冰川泥石流形成机理研究进展

铁永波; 李宗亮

冰川泥石流形成机理研究进展

成都地质矿产研究所, 四川, 成都, 610081

基金项目: 中国地质调查局"典型泥石流防治关键技术及示范"项目(1212010814038)

详细信息

作者简介:
铁永波(1979- ),男,云南大关人,博士,主要从事环境地质与灾害地貌学方面研究.E-mail:tyongbo@cgs.cn

中图分类号: XS01;S143.1;G353.11

Progress in the study of glacial debris flow mechanisms

Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, China

摘要: 由于冰川泥石流的广泛分布及其发育地的特殊性使得对其开展全面治理较为困难,因此,有效开展冰川泥石流的预警预报具有重要意义.虽然近年来对冰川泥石流的研究有了较多的成果,但目前对其形成机理的认识还存在很大的局限,在很大程度上制约了防灾减灾的进展.为深入探讨冰川泥石流的形成机理,文章回顾了国内外学者在相关领域的研究成果,系统总结了现有冰川泥石流形成机理的研究现状,并对冰川泥石流形成机理的未来研究方向做了展望.
- 冰川泥石流 /
- 形成机理 /
- 环境响应 /
- 研究进展
Abstract: The glacial debris flow is a widespread geomorphologic phenomenon.Due to the unique characteristics of the flow formation at glacier heads,it would be difficult to conduct a comprehensive control of glacial debris flows.Therefore,effectively forecasting the flow occurrence will provide us with an miportant preventative measure for mitigating the flow disaster.Although,some progresses have been made on the subject in recent years,the development of effective measures for disaster prevention and mitigation has been hampered by the lack of understanding of basic mechanisms that contribute to the formation of glacial debris flows.Recent progresses in the study of glacial debr is flow smechanisms are systemically reviewed,and the current states of the flow mechanism are reported on.Future prospects of research on the subject are put forwarded at last.Our result can provide a scientific basis for the flow mechanism study and the disaster prevention and mitigation.
- glacier debris flow /
- mechanism /
- response to environment /
- progress and advance

