[1]陈源井,余斌,朱渊,等.地震后泥石流临界雨量变化特征——以汶川地震区小岗剑沟为例[J].山地学报,2013,(03):356.
 CHEN Yuanjing,YU Bin,ZHU Yuan,et al.Characteristics of Critical Rainfall of Debris Flow after Earthquake——A Case Study of the Xiaogangjian Gully[J].Mountain Research,2013,(03):356.
点击复制

地震后泥石流临界雨量变化特征——以汶川地震区小岗剑沟为例()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2013年03期
页码:
356
栏目:
山地灾害
出版日期:
2013-01-01

文章信息/Info

Title:
Characteristics of Critical Rainfall of Debris Flow after Earthquake——A Case Study of the Xiaogangjian Gully
作者:
陈源井;余斌;朱渊;王涛;亓星;
成都理工大学地质灾害防治与地质环境保护国家重点实验室,四川 成都 610059
Author(s):
CHEN YuanjingYU BinZHU YuanWANG TaoQI Xing
State Key Laboratory of Geo-hazard Prevention and Geo-environment Protection,Chengdu University of Technology,Chengdu 610059,China
关键词:
小岗剑沟泥石流地震起动机理临界雨量
Keywords:
Xiaogangjian Gully debris flow earthquake initiation mechanism rainfall threshold
分类号:
P624.23
文献标志码:
A
摘要:
在地震的影响下,泥石流暴发所需的临界降雨条件降低。通过现场调查分析,首先得出小岗剑沟泥石流沟床起动的形成机理及其"地震-滑坡-碎屑堆积-降雨-泥石流"的形成特征,然后在建立了泥石流发生的临界雨量模式基础上,以小岗剑沟泥石流临界雨量为研究对象,采用将其地震前后临界雨量相比较的方法,得到了临界雨量的变化特征,并探索变化的原因。小岗剑沟2010年暴发泥石流的临界雨量约为地震前的21%,2011年暴发泥石流的临界雨量约为地震前的23%,地震后临界雨量大幅度下降。但随着泥石流活动的不断发生,临界雨量有逐渐恢复的趋势。
Abstract:
The triggering thresholds such as cumulative antecedent rainfall and one hour rainfall intensity significantly decreased after earthquake events. The formation mechanism of debris flows in Xiaogangjian Gully of Qingping Township,Mianzhu County,Sichuan Province,China was obtained by field survey and analysis on the initiation of debris flows. The description of “earthquake-landslide-deposits-rainfall-debris flows” was the formation characteristic of debris flow in this gully. Base on the occurrence model of rainfall threshold of debris flow,the drop characteristics of rainfall threshold was obtained by comparing the thresholds of before and after the earthquake. The rainfall threshold of 2010 is only 21% of the rainfall threshold before earthquake,and it is only 23% in 2011. The threshold dropped noticeably right after earthquake events, and rose gradually thereafter.

相似文献/References:

