首页|基于侵蚀降雨特征的湘江流域R因子修正算法

基于侵蚀降雨特征的湘江流域R因子修正算法

An amended computing method of R factor based on rainfall characteristic in Xiangjiang River Watershed

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降雨侵蚀因子R表示由降雨引起的土壤侵蚀的潜在能力,能够反映气候因素对土壤侵蚀能力的作用.根据湘江流域18个水文气象站近50 a的降雨量数据,采用针对不同类型降雨资料的不同R值的计算方法,对湘江流域近50 a的降雨侵蚀力R值进行估算.结果表明:Wischmemier年降雨侵蚀力经验公式与福建省降雨侵蚀力计算公式分别计算出的R1、R2值与章文波日降雨量估算方法计算出的R3值有较大误差,分别达到35.99%和45.58%,不适用于直接计算该区域的降雨侵蚀力R值;经过侵蚀降雨特征因子修正后的Wischmemier年降雨侵蚀力经验公式与福建省降雨侵蚀力计算公式计算出的年降雨侵蚀力R值精度比修正前大大提高,其平均误差减小到9.59%和5.53%,表明在缺少日降雨量数据资料的情况下,采用根据侵蚀降雨特征因子侵蚀降雨量与侵蚀降雨时间修正后的降雨侵蚀力计算公式能够更加精确地估算出研究区内降雨侵蚀力R值.
Rainfall erosivity factor R could express the potential ability of the soil loss and reflect the effect of climate factors on soil erosivity ability. At present, no study on computing method of R factor was reported in Hunan Province. In this study, different computing methods were employed to calculate rainfall erosivity factor R based on different types of precipitation records accqrding to 21 hydrology and weather stations during nearly 50 years in Xiangjiang River watershed. Results showed that compared to the rainfall erosivity factor R3 value computed with Zhang Wenbo method, both R1 and R2 values calculated by method of Wischmemier and Fujian Province respectively were not accurate enough to be used to evaluate the rainfall erosivity factory R in this area. The errors were up to 35. 99% and 45. 58% . However, after the two methods were amended by rainfall pattern factors, the precision of Rx and R2 values increased by 2 - 4 times and the average errors decreased to 9.59% and 5.53%. It can be concluded that under the situation of lacking full daily precipitation records, the amended, methods of Wischmemier and Fujian Province by rainfall pattern factories could performed optimal evaluation on rainfall erosivity factor R in this study area.

rainfall erosivity factory Rrainfall characteristic factoriesmodel amendmentXiangjiang River Watershed

寻瑞、王克林、于闽、宋希娟

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中国科学院亚热带农业生态研究所亚热带农业生态重点实验室,410125,长沙

中国科学院研究生院,100039,北京

湖南省国土资源厅,410004,长沙

降雨侵蚀力R 侵蚀降雨特征因子 模型修正 湘江流域

中国科学院知识创新工程项目中国科学院“农业生态系统氮磷循环与调控”创新团队项目

KZCX2-YW-T07KZCX2-YW-T07

2012

中国水土保持科学
中国水土保持学会

中国水土保持科学

CSTPCDCSCD
影响因子:0.902
ISSN:1672-3007
年,卷(期):2012.10(1)
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