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Comparison of shear and compression jammed packings of frictional disks
We compare the structural and mechanical properties of mechanically stable (MS) packings of frictional disks in two spatial dimensions (2D) generated with isotropic compression and simple shear protocols from discrete element modeling (DEM) simulations. We find that the average contact number and pa...
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Published in: | Granular matter 2019-11, Vol.21 (4), p.1-14, Article 109 |
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creator | Xiong, Fansheng Wang, Philip Clark, Abram H. Bertrand, Thibault Ouellette, Nicholas T. Shattuck, Mark D. O’Hern, Corey S. |
description | We compare the structural and mechanical properties of mechanically stable (MS) packings of frictional disks in two spatial dimensions (2D) generated with isotropic compression and simple shear protocols from discrete element modeling (DEM) simulations. We find that the average contact number and packing fraction at jamming onset are similar (with relative deviations
<
0.5
%
) for MS packings generated via compression and shear. In contrast, the average stress anisotropy
⟨
Σ
^
xy
⟩
=
0
for MS packings generated via isotropic compression, whereas
⟨
Σ
^
xy
⟩
>
0
for MS packings generated via simple shear. To investigate the difference in the stress state of MS packings, we develop packing-generation protocols to first unjam the MS packings, remove the frictional contacts, and then rejam them. Using these protocols, we are able to obtain rejammed packings with nearly identical particle positions and stress anisotropy distributions compared to the original jammed packings. However, we find that when we directly compare the original jammed packings and rejammed ones, there are finite stress anisotropy deviations
Δ
Σ
^
xy
. The deviations are smaller than the stress anisotropy fluctuations obtained by enumerating the force solutions within the null space of the contact networks generated via the DEM simulations. These results emphasize that even though the compression and shear jamming protocols generate packings with the same contact networks, there can be residual differences in the normal and tangential forces at each contact, and thus differences in the stress anisotropy. |
doi_str_mv | 10.1007/s10035-019-0964-9 |
format | article |
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<
0.5
%
) for MS packings generated via compression and shear. In contrast, the average stress anisotropy
⟨
Σ
^
xy
⟩
=
0
for MS packings generated via isotropic compression, whereas
⟨
Σ
^
xy
⟩
>
0
for MS packings generated via simple shear. To investigate the difference in the stress state of MS packings, we develop packing-generation protocols to first unjam the MS packings, remove the frictional contacts, and then rejam them. Using these protocols, we are able to obtain rejammed packings with nearly identical particle positions and stress anisotropy distributions compared to the original jammed packings. However, we find that when we directly compare the original jammed packings and rejammed ones, there are finite stress anisotropy deviations
Δ
Σ
^
xy
. The deviations are smaller than the stress anisotropy fluctuations obtained by enumerating the force solutions within the null space of the contact networks generated via the DEM simulations. These results emphasize that even though the compression and shear jamming protocols generate packings with the same contact networks, there can be residual differences in the normal and tangential forces at each contact, and thus differences in the stress anisotropy.</description><identifier>ISSN: 1434-5021</identifier><identifier>EISSN: 1434-7636</identifier><identifier>DOI: 10.1007/s10035-019-0964-9</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Anisotropy ; Complex Fluids and Microfluidics ; Computer simulation ; Contact stresses ; Discrete element method ; Disks ; Engineering ; Engineering Fluid Dynamics ; Engineering Thermodynamics ; Experiments ; Foundations ; Geoengineering ; Heat and Mass Transfer ; Hydraulics ; In Memoriam of Robert P. Behringer ; Industrial Chemistry/Chemical Engineering ; Jamming ; late Editor in Chief of Granular Matter ; Materials Science ; Mechanical properties ; Original Paper ; Physics ; Physics and Astronomy ; Predictions ; Research methodology ; Shear ; Soft and Granular Matter ; Variations</subject><ispartof>Granular matter, 2019-11, Vol.21 (4), p.1-14, Article 109</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2019</rights><rights>Granular Matter is a copyright of Springer, (2019). