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黄土高原沟壑区土壤抗冲性研究──以黄委会西峰水土保持试验站为例
引用本文:郑世清,周佩华,周保林.黄土高原沟壑区土壤抗冲性研究──以黄委会西峰水土保持试验站为例[J].水土保持通报,1994,14(1):12-16.
作者姓名:郑世清  周佩华  周保林
作者单位:中国科学院水利部西北水土保持研究所;中国科学院水利部西北水土保持研究所;中国科学院水利部西北水土保持研究所
摘    要:通过对西峰水保站1964-1980年径流小区观测资料的统计分析,结果表明,次暴雨侵蚀模数与径流深之间以幂函数相关为最好(g=aH^b)。笔以单位面积、单位径流深的冲刷量均值做为描述土壤抗冲性的指标,并对其影响因素进行了分析。

关 键 词:黄土高原  沟壑区  土壤抗冲性
收稿时间:1993/10/15 0:00:00

The Study on Soil Anti-Scourability in Loessal Plateau Gully Region
Zheng Shiqing,Zhou Peihua and Zhou Baolin.The Study on Soil Anti-Scourability in Loessal Plateau Gully Region[J].Bulletin of Soil and Water Conservation,1994,14(1):12-16.
Authors:Zheng Shiqing  Zhou Peihua and Zhou Baolin
Institution:Northwesten Institute of Soil and Water Conservation, Academia Sinica and Minitry of Water Resources, Yangling, Shaanxi, 712100;Northwesten Institute of Soil and Water Conservation, Academia Sinica and Minitry of Water Resources, Yangling, Shaanxi, 712100;Northwesten Institute of Soil and Water Conservation, Academia Sinica and Minitry of Water Resources, Yangling, Shaanxi, 712100
Abstract:Based on statistical analysis of observed data of experiment of water and soil runoff plots at Xifeng soil and water conservation station from 1964 to 1980,it is proved that there is a very close corelation (y=aHb )between individual rain fall erosive modulus and depth of runoff,which is a power funetion. The unit individual runoff depth (KW )was as soil anti-scour index which was used to evaluate the faetors affecting soil anti-scourability.
Keywords:loesssal plateau gully region  soil anti-scourability observed data of runoff plots
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