IMHE OpenIR  > 山地灾害与地表过程重点实验室
宁南县矮子沟628特大灾害性泥石流成因和特征
胡凯衡; 崔鹏; 马超; 周公旦; 田密; 杨东旭; 刘维明
2012
Source Publication山地学报
ISSN1008-2786
Volume030Issue:006Pages:696
Abstract2012—06—28T5:00,四川省凉山彝族自治州宁南县矮子沟突降强暴雨,引发了特大灾害性泥石流,造成严重的人员伤亡和财产损失。此次泥石流是在长时间的前期降雨和短历时的强降雨共同作用下,从上游支沟坡面和两侧冲沟短时间内形成的,具有发展和运动历时短,规模中等而峰值流量大,泥石流和洪水交替作用等特点。严重的沟道堵塞和中下游松散物质的补充,使得泥石流的峰值流量是清水流量的3~4倍。
Language英语
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/31665
Collection山地灾害与地表过程重点实验室
Affiliation中国科学院成都山地灾害与环境科学研究所
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
胡凯衡,崔鹏,马超,等. 宁南县矮子沟628特大灾害性泥石流成因和特征[J]. 山地学报,2012,030(006):696.
APA 胡凯衡.,崔鹏.,马超.,周公旦.,田密.,...&刘维明.(2012).宁南县矮子沟628特大灾害性泥石流成因和特征.山地学报,030(006),696.
MLA 胡凯衡,et al."宁南县矮子沟628特大灾害性泥石流成因和特征".山地学报 030.006(2012):696.
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