A grain-based model considering pre-existing cracks for modelling mechanical properties of crystalline rock
Mechanical properties of crystalline rock are greatly affected by its micro-structures which are characterized as highly-interlocked polygon grains and presence of micro-defects. Due to insufficient consideration of micro-structures in crystalline rock, previous simulations using discrete element me...
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Veröffentlicht in: | Computers and geotechnics 2020-11, Vol.127, p.103776, Article 103776 |
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creator | Zhang, Xiao-Ping Ji, Pei-Qi Peng, Jun Wu, Shun-Chuan Zhang, Qi |
description | Mechanical properties of crystalline rock are greatly affected by its micro-structures which are characterized as highly-interlocked polygon grains and presence of micro-defects. Due to insufficient consideration of micro-structures in crystalline rock, previous simulations using discrete element method (DEM) cannot realistically reproduce the mechanical properties of crystalline rock including crack closure behaviour and high ratio of uniaxial compressive strength (UCS) against tensile strength (TS). The irregular shape of minerals in crystalline rock is modelled by discrete element method (DEM) using grain-based model (GBM). Presence of initial cracks is incorporated into GBM by introducing two notional contact surfaces to model gradual closure behaviour under compressive loading, and to obtain a higher UCS/TS ratio. The stress-strain response and crack evolution including crack closure, crack initiation, crack coalescence as well as development of macroscopic shear failure can be realistically reproduced with the proposed model. A calibration procedure is proposed to match properties of Remiremont granite under room temperature. The influence of initial cracks on the rock is then comprehensively studied. The simulation results show a good agreement with the experimental outputs under various treatment temperatures. By modelling the polygon grain and pre-existing cracks, the simulated UCS/TS ratio can be more realistic and increased up to a value of 49. |
doi_str_mv | 10.1016/j.compgeo.2020.103776 |
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Due to insufficient consideration of micro-structures in crystalline rock, previous simulations using discrete element method (DEM) cannot realistically reproduce the mechanical properties of crystalline rock including crack closure behaviour and high ratio of uniaxial compressive strength (UCS) against tensile strength (TS). The irregular shape of minerals in crystalline rock is modelled by discrete element method (DEM) using grain-based model (GBM). Presence of initial cracks is incorporated into GBM by introducing two notional contact surfaces to model gradual closure behaviour under compressive loading, and to obtain a higher UCS/TS ratio. The stress-strain response and crack evolution including crack closure, crack initiation, crack coalescence as well as development of macroscopic shear failure can be realistically reproduced with the proposed model. A calibration procedure is proposed to match properties of Remiremont granite under room temperature. The influence of initial cracks on the rock is then comprehensively studied. The simulation results show a good agreement with the experimental outputs under various treatment temperatures. By modelling the polygon grain and pre-existing cracks, the simulated UCS/TS ratio can be more realistic and increased up to a value of 49.</description><identifier>ISSN: 0266-352X</identifier><identifier>EISSN: 1873-7633</identifier><identifier>DOI: 10.1016/j.compgeo.2020.103776</identifier><language>eng</language><publisher>New York: Elsevier Ltd</publisher><subject>Calibration ; Coalescence ; Coalescing ; Compressive strength ; Crack closure ; Crack initiation ; Cracks ; Crystal defects ; Crystal structure ; Crystalline rock ; Crystalline rocks ; Crystallinity ; Defects ; Discrete element method ; Discrete element method (DEM) ; High UCS/TS ratio ; Mechanical properties ; Micro-structure ; Minerals ; Modelling ; Polygons ; Room temperature ; Simulation ; Stress-strain curve ; Tensile strength</subject><ispartof>Computers and geotechnics, 2020-11, Vol.127, p.103776, Article 103776</ispartof><rights>2020 Elsevier Ltd</rights><rights>Copyright Elsevier BV Nov 