一种新的估计非高斯分布含水层渗透系数场的方法

孙猛, 骆乾坤, 孔志伟, 郭明, 刘明力, 钱家忠. 一种新的估计非高斯分布含水层渗透系数场的方法[J]. 水文地质工程地质, 2024, 51(3): 23-33. doi: 10.16030/j.cnki.issn.1000-3665.202308022
引用本文: 孙猛, 骆乾坤, 孔志伟, 郭明, 刘明力, 钱家忠. 一种新的估计非高斯分布含水层渗透系数场的方法[J]. 水文地质工程地质, 2024, 51(3): 23-33. doi: 10.16030/j.cnki.issn.1000-3665.202308022
SUN Meng, LUO Qiankun, KONG Zhiwei, GUO Ming, LIU Mingli, QIAN Jiazhong. A novel approach for estimating hydraulic conductivity of non-Gaussian aquifer[J]. Hydrogeology & Engineering Geology, 2024, 51(3): 23-33. doi: 10.16030/j.cnki.issn.1000-3665.202308022
Citation: SUN Meng, LUO Qiankun, KONG Zhiwei, GUO Ming, LIU Mingli, QIAN Jiazhong. A novel approach for estimating hydraulic conductivity of non-Gaussian aquifer[J]. Hydrogeology & Engineering Geology, 2024, 51(3): 23-33. doi: 10.16030/j.cnki.issn.1000-3665.202308022

一种新的估计非高斯分布含水层渗透系数场的方法

  • 基金项目: 国家重点研发计划项目(2022YFC3702200);安徽省自然科学基金项目(JZ2022AKZR0451)
详细信息
    作者简介: 孙猛(1997—),男,硕士研究生,主要从事地下水数值模拟研究。E-mail:sunmeng_alvin@163.com
    通讯作者: 骆乾坤(1984—),女,博士,副研究员,硕士生导师,主要从事地下水模拟和水资源优化管理研究。E-mail:QKLuo@hfut.edu.cn
  • 中图分类号: P641.2

A novel approach for estimating hydraulic conductivity of non-Gaussian aquifer

More Information
  • 集合卡尔曼滤波(ensemble Kalman filter, EnKF)是最流行的数据同化方法之一。然而,在处理非高斯问题时,EnKF存在局限性。为了解决非高斯问题并准确描述含水介质连通性,将正态分数变换(normal-score transformation, NST)与多重数据同化集合平滑器(ensemble smoother with multiple data assimilation, ES-MDA)相结合,提出NS-ES-MDA方法。通过对比实验,验证了NS-ES-MDA方法估计非高斯分布含水层渗透系数场的有效性。相较于重启正态分数集合卡尔曼滤波器(restart normal-score ensemble Kalman filter, rNS-EnKF)方法,NS-ES-MDA在吸收相同数据后,参数估计精度提升约34%,计算效率提升约35%。此外,NS-ES-MDA方法受“异参同效”现象的影响较小,具有较强的更新能力,能够保障得到较准确的参数估计值。研究可为非高斯分布含水层参数估计提供一种有效的求解方法。

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  • 图 1  参考场的设置以及场地的训练图像

    Figure 1. 

    图 2  初始参数集合以及所有情景中后验参数集合的均值场和方差场

    Figure 2. 

    图 3  初始参数集合以及所有情景的后验参数集合对应的控制点处水头预测情况

    Figure 3. 

    图 4  初始集合以及S0、S5在浓度控制点处的归一化浓度穿透曲线

    Figure 4. 

