Peak Breach Discharge Prediction for Landslide Dams Using a Bayesian-Optimized XGBoost Model and Sensitivity Analysis
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摘要:
准确且迅速地评估堰塞坝溃决洪峰流量,对应急抢险至关重要.基于机器学习方法预测突发型堰塞坝溃决参数是当前的研究热点,而目前堰塞坝数据库缺少足够案例量,且堰塞坝溃决洪峰流量预测模型无法考虑各影响因素之间的非线性映射关系,这导致模型的泛化能力弱.基于此,采用泥沙冲刷模型模拟堰塞坝溃决过程,从而扩充堰塞坝溃决案例数据库;建立贝叶斯算法优化的极端梯度提升(XGBoost)的机器学习算法;提出考虑堰塞坝几何形态参数(坝高、坝宽、坝长、坝体积)、堰塞湖库容、诱发因素、物质组成(侵蚀度和结构类型)等8个影响因素的非均质堰塞坝溃决洪峰流量机器学习预测模型;基于参数敏感性分析,进一步建立便于堰塞湖灾害应急抢险使用的简化三参数模型.结果表明,与传统模型相比,贝叶斯优化的XGBoost模型具有更高的预测精度;基于唐家山和白格堰塞坝案例分析证实本文模型预测溃决洪峰流量与真实值最大误差约20%.研究成果能够为堰塞坝应急抢险地质处置及区域防灾减灾提供有益参考.
Abstract:Accurate and rapid assessment of peak flood discharge from landslide dam breaches is crucial for emergency response efforts. Predicting breach parameters of sudden landslide dam failures using machine learning methods has become a current research focus. However, existing landslide dam database slack sufficient case records, and current predictive models for peak breach discharge fail to capture the nonlinear interactions among influencing factors, resulting in limited generalization capability. In response to this, this study employs a sediment erosion model to simulate the landslide dam breach process, thereby expanding the landslide dam breach case database. The Extreme Gradient Boosting (XGBoost) machine learning algorithm is used to predict the peak flood discharge of landslide dam breaches, and the Bayesian algorithm is employed to optimize the hyperparameters of the XGBoost model. An innovative machine learning prediction model for peak flood discharge of heterogeneous landslide dam breaches is proposed, considering eight influencing factors, including geometric parameters of the dam (height, width, length, volume), reservoir capacity, triggering factors, and material composition (erodibility and structural type). The results indicate that, compared to traditional models, the Bayesian-optimized XGBoost machine learning model exhibits higher prediction accuracy. Case analyses of Tangjiashan and Baige landslide dams confirm that the model's predicted peak flood discharge has a maximum error of approximately 20% compared to the actual values. This study provides a valuable reference for emergency response and regional disaster mitigation in the context of landslide dam breaches.
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Key words:
- landslide dam /
- dam breach /
- peak flood discharge /
- Bayesian optimization /
- XGBoost /
- engineering geology
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表 1 堰塞坝真实形态参数区间
Table 1. Parameter interval of real landslide dams
坝体类型 坝高∶坝顶宽 坝高∶坝底宽 上游坝坡坡度 下游坝坡坡度 坝体模型 1 0.2 26.56° 26.56° 堰塞坝案例库 0.2~3 0.02~1 11°~45° 11°~45° 表 2 模型优化参数
Table 2. Optimized model parameters
超参数名称 含义 范围 最终值 n_ estimators 决策树数量 (20, 100) 40 learning_ rate 学习率 (0.01, 1) 0.03 max_ depth 最大树深度 (1, 10) 6 表 3 不同堰塞坝溃决洪峰流量预测模型
Table 3. Different forecasting models for breach peak discharge of landslide dams
模型 参考文献 案例数 模型特征 $ {Q}_{\mathrm{p}}=6.3{H}_{\mathrm{d}}^{1.59} $ Costa and Schuster (1988) 36 单参数简单 $ {Q}_{\mathrm{p}}=3.130{H}_{\mathrm{d}}^{0.120}{W}_{\mathrm{d}}^{0.302}{V}_{\mathrm{d}}^{-0.106}{V}_{\mathrm{l}}^{0.453}{e}^{a} $ 石振明等(2014) 41 考虑坝体侵蚀度 $ \frac{{Q}_{\mathrm{p}}}{{g}^{1/2}{H}_{\mathrm{d}}^{5/2}}=0.828{\left(\frac{{H}_{\mathrm{d}}}{{H}_{\mathrm{r}}}\right)}^{-0.128}{\left(\frac{{H}_{\mathrm{d}}}{{W}_{\mathrm{d}}}\right)}^{-0.432}{\left(\frac{{V}_{\mathrm{d}}^{1/3}}{{H}_{\mathrm{d}}}\right)}^{-0.394}{\left(\frac{{V}_{\mathrm{l}}^{1/3}}{{H}_{\mathrm{d}}}\right)}^{1.151} $ 齐子杰等(2022) 57 未考虑坝体侵蚀度 $ \frac{{Q}_{\mathrm{p}}}{{g}^{1/2}{H}_{\mathrm{d}}^{5/2}}={\left(\frac{{H}_{\mathrm{d}}}{{H}_{\mathrm{r}}}\right)}^{-1.417}{\left(\frac{{H}_{\mathrm{d}}}{{W}_{\mathrm{d}}}\right)}^{-0.265}{\left(\frac{{V}_{\mathrm{d}}^{1/3}}{{H}_{\mathrm{d}}}\right)}^{-0.471}{\left(\frac{{V}_{\mathrm{l}}^{1/3}}{{H}_{\mathrm{d}}}\right)}^{1.569}{e}^{a} $ Peng and Zhang (2012) 45 考虑坝体侵蚀度的多参数模型 贝叶斯优化XGBoost机器学习模型 本文模型 122 考虑坝体侵蚀度的多参数模型 注:$ {Q}_{\mathrm{p}} $溃决洪峰流量,$ {H}_{\mathrm{d}} $堰塞坝高度,$ {W}_{\mathrm{d}} $堰塞坝宽度,$ {V}_{\mathrm{d}} $堰塞坝体积量,$ {V}_{\mathrm{l}} $堰塞湖库容,a堰塞坝体侵蚀度. 表 5 堰塞坝参数
Table 5. Landslide dam parameters
名称 坝高(m) 坝宽(m) 坝长(m) 坝体体积(m3) 库容(m3) 侵蚀度 结构类型 诱因 唐家山 82 611.8 406 20.4×106 247×106 中等 块石夹土 地震 白格 61 1 400 580 26×106 290×106 高 土夹碎石 山体失稳 表 6 不同堰塞坝溃决洪峰流量预测模型计算结果对比
Table 6. Comparison of calculation results of prediction models of breach peak discharge
案例名称 实测值(m3·s-1) 结果对比 本文全参数模型 本文三参数模型 唐家山 6 500 预测值(m3·s-1) 7 242.3 7 661.55 相对误差(%) 11.42 17.87 白格 10 000 预测值(m3·s-1) 11 013 12 175 相对误差(%) 10.13 21.75 -
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