Small-strain stiffness of compacted loess upon wetting, drying and loading: Experiments and model interpretation

IF 4.9 2区 工程技术 Q1 ENGINEERING, CIVIL
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Abstract

Stiffness of soil at very small strains G0 is mainly affected by void ratio, effective stress and suction. Empirical equations considering those factors have been proposed to estimate G0. However, for collapsible soil like loess, variations in suction might induce changes in void ratio of soil. The combined effect of these two factors poses challenges in accurately estimating of G0. This paper first presents an experimental study on the G0 of collapsible loess under various conditions, including as-compacted states, wetting/drying and K0 loading. G0 is estimated from shear wave velocity obtained with bender element technique. The changes of G0 with respect to void ratio, suction, effective stress, and wetting under K0 stress conditions are evaluated. Test results reveal that power relationships can be defined between G0 and void ratio, suction and effective stress, respectively. The changes in G0 along wetting/drying shows an “S” shape due to the different dominant effects on soil structure, as well as the induced non-uniform volume changes when suction change at different zones. Under K0 loading, G0 decreases upon wetting at stresses below the compaction stress, while it increases upon wetting at stresses above the compaction stress, due to the combined effects of densification caused by volume collapse during wetting and softening induced by suction decrease. Finally, a G0 model considering net stress and suction as independent stress variable is proposed. This model could effectively capture the change of G0 during wetting, drying and loading, as well as upon wetting under K0 loading for collapsible loess.

湿润、干燥和加载时压实黄土的小应变刚度:实验和模型解释
土壤在极小应变下的刚度 G0 主要受空隙率、有效应力和吸力的影响。已经提出了考虑这些因素的经验方程来估算 G0。然而,对于黄土等塌陷性土壤,吸力的变化可能会引起土壤空隙率的变化。这两个因素的综合影响给准确估算 G0 带来了挑战。本文首先介绍了不同条件下可塌陷黄土 G0 的实验研究,包括压实状态、湿润/干燥和 K0 荷载。G0 是根据弯管元件技术获得的剪切波速度估算的。评估了在 K0 应力条件下 G0 随空隙率、吸力、有效应力和湿润度的变化。试验结果表明,G0 分别与空隙率、吸力和有效应力之间存在幂函数关系。由于对土壤结构的主导作用不同,以及不同区域吸力变化时引起的不均匀体积变化,G0 随湿润/干燥的变化呈 "S "形。在 K0 荷载下,由于湿润过程中体积塌陷引起的致密化和吸力减小引起的软化的共同作用,G0 在应力低于压实应力的湿润过程中减小,而在应力高于压实应力的湿润过程中增大。最后,提出了一个将净应力和吸力作为独立应力变量的 G0 模型。该模型可有效捕捉塌陷黄土在湿润、干燥和加载过程中以及在 K0 加载条件下湿润时 G0 的变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Transportation Geotechnics
Transportation Geotechnics Social Sciences-Transportation
CiteScore
8.10
自引率
11.30%
发文量
194
审稿时长
51 days
期刊介绍: Transportation Geotechnics is a journal dedicated to publishing high-quality, theoretical, and applied papers that cover all facets of geotechnics for transportation infrastructure such as roads, highways, railways, underground railways, airfields, and waterways. The journal places a special emphasis on case studies that present original work relevant to the sustainable construction of transportation infrastructure. The scope of topics it addresses includes the geotechnical properties of geomaterials for sustainable and rational design and construction, the behavior of compacted and stabilized geomaterials, the use of geosynthetics and reinforcement in constructed layers and interlayers, ground improvement and slope stability for transportation infrastructures, compaction technology and management, maintenance technology, the impact of climate, embankments for highways and high-speed trains, transition zones, dredging, underwater geotechnics for infrastructure purposes, and the modeling of multi-layered structures and supporting ground under dynamic and repeated loads.
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