吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (4): 1155-1163.doi: 10.13278/j.cnki.jjuese.201504201
徐佩华1, 袁中凡1, 李广杰1, 李光1, 杜文浩1, 王月华2
Xu Peihua1, Yuan Zhongfan1, Li Guangjie1, Li Guang1, Du Wenhao1, Wang Yuehua2
摘要:
长白山火山次生泥石流是由长白山火山喷发引起的火口湖中的水沿长白山北坡缺口,以类似水库溃坝的形式突然溢出而形成的短时间、大体积的水流,是携带着地表的松散堆积物,沿着沟谷和山坡向下快速流动的一种类似洪流的特殊泥石流.笔者在野外地质调查和室内模拟试验的基础之上,采用FLOW-3D数值模拟软件,对长白山火山喷发引起的次生泥石流灾害进行大范围的数值模拟,并着重研究其对二道白河镇地区的影响程度,旨在为政府决策和防灾提供依据.结果表明:泥石流总体积为30.27亿m3时,二道白河镇将完全被泥石流淹没;不论哪种泥石流体积假设情况,泥石流都将到达二道白河镇,并对其造成危害;一旦火山爆发,二道白河镇居民可逃生时间只有30~42 min.
中图分类号:
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