四川康定日地沟"8·3"泥石流灾害大块石冲击特征分析OA
Analysis of impact characteristics of large boulders in the"August 3"debris flow disaster in Ridi gully,Kangding,Sichuan
裹挟大块石的泥石流往往会对建筑物和构筑物造成比常规泥石流更严重的破坏,如四川康定日地沟"8·3"特大型泥石流,裹挟大块石冲毁高速桥梁、淤埋房屋、堵塞康定河.文章通过现场调查结合现有泥石流裹挟大块石研究结论,分析了本次泥石流灾害的成灾特征,结合无人机航测图探究了大块石的分布、冲击特征及大块石成因,并提出相应的防治建议.结果表明:日地沟泥石流浆体冲击力为 102.39 kN,最大块石冲击力为 30 638.54 kN,块石冲击力可达泥石流浆体冲击力的 300倍以上;日地沟流域内崩滑体极为发育,滑坡 16处,崩塌 157处,泥石流流量较大,在断桥处泥石流峰值流量可达 1 600 m3/s;大块石分布密集程度与流域内崩滑体灾害发育状况成正比,频繁发生地震加剧崩滑体的发育,促进大块石的形成.日地沟流域内存在新增山体裂隙,山体崩滑的可能性极大.
Debris flows carrying large boulders often cause more severe damage to buildings and structures than conventional debris flows.The"August 3"extreme large debris flow in Ridi gully carried large boulders,destroyed an expressway bridge,buried houses,and blocked the Kangding River.Based on field investigation and existing research results on large boulders in debris flows,this paper analyzes the disaster-causing characteristics of the debris flow.It also explores the distribution,impact characteristics and causes of large boulders in combination with UAV aerial survey images,and puts forward corresponding prevention and control suggestions.The impact force of debris flow slurry in Ridi gully is 102.39 kN,and the maximum impact force of large boulders is 30 638.54 kN,which can be more than 300 times that of slurry.Collapses and landslides are extremely developed in the Ridi gully basin,with 16 landslides and 157 collapses.The debris flow discharge is large,and the peak debris flow discharge at the broken bridge can reach 1 600 m3/s.The distribution density of large boulders is positively correlated with the development degree of collapses and landslides in the basin.Frequent earthquakes intensify the development of collapses and landslides and promote the formation of large boulders.New mountain fissures exist in the Ridi gully basin,which is under great threat of mountain collapse and landslide.
申文豪;胡桂胜;贺拿;李雨阳
河南理工大学土木工程学院,河南 焦作 454000||中国科学院、水利部成都山地灾害与环境研究所,四川 成都 610041河南理工大学土木工程学院,河南 焦作 454000||中国科学院、水利部成都山地灾害与环境研究所,四川 成都 610041河南理工大学土木工程学院,河南 焦作 454000河南理工大学土木工程学院,河南 焦作 454000||中国科学院、水利部成都山地灾害与环境研究所,四川 成都 610041
天文与地球科学
日地沟泥石流块石冲击力分布特征
Ridi gullydebris flowboulderimpact forcedistribution characteristics
《中国地质灾害与防治学报》 2026 (3)
43-55,13
国家自然科学基金面上项目(42471095)国家重点研发计划课题(2023YFC3008301)四川省自然科学基金项目(2023NSFSC2086)
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