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Rate of consolidation of stone column-improved ground considering change in permeability and compressibility during consolidation

机译:考虑固结过程中渗透率和可压缩性变化的石柱改良地面固结率

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摘要

In the available mathematical formulations to determine the rate of radial consolidation of stone column-improved ground, the soil properties especially permeability and compressibility are assumed to be constant during consolidation process. However, permeability changes with void ratio (void ratio also changes with consolidation) and compressibility of soil varies along the consolidation curve (compressibility is a function of effective stress and void ratio). Thus, these properties are not constant during consolidation period. In the present paper, mathematical formulation is developed to determine the rate of consolidation of stone column-improved ground due to radial flow considering change in permeability and compressibility of soft soil during consolidation period. Equal strain approach has been considered in the analysis. The parabolic variation in permeability and compressibility within smear zone are incorporated in the formulation. It is observed that the variation of degree of consolidation due to change in stress concentration ratio and diameter ratio reduces when variable soil properties are considered. The difference between the degree of consolidation obtained considering variable and constant soil properties is almost constant due to variation of smear zone parameters. The time required to achieve 90% degree of consolidation increases or decreases (depending on the properties of soil) by around 50%-100% or up to 25%, respectively, when change in soil properties during consolidation is considered.
机译:在确定石柱改良地面的径向固结速率的可用数学公式中,假定固结过程中土壤特性(尤其是渗透性和可压缩性)是恒定的。但是,渗透率随空隙率而变化(空隙率也随固结率而变化),土壤的可压缩性沿固结曲线变化(可压缩性是有效应力和空隙率的函数)。因此,这些属性在合并期间不是恒定的。在本文中,考虑固结期间软土的渗透性和可压缩性的变化,开发了数学公式来确定由于径向流引起的石柱改良地面的固结速率。分析中考虑了等应变法。涂抹区域内的渗透性和可压缩性呈抛物线变化。观察到,当考虑可变的土壤特性时,由于应力集中比和直径比的变化而引起的固结度变化减小。由于涂片区参数的变化,考虑到可变和恒定的土壤特性而获得的固结度之间的差异几乎是恒定的。当考虑固结过程中土壤性质的变化时,达到90%固结度所需的时间分别增加或减少(取决于土壤的性质)大约50%-100%或最多25%。

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