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基于物理引导神经网络的库岸滑坡变形预测与预警模型

  

  • 出版日期:2026-08-21 发布日期:2026-08-21

Reservoir bank landslide deformation prediction and early warning model based on Physics-guided Neural Network

  • Online:2026-08-21 Published:2026-08-21

摘要: 针对库水位涨落下库岸边坡非线性变形预测精度不足与滞后问题,以白家包滑坡为例,提出一种基于物理引导神经网络(PGNN)的变形预测模型。首先通过数值模拟揭示库水波动下滑坡渗流滞后与稳定性演化机制,发现年度调度周期内库水位首次快速下降至低值附近时,边坡的安全系数降至最低,外部支撑最弱、孔压滞后效应最强,对应边坡最不利稳定状态。在此基础上, PGNN以多层感知机为基线网络,结合软阈值门控与多目标损失,依据安全系数阈值实现基础变形与非线性阶跃变形的解耦与预测。对比基线模型、LSTM和GRU,PGNN模型在三个监测点的预测均方根误差平均降低了61.7%、27.3%和38.4%,决定系数平均值提升至0.84,平均偏差均值接近于零。同时反演得到滑坡启动的临界安全系数阈值为1.091,可为库区滑坡预警判定与风险管控提供定量依据。

Abstract: To address the insufficient prediction accuracy and hysteresis effect of nonlinear deformation of reservoir bank slopes under reservoir water level fluctuation, taking the Baijiabao landslide as the research object, this study proposes a deformation prediction model based on Physics-guided Neural Network (PGNN). Firstly, numerical simulation is adopted to reveal the seepage hysteresis and stability evolution mechanism of landslides induced by reservoir water level variation. The results show that within the annual reservoir operation cycle, the safety factor of the slope reaches the minimum value when the reservoir water level first rapidly drops to the low level, accompanied by the weakest external support and the strongest pore water pressure hysteresis effect, which corresponds to the most unfavorable stability state of the slope. On this basis, the PGNN takes the multi-layer perceptron as its baseline network. Combined with soft threshold gating and a multi-objective loss function, it realizes the decoupling and prediction of fundamental deformation and nonlinear step deformation based on the threshold of the safety factor. Compared with the baseline model, LSTM, and GRU, the average root mean square error of prediction at three monitoring points of the PGNN model is reduced by 61.7%, 27.3% and 38.4% respectively, the average coefficient of determination is improved to 0.84, and the mean bias error is close to zero. Meanwhile, the critical safety factor threshold triggering landslide initiation is determined via simultaneous inversion as 1.091, which can provide a quantitative reference for early warning judgment and risk management and control of reservoir landslides.

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