[1]	MARTA C,SARA I,GIOVANNI M.Recent debris flow occurrences associated with glaciers in the Alps[J].Global and Planetary Change,2007,56:123-136.
[2]	李鸿琏,蔡祥兴.中国冰川泥石流的一些特征[J].水土保持通报,1989,9(6):1-9.(LI Hong-lian,CAI Xiang-xing.The glacial debris flow of China[J].Bulletin of Soil and Water Conservation,1989,9(6):1-9.(in Chinese))
[3]	程尊兰,朱平一,宫怡文.典型冰湖溃决型泥石流形成机制分析[J].山地学报,2003,21(6):716-720.(CHENG Zun-lan,ZHU Ping-yi,GONG Yi-wen.The conform mechanical analyses of typical glacier lake debris flow[J].Journal of Mountain Science,2003,21(6):716-720.(in Chinese))
[4]	余忠水,德庆卓嘎.西藏波密县天摩沟"9·4"特大泥石流灾害成因初步分析[J].中国地质灾害与防治学报,2009,20(1):6-10.(YU Zhong-shui,DEQING Zuo-ga,The cause of formation analysis of"9·4"over-size debris flow in Bomi Tianmo Gully,Tibet[J].The Chinese Journal of Geological Hazard and Control,2009,20(1):6-10.(in Chinese))
[5]	郑本兴,马秋华.嘎山区全新世冰川变化与泥石流发育的关系[J].山地研究,1994,12(1):1-8.(ZHENG Ben-xing,MA Qiu-Hua.Relationshipbetween the glacier variation and the debris flow development of the holocene in the Gongga Mountainous region[J].Mountain Research,1994,12(1):1-8.(in Chinese))
[6]	陈晓晴,崔鹏,陈斌如,等.海螺沟050811特大泥石流灾害及减灾对策[J].水土保持通报,2006,26(3):123-126.(CHEN Xiao-qing,CUI Peng,CHEN Bin-ru,et al.050811 large-scale debris flow in Hailuo valley and prevement countermeasures[J].Bulletin of Soil and Water Conservation,2006,26(3):123-126.(in Chinese))
[7]	CLAGUE J,EVANS S.A review of catastrophic drainage of moraine-dammed lakes in British Columbia[J].Quaternary Science Reviews,2000,19:1763-1783.
[8]	DELINE P,CHIARLE M.,MORTARA G.The July 2003 Frébouge debris flow(Mont Blanc Massif,Valley of Aosta,Italy):Water pocket outburst flood and ice avalanche damming[J].Geografia Fisica e Dinamica Quaternaria,2004,27:107-111.
[9]	HUGGEL C,HAEBERLI W.KAAB A.BIERI D,et al.An assessment procedure for glacial hazards in the Swiss Alps[J].Canadian Geotechnical Journal,2004,41:1068-1083.
[10]	费莱施曼.泥石流[M].北京:科学出版社,1985:242-266.(FLACEMAN M.Debris flow[M].Beijing:Science Press,1985:242-266.(in Chinese))
[11]	POPOY N.Glacial debris flows mitigation in Kazakstan:Assessment,prediction and control[C]//CHEN C L.Debris-flow hazard mitigation:Mechanics,prediction,and assessment,San Francisco:[s.n.],1997:113-122.
[12]	AMES A.A documentation of glacier tongue variations and lake development in the Cordillera Blanca[J].Glazialgeol,1998,34:1-36.
[13]	YAMADA T.Glacier lake and its outburst flood in the Nepal Himalaya[R].Tokyo:Data Center for.Glacier Research,Japanese Society of Snow and Ice,1998.
[14]	崔鹏,马东涛,陈宁生,等.冰湖溃决泥石流的形成、演化及减灾对策[J].第四纪研究,2003,6(23):621-628.(CUI Peng,MA Dong-tao,CHEN Ning-sheng,et al.The initiation,motion and mitigation of debris flow caused by glacial lake outburst[J].Qqaternary Science,2003,6(23):621-628.(in Chinese))
[15]	吴树仁,周平根,雷伟志.地质灾害防治领域重大科技问题讨论[J].地质力学学报,2004,10(1):1-6.(WU Shu-ren,ZHOU Ping-gen,LEI Wei-zhi.Discuss of important issue in geologic hazards prevention[J].Journal of Geomechanics,2004,10(1):1-6.(in Chinese))
[16]	铁永波,唐川.冰湖溃决灾害评价体系研究进展[J].水科学进展,2009,20(3):448-452.(TIE Yong-bo,TANG Chuan.Progress of glacier lake outburst assessment system[J].Advances in Water Science,2009,20(3):448-452.(in Chinese))
[17]	斯捷潘若夫.泥石流与泥石流体的基本特征及其量测方法[M].重庆:科学技术文献出版社重庆分社,1986:66-75.(PAROFSK.C.Debris flow,It's characteristics and it's measure[M].Chongqing:Chongqing Press of Technical,1986:66-75.(in Chinese))
[18]	MARTA C,SARA I,GIOVANNI M.Recent debris flow occurrences associated with glaciers in the Alps[J].Global and Planetary Change,2007,56:123-136.
[19]	WALDER J S,DRIEDGER C L.Frequent outburst floods from the South Tahoma Glacier,Mount Rainier,USA:Relation to debris flows,meteorological origin and implications for subglacial hydrology[J].Journal of Glaciology,1995,41:1-10.
[20]	ZIMMER M,HAEBERLI W.Climatic change and debris flow activity in high mountain areas:A case study in the Swiss Alps[J].Catena,1992,22:59-72.
[21]	车涛,晋锐,李新,等.近20年来西藏朋曲流域冰湖变化及潜在溃决冰湖分析[J].冰川冻土,2004,26(4):397-402.(CHE Tao,JIN Rui,LI Xin,et al.Glacial lakes variation and the potentially dangerous glacial lakes in the Pumqu Basin of Tibet during the last two decades[J].Journal of Glaciology and Geocryolog,2004,26(4):397-402.(in Chinese))
[22]	徐道明,冯清华.西藏喜马拉雅山区危险冰湖及其溃决特征[J].地理学报,1989,44(3):343-352.(XU Dao-ming,FENG Qing-hua.Dangerous glacial lake and outburst features in Xizang Himalayas[J].Acta Geographica Sinica,1989,44(3):343-352.(in Chinese))
[23]	程尊兰,朱平一,党超,等.臧东南冰湖溃决泥石流灾害及其发展趋势.冰川冻土[J],2008,30(6):954-959.(CHENG Zun-lan,ZHU Ping-yi,DANG Chao,et al.Glacier lake outburst debris flow hazard and evolution in southeast Tibet Are[J].Journal of Glaciology and Geocryolog,2008,30(6):954-959.(in Chinese))
[24]	PAUL F,HUGGEL C,KAA B A.Combining multispectral satellite data and a digital elevation model for mapping of debris-covered glaciers[J].Remote Sensing References of Environment,2004,89(4):510-518.
[25]	HAEBERLI W.MAISCH M,PAUL F.Mountain glaciers in global climate related observation networks[J].WMO-Bulletin,2002,51(1):18-25.
[26]	HUGGEL C,KEA B,HAEBER L I.Regional-scale GIS-models for assessment of hazards from glacier lake outbursts:Evalution and application in the Swiss Alps[J].Natural Hazards and Earth System Sciences,2003(3):647-662.
[27]	SCAMBOS T.HUBLE C.FAHNESTOCK M,et al.The link between climate warming and break-up of ice-shelves in the Antarctic Peninsula[J].Journal of Glaciology,2000,46:516-530.
[28]	COOK A J.FOX A J.VAUGHAN D G.Retreating glacier fronts on the Antarctic Peninsula over the past half-century[J].Science,2005,308:541-544.
[29]	施雅风.2050年前气候变暖冰川萎缩对水资源影响情景预估[J].冰川冻土,2001,23(4):333-341.(SHI Ya-feng.Estimation of the water resources based ou the glacier shrink caused by the climate warming before 2050[J].Journal of Glaciolgy and Geocryology,2001,23(4):333-341.(in Chinese))
[30]	苏珍,刘宗香,王文悌,等.青藏高原冰川对气候变化的响应及趋势预测[J].地球科学进展,1999,14(6):607-612.(SU Zhen,LIU Zong-xiang,WANG Wen-ti,et al.The response to climate change and its trend estimation of glacier in Qingzang[J].Advance of Earth Science,1999,14(6):607-612.(in Chinese))
[31]	苏珍,施雅风.小冰期以来季风温冰川对全球变暖的响应[J].冰川冻土,2000,22(3):223-229.(SU Zhen,SHI Ya-feng.Response to globe warming of season warm glacier since little ice age[J].Journal of Glaciolgy and Geocryology,2000,22(3):223-229.(in Chinese))
[32]	郑本兴,马秋华.贡嘎山区全新世冰川变化:气候变化与河流阶地发育[J].地理学报,1994,46(1):500-508.(ZHENG Ben-xing,MA Qiu-hua.The glacier variation,climate change and river terrace evolution of the holocene in the Gongga Mountainous region[J] Journal of Geographical Science,1994,46(1):500-508.(in Chinese))
[33]	李宗省,何元庆,贾文雄,等.全球变暖背景下海螺沟冰川近百年的变化[J].冰川冻土,2009,31(1):75-81.(LI Zong-sheng,HE Yuan-qing,JIA Wen-xiong,et al.Changes in Hailuogou Glacier during on the globe warming in recent century[J].Journal of Glaciolgy and Geocryology,2009,31(1):75-81.(in Chinese))
[34]	吕玉香,王根绪.1990～2007年贡嘎山海螺沟径流变化对气候变化的响应[J].冰川冻土,2008,30(6):960～66.(LÜ Yu-xiang,WANG Gen-xu.Response of runoff variation to climate change in Hailuogou Drainage basin in Gongga Mount in 1990-2007[J].Journal of Glaciolgy and Geocryology,2008,30(6):960～66.(in Chinese))
[35]	徐小飞,马东涛,何德伟,等.贡嘎山地区泥石流形成的水热组合分析[J].山地学报,2007,24(4):431-437.(XU Xiao-fei,MA Dong-tao,HE De-wei,et al.Analysis on hydro-thermal of debris flow form in Gongga Mountain area[J].Journal of Mountain Science,2007,24(4):431-437.(in Chinese))

