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Heave Failure as a Fourth Type of Seepage-Induced Internal Instability Problems Associated With Granular Soils

机译:失稳是与粒状土壤有关的第四类渗流引起的内部失稳问题

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Internal instability problems associated with granular soils involves washing out of the fine grains within the voids of the coarse grains. This movement may involve one or more of the following, mass loss, volume change, and permeability change. Leading to the occurrence of one of these possible cases, namely, suffusion (involves mass loss with no volume change), suffusion (involves mass lose with volume reduction), fluidization (involves volume change without mass loss). These three cases are well defined in the literatures; however the authors of this paper have found a fourth case (heave failure) was not taken in consideration. Heave failure involves both mass lose and increment in volume of the granular soil. Deep understanding of this case will prevent failure of geotechnical and hydraulic structures. Here in this paper the conditions that lead to the occurrence of heave failure are defined and illustration is made based on some experimental studies. Also it is found that the applied stresses on the soil can change the mode of internal instability failure from suffusion to suffusion / suffusion failure mode. editor
机译:与粒状土壤相关的内部不稳定性问题涉及洗掉粗粒空隙中的细粒。此运动可能涉及以下一项或多项,质量损失,体积变化和渗透率变化。导致这些可能情况之一的发生,即充液(涉及质量损失而不发生体积变化),充液(涉及质量损失但减少体积),流化(涉及体积变化而没有质量损失)。这三种情况在文献中都有很好的定义。但是,本文的作者发现没有考虑第四种情况(升沉失败)。升沉破坏涉及质量损失和粒状土壤体积的增加。对这种情况的深入了解将防止岩土和水力结构的失败。在此,本文定义了导致升沉破坏的条件,并根据一些实验研究进行了说明。还发现施加在土壤上的应力可以将内部不稳定性破坏的模式从注水转变为注水/注水破坏模式。编辑

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