    表 1  二维算例对数渗透系数参考场参数设置

    Table 1.  Parameters of the reference lnK

    岩性 变异函数
    类型
    均值
    /(m·d−1
    标准差
    /(m·d−1
    x方向
    变程/m
    y方向
    变程/m
    砂土 指数型 2.0 0.5 200 200
    黏土 指数型 −1.5 0.5 200 200
    下载: 导出CSV

    表 2  二维算例含水层渗透系数场估计的情景设置及估计结果

    Table 2.  Estimation of the two-dimensional aquifer hydraulic conductivity field in different scenarios

    情景 方法
    (迭代次数)
    IRMSE(lnK
    /(m·d−1
    IES(lnK
    /(m·d−1
    运行
    时间/s
    与S0
    比值/%
    S0 rNS-EnKF() 1.38 1.19 1680 100%
    S1 NS-ES-MDA(1) 1.40 1.31 254 15%
    S2 NS-ES-MDA(2) 1.28 1.18 354 21%
    S3 NS-ES-MDA(4) 1.05 0.95 628 37%
    S4 NS-ES-MDA(6) 0.92 0.82 901 54%
    S5 NS-ES-MDA(8) 0.91 0.76 1084 65%
    S6 NS-ES-MDA(10) 0.92 0.74 1285 76%
      注:rNS-EnKF不是迭代算法,没有迭代次数;IRMSE(lnK)代表集合均值与真实lnK值的均方根误差;IES(lnK)是后验参数集合的集合扩散;运行时间指在CPU主频为3.80 GHz的计算机上运行所用时间;与S0的比值为不同情景运行时间与S0运行时间的比值。
    下载: 导出CSV

    表 3  水头控制点处评价指标

    Table 3.  Metrics at head control points

    评价指标 初始集合 S0 S1 S2 S3 S4 S5 S6
    IRMSE(Head #1)/m 12.10 1.07 38.00 5.82 1.03 0.70 0.24 1.22
    IES(Head #1)/m 27.88 4.47 50.17 18.28 8.53 6.27 5.51 5.03
    INSE(Head #1) 0.03 0.99 −8.59 0.78 0.99 1.00 1.00 0.99
    IRMSE(Head #2)/m 57.96 3.14 230.50 41.99 5.30 6.14 3.00 1.42
    IES(Head #2)/m 50.92 12.54 202.68 76.99 26.19 14.53 9.68 8.84
    INSE(Head #2) 0.72 1.00 −3.40 0.85 1.00 1.00 1.00 1.00
    IRMSE(Head #3)/m 123.40 9.81 416.68 72.18 19.15 24.69 11.03 3.89
    IES(Head #3)/m 100.99 17.04 255.07 98.46 38.17 21.65 13.06 12.09
    INSE(Head #3) 0.70 1.00 −2.42 0.90 0.99 0.99 1.00 1.00
    下载: 导出CSV

    表 4  浓度控制点处的评价指标

    Table 4.  Metrics at concentration control points

    评价指标 初始集合 S0 S1 S2 S3 S4 S5 S6
    IRMSE(Conc #4)/(g·m−3 4.57 3.80 3.28 2.41 1.25 0.89 0.84 0.71
    IES(Conc #4)/(g·m−3 6.58 2.69 4.72 3.19 1.29 0.84 0.79 0.75
    INSE(Conc #4) −0.21 0.42 0.57 0.75 0.92 0.97 0.96 0.97
    IRMSE(Conc #5)/(g·m−3 1.86 2.74 3.09 2.54 0.80 0.28 0.24 0.25
    IES(Conc #5)/(g·m−3 2.61 1.64 2.18 1.84 0.99 0.55 0.38 0.33
    INSE(Conc #5) 0.34 0.79 0.67 0.72 0.95 0.99 0.99 0.99
    IRMSE(Conc #6)/(g·m−3 25.12 26.63 28.40 28.07 27.79 18.57 9.99 6.84
    IES(Conc #6)/(g·m−3 13.19 8.82 9.77 8.61 7.96 6.76 6.22 5.58
    INSE(Conc #6) −0.21 −0.83 −1.06 −0.98 −1.06 0.57 0.99 1.00
    下载: 导出CSV
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出版历程
收稿日期:  2023-08-04
修回日期:  2023-10-29
刊出日期:  2024-05-15

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