[1]邹 强,唐建喜,李淑松,等.基于水文响应单元的泥石流灾害易发性分区方法[J].山地学报,2017,(04):496-505.[doi:10.16089/j.cnki.1008-2786.000247]
 ZOU Qiang,*,TANG jianxi,et al.Susceptibility Assessment Method of Debris Flows Based on Hydrological Response Unit[J].Mountain Research,2017,(04):496-505.[doi:10.16089/j.cnki.1008-2786.000247]
点击复制

基于水文响应单元的泥石流灾害易发性分区方法()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2017年04期
页码:
496-505
栏目:
山地灾害
出版日期:
2017-07-30

文章信息/Info

Title:
Susceptibility Assessment Method of Debris Flows Based on Hydrological Response Unit
文章编号:
1008-2786-(2017)4-496-10
作者:
邹 强12唐建喜2李淑松2范建容1
1.中国科学院山地灾害与地表过程重点实验室 中国科学院、水利部成都山地灾害与环境研究所,成都 610041;
2.西南科技大学 环境与资源学院,四川 绵阳 621010
Author(s):
ZOU Qiang12* TANG jianxi2 LI Shusong2FAN Jianrong1
1.Key Laboratory of Mountain Hazards and Earth Surface Process/Institute of Mountain Hazards and Environment, Chinese Academy of Sciences(CAS), Chengdu 610041, China;
2.School of Environmental and Resource, Southwest University of Science and Technology, Mianyang 621010, Sichuan, China
关键词:
水文响应单元 泥石流 信息量模型 易发性 分区方法
Keywords:
hydrological response unit debris flow information value model susceptibility zoning method
分类号:
P694
DOI:
10.16089/j.cnki.1008-2786.000247
文献标志码:
A
摘要:
以水文响应单元和栅格单元为基础评价单元,运用因子贡献率法和信息量法两种评价模型对安宁河流域进行泥石流灾害易发性评价。研究结果表明,在流域尺度范围内,水文响应单元能够更好体现区域中的微观综合地貌特征,切合区域整体性描述; 基于水文响应单元的易发性分区不仅与历史泥石流实际分布情况的契合度较高,而且数学模型方法适应效率较高和区内孕灾条件体现更为明显。由此,建立基于水文响应单元泥石流灾害易发性分区对探求流域尺度范围内泥石流灾害易发性分区方法与评价制图是一个有益的尝试与拓展,可为制定减灾防灾决策提供科学参考。
Abstract:
In this article, an improved method with combination of grid cell and hydrological response unit as basic evaluation unit was introduced into our improved model to assess the susceptibility of debris flow at the Anning River basin.Information value method and contribute rate method were adopted in the susceptibility assessment model.The results confirmed that at watershed scale, susceptibility zones developed from this assessment model with hydrological response unit not only showed high consistence with the actual debris flow distribution but also agreed better with the regional geographical description as well as the micro geomorphologic characteristics of such area.In addition, the improved assessment model showed better calculation efficiency and well reflected the hazard fostering conditions.Thus, the proposed method is an effective improvement of debris flow susceptibility assessment at watershed scale and it also provide scientific support to disaster reduction and prevention.

参考文献/References:

