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Quantitative investigation of anisotropic characteristics of methane-induced strain in coal based on coal particle tracking method with X-ray computer tomography

机译:基于X射线计算机X射线断层摄影的煤颗粒跟踪方法定量研究煤中甲烷诱发应变的各向异性特征

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In order to quantify the anisotropic characteristics of coal swelling deformation during the process of methane adsorption, the inner mesoscopic structures of coal are scanned with computerized tomography (CT) and a coal particle tracking method (CPTM) is proposed to quantitatively calculate the strain of coal particulates in view of the pixel gray level matrix of CT image. The results show that the spatio-temporal distribution of coal mesoscopic deformation is inhomogeneous during the process of methane adsorption. From the spatial distribution, some parts of coal swell and other parts shrink. The mineral phase and porosity or fracture inside them are mainly swelling deformation and little shrinkage deformation. The swelling and shrinkage deformation is varying constantly with different gas pressure in the organic lithotypes of varying macerals and pore or fracture inside them. The expansion deformation tends to first squeeze the original pore or fracture inside them for more expansion space. From the temporal distribution, the magnitudes of adsorption deformation is also not uniform along with the decrease of gas pressure. After the adsorption balance, the change magnitudes of strain tend to decrease. The mesoscopic deformation of coal samples is anisotropic and the macroscopic deformation is swelling. This is verified by the cumulative total strain values of coal, which are obtained from the mesoscopic strain calculation results. This study presents mesoscopic CT and strain calculation results images of coal deformation. These data will provide the basis for the study of physical structure and mechanical properties of coal with adsorbing methane.
机译:为了定量分析甲烷吸附过程中煤溶胀变形的各向异性特征,利用计算机断层扫描技术(CT)对煤的内部介观结构进行了扫描,提出了一种煤颗粒跟踪法(CPTM)来定量计算煤的应变。考虑到CT图像的像素灰度矩阵,发现颗粒。结果表明,在甲烷吸附过程中,煤的介观形变的时空分布不均匀。从空间分布来看,煤的某些部分膨胀,而其他部分则缩小。其中的矿物相和孔隙或裂缝主要是溶胀变形和很少的收缩变形。溶胀和收缩变形随着气压的变化而不断变化,而这些气压在不同的岩浆和内部的孔隙或裂缝的有机岩性中是不同的。膨胀变形倾向于首先挤压原始的孔或内部的裂缝,以获得更多的膨胀空间。从时间分布来看,随着气体压力的降低,吸附变形的大小也不均匀。在吸附平衡之后,应变的变化幅度趋于减小。煤样品的介观形变是各向异性的,宏观形变是溶胀的。这由煤的累积总应变值验证,该值是从介观应变计算结果获得的。这项研究提出了煤变形的介观CT和应变计算结果图像。这些数据将为研究甲烷吸附甲烷的物理结构和力学性能提供依据。

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