[1]敖浩翔,刘晶,况明生,等.不同频率下的泥石流体特征数值计算方法研究——以大寨沟流域为例[J].水土保持研究,2006,13(04):93-95.
 AO Hao-xiang,LIU Jing,KUANG Ming-sheng,et al.Calculation of Characteristics Factors of Debris Flow Under Different Frequency——Take Dazhaigou Valley as an Example[J].Research of Soil and Water Conservation,2006,13(04):93-95.
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不同频率下的泥石流体特征数值计算方法研究——以大寨沟流域为例

参考文献/References:

[1] 水利部长江水利委员会水文局.水利水电工程设计洪水计算规范[M].北京:中国水利电力出版社,1993.
[2] 水利部长江水利委员会水文局.水利水电工程设计洪水计算手册[M].北京:中国水利电力出版社,1995.294-387.
[3] 刘汉超,等.泥石流防治工程设计规范[M].北京:地质出版社,2002.
[4] 谢洪.岷江干旱河谷区龙洞沟泥石流及其防治[J].自然灾害学报,2004,13(5):23-24.
[5] 张远瞩,等.泥石流流量计算方法研究[J].乐山师范学院学报,2004.19(5):107-109.
[6] 陈宁生,高延超,等.丹巴县邛山沟特大灾害性泥石流汇流过程分析[J].自然灾害学报,2004,13(3):106-107.

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备注/Memo

收稿日期:2005-12-15
基金项目:国家电力公司华东勘测设计研究院(白鹤滩水电站大寨沟、海子沟的泥石流影响及防治对策)
作者简介:敖浩翔(1982- ),男,硕士,研究方向为地貌与环境信息系统,主要从事自然灾害与GIS研究;

更新日期/Last Update: 1900-01-01