地震滑坡研究回顾与展望
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摘要
对国内外地震滑坡特别是汶川8.0级地震产生的地震滑坡的历史文献进行了系统回顾,认为地震滑坡的研究可以概括为发育分布规律统计研究和动力学机理研究。其中对于地震滑坡发育分布规律的研究较深入,取得了丰富的规律性认识;而关于动力学机理的研究,大多是基于表观现象的假设或推断,缺乏物理或数值模拟实验的验证。建议进一步开展:①基于地震波传播理论的物理或数值模拟;②高速远程滑坡形成机制与运动特征研究;③强震触发滑坡灾害链效应研究。
Based on the review of historical documents on earthquake-triggering landslides at home and abroad,the study of earthquake-triggering landslides can be divided into the statistic study of development distribution and dynamical mechanism study,of which the former type of study is quite deep and some rules have been generalized;while the latter type mainly includes hypotheses or assumptions induced from superficial phenomena,lacking physical or numerical simulation experimental tests.Therefore,further studies should be conducted in the following three aspects:(1) the physical or numerical simulation based on the transmission principle of seismic wave;(2) the development mechanism and motional features of high-speed and long-runout landslides;(3) the chain effect of landslides triggered by strong earthquakes.
Based on the review of historical documents on earthquake-triggering landslides at home and abroad,the study of earthquake-triggering landslides can be divided into the statistic study of development distribution and dynamical mechanism study,of which the former type of study is quite deep and some rules have been generalized;while the latter type mainly includes hypotheses or assumptions induced from superficial phenomena,lacking physical or numerical simulation experimental tests.Therefore,further studies should be conducted in the following three aspects:(1) the physical or numerical simulation based on the transmission principle of seismic wave;(2) the development mechanism and motional features of high-speed and long-runout landslides;(3) the chain effect of landslides triggered by strong earthquakes.
引文
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[26]Wang W N,Wu H L,Nakamura H,et al.Mass movementscaused by recent tectonic activity:the 1999 Chi-Chi earthquakein central Taiwan[M].The Island Arc12,2003:325-334.
[27]Chigira Yagi.Geological and geomorphological characteristics oflandslides triggered by the 2004 Mid Niigta prefecture earthquakein Japan[J].Engineering Geology,2006,82:202-221.
[28]Hiroshi P S,Hiroyuki H,Satoshi F,et al.Interpretation oflandslide distribution triggered by the 2005 Northern Pakistanearthquake using SPOT5 imagery[J].Landslides,2007,4:113-122.
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[30]Owen L A,Kamp U,Khattak G A,et al.Landslides triggeredby the 8 October 2005 Kashmir earthquake[J].Geomorphology,2008,94:1-9.
[31]康来迅.昌马断裂带滑坡之研究[J].内陆地震,1988,2(4):376-381.
[32]康来迅,邹谨敞.昌马断裂带地震滑坡的基本特征[J].华南地震,1995,15(1):49-54.
[33]黄润秋,李为乐.“5.12”汶川大地震触发地质灾害的发育分布规律研究[J].岩石力学与工程学报,2008,27(12):2585-2592.
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[35]Huang Runqiu,Li Weile.Analysis of the geo-hazards triggeredby the 12 May(2008)Wenchuan Earthquake,China[J].Bull.of Engineering Geology and the Environment,2009b,68:363-371.
[36]Huang Runqiu,Li Weile.Fault effect analysis of geohazardstriggered by Wechuan Earthquake[J].Chinese Journal of Engi-neering Geology,2009,17(1):19-28.
[37]祁生文,许强,刘春玲,等.汶川地震极重灾区地质背景及次生斜坡灾害空间发育规律[J].工程地质学报,2009,17(1):39-49.
[38]苏凤环,刘洪江,韩用顺.汶川地震山地灾害遥感快速提取及其分布特点分析[J].遥感学报,2008,12(6):956-963.
[39]吴树仁,石菊松,姚鑫,等.四川汶川地震地质灾害活动强度分析评价[J].地质通报,2008,27(11):1900-1906.
[40]Jibson R W,Harp E L,Michael J A.A method for producingdigital probabilistic seismic landslide hazard maps[J].Engi-neering Geology,2000,58:271-290.
[41]Miles S B,Keefer D K.Evaluation of CAMEL-comprehensiveareal model of earthquake-induced landslides[J].EngineeringGeology,2009,104:1-15.
[42]Kamp U,Growley B J,Khattak G A,et al.GIS-based land-slide susceptibility mapping for the 2005 Kashmir earthquake re-gion[J].Geomorphology,2008,101:631-642.
[43]乔建平,蒲晓虹,王萌,等.大地震诱发滑坡的分布特点及危险性区划研究[J].灾害学,2009,24(2):25-29.
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