[1]顾春杰,孙爽,宁娜,等.基于生产函数的区域泥石流灾害易损性研究[J].山地学报,2015,(03):303.
 GU Chunjie,SUN Shuang,NING Na,et al.Research on Debris Flow Disaster Vulnerability Based on the Production Function[J].Mountain Research,2015,(03):303.
点击复制

基于生产函数的区域泥石流灾害易损性研究()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2015年03期
页码:
303
栏目:
山地灾害
出版日期:
2015-06-01

文章信息/Info

Title:
Research on Debris Flow Disaster Vulnerability Based on the Production Function
作者:
顾春杰;孙爽;宁娜;马金珠;
兰州大学西部环境教育部重点实验室;
Author(s):
GU Chunjie SUN Shuang NING Na MA Jinzhu
Key Laboratory of Western China's Environmental Systems (MOE),Lanzhou University,222 South Tianshui Road, Lanzhou 730000,China
关键词:
易损性泥石流C-D生产函数历史灾情
Keywords:
vulnerability debris flow C-D production functionloss of history disaster
分类号:
P642.23
文献标志码:
A
摘要:
近年来人们对于自然灾害易损性的基本构成已经初步达成了共识,包括暴露性、敏感性和恢复适应能力,但对于其相互关系尚未有过深入的分析。易损性评价中多是将暴露性、敏感性和恢复适应能力等指标杂糅一起,或者虽然分开选择评价指标但在最后评价时依旧作为一体,没有对整个人地系统的内在机理深入分析。针对泥石流灾害,尝试综合分析整个人地环境的暴露性、敏感性、恢复适应能力之间关系及其对易损性的影响,借鉴经济学中的C-D生产函数建立了易损性的评价函数。在近50 a研究区历史灾情的统计分析基础上,确定了暴露性、敏感性的评价指标,并且由累积的各项损失情况确定敏感性评价指标权重,从灾害造成的直接经济损失出发对函数参数进行估计...
Abstract:
Recently the basic parts of natural disasters vulnerability have reached a preliminary consensus, which is including exposure, sensitivity and resilience, but there hasn't been any indepth analysis for its internal relationships. Vulnerability assessment aways mingle the exposure, sensitivity and resilience index together, or although the choice of evaluation index are separate, the final evaluation still as a whole, there is no inherent mechanism of the system analysis. This paper attempts a comprehensive analysis of the debris flow disaster, considering the relationship between exposure, sensitivity, resilience of the coupled human and environmental systems and the influence about vulnerability, with reference to the C-D production function in economics and established vulnerability assessment function. On the basis of analysis the loss of debris flow in the research area nearly 50 years history, the evaluation index of exposure and sensitivity are ascertained, and the weight of sensitivity evaluation index are determined by the accumulated loss of different types, then the function parameter are estimated from the direct economic losses of the disaster. By comparing the calculated results with different parameters, the contribution rate about sensitivity of human social and economic system for region vulnerability is about 0.8, far higher than the geological hazard exposure of the contribution rate of 0.2. Finally, the vulnerability evaluation method of production function is consummated, and then apply it to assess the current vulnerability in the study area, finally some suggestions are put forward on how to reduce the region vulnerability.

参考文献/References:

