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黄土高原不同类型暴雨的降水侵蚀特征
引用本文:焦菊英,王万中,等.黄土高原不同类型暴雨的降水侵蚀特征[J].干旱区资源与环境,1999,13(1):34-42.
作者姓名:焦菊英  王万中
作者单位:中国科学院水利部水土保持研究所
摘    要:本文对黄土高原的三种类型暴雨的降水、侵蚀特征进行了统计分析,结果表明:A型暴雨的雨量多为10-30mm,历时一般为30-120min,最大60min降雨量占总雨量的85%-100%;B型暴雨的雨量一般为30-100mm,降雨历时多在3h-18h之间,最大60min降雨量占总雨量的30%-70%;C型暴雨的雨量一般为60-130mm,历时大于24h,最大60min降雨量占总雨量的8%-25%。三种类型暴雨的空间分布不均匀程度是A型大于B型,B型大于C型,且A型比B型、C型大得多。A型暴雨是引起土壤侵蚀的主要暴雨,其侵蚀性降雨发生的比例占侵蚀性降雨总次数的52.7%,其侵蚀量占总侵蚀量的64%。在坡面和沟道小流域,70%的极强烈侵蚀是由A型暴雨产生的。

关 键 词:黄土高原  暴雨  雨型  降水特征  侵蚀特征

PRECIPITATION AND EROSION CHARACTERISTICS OF RAIN-STORM IN DIFFERENT PATTERN ON LOESS PLATEAU
Jiao Juying\ Wang Wanzhong\ Hao Xiaoping.PRECIPITATION AND EROSION CHARACTERISTICS OF RAIN-STORM IN DIFFERENT PATTERN ON LOESS PLATEAU[J].Journal of Arid Land Resources and Environment,1999,13(1):34-42.
Authors:Jiao Juying\ Wang Wanzhong\ Hao Xiaoping
Abstract:In this paper,the precipitation and erosion characteristics of three rainstrom types on the Loess Plateau are statistically analyzed.The results show that the individual rainfall amount of pattern A,pattern B and pattern C storm is generally 10-30mm,30-100mm and 60-130mm respectively,and the rainfall duration of the pattern A,B and C storm is usually 30-120minutes,3-18 hours and more than 24 hours,the proportion of maximum rainfall in 60 minutes in total amount is 85-100% of pattern A,30-70% of pattern B,and 8-25% of pattern C.The nonuniformity of spatial distribution of three strom types is pattern A more than pattern B,pattern B more than pattern C,and pattern A more than pattern B and C greatly.Pattern A is the main strom that causes soil and water loss,and it's proportion of erosive rainfall and soil loss in total is 52.7% and 64% respectively.In slope ,gully and watershed,70% of the extreme erosion is caused by pattern A strom. \ \
Keywords:the Loess Plateau  rainstrom  rainfall pattern  precipitation characteristics  erosion characteristics  
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