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c315t-c0ca57b5de778b28ee62c113b7303c6747b3cd8bdaade5e1a35ea260fcf5e763</citedby><cites>FETCH-LOGICAL-c315t-c0ca57b5de778b28ee62c113b7303c6747b3cd8bdaade5e1a35ea260fcf5e763</cites><orcidid>0000-0001-8473-2505 ; 0000-0002-5172-0361 ; 0000-0002-8272-5640 ; 0000-0002-3745-6349 ; 0000-0001-9812-7904 ; 0000-0001-7072-4272</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27923,27924</link.rule.ids></links><search><creatorcontrib>Xiong, Fansheng</creatorcontrib><creatorcontrib>Wang, Philip</creatorcontrib><creatorcontrib>Clark, Abram H.</creatorcontrib><creatorcontrib>Bertrand, Thibault</creatorcontrib><creatorcontrib>Ouellette, Nicholas T.</creatorcontrib><creatorcontrib>Shattuck, Mark D.</creatorcontrib><creatorcontrib>O’Hern, Corey S.</creatorcontrib><title>Comparison of shear and compression jammed packings of frictional disks</title><title>Granular matter</title><addtitle>Granular Matter</addtitle><description>We compare the structural and mechanical properties of mechanically stable (MS) packings of frictional disks in two spatial dimensions (2D) generated with isotropic compression and simple shear protocols from discrete element modeling (DEM) simulations. We find that the average contact number and packing fraction at jamming onset are similar (with relative deviations
<
0.5
%
) for MS packings generated via compression and shear. In contrast, the average stress anisotropy
⟨
Σ
^
xy
⟩
=
0
for MS packings generated via isotropic compression, whereas
⟨
Σ
^
xy
⟩
>
0
for MS packings generated via simple shear. To investigate the difference in the stress state of MS packings, we develop packing-generation protocols to first unjam the MS packings, remove the frictional contacts, and then rejam them. Using these protocols, we are able to obtain rejammed packings with nearly identical particle positions and stress anisotropy distributions compared to the original jammed packings. However, we find that when we directly compare the original jammed packings and rejammed ones, there are finite stress anisotropy deviations
Δ
Σ
^
xy
. The deviations are smaller than the stress anisotropy fluctuations obtained by enumerating the force solutions within the null space of the contact networks generated via the DEM simulations. These results emphasize that even though the compression and shear jamming protocols generate packings with the same contact networks, there can be residual differences in the normal and tangential forces at each contact, and thus differences in the stress anisotropy.</description><subject>Anisotropy</subject><subject>Complex Fluids and Microfluidics</subject><subject>Computer simulation</subject><subject>Contact stresses</subject><subject>Discrete element method</subject><subject>Disks</subject><subject>Engineering</subject><subject>Engineering Fluid Dynamics</subject><subject>Engineering Thermodynamics</subject><subject>Experiments</subject><subject>Foundations</subject><subject>Geoengineering</subject><subject>Heat and Mass Transfer</subject><subject>Hydraulics</subject><subject>In Memoriam of Robert P. Behringer</subject><subject>Industrial Chemistry/Chemical Engineering</subject><subject>Jamming</subject><subject>late Editor in Chief of Granular Matter</subject><subject>Materials Science</subject><subject>Mechanical properties</subject><subject>Original Paper</subject><subject>Physics</subject><subject>Physics and Astronomy</subject><subject>Predictions</subject><subject>Research methodology</subject><subject>Shear</subject><subject>Soft and Granular Matter</subject><subject>Variations</subject><issn>1434-5021</issn><issn>1434-7636</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp1UEtPwzAMjhBIjMEP4FZxD-TRNO0RTbAhTeKye-Qm7ui2Poi3A_-eTJ3EiYtt-XvI_hh7lOJZCmFfKFVtuJAVF1WR8-qKzWSuc24LXVxfZiOUvGV3RDshpKmknbHlYuhGiC0NfTY0GX0hxAz6kPm0j0jUJmAHXYchG8Hv235LZ2ITW39MGByy0NKe7tlNAwfCh0ufs83722ax4uvP5cfidc29lubIvfBgbG0CWlvWqkQslJdS11YL7Qub21r7UNYBIKBBCdogqEI0vjGYXpmzp8l2jMP3CenodsMppivIKSV0pXNdJpKcSD4ORBEbN8a2g_jjpHDntNyUlktpuXNarkoaNWkocfstxj_j_0W_RMxtqw</recordid><startdate>20191101</startdate><enddate>20191101</enddate><creator>Xiong, Fansheng</creator><creator>Wang, Philip</creator><creator>Clark, Abram H.