首页|干流公路桥涵堵塞对泥石流灾害的风险放大效应

干流公路桥涵堵塞对泥石流灾害的风险放大效应

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2020年8月17日,四川省平武县亚者造祖村干流沿岸4条沟相继暴发泥石流,导致G247国道多处断道和垮方,九绵高速项目部及民工驻地等多处遭受巨大损毁,泥石流裹挟的大量漂木汇入干流后,引发下游公路桥涵堵塞并回水淹没村庄,放大了灾害风险.为了避免类似灾害再次发生,灾后基于野外调查和遥感解译等手段,探讨了此次泥石流灾害风险特征,并重点分析了干流公路桥涵堵塞对泥石流灾害的风险放大效应.结果表明:(1)亚者造祖村"8·17"泥石流为低频稀性大规模群发性泥石流,暴发频率约为50年一遇.阿祖沟和杂排沟泥石流在规模上属特大型,麻石扎三号沟和夺补河五号沟泥石流在规模上属大型,堆积扇受灾面积约为16.66×104m2.(2)干流公路桥涵布设不当,导致泥石流裹挟的大量漂木堵塞桥涵,形成堰塞体,致使受灾面积增大了 16.78×104m2,风险范围扩大了约1倍.(3)对于植被覆盖良好的湿润山区,干流公路桥涵修建时应适当增大桥墩之间的轴向间距,给河道预留出一定的宽度和运行空间,避免因漂木堵塞放大泥石流灾害风险.研究可为类似山区干流公路桥涵合理规划及泥石流相关防治预警工作提供参考.
Risk amplification effect caused by main stream road bridges and culverts blockages due to debris flow
On August 17,2020,debris flows successively occurred in four ravines along the main stream of Yazhezaozu Village,Pingwu County,Sichuan Province.This event resulted in multiple collapses and interruptions along the G247 national highway,and extensive damage to the Jiumian expressway project site and laborer residences,among other areas.A significant volume of driftwood carried by the debris flow converged into the main stream,leading to the blockage of downstream road bridges and culverts,causing backflow and village flooding,thereby exacerbating the disaster risk.To prevent similar disasters in the future,post-disaster investigations using field surveys and remote sensing interpretations explored the characteristics of this debris flow disaster's risk.A primary focus was placed on analyzing the risk amplification effect caused by blockages in main stream road bridges and culverts due to debris flow.The results indicated:(1)The'8.17'debris flow in Yazhezaozu Village was a low-frequency,large-scale,rare,and extensive group occurrence,with an eruption frequency of approximately once every 50 years.The debris flows in Azu Gully and Zapai Gully were extremely large-scale,while Mashizha No.3 Gully and Duobu River No.5 Gully were large-scale,with an affected debris fan area of about 16.66× 104 square meters.(2)Improper layout of main stream road bridges and culverts resulted in the blockages of driftwood carried by the debris flow,forming dammed bodies,increasing the affected area by 16.78× 104 square meters,and enlarging the risk range by about 1-fold.(3)In well-vegetated,moist mountainous areas,when constructing main stream road bridges and culverts,it is advisable to appropriately increase the axial spacing between bridge piers,allowing for a certain width and operational space in the river channel.This will prevent the amplification of debris flow disaster risks caused by driftwood blockages.This study aims to provide guidance for the reasonable planning of main stream road bridges and culverts in similar mountainous areas and relevant prevention and early warning of debris flows.

debris flowbridges and culvertsdriftwoodblockagerisk

杨静萍、陈宁生、杨志全、彭泰鑫、田树峰、黄娜

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昆明理工大学公共安全与应急管理学院,云南 昆明 650093

中国科学院、水利部成都山地灾害与环境研究所,四川成都 610299

长江大学地球科学学院,湖北武汉 430100

高原科学与可持续发展研究院,青海西宁 810016

中国科学院大学,北京 100049

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泥石流 桥涵 漂木 堵塞 风险

国家自然科学基金项目青海省自然科学基金项目国家重点研发项目课题国家资助博士后计划

423611448802024-ZJ-9042023YFC3008301GZC20232571

2024

中国地质灾害与防治学报
中国地质环境监测院

中国地质灾害与防治学报

CSTPCD
影响因子:1.096
ISSN:1003-8035
年,卷(期):2024.35(5)