Effect of shape and orientation on rigid particle rotation and matrix deformation in simple shear flow

The rotation behaviour of rigid particles from a wide range of symmetry classes was analysed in a series of three-dimensional analogue experiments, in which the particles were embedded in a transparent linear–viscous matrix deformed to large shear strains. Comparison of the measured trajectories wit...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of structural geology 2001, Vol.23 (1), p.113-125
Hauptverfasser: Arbaret, Laurent, Mancktelow, Neil S, Burg, Jean-Pierre
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 125
container_issue 1
container_start_page 113
container_title Journal of structural geology
container_volume 23
creator Arbaret, Laurent
Mancktelow, Neil S
Burg, Jean-Pierre
description The rotation behaviour of rigid particles from a wide range of symmetry classes was analysed in a series of three-dimensional analogue experiments, in which the particles were embedded in a transparent linear–viscous matrix deformed to large shear strains. Comparison of the measured trajectories with theoretical periodic paths for rigid ellipsoids shows that quadratic, slightly orthorhombic and monoclinic particles have trajectory paths and rotation rates closest to theory. Orthorhombic and monoclinic particles, with a minimum aspect ratio >1.5, develop non-periodic trajectories. The results establish that the simplified theoretical model for ellipsoidal forms is a good approximation for a wide range of natural particle shapes. The relationship between the rotation of a rigid particle and deformation of the adjacent matrix was also determined in a series of experiments by placing the particle at different depths relative to an imprinted grid. The results are well illustrated by the surface passing through the centre of the particle and initially parallel to the shear plane. Two deformed regions in the matrix are recognised. In the first region, the matrix rotates with the particle, together forming an approximately ellipsoidal object. The second region is dominated by folds, of limited extent along the rotation axis and greatest extent in a direction that rotates asymptotically toward the shear direction. The folds rotate more slowly than the principal direction of maximum finite stretch.
doi_str_mv 10.1016/S0191-8141(00)00067-5
format Article
fullrecord <record><control><sourceid>elsevier_hal_p</sourceid><recordid>TN_cdi_hal_primary_oai_HAL_hal_00089703v1</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0191814100000675</els_id><sourcerecordid>S0191814100000675</sourcerecordid><originalsourceid>FETCH-LOGICAL-a477t-2b864d8bc86552bb19d56b6ca4efea359b6965981d21703ad9f0ffbfde4e48d63</originalsourceid><addsrcrecordid>eNqFkEFLwzAYQIMoOKc_QcjRHar52iZNTzLGdMLAg3oOaZO4SNuUpEz996br2FUIBL6890EeQrdA7oEAe3gjUELCIYc7QhaEEFYk9AzNgBdZAimBczQ7IZfoKoQvEj0K-QyZtTG6HrAzOOxkr7HsFHbe6m6Qg3UdjsfbT6twL_1g60Zj745PI9rKwdsfrLRxvp3GtsPBtn0kw05Lj03jvq_RhZFN0DfHe44-ntbvq02yfX1-WS23icyLYkjSirNc8armjNK0qqBUlFWslrk2Wma0rFjJaMlBpVCQTKrSEGMqo3Suc65YNkeLae9ONqL3tpX-VzhpxWa5FeMs1uFlVPcQWTqxtXcheG1OAhAxhhWHsGKsFj1xCCto9B4nT8eP7K32ItSxV62V9TGlUM7-s-EPgHeA2g</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Effect of shape and orientation on rigid particle rotation and matrix deformation in simple shear flow</title><source>Elsevier ScienceDirect Journals Complete</source><creator>Arbaret, Laurent ; Mancktelow, Neil S ; Burg, Jean-Pierre</creator><creatorcontrib>Arbaret, Laurent ; Mancktelow, Neil S ; Burg, Jean-Pierre</creatorcontrib><description>The rotation behaviour of rigid particles from a wide range of symmetry classes was analysed in a series of three-dimensional analogue experiments, in which the particles were embedded in a transparent linear–viscous matrix deformed to large shear strains. Comparison of the measured trajectories with theoretical periodic paths for rigid ellipsoids shows that quadratic, slightly orthorhombic and monoclinic particles have trajectory paths and rotation rates closest to theory. Orthorhombic and monoclinic particles, with a minimum aspect ratio &gt;1.5, develop non-periodic trajectories. The results establish that the simplified theoretical model for ellipsoidal forms is a good approximation for a wide range of natural particle