王佳琪;马瑞;孙自永;

• 1:中国地质大学(武汉)环境学院

摘要(Abstract)：

在地表水-地下水作用带内,水流途径、流速、滞留时间的差异及地表水-地下水的交换量从不同方面控制着氮素污染物的反应迁移过程,并影响污染物在地表水与地下水间的通量。因此,精细刻画地表水-地下水作用带内的水流模式是研究氮素污染物反应迁移及归宿的关键问题。受含水介质异质性、水流模式的复杂性及其与地球化学和生物地球化学过程的耦合作用影响,地表水-地下水作用带内氮素污染物的反应迁移和归宿极为复杂,研究十分困难。水流和污染物反应迁移耦合模型可将地下水流、污染物的物理迁移过程及其地球化学和生物化学过程有机整合在一起,能更好地揭示氮素污染物反应迁移的过程和机理,预测其发展趋势,可为研究地表水-地下水作用带内氮素污染物的反应迁移和归宿提供有力工具。

关键词(KeyWords)： 地表水与地下水相互作用带;氮素污染物;水流模式;反应迁移模型

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金优秀青年基金项目(41722208)

作者(Author): 王佳琪;马瑞;孙自永;

Email:

DOI: 10.19509/j.cnki.dzkq.2019.0429

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