Hydro-mechanical coupling effects on volume change and water retention behaviour of unsaturated expansive soils during compression

被引:0
|
作者
College of Civil Engineering, Xinyang Normal University, Xinyang [1 ]
464000, China
不详 [2 ]
430071, China
机构
[1] College of Civil Engineering, Xinyang Normal University, Xinyang
[2] State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan
来源
Yantu Gongcheng Xuebao | / 4卷 / 629-640期
关键词
Compacted expansive soil; Degree of saturation; Hydro-mechanical coupling; Suction; Unsaturated soil; Volume change behaviour; Water density in soil; Water retention behaviour;
D O I
10.11779/CJGE201504008
中图分类号
学科分类号
摘要
During compression of unsaturated soils, the volume change and water content change interact simultaneously. The hydro-mechanical coupling effects on both of them are comprehensively investigated. For this purpose, tests on water density in soils and suction-controlled (0~1000 kPa) one-dimensional compression tests on saturated and unsaturated soils are carried out for Jingmen expansive soils. The conclusions are drawn as follows: (1) For the volume change behaviour, the yielding point can be observed on the load-compression curve, and the compression ones under higher suction intersect the curves under lower suction sequentially. The unloading curves appear to be linear, and the slopes of which decrease with the increasing suction. The volume change formula is presented, which is capable of predicting the shrinkage due to suction increase, volume compression/expansion due to loading/unloading, yielding, and the variety of compressibility due to suction change. (2) For the water retention behaviour during compression, the water content changes slightly under higher suction. When compressed to the net vertical pressure of 2941.8 kPa, the water contents under the four different suctions are similar. A three-parameter Logistic function is presented for simulating the coupling effects of suction and net vertical stress on water content. (3) The degree of saturation increases during both loading and unloading, both of which mean 'wetting'. However, the water content decreases during loading, which means 'drying'. The reason for this discrepancy is that the change of degree of saturation can be affected by change of the water content as well as that of void ratio. ©, 2015, Chinese Society of Civil Engineering. All right reserved.
引用
收藏
页码:629 / 640
页数:11
相关论文
共 32 条
  • [21] Jacinto A.C., Villar M.V., Ledesma A., Influence of water density on the water-retention curve of expansive clays, Géotechnique, 62, 8, pp. 657-667, (2012)
  • [22] Wang Q., Cui Y.-J., Tang A.M., Et al., Time- and density-dependent microstructure features of compacted bentonite, Soils and Foundations, 54, 4, pp. 657-666, (2014)
  • [23] Alonso E.E., Gens A., Josa A., A constitutive model for partially saturated soils, Géotechnique, 40, 3, pp. 405-430, (1990)
  • [24] Kong L.-W., Zhou B.-C., Bai H., Et al., Experimental study of deformation and strength characteristics of Jingmen unsaturated expansive soil, Rock and Soil Mechanics, 31, 10, pp. 3036-3042, (2010)
  • [25] Zhou B.-C., Zhang Y.-J., Tang Z.-S., Et al., Hydraulic hysteresis effect on void ratio-water content-suction behavior of Jingmen compacted expansive soil, Journal of Hydraulic Engineering, 44, 2, pp. 164-172, (2013)
  • [26] Test Guide of Soil, (1999)
  • [27] Perez-Garcia N., Houston S.L., Houston W.N., Et al., An oedometer-type pressure plate SWCC apparatus, Geotechnical Testing Journal, 31, 2, pp. 115-123, (2008)
  • [28] Butterfield R., A natural compression law for soils (an advance on e-lg p'), Géotechnique, 29, 4, pp. 469-480, (1979)
  • [29] Fredlund D.G., Rahardjo H., Soil Mechanics for Unsaturated Soils, (1993)
  • [30] Gens A., Soil-environment interactions in geotechnical engineering, Géotechnique, 60, 1, pp. 3-74, (2010)