摘要
研究了鄂东南5种母质发育的红壤水分特征曲线、土壤水分扩散率,推导了土壤非饱和导水率。对试验资料进行了回归分析,得出了土壤水吸力( )与土壤含水量(θ)、土壤水分扩散率(D)与土壤水饱和度(G)、土壤非饱和导水率(K)与土壤水饱和度(G)的经验公式,并将参数与土壤性质进行了相关分析, -θ、D-G之间的参数与土壤性质关系很密切。实测的土壤饱和导水率与土壤通气孔隙度关系密切。
The soil water characteristic curve and the hydraulic diffusivity (D) of the red soil derived from five parent materials in southeast of Hubei province were studied.The unsaturated hydraulic conductivity(K) was computered. By the regressive analysis of experimental data the empirical relationships of -θ,D-G,K-G were given and by the regressive analysis of parameters of ψ-θ, D-G and the soil properties the relationships between the parameters of ψ-θ,D-G and some properties of the soils were very close(-soil water suction;θ-soil water content; G-soil water saturation degree). The relationship between saturated hydraulic conductivity by experimental measurement and aeration porosity were close.
出处
《华中农业大学学报》
CAS
CSCD
北大核心
1995年第1期53-57,共5页
Journal of Huazhong Agricultural University
关键词
红壤
土壤水分
参数
土壤物理性质
red soil
soil water movement parameter
soil property