[1]丁明涛,程尊兰,王青.“4·20”芦山地震灾区次生山地灾害易发性评价[J].山地学报,2014,(01):117.
 DING Mingtao,CHENG Zunlan,WANG Qing.Susceptibility Assessment on Secondary Mountain Hazards in “4·20”Lushan Earthquakestricken Area[J].Mountain Research,2014,(01):117.
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“4·20”芦山地震灾区次生山地灾害易发性评价()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2014年01期
页码:
117
栏目:
“4?21”芦山地震
出版日期:
2014-01-01

文章信息/Info

Title:
Susceptibility Assessment on Secondary Mountain Hazards in “4·20”Lushan Earthquakestricken Area
作者:
丁明涛;程尊兰;王青
1. 西南科技大学环境与资源学院,四川 绵阳621010;
2. 中国科学院水利部成都山地灾害与环境研究所,四川 成都610041
Author(s):
DING Mingtao CHENG Zunlan WANG Qing
1. School of Environment and Resource, Southwest University of Science and Technology,Mianyang 621010,Sichuan China;
2. Institute of Mountain Hazards and Environment,Chinese Academy of Sciences,610041 Chengdu, China
关键词:
芦山地震灾区次生山地灾害易发性评价信息量模型
分类号:
P642.2,P694,X43
文献标志码:
A
摘要:
选择"4·20"芦山地震灾区为研究区,在野外实地考察的基础上,结合高精度遥感影像解译分析,针对地震灾区滑坡、崩塌和泥石流等次生山地灾害的形成条件展开系统分析;在ArcGIS 9.3软件支持下,采用信息量模型,选择坡向、坡度、地层岩性、断裂带、河流冲刷作用、地震烈度和降水量7个影响因子作为芦山地震灾区次生山地灾害易发性评价的指标参数,将其划分为高易发区、中易发区和低易发区,该评价结果与实地考察结果基本吻合。基于GIS的信息量模型能够很好地为芦山地震灾区次生山地灾害易发性区划研究提供指导,其结果可以用来解决次生山地灾害易发性评价中效率低、精度差、费时费力等问题,从而实现次生山地灾害易发性评价的信息化和科学化。

参考文献/References:

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[2] Wei Fangqiang, Su Pengcheng, Jiang Yuhong. Distribution characteristics of landslides and debris flows in the Wenchuan earthquake region before and after the earthquake [J]. Disaster Advances, 2012, 5(4): 285-294
[3] Ding Mingtao, Wei Fangqiang. Distribution characteristics of debris flows and landslides in Three Rivers Parallel Area [J]. Disaster Advances, 2011, 4(3): 7-14
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[6] Lin M L, Tung C C. A GIS-based potential analysis of the landslides induced by the Chi-Chi earthquake [J]. Engineering Geology, 2003, 64: 63-77
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[9] Xie Hong, Zhong Dunlun. Features and risk zonation of debris flow in Futangba Ravine of Wenchuan County of Min River [J]. The Chinese Journal of Geological Hazard and Control, 2003, 14(4), 30-32 [谢洪, 钟敦伦. 岷江上游汶川县佛堂坝沟泥石流特征及危险性分区[J]. 中国地质灾害与防治学报, 2003, 14(4): 30-32]
[10] Mingtao Ding, Qing Wang. Delineation of rural settlement boundaries in the upper reaches of Min River, China [J]. Applied Mechanics and Materials, 2012, 204-208: 2744-2748

相似文献/References:

[1]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,(01):257.

备注/Memo

备注/Memo:
收稿日期(Received date):2012-07-05;改回日期(Accepted) : 2013-07-26。
基金项目(Foundation item):国家自然科学
基金项目(No. 41101164,No.41371185),中国科学院水利部成都山地灾害与环境研究所方向性项目(No. SDS-135-1204-01)。[Supported by the NSFC (No. 41101164,No.4137118), Directional Project of Institute of Mountain Hazards and Environment of CAS (No. SDS-135-1204-01).]
作者简介(Biography):丁明涛(1981-),男,博士,副教授,主要从事地质灾害风险评估及其预测预报研究。[Mingtao Ding (1981- ), male, Ph D, associate professor, specialized in risk assessment and prediction of geological disaster.]E-mail: mingtaoding@163.com
更新日期/Last Update: 1900-01-01