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冰川泥石流形成机理研究进展

作者简介:
铁永波(1979- ),男,云南大关人,博士,主要从事环境地质与灾害地貌学方面研究.E-mail:tyongbo@cgs.cn

Progress in the study of glacial debris flow mechanisms

计量

冰川泥石流形成机理研究进展

成都地质矿产研究所, 四川, 成都, 610081

作者简介:
铁永波(1979- ),男,云南大关人,博士,主要从事环境地质与灾害地貌学方面研究.E-mail:tyongbo@cgs.cn

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Progress in the study of glacial debris flow mechanisms

Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, China

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冰川泥石流形成机理研究进展

作者简介: 铁永波(1979- ),男,云南大关人,博士,主要从事环境地质与灾害地貌学方面研究.E-mail:tyongbo@cgs.cn

Progress in the study of glacial debris flow mechanisms

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冰川泥石流形成机理研究进展

成都地质矿产研究所, 四川, 成都, 610081

作者简介: 铁永波(1979- ),男,云南大关人,博士,主要从事环境地质与灾害地貌学方面研究.E-mail:tyongbo@cgs.cn

English Abstract

Progress in the study of glacial debris flow mechanisms

Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, China

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目录

作者简介:
铁永波(1979- ),男,云南大关人,博士,主要从事环境地质与灾害地貌学方面研究.E-mail:tyongbo@cgs.cn

作者简介:
铁永波(1979- ),男,云南大关人,博士,主要从事环境地质与灾害地貌学方面研究.E-mail:tyongbo@cgs.cn