[1] 黄润秋，裴向军，李天斌. 汶川地震触发大光包巨型滑坡基本特征及形成机理分析[J]. 工程地质学报，2008，16(6)：730–741. (HUANG Runqiu，PEI Xiangjun，LI Tianbin. Basic characteristics and formation mechanism of the largest scale landslide at Daguangbao occurred during the Wenchuan earthquake[J]. Journal of Engineering Geology，2008，16(6)：730–741.(in Chinese))

[2] TANG C，ZHU J，DING J. Catastrophic debris flows triggered by a 14 August 2010 rainfall at the epicenter of the Wenchuan earthquake[J]. Landslides，2011，8(4)：485–497.

[3] GUZZTTI F，ARDIZZONE F，CARDINALI M，et al. Distribution of landslides in the Upper Tiber River basin，central Italy[J]. Geomorphology，2008，96(1)：105–122.

[4] HOVIUS N，STARK C，ALLEN P. Sediment flux from a mountain belt derived by landslide mapping[J]. Geology，1997，25(3)：231–234.

[5] TSENG C，LIN C，STARK C，et al. Application of a multi-temporal，LiDAR-derived，digital terrain model in a landslide-volume estimation[J]. Earth Surface Processes and Landforms，2013，38(13)：1 587–1 601.

[6] KORUP O. Effects of large deep-seated landslides on hillslope morphology，western Southern Alps，New Zealand[J]. Journal of Geophysical Research，2006，111(F1)：151–162. 

[7] 刘青泉，李家春，陈  力，等. 坡面流及土壤侵蚀动力学(II)—土壤侵蚀[J]. 力学进展，2004，34(4)：493–506.(LIU Qingquan，LI Jiachun，CHEN Li，et al，Dynamics of overland flow and soil erosion (II)—soil erosion[J]. Advances in Mathematic，2004，34(4)：493–506(in Chinese))

[8] 吴  永，裴向军，何思明，等. 降雨型泥石流对沟床侵蚀的水力学机理[J]. 浙江大学学报：工学版，2013，47(9)：1 585–1 592.(WU Yong，PEI Xiangjun，HE Siming，et al. Hydraulic mechanism of gully bed erosion by debris flow in rainfall[J]. Journal of Zhejiang University：Engineering Science，2013，47(9)：1 585–1 592. (in Chinese))

[9] OUYANG Z Y，HE S M，TANG C. Numerical analysis of dynamics of debris flow over erodible beds in Wenchuan earthquake-induced area[J]. Engineering Geology，2015，194(28)：62–72.

[10] 庄建琦，崔鹏，胡凯衡，等. 沟道松散物质起动形成泥石流实验研究[J]. 四川大学学报：工程科学版，2010，42(5)：230–236.( ZHUANG Jianqi，CUI Peng，HU Kaiheng，et al. Research on debris flow initiation due to bed failure after Wen chuan earthquake[J]. Journal of Sichuan University：Engineering Science，2010，42(5)：230–236.(in Chinese))

[11] 丁  军. 强震区泥石流活动规模与最大堆积长度预测研究[硕士学位论文][D]. 成都：成都理工大学，2011.(DING Jun. Research on magnitude and runout distance of debris-flows in strong earthquake area[M. S. Thesis][D]. Chengdu：Chengdu University of Technology，2011.(in Chinese))

[12] WHITEHOUSE I. Distribution of large rock avalanche deposits in the Central Southern Alps，New Zealand[J]. New Zealand Journal of Geology and Geophysics，1983，26(3)：271–279.

[13] GUZZTTI F，ARDIZZONE F，CARDINALI M，et al. Landslides volumes and landslide mobilization rates in Umbria，central Italy[J]. Earth and Panetary Sciences Letters，2009，279(3)：222–229.

[14] SIMONETT D S. Landslide distribution and earthquakes in the Bewani and Torricelli Mountains，New Guinea. Landform studies from Australia and New Guinea-a statistic analysis[C]// Landform Studies from Australia and New Guinea. Cambridge，UK：Cambridge University Press，1967：64–84.

[15] WOOLHIER D A，liggelt J A. Unsteady one-dimensional flow over a plane-the rising hydrograph[J]. Cond Plant Growth Jpn，1996，3(3)：753–771.

[16] 刘青泉，陈  力，李家春. 坡度对坡面土壤侵蚀的影响分析[J]. 应用数学和力学，2001，22(5)：449–457.(LIU Qingquan，CHEN Li，LI Jiachun，Influences of slope gradient on soil erosion[J]. Applied Mathematics and Mechanics，2001，22(5)：449–457.(in Chinese))

[17] LIMA J L M P. Model KININF for overland flow on pervious surface[C]// Overland Flow. [S. l.]：UCL Press，1992

[18] 曹文洪. 土壤侵蚀的坡度界限研究[J]. 水土保持通报，1998，13(4)：1–5.(CAO Wenhong，Slope gradient limited study of soil erosion[J]. Bulletin of Soil and Water Conservation，1998，13(4)：1–5.(in Chinese))

[19] 洪正修. 关于泥石流流速计算公式的探讨[J]. 铁道工程学报，1988，(1)：87–94.(HONG Zhengxiu，Discussion on debris flow velocity calculation formula[J]. Journal of Railway Engineering Society，1988，(1)：87–94.(in Chinese))

[20] 倪九派，魏朝富，谢德体，等. 坡度对山峡库区紫色土坡度径流侵蚀的影响分析[J]. 泥沙研究，2009，(2)：29–33.(NI Jiupai，WEI Chaofu，XIE Delin，et al. Influence of slope gradient on runoff erosion of purple soil slope in the Three Gorges Reservoir area[J]. Journal of Sediment Research，2009，(2)：29–33.(in Chinese))

[21] 张  雄，裴向军. 泥石流启动的临界地表径流深度研究[J]. 成都大学学报：自然科学版，2014，33(3)：286–289.(ZHANG Xiong，PEI Xiangjun，Critical surface runoff depth study of debris flow start up[J]. Journal of Chengdu University：Natural Science，2014，33(3)：286–289.(in Chinese))

[22] YAIR A， KLEIU M. The influence of surface properties on flow and erosion processes on debris covered slopes in an arid area[J]. Catena，1973，1(1)：1–8.

[23] 汤立群，陈国祥，蔡名扬. 黄土丘陵区小流域产沙数学模型[J]. 河海大学学报：自然科学版，1990，18(6)：10–15.(TANG Liqun，CHEN Guoxiang，CAI Mingyang，A mathematical model of sediment yield on small watershed in the gullied-hilly loess plateau[J]. Journal of Hohai University：Natural Sciences，1990，18(6)：10–15.(in Chinese))