A simplified directly determination of soil-water retention curve from pore size distribution

被引:10
作者
Niu, Geng [1 ,2 ]
Shao, Longtan [1 ]
Sun, De'an [3 ]
Guo, Xiaoxia [1 ,2 ]
机构
[1] Dalian Univ Technol, State Key Lab Struct Anal Ind Equipment, Dalian 116024, Liaoning, Peoples R China
[2] Dalian Univ Technol, Dept Engn Mech, Dalian 116024, Liaoning, Peoples R China
[3] Shanghai Univ, Dept Civil Engn, Shanghai 200444, Peoples R China
基金
中国国家自然科学基金;
关键词
soil water retention curve; pore size distribution; air-entry condition; residual condition; mercury intrusion porosimetry; VOLUME CHANGE; HYDRAULIC CONDUCTIVITY; UNSATURATED SOIL; BEHAVIOR; SATURATION; SUCTION; MODEL; PERMEABILITY; DENSITIES; EQUATIONS;
D O I
10.12989/gae.2020.20.5.411
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Numbers fitting-curve equations have been proposed to predict soil-water retention curve (SWRC) whose parameters have no definitude physical meaning. And these methods with precondition of measuring SWRC data is time-consuming. A simplified directly method to estimate SWRC without parameters obtained by fitting-curve is proposed. Firstly, the total SWRC can be discretized into linear segments respectively. Every segment can be represented by linear formulation and every turning point can be determined by the pore-size distribution (PSD) of Mercury Intrusion Porosimetry (MIP) tests. The pore diameters governing the air-entry condition (AEC) and residual condition (RC) can be determined by the PSDs of MIP test. The PSD changes significantly during drying in SWR test, so the determination of AEC and RC should use the PSD under corresponding suction conditions. Every parameter in proposed equations can be determined directly by PSD without curve-fitting procedure and has definitude physical meaning. The proposed equations give a good estimation of both unimodal and bimodal SWRCs.
引用
收藏
页码:411 / 420
页数:10
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