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江西兴国侵蚀荒山森林小流域的降水流出特性分析 被引量:1

THE ANALYSIS OF WATERFLOW PROPERTY FROM PRECIPITATION AT AN ERODED SMALL WATERSHED IN XINGGUO OF JIANGXI PROVINCE
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摘要 用小流域和量水堰方法6a 多的观测资料,分析了江西兴国一个面积为2.9hm^2的侵蚀荒山森林小流域的降水流出特性。年流量(Q)随年降水量(P)的增多而增加,Q/P 为48.0%~63.7%。P-Q 的差数在737mm~1128mm 之间,大体上是稳定的。由于表面水占流出量的主要部分,因而流量水平的变化极大。观测期间的流量水平最高为93.3mm/h,持续5min,最低为0.01mm/h。月流量与月降水量、日流量与日雨量、以及小时流量与小时雨量之间都基本上是线性关系。 According to observational data in six years through watershed and gauging weir approach,wa- terflow property from precipitation at a eroded small watershed covered an area of 2.9ha was analysed. The vegetation at the small watershed was deteriorated forest.Annual discharge(Q)was more and more with increase in annual precipitaton(P),Q/P was 48.0%~63.7%.The difference of P-Q was 737mm ~1 128mm,and was basically stable.Owing to surface flow made up significant part in the discharge, the variations in discharge level was tremendous,in observational period the maximum of discharge level was 93.3mm/h and continued 5min.,the minimum was 0.01mm/h.The relation of monthly discharge to monthly precipitation,the relation of daily discharge to daily rainfall,and the relation of hourly discharge to hourly rainfall were all basically linear.
出处 《资源科学》 CSSCI CSCD 北大核心 2001年第z1期76-88,共13页 Resources Science
关键词 流出特性 流量水平 流量曲线 暴雨流出 表面流出 Waterflow Property Discharge level Discharge graph Rainstorm flow Surface flow
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  • 1[1]G. E. Likens et al. Biogeochemistry of a Forested Ecosystem [M]. Springer-Verlag, 1997.
  • 2[4]中国科学院南方山区综合科学考察队.江西省泰和县自然资源和农业区划[C].能源出版社,1982.
  • 3中野秀章 李云森(译).森林水文学[M].北京:中国林业出版社,1988..
  • 4[6]山口伊佐夫.增水曲线の分析と流量配分[M].大政正隆·森林学[C]共立出版株式会社,1978.

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