[1] CUI P, CHEN X Q, ZHU Y Y, et al.The Wenchuan Earthquake(May 12, 2008), Sichuan Province, China, and resulting geohazards [J].Natural Hazards.2011, 56:19-36.
[2] 刘传正, 苗天宝, 陈红旗, 等.甘肃舟曲2010年8月8日特大山洪泥石流灾害的基本特征及成因[J].地质通报, 2011,30(1):141-150.[LIU Chuanzheng, MIAO Tianbao, CHEN Hongqi, et al.Basic feature and origin of the “8·8”mountain torrent-debris flow disaster happened in Zhouqu County, Gansu, China, Aug.8, 2010 [J].Geological Bulletin of China, 2011,30(1):141-150.]
[3] 彭亮, 马兴华, 金家琼, 等.“4·14”玉树地震断裂带对震后地质灾害影响作用分析[J].自然灾害学报, 2014,23(5):78-83.[PENG Liang, MA Xinghua, JIN Jiaqiong, et al.Analysis of influence of “4.14” Yushu earthquake fault zone on post-earthquake geological disasters [J].Journal of Natural Disasters.2014, 23(5):78-83.]
[4] 唐川, 马国超.基于地貌单元的小区域地质灾害易发性分区方法研究[J].地理科学, 2015, 35(1): 92-97.[TANG Chuan, MA Guochao.Small regional geohazards susceptibility mapping based on geomorphic unit [J].Scientia Geographica Sinica, 2015, 35(1):92-97.]
[5] ALEOTTI P, CHOWDHURY R.Landslide hazard assessment: summary review and new perspectives [J].Bulletin of Engineering Geology and the Environment, 1999, 58(1):21-44.
[6] CARRARA A.Multivariate models for landslide hazard evaluation [J].Mathematical Geology, 1983, 15(3): 403 - 426.
[7] MONTGOMERY D.R, DIETRICH W.E.A physically based model for the topographic control on shallow landsliding [J].Water Resource Research, 1994, 30(4): 1157-1171.
[8] 程尊兰, 朱平一, 刘雷激.泥石流活动与雨强的关系——以雅砻江下游金龙沟为例[J].自然灾害学报, 1998, 7(1): 118 - 120.[CHENG Zunlan, ZHU Pingyi, LIU Leiji.The relationship between debris flow activity and rainfall intensity [J].Journal of Natural Disasters.1998, 7(1):118-120.]
[9] RICKENMANN D.Empirical relationships for debris flows [J].Natural hazards, 1999, 19(1): 47-77.
[10] 刘希林, 唐川.泥石流危险性评价[M].北京: 科学出版社, 1995.[LIU Xilin, TANG Chuan.Debris flow hazard assessment [M].Beijing: Science Press, 1995.]
[11] CONOSCENTI C, DI Maggio C, ROTIGLIANO E.GIS analysis to assess landslide susceptibility in a fluvial basin of NW Sicily Italy [J].Geomorphology, 2008, 94(3-4):325-339.
[12] OHLMACHER G C, DAVIS J C.Davis.Using multiple logistic regression and GIS technology to predict landslide hazard in northeast Kansas, USA [J].Engineering Geology, 2003, 69(3-4):331-343.
[13] PACHAURI A K, ABHIRUP Chatterjee, REETA Gaur.Enveloping relief surfaces of landslide terrain [J].Journal of Mountain Science, 2007, 3(9):203~208.
[14] 刘斌涛, 陶和平, 刘邵权, 等.川滇黔接壤地区自然灾害危险度评价[J].地理研究, 2014, 33(2):225-236.[LIU Bintao, Tao Heping, Liu Shaoquan, et al.Assessment and analysis of natural hazards danger degree in the Sichuan-Yunnan- Guizhou bordering area of Southwest China [J].Geographical Research, 2014, 33(2): 225-236.]
