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A bond contact model for methane hydrate-bearing sediments with interparticle cementation

机译:含颗粒间胶结的含甲烷水合物沉积物的键接触模型

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摘要

While methane hydrates (MHs) can be present in various forms in deep seabeds or permafrost regions, this paper deals with MH-bearing sediments (MHBS) where the MH has formed bonds between sand grains. A bond model based on experimentally validated contact laws for cemented granules is introduced to describe the mechanical behavior of the MH bonds. The model parameters were derived from measured values of temperature, water pressure and MH density. Bond width and thickness adopted for each bond of the MHBS were selected based on the degree of MH saturation. The model was implemented into a 2D distinct element method code. A series of numerical biaxial standard compression tests were carried out for various degrees of MH saturation. A comparison with available experimental data shows that the model can effectively capture the essential features of the mechanical behavior of MHBS for a wide range of levels of hydrate saturation under drained and undrained conditions. In addition, the analyses presented here shed light on the following: (1) the relationship between level of cementation and debonding mechanisms taking place at the microscopic level and the observed macro-mechanical behavior of MHBS and (2) the relationship between spatial distribution of bond breakages and contact force chains with the observed strength, dilatancy and deformability of the samples. Copyright © 2014 John Wiley & Sons, Ltd.\ud
机译:尽管甲烷水合物(MHs)可以多种形式存在于深海海床或多年冻土区,但本文涉及的是MH含沙(MHBS),其中MH已在砂粒之间形成了键。引入了基于实验验证的胶结颗粒接触定律的键模型来描述MH键的力学行为。模型参数来自温度,水压和MH密度的测量值。基于MH饱和度选择MHBS各个键所采用的键宽度和厚度。该模型被实现为2D不同元素方法代码。针对不同程度的MH饱和度进行了一系列的数值双轴标准压缩试验。与可用实验数据的比较表明,该模型可以有效地捕获排水和不排水条件下各种水合物饱和度水平下MHBS力学行为的基本特征。此外,这里提供的分析还可以发现以下几点:(1)微观水平上的胶结水平和脱胶机理与所观察到的MHBS宏观力学行为之间的关系,以及(2)MHBS的空间分布之间的关系。结合力断裂和接触力链,具有观察到的样品强度,膨胀性和可变形性。版权所有©2014 John Wiley&Sons,Ltd. \ ud

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