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    物理引导的库岸谷幅变形智能预测模型

    陈铭熙 林朋辉 蒋舒 姜清辉

    陈铭熙, 林朋辉, 蒋舒, 姜清辉, 2026. 物理引导的库岸谷幅变形智能预测模型. 地球科学, 51(2): 560-577. doi: 10.3799/dqkx.2025.216
    引用本文: 陈铭熙, 林朋辉, 蒋舒, 姜清辉, 2026. 物理引导的库岸谷幅变形智能预测模型. 地球科学, 51(2): 560-577. doi: 10.3799/dqkx.2025.216
    Chen Mingxi, Lin Penghui, Jiang Shu, Jiang Qinghui, 2026. Research on Physics-Guided Intelligent Prediction Model for Valley Contraction Deformation of Reservoir Bank Slopes. Earth Science, 51(2): 560-577. doi: 10.3799/dqkx.2025.216
    Citation: Chen Mingxi, Lin Penghui, Jiang Shu, Jiang Qinghui, 2026. Research on Physics-Guided Intelligent Prediction Model for Valley Contraction Deformation of Reservoir Bank Slopes. Earth Science, 51(2): 560-577. doi: 10.3799/dqkx.2025.216

    物理引导的库岸谷幅变形智能预测模型

    doi: 10.3799/dqkx.2025.216
    基金项目: 

    广西自然科学基金项目 2024GXNSFBA010226

    广西科技重大专项 AA23023016

    广西科技基地和人才专项项目 AD23026111

    国家自然科学基金项目 52509141

    广西青年科技人才工程资助 GXYESS2025142

    广西青苗人才计划项目 ZX02080030324020

    详细信息
      作者简介:

      陈铭熙(1993-),男,助理教授,博士,主要从事滑坡灾害预测预警与风险评估等方面的教学和科研. ORCID:0000-0003-3988-8329. E-mail:chenmingxi@gxu.edu.cn

      通讯作者:

      姜清辉, ORCID:0000-0002-6511-8208. E-mail: jqh1972@whu.edu.cn

    • 中图分类号: P694

    Research on Physics-Guided Intelligent Prediction Model for Valley Contraction Deformation of Reservoir Bank Slopes

    • 摘要: 库岸谷幅持续收缩变形会威胁大坝安全,因此谷幅变形预测对大坝安全管理至关重要.以溪洛渡水电站谷幅变形为研究对象,提出一种基于物理引导的智能预测模型,开展谷幅变形预测. 基于谷幅变形规律分析,建立统计回归物理模型(STPM),获取不同诱发因素对谷幅变形贡献的位移分量. 据此,以各分量为输入,联合灰色关联度分析(GRA)、长短期记忆网络(LSTM)和随机森林(RF),构建基于物理引导的机器学习预测框架(STPM-GRA-LSTM-RF),开展不确定性预测分析. 研究结果表明:(1)溪洛渡谷幅变形主要由黏塑性变形、黏弹性变形和有效应力引起,对总位移平均贡献率分别为67.71%、29.75%及2.51%;(2)与STPM模型、LSTM模型、SVM模型和XGBoost模型相比,本文提出模型的预测精度更高,并因其考虑了谷幅变形机制,可靠性显著提升. 研究成果为类似库岸高边坡的变形预测与安全管控提供有价值的参考.

       

    • 图  1  溪洛渡水库鸟瞰图(来源于Google Earth)

      Fig.  1.  Aerial view of Xiluodu Reservoir (from Google Earth)

      图  2  溪洛渡水库地质剖面图

      Fig.  2.  Geological profile of Xiluodu Reservoir

      图  3  溪洛渡水库谷幅测线布置平面图

      Fig.  3.  Configuration of valley measuring lines for Xiluodu Reservoir

      图  4  溪洛渡谷幅变形与库水位监测曲线

      Fig.  4.  Monitoring curves of valley deformation and reservoir water level at Xiluodu Reservoir

      图  5  VD3谷幅变形、变形速率及库水位曲线

      Fig.  5.  Valley deformation, deformation velocity and reservoir water level of the measuring line VD3