[1]蒋志林,朱静,常鸣,等.汶川地震区红椿沟泥石流形成物源量动态演化特征[J].山地学报,2014,(01):81.
 JIANG Zhilin,ZHU Jing,CHANG Ming,et al.Dynamic Evolution Characteristics of Hongchun Gully Source Area of Debris Flow in Wenchuan Earthquake Region[J].Mountain Research,2014,(03):81.
[2]常鸣,唐川,蒋志林,等.强震区都江堰市龙池镇泥石流物源的遥感动态演变[J].山地学报,2014,(01):89.
 CHANG Ming,TANG Chuan,JIANG Zhilin,et al.Dynamic Evolution Process of Sediment Supply for Debris Flow Occurrence in Longchi of Dujiangyan,Wenchuan Earthquake Area[J].Mountain Research,2014,(03):89.
[3]王 钧,欧国强,杨 顺,等.地貌信息熵在地震后泥石流危险性评价中的应用[J].山地学报,2013,(01):83.
 WANG Jun,OU Guoqiang,YANG Shun,et al.Applicability of Geomorphic Information Entropy in the Postearthquake Debris Flow Risk Assessment[J].Mountain Research,2013,(03):83.
[4]王东坡,何思明,葛胜锦,等.“9?07”彝良地震诱发次生山地灾害调查及减灾建议[J].山地学报,2013,(01):101.
 WANG Dongpo,HE Siming,GE Shengjin,et al.Mountain Hazards Induced by the Earthquake of Sep 07,2012 in Yiliang and the Suggestions of Disaster Reduction[J].Mountain Research,2013,(03):101.
[5]喻 武,万 丹,汪书丽,等.藏东南泥石流沉积区植物群落结构和物种多样性特征[J].山地学报,2013,(01):120.
 YU Wu,WAN Dan,WANG Shuli,et al.Community Structure and Species Diversity of Debris Flow Deposition Area in Southeast of Tibet,China[J].Mountain Research,2013,(03):120.
[6]崔鹏,陈晓清,张建强,等.“4·20”芦山7.0级地震次生山地灾害活动特征与趋势[J].山地学报,2013,(03):257.
 CUI Peng,CHEN Xiaoqing,ZHANG Jianqiang,et al.Activities and Tendency of Mountain Hazards Induced by the Ms7.0 Lushan Earthquake,April 20,2013[J].Mountain Research,2013,(03):257.
[7]邹强,崔鹏,杨伟,等.G318川藏公路段泥石流危险性评价[J].山地学报,2013,(03):342.
 ZOU Qiang,CUI Peng,YANG Wei.Hazard Assessment of Debris Flows along G318 Sichuan-Tibet Highway[J].Mountain Research,2013,(03):342.
[8]王根龙,张茂省,于国强,等.舟曲2010年“8·8”特大泥石流灾害致灾因素[J].山地学报,2013,(03):349.
 WANG Genlong,ZHANG Maosheng,YU Guoqiang,et al.Factor Analysis for Catastrophic Debris Flows on August 8,2010 in Zhouqu City of Gansu,China[J].Mountain Research,2013,(03):349.
[9]游勇,柳金峰,陈兴长,等.芦山“4·20”地震后宝兴县城打水沟泥石流发育趋势及防治方案[J].山地学报,2013,(04):495.
 YOU Yong,LIU Jinfeng,CHEN Xingzhang.The Potential Tendency and Mitigation Measures of Dashui Gully in Baoxing Coutny after Lushan“4?20”Earthquake of Schuan[J].Mountain Research,2013,(03):495.
[10]乐茂华,朱静,黄勋,等.雍家沟泥石流活动特征与堵江[J].山地学报,2013,(05):573.
 LE Maohua,ZHU Jing,HUANG Xun,et al.Activity Characteristics and Damming of Yongjiagou Debris Flow in Qingping Area after Wenchuan Earthquake[J].Mountain Research,2013,(03):573.
[11]杨东旭,陈晓清,游勇,等.汶川地震区绵竹小岗剑沟泥石流发展趋势[J].山地学报,2012,(06):701.
 YANG Dongxu,CHEN Xiaoqing,YOU Yong,et al.The Debris Flow Development Trend of in Xiaogangjian Gully in Mianzhu County,Wenchuan Earthquake Zone[J].Mountain Research,2012,(03):701.

备注/Memo

备注/Memo:
收稿日期(Received date):2013-01-25;改回日期(Accepted):2013-04-10。
基金项目(Foundation item):贵州省地质灾害监测预警与决策支持平台研究子项目贵州省泥石流启动机理及预警预报研究(编号 ZG0064)。[Guizhou Province Geological Disaster Monitoring and Early Warning and Decision Support Platform Research Subprojects: Guizhou Province Debris Flow Start Mechanism and Early Warning and Forecasting(No.ZG0064).]
作者简介(Biography):陈源井(1987-),男,四川郫县人,硕士研究生,主要从事地质灾害防治相关工作。[Chen Yuanjing( 1987-) ,male,Han nationality,born in Pixian County, Sichuan,graduated student,Undertaking research on prevention of geological disasters.]E-mail:877811775@qq.com
更新日期/Last Update: 1900-01-01