山崩连续体模式之数值仿真(英文)  

Landslide simulations with continuum hydrodynamic models

作　　者：郭志禹[1] 张国桢[2] 蕃安佑[1,2] 陈健志[3] 戴义钦 董家钧 陈柔妃 

机构地区：[1]中央研究院应用科学研究中心,台北11529 [2]台北科技大学土木系,台北10608 [3]国立中央大学地球科学系,中坜32001 [4]成功大学水利及海洋工程学系,台南70101 [5]国立中央大学应用地质研究所,中坜32001 [6]中国文化大学地质系,台北11114

出　　处：《福建地质》2010年第A01期141-143,共3页Geology of Fujian

摘　　要：Recent advances in landslide/avalanche modeling have been enabling us to investigate the kinematics of such catastrophic events with much more details.Taiwan is located in a region where seismic activities and extreme weather conditions frequently occur.One of their common consequences is the slope failure.In the past decodes,we witnessed at least three giant landslides:Tsaoling,Jiufenershan landslides,triggered by the Chi-Chi earthquakeRecent advances in landslide/avalanche modeling have been enabling us to investigate the kinematics of such catastrophic events with much more details. Taiwan is located in a region where seismic activities and extreme weather conditions frequently occur. One of their common consequences is the slope failure. In the past decodes, we witnessed at least three giant landslides： Tsaoling, Jiufenershan landslides, triggered by the Chi-Chi earthquake in 1999, and Shiaolin landslide, triggered by the heavy rainfall of Morakot typhoon in 2009.

关 键 词：山崩模拟 浅水波方程 广义地型 小林村山崩 

分 类 号：P642.21[天文地球—工程地质学]