[15] 李秀珍, 刘希林, 苏鹏程.四川凉山州安宁河流域泥石流危险性评价[J].防灾减灾工程学报, 2005,25(4): 426-430.[LI Xiuzhen, LIU Xilin, SU Pengcheng.Assessment on regional debris flow Hazardousness of Anning River valley in Liangshan prefecture, Sichuan [J].Journal of Disaster Prevention and Mitigation Engineering.2005, 25(4): 426-430.]
[16] 四川省西昌市志编纂委员会.西昌县志[M].成都: 四川人民出版社, 1996.[City annals compilation committee of Xichang in Sichuan province.County annals [M].Chengdu: Sichuan people's Publishing House, 1996.]
[17] 常晓军, 丁俊魏, 伦武, 等.四川安宁河流域地质灾害发育分布规律浅析[J].地质学报, 2008, 28(1): 35-40.[CHAO Xiaojun, DING Junwei, LUN Wu, et al.Development of geological hazards in the Anning River valley, Sichuan [J].Acta Geologica Sinica, 2008, 28(1): 35-40.]
[18] 王晓朋, 潘懋, 徐岳仁.基于流域单元的泥石流区域危险性评价[J].山地学报, 2006, 24(2):177-180.[WANG Xiaopeng, PAN Mao, XU Yueren.Debris flow hazard zonation based on cathment-unit [J].Journal of Mountain Science, 2006, 24(2):177-180.]
[19] 唐川.云南怒江流域泥石流敏感性空间分析[J].地理研究,2005,24(2):178-185.[TANG Chuan.Susceptibility spatial analysis of debris flows in the Nujiang River Basin of Yunnan [J].Geographical Research, 2005, 24(2): 178-185.]
[20] CASCINI L.Applicability of landslide susceptibility and hazard zoning at different scales [J].Engineering Geology, 2008, 102:164-177.
[21] 邹强, 王青, 刘延国.基于GIS与Logistic模型的公路泥石流易发性分析方法[J].水土保持通报,2014,(34)3: 185-189.[ZOU Qiang, WANG Qing, LIU Yanguo.A debris-flow susceptibility evaluation method using GIS and Logistic Model [J].Bulletin of Soil and Water Conservation, 2014,(34)3: 185-189.]
[22] 汤国安, 杨昕.ArcGIS地理信息系统空间分析实验教程[M].北京:科学出版社,2012.[TANG Guoan, YANG Xin.ArcGIS spatial analysis of Geographic Information System textbook [M].Beijing: Science press, 2012.]
[23] 乔建平,朱阿兴,吴彩燕,田宏岭.采用本底因子贡献率法的三峡库区滑坡危险度区划[J].山地学报, 2006,24(5):569-573.[QIAO Jianping, ZHU Axing, WU Caiyan, et al.Bottom factors applied to the zoning study of the risk levels of landslides in Three Gorges reservoir area [J].Journal of Mountain Science, 2006, 24(5):569-573.]
[24] SAATY T L.The analytic hierarchy process [M].New York: McGraw-Hill, 1980.
[25] 邹强, 崔鹏, 杨伟.G318川藏公路段泥石流危险性评价[J].山地学报, 2013, 31(3):342-348.[ZOU Qiang, CUI Peng, YANG Wei.Hazard assessment of debris flows along G318 Sichuan-Tibet Highway [J].Journal of Mountain Science, 2013, 31(3):342-348.]
[26] 高克昌,崔鹏,赵纯勇,等.基于地理信息系统和信息量模型的滑坡危险性评价——以重庆万州为例[J].岩石力学与工程学报, 2006,25(5):991-996.[GAO Kechang,CUI Peng,ZHAO Chunyong,et al.Landslide hazard evaluation of Wanzhou based on GIS information value method in the Three Gorges Reservoir [J].Chinese Journal of Rock Mechanics and Engineering, 2006, 25(5): 991-996.]