shapes. The relationship between the rotation of a rigid particle and deformation of the adjacent matrix was also determined in a series of experiments by placing the particle at different depths relative to an imprinted grid. The results are well illustrated by the surface passing through the centre of the particle and initially parallel to the shear plane. Two deformed regions in the matrix are recognised. In the first region, the matrix rotates with the particle, together forming an approximately ellipsoidal object. The second region is dominated by folds, of limited extent along the rotation axis and greatest extent in a direction that rotates asymptotically toward the shear direction. The folds rotate more slowly than the principal direction of maximum finite stretch.</description><identifier>ISSN: 0191-8141</identifier><identifier>EISSN: 1873-1201</identifier><identifier>DOI: 10.1016/S0191-8141(00)00067-5</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Earth Sciences ; Sciences of the Universe ; Volcanology</subject><ispartof>Journal of structural geology, 2001, Vol.23 (1), p.113-125</ispartof><rights>2001 Elsevier Science Ltd</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a477t-2b864d8bc86552bb19d56b6ca4efea359b6965981d21703ad9f0ffbfde4e48d63</citedby><cites>FETCH-LOGICAL-a477t-2b864d8bc86552bb19d56b6ca4efea359b6965981d21703ad9f0ffbfde4e48d63</cites><orcidid>0000-0003-4904-9035</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0191814100000675$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,314,776,780,881,3537,4010,27900,27901,27902,65306</link.rule.ids><backlink>$$Uhttps://insu.hal.science/hal-00089703$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Arbaret, Laurent</creatorcontrib><creatorcontrib>Mancktelow, Neil S</creatorcontrib><creatorcontrib>Burg, Jean-Pierre</creatorcontrib><title>Effect of shape and orientation on rigid particle rotation and matrix deformation in simple shear flow</title><title>Journal of structural geology</title><description>The rotation behaviour of rigid particles from a wide range of symmetry classes was analysed in a series of three-dimensional analogue experiments, in which the particles were embedded in a transparent linear–viscous matrix deformed to large shear strains. Comparison of the measured trajectories with theoretical periodic paths for rigid ellipsoids shows that quadratic, slightly orthorhombic and monoclinic particles have trajectory paths and rotation rates closest to theory. Orthorhombic and monoclinic particles, with a minimum aspect ratio &gt;1.5, develop non-periodic trajectories. The results establish that the simplified theoretical model for ellipsoidal forms is a good approximation for a wide range of natural particle shapes. The relationship between the rotation of a rigid particle and deformation of the adjacent matrix was also determined in a series of experiments by placing the particle at different depths relative to an imprinted grid. The results are well illustrated by the surface passing through the centre of the particle and initially parallel to the shear plane. Two deformed regions in the matrix are recognised. In the first region, the matrix rotates with the particle, together forming an approximately ellipsoidal object. The second region is dominated by folds, of limited extent along the rotation axis and greatest extent in a direction that rotates asymptotically toward the shear direction. The folds rotate more slowly than the principal direction of maximum finite stretch.</description><subject>Earth Sciences</subject><subject>Sciences of the Universe</subject><subject>Volcanology</subject><issn>0191-8141</issn><issn>1873-1201</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><recordid>eNqFkEFLwzAYQIMoOKc_QcjRHar52iZNTzLGdMLAg3oOaZO4SNuUpEz996br2FUIBL6890EeQrdA7oEAe3gjUELCIYc7QhaEEFYk9AzNgBdZAimBczQ7IZfoKoQvEj0K-QyZtTG6HrAzOOxkr7HsFHbe6m6Qg3UdjsfbT6twL_1g60Zj745PI9rKwdsfrLRxvp3GtsPBtn0kw05Lj03jvq_RhZFN0DfHe44-ntbvq02yfX1-WS23icyLYkjSirNc8armjNK0qqBUlFWslrk2Wma0rFjJaMlBpVCQTKrSEGMqo3Suc65YNkeLae9ONqL3tpX-VzhpxWa5FeMs1uFlVPcQWTqxtXcheG1OAhAxhhWHsGKsFj1xCCto9B4nT8eP7K32ItSxV62V9TGlUM7-s-EPgHeA2g</recordid><startdate>2001</startdate><enddate>2001</enddate><creator>Arbaret, Laurent</creator><creator>Mancktelow, Neil