[1] 唐川.泥石流扇形地研究[J].云南底质,1990,26(3):239-246.
[2] 董桂芝,赵波,韦京莲.北京市北山泥石流分布规律及形成过程[J].北京地质,1994(4):8-11.
[3] 陈杰,韦方强,崔鹏.小江流域泥石流堆积扇形成的制约因素及其特征[J].地理科学,2005,25(6):703-708.
[4] 费祥俊.中国泥石流[M].北京:中国科学出版社,2004.
[5] 崔之久.泥石流沉积与环境[M].北京:中国科学出版社,1996.
[6] 谢洪,钟敦伦,李泳.泥石流野外调查方法[J].水土保持通报,2002,22(6):59-61.
[7] 倪化勇,刘希林.泥石流粒度分维的初步研究[J].水土保持研究,2006,13(5):89-91.
[8] 胡封兵.西白莲峪堆积物特征和北京山区泥石流防治探讨[D].北京:北京林业大学,2007.
[9] GAO Jiarong.Characteristics and Development of the Debris-flow Fan in Dalancha Gully,Beijing[J].Journal of Mountain Science,2008,22(1):90-96.
[1]王高峰,唐川,王洪德,等.初咱磨子沟泥石流特征及危险性评价研究[J].水土保持研究,2012,19(04):234.
WANG Gao-feng,TANG Chuan,WANG Hong-de,et al.Characteristics and Hazard Assessment of Debris Flows in Chuzanmozigou Catchment[J].Research of Soil and Water Conservation,2012,19(01):234.
[2]田冰,王裕宜.基于功率谱分析的蒋家沟泥石流侵蚀输沙量准周期的探讨[J].水土保持研究,2012,19(04):244.
TIAN Bing,WANG Yu-yi.Power Spectral Analysis on Periodicity of Sediment Transport in Debris Flow in Jiangjiagou Watershed[J].Research of Soil and Water Conservation,2012,19(01):244.
[3]胡桂胜,陈宁生,邓虎.基于GIS的西藏林芝地区泥石流易发与危险区分析[J].水土保持研究,2012,19(03):195.
HU Gui-sheng,CHEN Ning-sheng,DENG Hu.Analysis of Debris Flow-prone and Dangerous Area in Nyingchi of Tibet Based on GIS[J].Research of Soil and Water Conservation,2012,19(01):195.
[4]李朝安,胡卸文,李冠奇,等.四川省“8·13”特大泥石流灾害成生机理与防治原则[J].水土保持研究,2012,19(02):257.
LI Chao-an,HU Xie-wen,LI Guan-qi,et al.Formation Mechanism of the ’8·13’ Catastrophic Debris Flow in Sichuan and the Principles of Controlling[J].Research of Soil and Water Conservation,2012,19(01):257.
[5]张黎勇.皖南山区山体滑坡、泥石流的成因及其防治[J].水土保持研究,1997,4(01):171.
Zhang Liyong.The Cause and Prevention of Slideslope, Debris Flow in the Hilly Areas of Southern Anhui Province[J].Research of Soil and Water Conservation,1997,4(01):171.
[6]李树德.中国滑坡、泥石流灾害的时空分布特点[J].水土保持研究,1999,6(04):33.
Li Shude.The Temporal and Spacial Distribution of Landslide and Debris Flow Disasters in China[J].Research of Soil and Water Conservation,1999,6(01):33.
[7]吴正华.北京泥石流灾害及其降水触发条件[J].水土保持研究,2001,8(01):67.
WU Zhenghua.The Mud-rock Flow Disaster and Their Touch off Condition by Rainfall in Beijing Area[J].Research of Soil and Water Conservation,2001,8(01):67.
[8]崔之久,冯金良.东川蒋家沟泥石流沉积亚相组合特征[J].水土保持研究,2001,8(02):2.
CUI Zhi-jiu,FENG Jin-liang.Combination Features of Depositional Sub-facies of Debris-flowon the Jiangjiagou Valley, Yunnan Province[J].Research of Soil and Water Conservation,2001,8(01):2.
[9]冯金良,崔之久,李庆辰.太行山区下瓦岔泥石流灾害实录[J].水土保持研究,2001,8(02):41.
FENG Jin-liang,CUI Zhi-jiu,LI Qing-chen.The Record of Xiawacha Debris-flow in Taihang Mountains[J].Research of Soil and Water Conservation,2001,8(01):41.
[10]李永化,张小咏,崔之久.陇南山地泥石流期、气候期与构造期的耦合[J].水土保持研究,2003,10(02):96.
LI Yonghua,ZHANG Xiaoyong,CUI Zhijiu.Coupling of Debris Flow Period, Climate Period and Tectonic Period in the Mountainous Area of Longnan[J].Research of Soil and Water Conservation,2003,10(01):96.
[11]吕学军,佘猛.泥石流堆积物粒度分维的讨论[J].水土保持研究,2007,14(04):105.
LÜ,Xue-jun,SHE Meng.Discussion on Grain-size Fractal Dimension of Debris Flow Accumulations[J].Research of Soil and Water Conservation,2007,14(01):105.
收稿日期:2009-7-6。
基金项目:国家自然基金(40771128);国际合作项目(2009DFA32490)
作者简介:吕晶(1983- ),女,吉林白城人,硕士研究生,研究方向:山地灾害防治.E-mail:lvjing730@sohu.com
通讯作者:高甲荣(1963- ),男,副教授,主要从事流域管理和山地灾害防治研究.E-mail:jiaronggao@sohu.com