相似文献/References:

[1]谢湘平,苏鹏程,王小军,等.工程弃渣泥石流易发性评估方法[J].山地学报,2016,(02):216.[doi:10.16089/j.cnki.1008-2786.000121]
 XIE Xiangping,SU Pengcheng,WANG Xiaojun,et al.Occurrence Probability of Channel Waste-slag Debris Flow Assessment[J].Mountain Research,2016,(04):216.[doi:10.16089/j.cnki.1008-2786.000121]
[2]陈 剑,黎 艳,许 冲.金沙江干热河谷区泥石流易发性评价模型及应用[J].山地学报,2016,(04):460.[doi:10.16089/j.cnki.1008-2786.000151]
 CHEN Jian,LI Yan,XU Chong.Susceptibility Assessment Model of Debris Flows in the Dry-hot Valley of the Jinsha River and Its Application[J].Mountain Research,2016,(04):460.[doi:10.16089/j.cnki.1008-2786.000151]
[3]廖丽萍,朱颖彦*,杨志全,等.震区砾石土泥石流起动临界状态与力学性状[J].山地学报,2017,(04):506.[doi:10.16089/j.cnki.1008-2786.000248]
 LIAO Liping,,et al.The Mechanical Property of Gravel Soil in Seismic Area and Its Critical State in Initiating Debris Flow[J].Mountain Research,2017,(04):506.[doi:10.16089/j.cnki.1008-2786.000248]
[4]方迎潮,王道杰*,何松膛,等.云南东川蒋家沟泥石流2003-2014年冲淤演变特征[J].山地学报,2018,(06):907.[doi:10.16089/j.cnki.1008-2786.000386]
 FANG Yingchao,WANG Daojie*,HE Songtang,et al.Characteristics of Debris Flow Erosion and Deposition at Jiangjia Gully, Dongchuan, Yunnan Province, China for 2003-2014[J].Mountain Research,2018,(04):907.[doi:10.16089/j.cnki.1008-2786.000386]
[5]陈宁生*,佘德彬.基于弃渣综合利用的矿山泥石流灾害防治新模式--以冕宁盐井沟泸沽铁矿为例[J].山地学报,2019,(01):78.[doi:10.16089/j.cnki.1008-2786.000401]
 CHEN Ningsheng,SHE Debin.A New Approach to Debris Flow Disaster Control Based on Comprehensive Utilization of Waste Slag—A Case Study of Lugu Iron Mine at the Yanjing Valley of Mianning County, Sichuan, China[J].Mountain Research,2019,(04):78.[doi:10.16089/j.cnki.1008-2786.000401]
[6]王凤娘,贺 拿,陈 容,等.九寨沟县西番沟泥石流调查[J].山地学报,2019,(04):622.[doi:10.16089/j.cnki.1008-2786.000453]
 WANG Fengniang,HE Na,CHEN Rong,et al.Investigation of Debris Flow in Xifangou, Jiuzhaigou County, China[J].Mountain Research,2019,(04):622.[doi:10.16089/j.cnki.1008-2786.000453]
[7]徐根祺,李丽敏*,温宗周,等.基于宽度学习模型的泥石流灾害预报[J].山地学报,2019,(6):868.[doi:10.16089/j.cnki.1008-2786.000477]
 XU Genqi,LI Limin*,WEN Zongzhou,et al.Debris Flow Disaster Prediction Based on Broad Learning Model[J].Mountain Research,2019,(04):868.[doi:10.16089/j.cnki.1008-2786.000477]
[8]谢湘平,王小军,闫春岭.漂木灾害研究现状及研究展望[J].山地学报,2020,(4):552.[doi:10.16089/j.cnki.1008-2786.000533]
 XIE Xiangping,WANG Xiaojun,YAN Chunling.A Review of the Research on Woody Debris Related Disaster and Its Prospect[J].Mountain Research,2020,(04):552.[doi:10.16089/j.cnki.1008-2786.000533]
[9]姚鸿坤,邹 强*,蒋 虎,等.泥石流承灾体群体效应特征反演——以7·12四川平武县黑水沟泥石流为例[J].山地学报,2024,(1):47.[doi:10.16089/j.cnki.1008-2786.000803]
 YAO Hongkun,ZOU Qiang*,JIANG Hu,et al.Collective Effects of Debris Flow Striking on Structure Clusters Downstream: A Case Study of the Heishui Gully Debris Flow on July 12th in Pingwu County, Sichuan Province, China[J].Mountain Research,2024,(04):47.[doi:10.16089/j.cnki.1008-2786.000803]

备注/Memo

备注/Memo:
收稿日期(Received date)::2016-09-08; 改回日期(Accepted date): 2016-11-16
基金项目(Foundation item):国家自然科学基金重点基金项目(41401598); 数字制图与国土信息应用工程国家测绘地理信息局重点实验室开放基金资助项目(DM2016SC03); 四川旅游发展研究中心项目(LYM12-11); 四川省科技支撑项目(2014SZ0163)[Key Project of National Natural Science Foundation of China(41401598); Research Foundation of Key Laboratory of Digital Mapping and Land Information Application of National Administration of Surveying, Mapping and Geoinformation [DM2016SC03]; Program of Sichuan Tourism Development Research Center [LYM12-11]; Science and Technology Programs of Sichuan Province [2014SZ0163]
作者简介(Biography):邹强(1982-),男,副教授,主要从事山地灾害与GIS研究[Qiang Zou(1982-):male,associate professor, research on mountain hazards and GIS.] E-Mail:zouqiang@imde.ac.cn.
更新日期/Last Update: 2017-07-30