基于地貌演化阶段的公路泥石流危险性评价  

Hazard assessment of debris flow along highway based on geomorphic evolution stages

作　　者：陈远川[1,2] 陈洪凯[2] 唐红梅[2] 

机构地区：[1]重庆文理学院经济管理学院,重庆402160 [2]重庆交通大学岩土工程研究所,重庆400074

出　　处：《长安大学学报（自然科学版）》2013年第5期45-51,共7页Journal of Chang’an University(Natural Science Edition)

基　　金：国家自然科学基金项目(41071017);交通运输部西部交通建设科技项目(2009 318 221 035)

摘　　要：为了运用地学方法对公路泥石流危险性进行评价,建立了泥石流沟不同地貌演化阶段与泥石流灾害规模、频率的关系,构建了泥石流沟不同演化阶段与泥石流灾害危险性等级之间的映射关系,据此进行公路泥石流灾害危险性评价。以横断山区美姑河流域公路泥石流为例,从区域新构造应力场、泥石流物源和气象条件3个方面分析了泥石流灾害发育的宏观规律,并应用泥石流沟发育阶段与泥石流灾害危险性等级的映射关系评价美姑河流域沿河公路泥石流灾害危险性。研究结果表明:泥石流沟谷地貌的整个演化过程中,在壮年偏幼年期泥石流灾害危险性等级最高,各发育阶段按泥石流灾害危险性大小由高到低排序为壮年偏幼、壮年、幼年、壮年偏老、老年;横断山区美姑河流域公路泥石流沟77.5%处于危及公路地质安全的状态。Based on the relationships between evolution stage of debris flow gully and disaster scale, frequency, and hazard level, highway debris flow hazard can be assessed. The macro-law of forming debris flow disaster in Meigu river basin was analyzed from the perspective of regional new tectonic stress field.material sources and meteorological conditions. The established relation- ship between evolution stage of debris flow gully and debris flow hazard level was applied to the highway debris flow hazard assessment for Meigu river. The results show that in strong-to-young stage the debris flow gully has the highest hazard level, and the rank of hazard level in life cycle of debris flow gully from high to low is strong-to-young, strong, young, strong-to-old and old. 77.5% of the debris flow gullies along Meigu river highway are in the state of endangering high- way geology security.

关 键 词：道路工程 山区沿河公路 公路泥石流 危险性评价 地貌演化 美姑河 

分 类 号：U418.56[交通运输工程—道路与铁道工程] P642.23[天文地球—工程地质学]