Rock Mechanical Property Influenced by Inhomogeneity

In order to identify the microstructure inhomogeneity influence on rock mechanical property, SEM scanning test and fractal dimension estimation were adopted. The investigations showed that the self-similarity of rock microstructure markedly changes with the scanned microscale. Different rocks behave...

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Main Authors: Yunliang Tan, Dongmei Huang, Ze Zhang
Format: Article
Language:English
Published: Hindawi Limited 2012-01-01
Series:Advances in Materials Science and Engineering
Online Access:http://dx.doi.org/10.1155/2012/418729
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spelling doaj-f92551ae2ebc429a9414239397938d032020-11-24T23:15:16ZengHindawi LimitedAdvances in Materials Science and Engineering1687-84341687-84422012-01-01201210.1155/2012/418729418729Rock Mechanical Property Influenced by InhomogeneityYunliang Tan0Dongmei Huang1Ze Zhang2State Key Laboratory of Mine Disaster Prevention and Control, Shandong University of Science and Technology, Shandong, Qingdao 266590, ChinaState Key Laboratory of Mine Disaster Prevention and Control, Shandong University of Science and Technology, Shandong, Qingdao 266590, ChinaState Key Laboratory of Mine Disaster Prevention and Control, Shandong University of Science and Technology, Shandong, Qingdao 266590, ChinaIn order to identify the microstructure inhomogeneity influence on rock mechanical property, SEM scanning test and fractal dimension estimation were adopted. The investigations showed that the self-similarity of rock microstructure markedly changes with the scanned microscale. Different rocks behave in different fractal dimension variation patterns with the scanned magnification, so it is conditional to adopt fractal dimension to describe rock material. Grey diabase and black diabase have high suitability; red sandstone has low suitability. The suitability of fractal-dimension-describing method for rocks depends on both investigating scale and rock type. The homogeneities of grey diabase, black diabase, grey sandstone, and red sandstone are 7.8, 5.7, 4.4, and 3.4, separately; their average fractal dimensions of microstructure are 2.06, 2.03, 1.72, and 1.40 correspondingly, so the homogeneity is well consistent with fractal dimension. For rock material, the stronger brittleness is, the less profile fractal dimension is. In a sense, brittleness is an image of rock inhomogeneity in macroscale, while profile fractal dimension is an image of rock inhomogeneity in microscale. To combine the test of brittleness with the estimation of fractal dimension with condition will be an effective approach for understanding rock failure mechanism, patterns, and behaviours.http://dx.doi.org/10.1155/2012/418729
collection DOAJ
language English
format Article
sources DOAJ
author Yunliang Tan
Dongmei Huang
Ze Zhang
spellingShingle Yunliang Tan
Dongmei Huang
Ze Zhang
Rock Mechanical Property Influenced by Inhomogeneity
Advances in Materials Science and Engineering
author_facet Yunliang Tan
Dongmei Huang
Ze Zhang
author_sort Yunliang Tan
title Rock Mechanical Property Influenced by Inhomogeneity
title_short Rock Mechanical Property Influenced by Inhomogeneity
title_full Rock Mechanical Property Influenced by Inhomogeneity
title_fullStr Rock Mechanical Property Influenced by Inhomogeneity
title_full_unstemmed Rock Mechanical Property Influenced by Inhomogeneity
title_sort rock mechanical property influenced by inhomogeneity
publisher Hindawi Limited
series Advances in Materials Science and Engineering
issn 1687-8434
1687-8442
publishDate 2012-01-01
description In order to identify the microstructure inhomogeneity influence on rock mechanical property, SEM scanning test and fractal dimension estimation were adopted. The investigations showed that the self-similarity of rock microstructure markedly changes with the scanned microscale. Different rocks behave in different fractal dimension variation patterns with the scanned magnification, so it is conditional to adopt fractal dimension to describe rock material. Grey diabase and black diabase have high suitability; red sandstone has low suitability. The suitability of fractal-dimension-describing method for rocks depends on both investigating scale and rock type. The homogeneities of grey diabase, black diabase, grey sandstone, and red sandstone are 7.8, 5.7, 4.4, and 3.4, separately; their average fractal dimensions of microstructure are 2.06, 2.03, 1.72, and 1.40 correspondingly, so the homogeneity is well consistent with fractal dimension. For rock material, the stronger brittleness is, the less profile fractal dimension is. In a sense, brittleness is an image of rock inhomogeneity in macroscale, while profile fractal dimension is an image of rock inhomogeneity in microscale. To combine the test of brittleness with the estimation of fractal dimension with condition will be an effective approach for understanding rock failure mechanism, patterns, and behaviours.
url http://dx.doi.org/10.1155/2012/418729
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