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首页> 外文期刊>Journal of Asian earth sciences >Prediction of the wetting-induced collapse behaviour using the soil-water characteristic curve
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Prediction of the wetting-induced collapse behaviour using the soil-water characteristic curve

机译:利用土水特征曲线预测湿润塌陷行为

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摘要

Collapsible soils go through three distinct phases in response to metric suction decrease during wetting: pre collapse phase, collapse phase and post-collapse phase. It is reasonable and conservative to consider a strain path that includes a pre-collapse phase in which constant volume is maintained and a collapse phase that extends to the final metric suction to be experienced by collapsible soils during wetting. Upon this assumption, a method is proposed for predicting the collapse behaviour due to wetting. To use the proposed method, two parameters, critical suction and collapse rate, are required. The former is the suction value below which significant collapse deformations take place in response to matric suction decease, and the later is the rate at which void ratio reduces with metric suction in the collapse phase. The value of critical suction can be estimated from the water entry value taking account of both the microstructure characteristics and collapse mechanism of fine-grained collapsible soils; the wetting soil-water characteristic curve thus can be used as a tool. Five sets of data of wetting tests on both compacted and natural collapsible soils reported in the literature were used to validate the proposed method. The critical suction values were estimated from the water-entry value with parameter a that is suggested to vary between 0.10 and 0.25 for compacted soils and to be lower for natural collapsible soils. The results of a field permeation test in collapsible loess soils were also used to validate the proposed method. The relatively good agreement between the measured and estimated collapse deformations suggests that the proposed method can provide reasonable prediction of the collapse behaviour due to wetting.
机译:可湿性土壤在润湿过程中响应于度量吸力下降而经历三个不同的阶段:塌陷前阶段,塌陷阶段和塌陷后阶段。考虑到应变路径是合理且保守的,该应变路径包括一个预塌陷阶段(在该阶段中保持恒定的体积)和一个塌陷阶段,该阶段一直持续到湿润过程中可塌陷土壤经历的最终公制吸力。基于该假设,提出了一种用于预测由于润湿而引起的坍塌行为的方法。为了使用所提出的方法,需要两个参数,临界吸力和坍塌率。前者是吸力值,在该值以下,响应于矩阵吸力下降而发生明显的塌陷变形,而后者是在塌陷阶段中空压率随公制吸力而减小的速率。临界吸力的值可以从入水值估算,同时考虑细粒可塌陷土壤的微观结构特征和崩塌机理。因此,润湿的土壤-水特征曲线可以用作工具。文献报道了五组压实和天然可湿性土壤的润湿测试数据,以验证该方法的有效性。临界吸力值是根据参数为a的进水值估算的,对于压实土壤,建议在0.10到0.25之间变化,而对于自然可塌陷土壤,则较低。在湿陷性黄土中的田间渗透测试结果也被用来验证该方法。实测和估计的塌陷变形之间的相对较好的一致性表明,所提出的方法可以为由于润湿而导致的塌陷行为提供合理的预测。

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