考虑水体面积变化的鄱阳湖平原区地表-地下水相互作用模拟

姜文瑜, 刘波, 邓月萍, 李云良, 束龙仓, 王文鹏. 考虑水体面积变化的鄱阳湖平原区地表-地下水相互作用模拟[J]. 水文地质工程地质, 2023, 50(4): 95-104. doi: 10.16030/j.cnki.issn.1000-3665.202209048
引用本文: 姜文瑜, 刘波, 邓月萍, 李云良, 束龙仓, 王文鹏. 考虑水体面积变化的鄱阳湖平原区地表-地下水相互作用模拟[J]. 水文地质工程地质, 2023, 50(4): 95-104. doi: 10.16030/j.cnki.issn.1000-3665.202209048
JIANG Wenyu, LIU Bo, DENG Yueping, LI Yunliang, SHU Longcang, WANG Wenpeng. Simulation of surface water - groundwater interaction in the plain area of the Poyang Lake considering the change of water body area[J]. Hydrogeology & Engineering Geology, 2023, 50(4): 95-104. doi: 10.16030/j.cnki.issn.1000-3665.202209048
Citation: JIANG Wenyu, LIU Bo, DENG Yueping, LI Yunliang, SHU Longcang, WANG Wenpeng. Simulation of surface water - groundwater interaction in the plain area of the Poyang Lake considering the change of water body area[J]. Hydrogeology & Engineering Geology, 2023, 50(4): 95-104. doi: 10.16030/j.cnki.issn.1000-3665.202209048

考虑水体面积变化的鄱阳湖平原区地表-地下水相互作用模拟

  • 基金项目: 江西省水利厅科技项目(202223YBKT31;202324YBKT13);中央高校基本科研业务费项目(B220201028);国家重点研发计划项目(2021YFC3200502)
详细信息
    作者简介: 姜文瑜(1999-),女,硕士研究生,主要从事地下水数值模拟研究。E-mail: jiangwenyu1999@163.com
    通讯作者: 刘波(1980-),女,博士,副教授,主要从事地下水资源评价及模拟研究。E-mail: liubohhu@hhu.edu.cn
  • 中图分类号: P641

Simulation of surface water - groundwater interaction in the plain area of the Poyang Lake considering the change of water body area

More Information
  • 湖泊的水情变化会影响其与地下水之间的物理水文过程和生态行为,鄱阳湖独特的“河湖相”转换特征使得该地区地表-地下水交换过程更加复杂。采用Visual MODFLOW构建三维非稳定流地下水流数值模型,利用LAK3子程序模块,通过输入五河入湖以及鄱阳湖流入长江的水量,实现湖水面积的动态模拟。结果表明,2019年湖水位模拟值与实测值的均方根误差为0.225 m,地下水水位模拟值与实测值的均方根误差为0.571 m;模型模拟鄱阳湖水面积环比变幅−41%~83%,与遥感影像结论吻合。该模型减少了湖泊作为边界条件的约束,可以有效刻画鄱阳湖频繁变化的湖水位和水体面积,准确模拟地下水流场和地表-地下水相互作用关系对湖泊水体高度动态变化的响应。枯水期主要由地下水补给湖水,交换量为2.03×107~10.58×107 m3/mon;丰水期湖水补给地下水,交换量为2.04×107~16.53×107 m3/mon,湖区及周边地下水水位相比枯水期平均抬升2~3 m,地下水由湖区流向周边地区。本研究为地表水体剧烈变化地区提供了有效的数值模拟方法,研究结果可为鄱阳湖平原区未来水资源管理和环境评价提供基础。

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  • 图 1  研究区水文地质图和剖面图

    Figure 1. 

    图 2  模型范围、边界类型以及模型渗透系数分区

    Figure 2. 

    图 3  Obs1、Obs2、Obs3地下水水位模拟值与观测值对比及湖水位模拟值与观测值对比图

    Figure 3. 

    图 4  鄱阳湖遥感影像水体信息提取图及水面积模拟图

    Figure 4. 

    图 5  2019年1月和7月地下水流场模拟结果对比图

    Figure 5. 

    图 6  湖泊水均衡模拟结果图

    Figure 6. 

    图 7  研究区补排关系图

    Figure 7. 

    表 1  研究区各分区渗透系数取值

    Table 1.  The hydraulic conductivity values in each subdomain of the study area / (m·d−1

    参数区编号
    第1~3层渗透系数 0.1 5 15 20 35 15 25 5
    第4层渗透系数 10 10 20 25 35 20 25 15
    下载: 导出CSV
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出版历程
收稿日期:  2022-09-18
修回日期:  2023-01-13
刊出日期:  2023-07-15

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