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,(1):61-64
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非恒定降雨入渗下砂土和壤土非饱和性状
孙元元
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
DOI:
分类号:TV139.1
基金项目:
Unsaturated characteristics of sand and loam soils with unstable rainfall and infiltration
SUN Yuan-yuan
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.
Key words:  unstable rainfall  exponential distribution  unsaturated characteristics  sandy soil  loam soil  numerical model
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