A New Stress–Strain Curve Prediction Model for Moraine Soil Under Freeze-Thaw Cycles Considering Mechanical Degradation Characteristics

IF 3.6 2区 工程技术 Q2 ENGINEERING, GEOLOGICAL
Tuo Lu, Yongbo Tie, Sai K. Vanapalli, Zhaoyu Li
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引用次数: 0

Abstract

The stress-strain behavior of remolded moraine soils is highly sensitive to freeze-thaw (F-T) cycles. However, studies on the evolution of the stress-strain curve and microstructure in remolded moraine soils under F-T cycles remain limited. To address this gap, a comprehensive experimental program was conducted that included F-T cycle tests, triaxial shear tests (TST), and micro-CT scanning to examine the influence of F-T cycles on a remolded moraine soil from Linzhi City, Xizang. In addition, a novel Duncan-Chang-Jiang-Lu (DC-JL) model has been proposed in this study to fit and predict stress-strain curves. The results show that F-T cycles cause a marked reduction in shear strength (TSS) and the initial average elastic modulus (E0) following softening and a hyperbolic bulge failure mode. TSS decreases by 12%∼30%, and E0 decreases by 30%∼45%. The DC-JL model reliably predicts stress-strain curves for any F-T cycle within the experimental range (N = 0–20) using results from N = 0, 2, 5, 10, and 20 cycles. Furthermore, the residual strength provided by the DC-JL model closely matches the experimental data. F-T cycles significantly impact mechanical behavior by deteriorating the internal microstructure, increasing micro-porosity (from 14.25% to 18.69%), and leading to the formation of numerous cracks. The findings of this study are not only valuable for a better understanding of freeze-thaw degradation in moraine soils but also for assessing long-term stability using the proposed new model.

考虑机械退化特性的冰碛土冻融循环应力-应变曲线预测新模型
重塑冰碛土的应力应变行为对冻融循环高度敏感。然而,对于F - T循环作用下重塑冰碛土的应力-应变曲线和微观结构的演变研究仍然有限。为了解决这一问题,研究人员开展了一项综合实验计划,包括F - T循环试验、三轴剪切试验(TST)和微CT扫描,以研究F - T循环对西藏林芝市重塑冰碛土的影响。此外,本研究还提出了一种新的Duncan - Chang - Jiang - Lu (DC - JL)模型来拟合和预测应力-应变曲线。结果表明,F - T循环导致剪切强度(TSS)和初始平均弹性模量(e0)在软化和双曲膨胀破坏模式后显著降低。TSS降低12% ~ 30%,e0降低30% ~ 45%。DC - JL模型使用N = 0,2,5,10和20个循环的结果,可靠地预测了实验范围内(N = 0 - 20)任何F - T循环的应力-应变曲线。此外,DC - JL模型提供的残余强度与实验数据非常吻合。F - T循环通过破坏内部微观组织,增加微孔隙率(从14.25%增加到18.69%),并导致大量裂纹的形成,从而显著影响力学行为。这项研究的发现不仅对更好地理解冰碛土壤的冻融退化有价值,而且对使用所提出的新模型评估长期稳定性也有价值。
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
CiteScore
6.40
自引率
12.50%
发文量
160
审稿时长
9 months
期刊介绍: The journal welcomes manuscripts that substantially contribute to the understanding of the complex mechanical behaviour of geomaterials (soils, rocks, concrete, ice, snow, and powders), through innovative experimental techniques, and/or through the development of novel numerical or hybrid experimental/numerical modelling concepts in geomechanics. Topics of interest include instabilities and localization, interface and surface phenomena, fracture and failure, multi-physics and other time-dependent phenomena, micromechanics and multi-scale methods, and inverse analysis and stochastic methods. Papers related to energy and environmental issues are particularly welcome. The illustration of the proposed methods and techniques to engineering problems is encouraged. However, manuscripts dealing with applications of existing methods, or proposing incremental improvements to existing methods – in particular marginal extensions of existing analytical solutions or numerical methods – will not be considered for review.
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