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AN ELASTO-PLASTIC CONSTITUTIVE MODEL FOR GAS HYDRATE-BEARING SOILS

机译:含气水合物土的弹塑性本构模型

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Methane gas hydrate,usually found beneath permafrost and in marine continental margin sediments worldwide,has attracted interest as a possible energy resource and as a potential agent in climate change and seafloor instability.Here,in order to describe the mechanical behavior of gas hydrate-beating sediments (GHBS),an elastoplastic model is proposed based on the framework of a critical state model.The presence of gas hydrate can increase yield stress,enhancing the cohesion,peak strength and stiffness of the earth materials.Therefore,GHBS is considered as the bonded material in the proposed model.A new bonding strength parameter is introduced into the yield function to evaluate the effect of gas hydrate on the yield behavior of the earth materials.Bonding strength of the GHBS subjected to mechanical loading and/or hydrate dissociation may be drastically reduced,causing strain softening after peak strength.Dilatancy is assumed to be a function of the bonding strength and the stress ratio,instead of the single parameter stress ratio,which can reflect the direction of plastic strain increment more realistically.The proposed model can transform into the modified Cam Clay model when hydrate saturation reduces to zero.Finally,the proposed model has been used to predict the stressstrain behaviors of GHBS in triaxial tests,and it is demonstrated that the proposed model is capable of capturing the main features of the behavior of GHBS.
机译:甲烷水合物通常在多年冻土层以下以及世界范围内的海洋大陆边缘沉积物中发现,作为一种可能的能源以及潜在的气候变化和海底不稳定性因素,引起了人们的关注。在此,为了描述搅动天然气水合物的力学行为沉积物(GHBS),基于临界状态模型的框架,提出了一种弹塑性模型。天然气水合物的存在可以增加屈服应力,增强土体的内聚力,峰值强度和刚度。模型中的粘结材料。将新的粘结强度参数引入屈服函数,以评估气体水合物对土壤材料的屈服行为的影响.GHBS在机械载荷和/或水合物分解下的粘结强度可能为急剧减小,导致峰值强度后应变软化。假定剪胀性是粘结强度和应力比的函数而不是单参数应力比,它可以更真实地反映塑性应变增量的方向。当水合物饱和度降低到零时,该模型可以转化为改进的Cam Clay模型。 GHBS在三轴试验中的应力应变行为,证明该模型能够捕捉GHBS行为的主要特征。

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