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非恒定降雨入渗下砂土和壤土非饱和性状
引用本文:孙元元. 非恒定降雨入渗下砂土和壤土非饱和性状[J]. 水利水运工程学报, 2007, 0(1): 61-64
作者姓名:孙元元
作者单位:南京水利科学研究院,江苏,南京,210029
摘    要:采用Gardner提出的对于土壤土-水特征曲线的指数分布假设建立数学模型,通过改变边界条件,对含水层厚度为有限和无穷深的砂土和壤土,在不同非恒定降雨强度条件下土壤非饱和性状分别进行数值模拟,得出了相应的非饱和性状变化情况.

关 键 词:非恒定降雨   指数分布   非饱和性状   砂土   壤土   数值模拟
文章编号:1009-640X(2007)01-0061-04
修稿时间:2006-01-23

Unsaturated characteristics of sand and loam soils with unstable rainfall and infiltration
SUN Yuan-yuan. Unsaturated characteristics of sand and loam soils with unstable rainfall and infiltration[J]. Hydro-Science and Engineering, 2007, 0(1): 61-64
Authors:SUN Yuan-yuan
Affiliation:Nanjing Hydraulic Research Institute, Nanjing 210029, China
Abstract:Based on the exponential distribution hypothesis for the soil-water characteristic curve of soils proposed by Gardner, a mathematical model is developed. By changing the boundary conditions, the unsaturated characteristics of sand and loam soils with finite and infinite depth of water-bearing bed under different unstable rainfall intensities are numerically modeled respectively, and the corresponding variations of unsaturated characteristics are obtained.
Keywords:unstable rainfall   exponential distribution   unsaturated characteristics   sandy soil   loam soil  numerical model
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