      图  6  不同库水条件下VD3谷幅变形时间曲线

      Fig.  6.  Displacement-time curve of the measuring line VD3 under different reservoir water conditions

      图  7  谷幅变形拟合结果

      a. VD1;b.VD3;c.VD5

      Fig.  7.  The fitting results of valley deformation

      图  8  基于物理引导的谷幅变形预测流程图

      Fig.  8.  Flowchart of physics-guided prediction model for valley deformation

      图  9  单个LSTM单元结构图

      Fig.  9.  Schematic diagram of a single LSTM unit structure

      图  10  LSTM全网络结构图

      Fig.  10.  Rchitecture diagram of the LSTM network

      图  11  超参数敏感性分析

      Fig.  11.  Sensitivity analysis of hyperparameters

      图  12  灰色关联度计算结果

      a.VD1灰色关联度计算结果;b. VD3灰色关联度计算结果;c. VD5灰色关联度计算结果

      Fig.  12.  Calculation results of grey correlation degree

      图  13  不同模型预测结果

      a. VD1;b. VD3;c. VD5

      Fig.  13.  Prediction results across models

      图  14  不同模型预测区间对比

      Fig.  14.  Comparative analysis of prediction intervals across different models

      图  15  点预测评价指标

      a. VD1;b. VD3;c. VD5

      Fig.  15.  Evaluation metrics for point prediction

      图  16  区间预测评价指标

      Fig.  16.  Evaluation metrics for interval prediction

      图  17  模型外推预测结果

      a. VD1;b. VD3;c. VD5

      Fig.  17.  Extrapolated predictive outputs of the model

      图  18  特征重要性

      a. VD1;b. VD3;c. VD5

      Fig.  18.  Importance of features

      表  1  统计回归物理模型参数计算结果

      Table  1.   Calculation results of model parameters in statistical regression physical model

      谷幅测线 α1 α2 α3 b1 α4 R2
      VD1 0.050 105.649 2.336 23.898 0.015 0.97
      VD3 0.067 91.995 2.930 21.885 0.015 0.97
      VD5 0.046 113.745 2.636 29.000 0.012 0.96
      下载: 导出CSV

      表  2  超参数设置表

      Table  2.   Configuration settings of hyperparameters

      参数 定义 设置值
      batch_size 每次训练选取的数据样本数量 64
      optimizer 优化调整网络的权重和偏置 Adam
      epoch 模型训练时期次数 300~400
      dropout 模型训练阶段忽略单元 0.01
      hidden_size 隐藏层的维度大小 32、128
      损失函数 衡量预测值与真实值的差距 Huber
      隐藏层数 神经网络中的中间层 2
      下载: 导出CSV

      表  3  点预测评价指标对比

      Table  3.   Comparison of point prediction evaluation metrics

      测线 MAE MSE RMSE MAPE R2
      VD1a 0.99 1.49 1.22 2.24% 0.99
      VD1b 2.01 6.35 1.49 5.22% 0.97
      VD1c 2.92 14.25 3.78 6.81% 0.94
      VD1d 1.43 3.89 1.97 4.83% 0.98
      VD1e 2.02 6.24 2.50 6.57% 0.97
      VD1d 2.02 6.24 2.50 6.57% 0.97
      VD3a 1.18 1.95 1.40 2.22% 0.99
      VD3b 2.02 7.32 2.71 4.93% 0.98
      VD3c 3.36 18.51 4.30 6.95% 0.94
      VD3d 1.67 5.01 2.23 3.61% 0.98
      VD3e 2.78 11.54 3.40 7.35% 0.97
      VD5a 0.92 1.38 1.17 1.89% 0.99
      VD5b 1.72 6.07 2.46 4.51% 0.97
      VD5c 3.05 15.55 3.94 6.63% 0.93
      VD5d 1.57 4.34 2.08 3.54% 0.98
      VD5e 2.77 9.99 3.16 5.11% 0.96
      注:a代表STPM-GRA-LSTM-RF;b代表LSTM模型;c代表SVM模型;d代表XGBoost模型;e代表STPM模型
      下载: 导出CSV
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    • 收稿日期:  2025-04-27
    • 刊出日期:  2026-02-25

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