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    基于贝叶斯优化XGBoost的堰塞坝溃决洪峰流量预测模型及参数敏感性研究

    吴昊 吴家伟 郑德凤 钟启明 年廷凯

    吴昊, 吴家伟, 郑德凤, 钟启明, 年廷凯, 2026. 基于贝叶斯优化XGBoost的堰塞坝溃决洪峰流量预测模型及参数敏感性研究. 地球科学, 51(4): 1489-1498. doi: 10.3799/dqkx.2025.238
    引用本文: 吴昊, 吴家伟, 郑德凤, 钟启明, 年廷凯, 2026. 基于贝叶斯优化XGBoost的堰塞坝溃决洪峰流量预测模型及参数敏感性研究. 地球科学, 51(4): 1489-1498. doi: 10.3799/dqkx.2025.238
    Wu Hao, Wu Jiawei, Zheng Defeng, Zhong Qiming, Nian Tingkai, 2026. Peak Breach Discharge Prediction for Landslide Dams Using a Bayesian-Optimized XGBoost Model and Sensitivity Analysis. Earth Science, 51(4): 1489-1498. doi: 10.3799/dqkx.2025.238
    Citation: Wu Hao, Wu Jiawei, Zheng Defeng, Zhong Qiming, Nian Tingkai, 2026. Peak Breach Discharge Prediction for Landslide Dams Using a Bayesian-Optimized XGBoost Model and Sensitivity Analysis. Earth Science, 51(4): 1489-1498. doi: 10.3799/dqkx.2025.238

    基于贝叶斯优化XGBoost的堰塞坝溃决洪峰流量预测模型及参数敏感性研究

    doi: 10.3799/dqkx.2025.238
    基金项目: 

    国家自然科学基金资助项目 U2443227

    国家自然科学基金资助项目 42577172

    国家自然科学基金资助项目 42207228

    详细信息
      作者简介:

      吴昊(1992-),男,副教授,博士,主要从事滑坡灾害链演化机理与数智减灾技术方面的研究. ORCID:0000-0002-9380-7369. E-mail:wuhaogeot@njtech.edu.cn

      通讯作者:

      年廷凯(1971-),男,教授,博导,主要从事岩土工程、地质灾害与生态护坡方面的研究. ORCID: 0000-0002-1458-5500. E-mail: tknian@dlut.edu.cn

    • 中图分类号: P642

    Peak Breach Discharge Prediction for Landslide Dams Using a Bayesian-Optimized XGBoost Model and Sensitivity Analysis

    • 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.

       

    • 图  1  基于贝叶斯优化XGBoost的堰塞坝溃决洪峰流量预测模型构建方法

      Fig.  1.  Method for constructing the prediction model of peak flood discharge of landslide dam breach based on Bayesian Optimization XGBoost

      图  2  贝叶斯优化XGBoost预测模型全数据(a)和测试集(b)预测结果

      Fig.  2.  Prediction results on full data set (a) and test data set (b)

      图  3  预测模型在测试集中泛化能力对比

      Fig.  3.  Comparison of generalization ability of prediction model in test set

      图  4  敏感性分析结果

      Fig.  4.  Sensitivity analysis results

      图  5  三参数预测模型全数据集预测结果(a)和测试集预测结果(b)

      Fig.  5.  Three-parameter prediction model results in full data (a) and test data (b)

      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°
      下载: 导出CSV

      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
      下载: 导出CSV

      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.
      下载: 导出CSV

      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 土夹碎石 山体失稳
      下载: 导出CSV

      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
      下载: 导出CSV
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    • 收稿日期:  2025-07-23
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