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DEM simulation of the undrained shear behavior of sand containing dissociated gas hydrate

机译:含游离气体水合物砂的不排水剪切特性的DEM模拟

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摘要

A numerical simulation technique is proposed using discrete element method (DEM) to study the undrained shear behavior of sand containing dissociated gas hydrate. Dissociation of gas hydrate in sand samples under undrained conditions is simulated first, followed by undrained bi-axial compression of these samples, which consist of three phases, i.e., sand particles, water, and methane gas. The simulations demonstrate that hydrate dissociation under undrained conditions generates significant excess pore pressure and volumetric dilation, the magnitudes of which are found to be comparable with those predicted by theoretical analysis. During the undrained bi-axial compression, sampleswith different initial degrees of hydrate saturation exhibit markedly different shear behavior. Complete strain softening behavior, i.e., static liquefaction, is observed for the samples with relatively high initial degrees of hydrate saturation, while other samples reach quasi-steady state followed by strain hardening at large strains. The observed static liquefaction is believed to be a combined result of the looser sand structure induced by hydrate dissociation, and the essentially stiff modulus of fluid under high pore pressure, despite the existence of gas in sand pores. The influence of initial sample porosity and particle shape is also investigated.
机译:提出了一种使用离散元法(DEM)的数值模拟技术,以研究含游离气体水合物的砂的不排水剪切特性。首先模拟了在不排水条件下砂样品中气体水合物的解离,然后对这些样品进行不排水双轴压缩,其由三个阶段组成,即砂粒,水和甲烷气。模拟表明,在不排水的条件下,水合物的解离会产生明显的过大孔隙压力和体积膨胀,其大小与理论分析所预测的相当。在不排水的双轴压缩过程中,初始水合物饱和度不同的样品表现出明显不同的剪切行为。对于初始水合物饱和度相对较高的样品,观察到完全的应变软化行为,即静态液化,而其他样品达到准稳态,然后在大应变下硬化。据信观察到的静态液化是水合物离解引起的较松散的砂结构和在高孔隙压力下流体的基本刚性模量的综合结果,尽管砂孔中存在气体。还研究了初始样品孔隙率和颗粒形状的影响。

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