用空气注入法对土壤去饱和进行数值分析

Sebastián Sepúlveda-Cano, C. A. Vega-Posada, E. García-Aristizabal
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引用次数: 0

摘要

通过数值分析来评估通过空气注入(即土壤去饱和)改善的粗粒、饱和砂质沉积物的有效空气推进半径(Reff)。众所周知,饱和砂土的液化循环阻力很大程度上受孔隙中气体存在的影响。对影响Reff和控制脱饱和过程的土体主要水力参数和瞬态气体的注气条件进行了参数化研究。考察了a)土水特征曲线、b)本征渗透率、c)注入压力和d)注入空气时间的影响。结果表明,注入压力和土体的固有渗透性是影响反冲程度的主要因素。算例分析表明,在注入压力一定的情况下,土壤的Reff值达到最大值。当土壤的固有渗透性增大时,达到该阈值的速度更快。结果旨在缩短现有的知识差距,并有助于开发空气注入去饱和技术的设计方法。
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Numerical analysis of soil desaturation by an air injection method
A numerical analysis is conducted to evaluate the effective radius of air advance (Reff) in coarse-grained, saturated, sandy deposits improved by means of air injection (i.e., soil desaturation). It is well-known that the cyclic resistance to liquefaction of a saturated sandy deposit is highly affected by the presence of gas in the void space. A parametric study is performed to investigate the soil’s main hydraulic parameters and air-injection conditions of the transient gas affecting Reff and controlling the desaturation process. The effects of the a) soil-water characteristic curve, b) intrinsic permeability, c) injection pressure, and d) duration of air injection are investigated. It is shown that the injection pressure and soil’s intrinsic permeability are the main factors influencing the extent of Reff. The analysed cases showed that, for a fixed injection pressure, the soil will achieve a maximum value for Reff. This threshold value is reached more rapidly when the soil’s intrinsic permeability increases. The results aim to shorten existing knowledge gaps and contribute to the development of design methodologies for air-injection desaturation techniques.
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