2020</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c389t-e3d293b79198dca98f5ef5343a75e74cb1e292882c225c1547427f5d1f7badd83</citedby><cites>FETCH-LOGICAL-c389t-e3d293b79198dca98f5ef5343a75e74cb1e292882c225c1547427f5d1f7badd83</cites><orcidid>0000-0002-6076-2387 ; 0000-0001-8813-4844</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.compgeo.2020.103776$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids></links><search><creatorcontrib>Zhang, Xiao-Ping</creatorcontrib><creatorcontrib>Ji, Pei-Qi</creatorcontrib><creatorcontrib>Peng, Jun</creatorcontrib><creatorcontrib>Wu, Shun-Chuan</creatorcontrib><creatorcontrib>Zhang, Qi</creatorcontrib><title>A grain-based model considering pre-existing cracks for modelling mechanical properties of crystalline rock</title><title>Computers and geotechnics</title><description>Mechanical properties of crystalline rock are greatly affected by its micro-structures which are characterized as highly-interlocked polygon grains and presence of micro-defects. Due to insufficient consideration of micro-structures in crystalline rock, previous simulations using discrete element method (DEM) cannot realistically reproduce the mechanical properties of crystalline rock including crack closure behaviour and high ratio of uniaxial compressive strength (UCS) against tensile strength (TS). The irregular shape of minerals in crystalline rock is modelled by discrete element method (DEM) using grain-based model (GBM). Presence of initial cracks is incorporated into GBM by introducing two notional contact surfaces to model gradual closure behaviour under compressive loading, and to obtain a higher UCS/TS ratio. The stress-strain response and crack evolution including crack closure, crack initiation, crack coalescence as well as development of macroscopic shear failure can be realistically reproduced with the proposed model. A calibration procedure is proposed to match properties of Remiremont granite under room temperature. The influence of initial cracks on the rock is then comprehensively studied. The simulation results show a good agreement with the experimental outputs under various treatment temperatures. By modelling the polygon grain and pre-existing cracks, the simulated UCS/TS ratio can be more realistic and increased up to a value of 49.</description><subject>Calibration</subject><subject>Coalescence</subject><subject>Coalescing</subject><subject>Compressive strength</subject><subject>Crack closure</subject><subject>Crack initiation</subject><subject>Cracks</subject><subject>Crystal defects</subject><subject>Crystal structure</subject><subject>Crystalline rock</subject><subject>Crystalline rocks</subject><subject>Crystallinity</subject><subject>Defects</subject><subject>Discrete element method</subject><subject>Discrete element method (DEM)</subject><subject>High UCS/TS ratio</subject><subject>Mechanical properties</subject><subject>Micro-structure</subject><subject>Minerals</subject><subject>Modelling</subject><subject>Polygons</subject><subject>Room temperature</subject><subject>Simulation</subject><subject>Stress-strain curve</subject><subject>Tensile strength</subject><issn>0266-352X</issn><issn>1873-7633</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNqFkE1LxDAQhoMouK7-BKHguWuTNE1zkmXxCxa8KHgLaTJd022bmnTF_femdO-ehgzPOzN5ELrF2QpnuLhvVtp1ww7cimRk6lHOizO0wCWnKS8oPUeLjBRFShn5vERXITRZzIlSLNB-ney8sn1aqQAm6ZyBNtGuD9aAt_0uGTyk8GvDOD20V3ofktr5mWynZgf6S_VWqzbCbgA_WgiJqyN9DKOaIEi80_trdFGrNsDNqS7Rx9Pj--Yl3b49v27W21TTUowpUEMErbjAojRaibJmUDOaU8UZ8FxXGIggZUk0IUxjlvOc8JoZXPNKGVPSJbqb58Zzvg8QRtm4g-_jSklylhciiyIixWZKexeCh1oO3nbKHyXO5ORVNvLkVU5e5ew15h7mHMQv_FjwMmgLvQZjPehRGmf_mfAHNReFZw</recordid><startdate>202011</startdate><enddate>202011</enddate><creator>Zhang, Xiao-Ping</creator><creator>Ji, Pei-Qi</creator><creator>Peng, Jun</creator><creator>Wu, Shun-Chuan</creator><creator>Zhang, Qi</creator><general>Elsevier Ltd</general><general>Elsevier BV</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SC</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>JQ2</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><scope>L~C</scope><scope>L~D</scope><orcidid>https://orcid.org/0000-0002-6076-2387</orcidid><orcidid>https://orcid.org/0000-0001-8813-4844</orcidid></search><sort><creationdate>202011</creationdate><title>A grain-based model considering pre-existing cracks for modelling mechanical properties of crystalline rock</title><author>Zhang, Xiao-Ping ; Ji, Pei-Qi ; Peng, Jun ; Wu, Shun-Chuan ; Zhang, Qi</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c389t-e3d293b79198dca98f5ef5343a75e74cb1e292882c225c1547427f5d1f7badd83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Calibration</topic><topic>Coalescence</topic><topic>Coalescing</topic><topic>Compressive strength</topic><topic>Crack closure</topic><topic>Crack initiation</topic><topic>Cracks</topic><topic>Crystal defects</topic><topic>Crystal structure</topic><topic>Crystalline rock</topic><topic>Crystalline rocks</topic><topic>Crystallinity</topic><topic>Defects</topic><topic>Discrete element method</topic><topic>Discrete element method (DEM)</topic><topic>High UCS/TS ratio</topic><topic>Mechanical properties</topic><topic>Micro-structure</topic><topic>Minerals</topic><topic>Modelling</topic><topic>Polygons</topic><topic>Room temperature</topic><topic>Simulation</topic><topic>Stress-strain curve</topic><topic>Tensile strength</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhang, Xiao-Ping</creatorcontrib><creatorcontrib>Ji, Pei-Qi</creatorcontrib><creatorcontrib>Peng, Jun</creatorcontrib><creatorcontrib>Wu, Shun-Chuan</creatorcontrib><creatorcontrib>Zhang, Qi</creatorcontrib><collection>CrossRef</collection><collection>Computer and Information Systems Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>ProQuest Computer Science Collection</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Computer and Information Systems Abstracts Academic</collection><collection>Computer and Information Systems Abstracts Professional</collection><jtitle>Computers and geotechnics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhang, Xiao-Ping</au><au>Ji, Pei-Qi</au><au>Peng, Jun</au><au>Wu, Shun-Chuan</au><au>Zhang, Qi</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A grain-based model considering pre-existing cracks for modelling mechanical properties of crystalline rock</atitle><jtitle>Computers and geotechnics</jtitle><date>2020-11</date><risdate>2020</risdate><volume>127</volume><spage>103776</spage><pages>103776-</pages><artnum>103776</artnum><issn>0266-352X</issn><eissn>1873-7633</eissn><abstract>Mechanical properties of crystalline rock are greatly affected by its micro-structures which are characterized as highly-interlocked polygon grains and presence of micro-defects. Due to insufficient consideration of micro-structures in crystalline rock, previous simulations using discrete element method (DEM) cannot realistically reproduce the mechanical properties of crystalline rock including crack closure behaviour and high ratio of uniaxial compressive strength (UCS) against tensile strength (TS). The irregular shape of minerals in crystalline rock is modelled by discrete element method (DEM) using grain-based model (GBM). Presence of initial cracks is incorporated into GBM by introducing two notional contact surfaces to model gradual closure behaviour under compressive loading, and to obtain a higher UCS/TS ratio. The stress-strain response and crack evolution including crack closure, crack initiation, crack coalescence as well as development of macroscopic shear failure can be realistically reproduced with the proposed model. A calibration procedure is proposed to match properties of Remiremont granite under room temperature. The influence of initial cracks on the rock is then comprehensively studied. The simulation results show a good agreement with the experimental outputs under various treatment temperatures. By modelling the polygon grain and pre-existing cracks, the simulated UCS/TS ratio can be more realistic and increased up to a value of 49.</abstract><cop>New York</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.compgeo.2020.103776</doi><orcidid>https://orcid.org/0000-0002-6076-2387</orcidid><orcidid>https://orcid.org/0000-0001-8813-4844</orcidid></addata></record> |
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subjects | Calibration Coalescence Coalescing Compressive strength Crack closure Crack initiation Cracks Crystal defects Crystal structure Crystalline rock Crystalline rocks Crystallinity Defects Discrete element method Discrete element method (DEM) High UCS/TS ratio Mechanical properties Micro-structure Minerals Modelling Polygons Room temperature Simulation Stress-strain curve Tensile strength |
title | A grain-based model considering pre-existing cracks for modelling mechanical properties of crystalline rock |
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