摘要
通过2003~2004年两年的径流小区试验,运用反推法和经验公式确定土壤可蚀性因子(K)的取值,并对两种结果进行比较分析得出衡阳紫色页岩地区的土壤可蚀性因子(K)的取值范围在0.34~0.37之间,为正确认识当地土壤特性从而提出有效减小水土流失危害的对策提供科学依据。
In order to confirm the factor(K) of soil erodibility in purple rock hilly area of southern China, the methods of inversion formula of universal soil loss equation(USLE) and empirical equation were using to get the span of K based on the data gotten from the runoff plot during two years (2003~2004), The result shows that the K value is between 0.34 and 0.37.
出处
《水土保持研究》
CSCD
北大核心
2006年第6期41-43,共3页
Research of Soil and Water Conservation
基金
长江上游水土保持委员会办公室基金项目:"南方丘陵紫色岩水土流失综合治理模式与效益研究"(2002-2004)资助
关键词
紫色页岩
土壤可蚀性因子K
通用土壤流失方程
purple shale rock
factor of soil erodibility
universal soil loss equation model