Citation: | HU Xiewen, LÜ, Xiaoping, HUANG Runqiu, REN Xiaoming, WANG Xuerui, LIU Juan. Analyses of River-Blocking and Breaking Mode of "9·24" Debris Flow near Tangjiashan Barrier Dam[J]. Journal of Southwest Jiaotong University, 2009, 22(3): 312-320,326. |
胡卸文,吕小平,黄润秋,等.唐家山堰寨湖大水沟泥石流发育特征及堵江危害性评价[J].岩石力学与工程学报,2009,28(4):850-858.HU Xiewen,L(U) Xiaoping,HUANG Runqiu,et al.Developmental features and evaluation of blocking dangers of Dashui ditch debris flow in Tangjiashan dammed lake[J].Chinese Journal of Rock Mechanics and Engineering,2009,28(4):850-858.[2] 胡卸文,黄润秋,施裕兵,等.唐家山滑坡堵江机制及堰塞坝溃坝模式分析[J].岩石力学与工程学报,2009,28(1):181-189HU Xiewen.HUANG Runqiu,SHI Yubing,et al.Analysis on blocking river mechanism of Tangjiashan landslide and dam-breaking mode of its barrier dam[J].Chinese Journal of Rock Mechanics and Engineering,2009,28(1):181-189.[3] 唐兴邦.中国泥石流[M].北京:商务印书馆,2000:246-295.[4] 陈洪凯,唐春梅,陈野鹰.公路泥石流研究及治理[M].人民交通出版社,2004:47-58.[5] 谢洪,钟敦伦,韦方强.我国山区城镇泥石流灾害及其成因[J].山地学报,2006,24(1):79-87.XIE Hong,ZHONG Dunlun,WEI Fangqiang.Debris flow hazards and their formation causes in mountain urban area of China[J].Journal of Mountain Science,2006,24(1):79-87.[6] HUNGR O.Analysis of debris flow surges using the theory of uniformly progressive flow[J].Earth Surface Processes and Landforms,2000,25:483-495.[7] IVEILSON M,RCOSTN E J,LAHUSEN G R.Large-scale debris-flow flume becomes operational in Oregon[C]∥Landslide News.[S.l.] :[S.n.] ,1993:29-30.[8] TAMOTSU T.Debris flow[M].Rotterdam:A.A.Balkma,1991:26-89.[9] 张金山,沈兴菊,谢洪.泥石流堵河影响因素研究--以岷江上游为例[J].灾害学,2007,22(2):82-86.ZHANG Jinshan,SHEN Xingju,XIE Hong.Study on factors affecting the fiver-blocking due to debris-flow in the upper reaches of Minjiang River[J].Journal of Catastrophology,2007,22(2):82-86.[10] 刘希林,唐川.泥石流危险性评价[M].北京:科学出版社,1995:84-91.[11] 王裕宜,胡凯衡.泥石流体的流变和冲淤特征及其与危险度的关系[J].自然灾害学报,2007,16(1):17-22.WANG Yuyi,HU Kaiheng.Relationship between rheology/erosion-deposit properties of debris flow and its hazard degree[J].Journal of Natural Disasters,2007,16(1):17-22.
|