[1] Janssena M A, Schoon M L, Ke W et al. Scholarly net works oil resilience,vulnerability and adaptation within the human dimensions of global environmental change[J].Global Environmental Change, 2006, 16(3): 240-252
[2] Li He, Zhang Pingyu, Cheng Yeqing. Concepts and assessment methods of vulnerability[J]. Progress in Geography, 2008, 27(2): 18-25 [李鹤, 张平宇, 程叶青. 脆弱性的概念及其评价方法[J]. 地理科学进展, 2008, 27(2): 18-25]
[3] Adger W N, Brooks N, Bentham G, et al. New Indicators of Vulnerability and Adaptive Capacity[R]. Norwich: Tyndall Centre for Climate Change Research(Technical Report No.7), 2004.
[4] Adrianto L, Matsuda Y. Developing economic vulnerability indices of environmental disasters in small island regions[J]. Environmental Impact Assessment Review, 2002,22(4): 93-414
[5] Downing T E. Towards a Vulnerability Science[G]//IHDP Newsletter Update3, 2000.
[6] Cutter S L. A Research Agenda for Vulnerability Science and Environmental Hazards[G]//IHDP Newsletter Update 2,2001.
[7] Cutter S L. The vulnerability of science and the science of vulnerability[J]. Annals of the Association of American Geographers,2003, 93(1): 1-12
[8] Kasperson J X, Kasperson R E. International Workshop on Vulnerability and Global Environmental Change[R]. SEI Risk and Vulnerability Programme Report 2001-01,Stockholm Environment Institute (SEI), Stockholm, Sweden, 2001.
[9] Kates R W, Clark W C, Corell R, et al. Environment and development: sustainability science[J]. Science, 2001, 292(5517): 641-642
[10] Eakin H, Luers A L. Assessing the vulnerability of socialenvironmental systems[J]. Annual Review of Environment and Resources,2006, 31: 365-394
[11] Schroter D, Metzger M J, Cramer W, et al. Vulnerability assessmentanalysing the humanenvironment system in the face of global environmental change[J]. The ESS Bulletin, 2004, 2(2): 11 -17
[12]Tian Yaping, Xiang Qingcheng, Wang Peng. Coupled human environment system vulnerability and evaluation index system[J]. Geographical Research , 2013, 32(1): 55-63 [田亚平, 向清成, 王鹏. 区域人地耦合系统脆弱性及其评价指标体系[J]. 地理研究, 2013, 32(1): 55-63]
[13] Li He, Zhang Pingyu. Vulnerability of urban employment of mining cities in Northeast China[J]. Geographical Research, 2009, 28(3): 751-760 [李鹤, 张平宇. 东北地区矿业城市社会就业脆弱性分析[J]. 地理研究, 2009, 28(3): 751-760]
[14] Eakin H, Luers A L. Assessing the vulnerability of socialenvironmental systems[J]. Annual Review of Environment and Resources,2006,31: 365-394
[15] Shi Peijun, Wang Jing'ai, Chen Jing,et al. The future of humanenvironment interaction research in geography: Lessons from the 6th open meeting of IHDP[J]. Acta Geographica Sinica, 2006, 61(2): 115-126 [史培军, 王静爱, 陈婧,等. 当代地理学之人地相互作用研究的趋向: 全球变化人类行为计划(IHDP) 第六届开放会议透视[J]. 地理学报, 2006, 61(2): 115-126]
[16] Yuan Bin, He Faguo, Li Junpen,et al. The relationship of debris flow activity and rainfall characteristics in Gansu Wudu area[J]. Journal of Lanzhou University:Natural Science,2012,48(6) :15-20 [袁斌, 和法国,李军鹏,等 甘肃武都区泥石流活动与降雨特征关系[J].兰州大学学报:自然科学版,2012,48(6) :15-20]
[17] Ning Na, Tian Liming, Zhang Peng et al. Risk assessment of debris flow in Wudu area of southern Gansu[J]. Mountain Research, 2013, 31(5): 601-609 [宁娜, 田黎明, 张鹏,等. 甘肃南部武都地区泥石流危险性评价[J]. 山地学报, 2013, 31(5): 601-609 ]
[18] Gong Jie, Zhao Caixia, Wang Heling,et al. Ecological risk assessment of geological disasters in mountainous area of Longnan——A case study in Wudu District of Longnan city[J]. Mountain Research, 2012,30(5): 570-577 [巩杰, 赵彩霞, 王合领,等. 基于地质灾害的陇南山区生态风险评价——以陇南市武都区为例[J]. 山地学报,2012, 30(5): 570-577]
[19] Wang Ruiyan, Zhao Gengxin, Zhou Wei et al. Assessment and dynamic changes of environmental vulnerability at county level: A case study in Kenli County of the Yellow River Delta[J]. China. Acta Ecologica Sinica, 2009, 29(7): 3790-3799 [王瑞燕, 赵庚星, 周伟,等. 县域生态环境脆弱性评价及其动态分析:以黄河三角洲垦利县为例[J]. 生态学报, 2009, 29(7): 3790-3799]
[20] Li Zexin, Wang Rong. Traffic environment characteristics and control measures of mountainous city road[J]. Mountain Research, 2014, 32(1): 46-51 [李泽新, 王蓉. 山地城市道路交通环境特点及其控制对策[J]. 山地学报, 2014, 32(1): 46-51]

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]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.
[10]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.
[11]刘希林.泥石流风险评价中若干问题的探讨[J].山地学报,2000,(04):341.

备注/Memo

备注/Memo:
收稿日期(Received date):2014-08-12;修回日期(Accepted):2014-09-06。
基金项目(Foundation item):国家科技支撑计划项目“白龙江流域滑坡泥石流灾害多尺度风险评价与技术研究”(2011BAK12B05)资助。[Supported by National Science and Technology Pillar Program "Risk evaluation and technology research of multiscale landslide and debris flow disaster in Bai Longjiang Valley "(2011BAK12B05).]
作者简介(Biography):顾春杰(1986-),女,满族,河北承德人,硕士研究生,主要从事水文过程与地质灾害方面的研究。[Gu Chunjie,female,born in Chende,Hebei,master graduate student, majoring in the research on hydrological process and debris flow risks assessment.]E-mail:guchj13@lzu.edu.cn,Tel:15294116597
更新日期/Last Update: 1900-01-01