. Finally, the geophysical inversion of aquifer heterogeneity, stochastic theory and development of stochastic simulation software, scale conversion and uncertainty of velocity connectivity, and the relationship between heterogeneity and hydrogeological condition on the major four aspects of the future research direction is pointed out.

Key words： Heterogeneous aquifer; Moment analysis; Multi-scale; Uncertainty; Connectivity

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