Analysis of diverse suctions in compact accumulation model composed of ball-shaped particles
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Analysis of diverse suctions in compact accumulation model composed of ball-shaped particles
Vol. 29, Issue 11, (2008)
作者机构:
1. 天津城市建设学院 土木工程系,天津,300384
2. 天津市软土特性与工程环境重点实验室,天津,300384
3. 大连理工大学 土木水利学院岩土工程研究所,大连,116024
作者简介:
基金信息:
DOI:
CLC:TU431
Online First:07 August 2013,
Published:2008
稿件说明:
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LI Shun-qun, LUAN Mao-tian, ZHAO Rui-bin, et al. Analysis of diverse suctions in compact accumulation model composed of ball-shaped particles[J]. 2008, 29(11).
DOI:
LI Shun-qun, LUAN Mao-tian, ZHAO Rui-bin, et al. Analysis of diverse suctions in compact accumulation model composed of ball-shaped particles[J]. 2008, 29(11).DOI:
Analysis of diverse suctions in compact accumulation model composed of ball-shaped particles
Based on assumed pendular state of isolated pore water
general thermodynamics theory
numerical and statistical methods
the former analytical procedure proposed in literatures is employed to study diverse suctions in state B
compact accumulation model composed of ball-shaped particles with discontinuous water and continuous air (DWCA) in its void. Development law of the three types of suctions as well as corresponding equivalent suctions with increasing saturation degree
and expression for suction ratio with contact angle and saturation degree or saturation radius as the two parameters are derived for unsaturated material in state B. The results of numerical method show that suction ratio is less than 1 in state B; and that is very different from that in state A
the incompact accumulation model composed of ball-shaped particles with DWCA. Therefore
it can be concluded that effect of tension suction on shear strength and deformation of unsaturated granular materials
usually unsaturated soils
will fall down to a certain extent comparing with that of matric suction with increase of compactness. With change of saturation degree
variation trend of the three types of suctions
especially the three equivalent suctions in state B is basically coincident with that in state A. Both in state B and in state A
logarithmic suction ratio is distinctly linear to saturation radius. Furthermore
relationship between suction ration and saturation degree in state B is linear too; but this is very different from that in state A.