Small-strain stiffness of Zenoz kaolin in unsaturated conditions

被引:1
|
作者
Biglari, Mahnoosh [1 ]
d'Onofrio, Anna [2 ]
Mancuso, Claudio [2 ]
Jafari, Mohammad Kazem [3 ]
Shafiee, Ali [3 ]
Ashayeri, Iman [1 ]
机构
[1] Razi Univ, Dept Civil Engn, Kermanshah, Iran
[2] Univ Naples Federico II, Dipartimento Ingn Idraul Geotecn & Ambientale, Naples, Italy
[3] Int Inst Earthquake Eng & Seismol, Tehran, Iran
关键词
unsaturated kaolin; small-strain behavior; volumetric behavior; stress history; isotropic compression and wetting; INITIAL SHEAR STIFFNESS; STRESS; HISTORY; RATIO; SOIL;
D O I
10.1139/T11-105
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
An experimental study has been carried out to investigate the effects of isotropic compression, wetting, and drying on the initial shear stiffness of Zenoz kaolin, an unsaturated lean clay, both in normally consolidated and overconsolidated conditions. The proposed study was conducted using fixed-free resonant column - torsional shear (RCTS). Specimens were compacted using the undercompaction technique. Initial shear stiffness was measured almost continuously along complex stress paths including (i) an initial equalization stage to a suction value of 0, 50, 150, and 300 kPa; (ii) an isotropic compression stage at constant suction, up to a net stress high enough to move the loading collapse line; (iii) an isotropic unloading stage at constant suction; (iv) a wetting and (or) drying path. The mentioned stress path allowed elimination or determination of the overconsolidation effect on the initial shear stiffness measured. The behavior observed is qualitatively similar to that of saturated soil, while wetting data clearly indicate that G(0) depends significantly on volumetric behavior. In normally consolidated samples where wetting is accompanied by collapse, reduction in suction has no remarkable effect on G(0). Conversely, in overconsolidated samples G(0) reduces significantly as suction decreases.
引用
收藏
页码:311 / 322
页数:12
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