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贡嘎山东坡雅家埂河特大型泥石流动力学特征
引用本文:宋志,李宗亮,巴仁基,刘宇杰.贡嘎山东坡雅家埂河特大型泥石流动力学特征[J].西安地质学院学报,2010(4):416-419,435.
作者姓名:宋志  李宗亮  巴仁基  刘宇杰
作者单位:中国地质调查局成都地质调查中心,四川成都610082
基金项目:中国地质调查局项目(1212010814038)
摘    要:对2005年8月11日贡嘎山东坡雅家埂河特大型泥石流运动过程进行了描述,并采用现场实地勘查等手段,定量计算泥石流流速和流量等动力学特征,还运用得到的流量反演泥石流运动过程,从而得到雅家埂河特大型泥石流的形成机理。结果表明:雅家埂河特大型泥石流的形成与降雨有直接关系;雅家埂河支沟泥石流的群发性造成主河泥石流规模巨大;经对雅家埂河流域泥石流形成、发生的历史分析,推断出该流域泥石流存在18~21年的暴发周期;雅家埂河松散物源充足,降雨与水源丰富,地形地貌陡峭,极易再次发生规模较大的泥石流。

关 键 词:泥石流  支沟  雅家埂河  实地勘查  动力学特征  贡嘎山

Kinetic Characteristics of Oversize Mud-rock Flow in Yajiageng River of Eastern Gongga Mountain
Authors:SONG Zhi  LI Zong-liang  BA Ren-ji  LIU Yu-jie
Institution:(Chengdu Center of Geological Survey,China Geology Survey,Chengdu 610082,Sichuan,China)
Abstract:Motor process of oversize mud-rock flow in Yajiageng River of Eastern Gongga Mountain on August 11,2005 was described;kinetic characteristics of mud-rock flow were calculated quantificationally with the means of field survey,and was used to simulate the motor process of mud-rock flow in order to find the mechanism of oversize mud-rock flow in Yajiageng River.The results showed that formation of oversize mud-rock flow in Yajiageng River was directly related to the rainfall;mud-rock flow in tributary ditch of Yajiageng River meantime happened,and caused that the flow in the master river was huge;the eruptive period was 18-21 years according to the history of mud-rock flow in Yajiageng River;because loose material was plentiful,rainfall and water were rich and terrain was precipitous,oversize mud-rock flow in Yajiageng River could happen again.
Keywords:mud-rock flow  tributary ditch  Yajiageng River  field survey  kinetics characteristic  Gongga Mountain
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