Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
7045100 | Applied Thermal Engineering | 2018 | 46 Pages |
Abstract
The thermal effects on micro-properties of granite were experimentally studied. The volumetric porosity was observed by the X-ray Computed Tomography (CT) technique and three-dimensional (3D) image reconstruction. Two indexes (heterogeneity coefficient and anisotropy coefficient) were proposed to describe the micro-properties of granite. The thermal effects on these two indexes were discussed. The results shows that micro-porosity increases as temperature increases between 400â¯Â°C and 800â¯Â°C. It is slightly influenced by temperature beyond this range. Both of the heterogeneity and anisotropy of thermal treated granite increase to their maximums as temperature increases to 500â¯Â°C, than decrease to constants as temperature further increases. The heterogeneity and anisotropy of granite are mainly dominated by the initial cracks below 200â¯Â°C. The thermal induced cracks are mainly in the regions of lower density mineral grains below 400â¯Â°C. Boundary cracks and trans-granular cracks generate significantly above 500â¯Â°C.
Related Topics
Physical Sciences and Engineering
Chemical Engineering
Fluid Flow and Transfer Processes
Authors
L.F. Fan, J.W. Gao, Z.J. Wu, S.Q. Yang, G.W. Ma,