S</creator><creator>Burg, Jean-Pierre</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>AAYXX</scope><scope>CITATION</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0003-4904-9035</orcidid></search><sort><creationdate>2001</creationdate><title>Effect of shape and orientation on rigid particle rotation and matrix deformation in simple shear flow</title><author>Arbaret, Laurent ; Mancktelow, Neil S ; Burg, Jean-Pierre</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a477t-2b864d8bc86552bb19d56b6ca4efea359b6965981d21703ad9f0ffbfde4e48d63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2001</creationdate><topic>Earth Sciences</topic><topic>Sciences of the Universe</topic><topic>Volcanology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Arbaret, Laurent</creatorcontrib><creatorcontrib>Mancktelow, Neil S</creatorcontrib><creatorcontrib>Burg, Jean-Pierre</creatorcontrib><collection>CrossRef</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Journal of structural geology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Arbaret, Laurent</au><au>Mancktelow, Neil S</au><au>Burg, Jean-Pierre</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Effect of shape and orientation on rigid particle rotation and matrix deformation in simple shear flow</atitle><jtitle>Journal of structural geology</jtitle><date>2001</date><risdate>2001</risdate><volume>23</volume><issue>1</issue><spage>113</spage><epage>125</epage><pages>113-125</pages><issn>0191-8141</issn><eissn>1873-1201</eissn><abstract>The rotation behaviour of rigid particles from a wide range of symmetry classes was analysed in a series of three-dimensional analogue experiments, in which the particles were embedded in a transparent linear–viscous matrix deformed to large shear strains. Comparison of the measured trajectories with theoretical periodic paths for rigid ellipsoids shows that quadratic, slightly orthorhombic and monoclinic particles have trajectory paths and rotation rates closest to theory. Orthorhombic and monoclinic particles, with a minimum aspect ratio &gt;1.5, develop non-periodic trajectories. The results establish that the simplified theoretical model for ellipsoidal forms is a good approximation for a wide range of natural particle shapes. The relationship between the rotation of a rigid particle and deformation of the adjacent matrix was also determined in a series of experiments by placing the particle at different depths relative to an imprinted grid. The results are well illustrated by the surface passing through the centre of the particle and initially parallel to the shear plane. Two deformed regions in the matrix are recognised. In the first region, the matrix rotates with the particle, together forming an approximately ellipsoidal object. The second region is dominated by folds, of limited extent along the rotation axis and greatest extent in a direction that rotates asymptotically toward the shear direction. The folds rotate more slowly than the principal direction of maximum finite stretch.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/S0191-8141(00)00067-5</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0003-4904-9035</orcidid><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0191-8141
ispartof Journal of structural geology, 2001, Vol.23 (1), p.113-125
issn 0191-8141
1873-1201
language eng
recordid cdi_hal_primary_oai_HAL_hal_00089703v1
source Elsevier ScienceDirect Journals Complete
subjects Earth Sciences
Sciences of the Universe
Volcanology
title Effect of shape and orientation on rigid particle rotation and matrix deformation in simple shear flow
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-29T06%3A43%3A52IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-elsevier_hal_p&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Effect%20of%20shape%20and%20orientation%20on%20rigid%20particle%20rotation%20and%20matrix%20deformation%20in%20simple%20shear%20flow&rft.jtitle=Journal%20of%20structural%20geology&rft.au=Arbaret,%20Laurent&rft.date=2001&rft.volume=23&rft.issue=1&rft.spage=113&rft.epage=125&rft.pages=113-125&rft.issn=0191-8141&rft.eissn=1873-1201&rft_id=info:doi/10.1016/S0191-8141(00)00067-5&rft_dat=%3Celsevier_hal_p%3ES0191814100000675%3C/elsevier_hal_p%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rft_els_id=S0191814100000675&rfr_iscdi=true