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Shape effect of elongated soil particles on Discrete Element Modelling of methane hydrate soil sediments

机译:细长土壤颗粒的形状效应对甲烷水合物土壤沉积物离散元模拟的影响

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Investigations on the geomechanical behaviour of methane hydrate bearing soil has attracted increasing interest, as methane hydrate is a potential energy resource from which methane gas can be extracted in the dissociation of hydrate-bearing sediments. This geomechanical behaviour has impacts on geotechnical issues, such as the stability of the seabed sediment layers and the proximity of wellbores. In this numerical study of Discrete Element Modelling (DEM), triaxial compression tests were simulated to study the behaviour of methane hydrate sediments with two different assumptions on hydrate formation patterns: pore-filling case and cementation case. The soil particles were generated separately using three models: spherical particles and elongated clumps with two different aspect ratios. These were used in order to investigate the influence of soil particle shape on the geomechanical behaviour of hydrate-bearing sediments. Three soil models of different aspect ratios were generated by the same grain size distribution and inter-particle friction. The results of the DEM samples shearing at the same initial void ratio were compared. It was found that the behaviour of methane hydrate soil sediments with elongated shape soil particles seemed to be similar to that of the natural hydrate-bearing sandy sediments retrieved from the Nankai Trough. The stiffness and strength were both enhanced with an increase in aspect ratio. The values of stiffness and strength obtained from the DEM modelling became closer to the experimental results as the aspect ratio of soil particles increased. In addition, the hydrates also strengthened the sediments' skeleton. Furthermore, it was found that the hydrate growth patterns greatly influenced the hydrate-bearing soil sediments. For the given particle shape, the cementation case gave larger stiffness and strength than the pore-filling case.
机译:由于甲烷水合物是一种潜在的能源,可以从含水合物沉积物中分离出甲烷气体,因此对含甲烷水合物的土壤的地质力学行为的研究引起了越来越多的兴趣。这种岩土力学行为会影响岩土工程问题,例如海床沉积物层的稳定性和井眼的距离。在离散元建模(DEM)的数值研究中,模拟了三轴压缩试验,以对甲烷水合物沉积物的行为进行研究,其中有两个不同的水合物形成模式假设:孔隙填充情况和胶结作用情况。土壤颗粒是使用三种模型分别生成的:球形颗粒和具有两种不同长宽比的细长块。这些是为了研究土壤颗粒形状对含水合物沉积物的地质力学行为的影响。通过相同的粒度分布和颗粒间摩擦产生了三种不同长宽比的土壤模型。比较了在相同初始空隙率下剪切的DEM样品的结果。研究发现,具有长形土壤颗粒的甲烷水合物土壤沉积物的行为似乎与从南开海槽中回收的天然含水质砂质沉积物的行为相似。刚度和强度都随着纵横比的增加而增强。随着土壤颗粒长径比的增加,从DEM模型获得的刚度和强度值变得更接近于实验结果。此外,水合物还增强了沉积物的骨架。此外,还发现水合物的生长方式极大地影响了含水合物的土壤沉积物。对于给定的颗粒形状,胶结情况比填充孔的情况具有更大的刚度和强度。

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