Changes in thermal conductivity, suction and microstructure of a compacted lime-treated silty soil during curing

被引:38
|
作者
Wang, Yejiao [1 ]
Cui, Yu-Jun [1 ]
Anh Minh Tang [1 ]
Tang, Chao-Sheng [2 ]
Benahmed, Nadia [3 ]
机构
[1] Ecole Ponts ParisTech, UR Navier CERMES, 6-8 Ave Blaise Pascal,Cite Descartes, F-77455 Champs Sur Marne 2, Marne La Vallee, France
[2] Nanjing Univ, Sch Earth Sci & Engn, 163 Xianlin Rd, Nanjing 210093, Jiangsu, Peoples R China
[3] IRSTEA, Grp Rech Ouvrages Hydraul, 3275 Route Cezanne,CS 40061, F-13182 Aix En Provence 5, France
关键词
Thermal conductivity; Suction; Microstructure; Lime-treated soil; Curing time; Mercury intrusion porosimetry; CLAYEY SOIL; BOOM CLAY; STABILIZATION; TEMPERATURE; BEHAVIOR;
D O I
10.1016/j.enggeo.2016.01.008
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
An experimental study was conducted to investigate changes of thermal conductivity, suction and microstructure of a lime-treated silty soil during curing. The soil samples were prepared with 2% lime and compacted dry (17%) and wet (22%) of optimum. The thermal conductivity, total suction and pore size distribution were determined at various curing times. Results show that the thermal conductivity of samples compacted on the dry side decreases slightly with curing time, while the curing time effect on the samples compacted on the wet side is insignificant. The total suction generally increases with curing time even though the soil water content was kept constant. The pore size distribution characteristics are mainly related to its moulding water content. As the samples are compacted on the dry side, the pore size distribution shows typical bi-modal characteristics, with a population of macro-pores and a population of micro-pores. By contrast, as the samples are compacted on the wet side, the pore size distribution shows typical uni-modal characteristics. It is found that the modal size of both the large and small pores decrease with curing time. (c) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:114 / 121
页数:8
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