非稳态潜流交换过程研究进展

吴成城, 张小琴, 鲁程鹏, 束龙仓, 刘波. 非稳态潜流交换过程研究进展[J]. 水文地质工程地质, 2022, 49(5): 157-165. doi: 10.16030/j.cnki.issn.1000-3665.202108011
引用本文: 吴成城, 张小琴, 鲁程鹏, 束龙仓, 刘波. 非稳态潜流交换过程研究进展[J]. 水文地质工程地质, 2022, 49(5): 157-165. doi: 10.16030/j.cnki.issn.1000-3665.202108011
WU Chengcheng, ZHANG Xiaoqin, LU Chengpeng, SHU Longcang, LIU Bo. Research progress of the unsteady hyporheic flow exchange process[J]. Hydrogeology & Engineering Geology, 2022, 49(5): 157-165. doi: 10.16030/j.cnki.issn.1000-3665.202108011
Citation: WU Chengcheng, ZHANG Xiaoqin, LU Chengpeng, SHU Longcang, LIU Bo. Research progress of the unsteady hyporheic flow exchange process[J]. Hydrogeology & Engineering Geology, 2022, 49(5): 157-165. doi: 10.16030/j.cnki.issn.1000-3665.202108011

非稳态潜流交换过程研究进展

  • 基金项目: 国家自然科学基金项目(41971027)
详细信息
    作者简介: 吴成城(1997-),男,博士研究生,主要从事水文学及水资源研究。E-mail:220401010005@hhu.edu.cn
    通讯作者: 鲁程鹏(1984-),男,教授,博士生导师,主要从事水文学及水资源研究。E-mail:luchengpeng@hhu.edu.cn
  • 中图分类号: P641.2

Research progress of the unsteady hyporheic flow exchange process

More Information
  • 潜流交换研究涉及地表水-地下水系统交互作用的物理机制、影响因素和生化作用等方面,是近年来水文学、生态学、环境学等学科的研究热点。潜流交换过程包含水流运动、溶质运移以及能量传输过程。以稳态流动条件作为控制因素的潜流交换研究成果已经不能满足相关学科发展的要求。因此,近年来非稳态潜流交换过程的研究及其成果渐受关注。当前相关研究多以物理模型试验为主(如室内水槽试验、示踪试验),辅以数值模拟或遥感技术进行验证,进而总结非稳态潜流交换过程水动力交换和能量交换过程规律。未来研究应在多时空尺度,集合多种高精度监测手段,研究潜流交换中的影响因素(如河流水位波动),开发更精确的地表水-地下水耦合模型,系统认识非稳态潜流交换过程。有关非稳态潜流交换的研究结论将有效指导水资源保护与生态环境修复和综合治理。

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出版历程
收稿日期:  2021-08-14
修回日期:  2021-09-17
刊出日期:  2022-09-15

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