</creator><creator>Bertrand, Thibault</creator><creator>Ouellette, Nicholas T.</creator><creator>Shattuck, Mark D.</creator><creator>O’Hern, Corey S.</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7SR</scope><scope>7TB</scope><scope>7XB</scope><scope>88I</scope><scope>8AO</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>KB.</scope><scope>KR7</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PDBOC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>Q9U</scope><orcidid>https://orcid.org/0000-0001-8473-2505</orcidid><orcidid>https://orcid.org/0000-0002-5172-0361</orcidid><orcidid>https://orcid.org/0000-0002-8272-5640</orcidid><orcidid>https://orcid.org/0000-0002-3745-6349</orcidid><orcidid>https://orcid.org/0000-0001-9812-7904</orcidid><orcidid>https://orcid.org/0000-0001-7072-4272</orcidid></search><sort><creationdate>20191101</creationdate><title>Comparison of shear and compression jammed packings of frictional disks</title><author>Xiong, Fansheng ; Wang, Philip ; Clark, Abram H. ; Bertrand, Thibault ; Ouellette, Nicholas T. ; Shattuck, Mark D. ; O’Hern, Corey S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c315t-c0ca57b5de778b28ee62c113b7303c6747b3cd8bdaade5e1a35ea260fcf5e763</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Anisotropy</topic><topic>Complex Fluids and Microfluidics</topic><topic>Computer simulation</topic><topic>Contact stresses</topic><topic>Discrete element method</topic><topic>Disks</topic><topic>Engineering</topic><topic>Engineering Fluid Dynamics</topic><topic>Engineering Thermodynamics</topic><topic>Experiments</topic><topic>Foundations</topic><topic>Geoengineering</topic><topic>Heat and Mass Transfer</topic><topic>Hydraulics</topic><topic>In Memoriam of Robert P. Behringer</topic><topic>Industrial Chemistry/Chemical Engineering</topic><topic>Jamming</topic><topic>late Editor in Chief of Granular Matter</topic><topic>Materials Science</topic><topic>Mechanical properties</topic><topic>Original Paper</topic><topic>Physics</topic><topic>Physics and Astronomy</topic><topic>Predictions</topic><topic>Research methodology</topic><topic>Shear</topic><topic>Soft and Granular Matter</topic><topic>Variations</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Xiong, Fansheng</creatorcontrib><creatorcontrib>Wang, Philip</creatorcontrib><creatorcontrib>Clark, Abram H.</creatorcontrib><creatorcontrib>Bertrand, Thibault</creatorcontrib><creatorcontrib>Ouellette, Nicholas T.</creatorcontrib><creatorcontrib>Shattuck, Mark D.</creatorcontrib><creatorcontrib>O’Hern, Corey S.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Engineered Materials Abstracts</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Pharma Collection</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central</collection><collection>ProQuest Central Essentials</collection><collection>AUTh Library subscriptions: ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Materials Science Collection</collection><collection>ProQuest Central Korea</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>Materials Research Database</collection><collection>Materials Science Database</collection><collection>Civil Engineering Abstracts</collection><collection>ProQuest Engineering Collection</collection><collection>ProQuest Science Journals</collection><collection>Engineering Database</collection><collection>Materials Science Collection</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Granular matter</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Xiong, Fansheng</au><au>Wang, Philip</au><au>Clark, Abram H.</au><au>Bertrand, Thibault</au><au>Ouellette, Nicholas T.</au><au>Shattuck, Mark D.</au><au>O’Hern, Corey S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Comparison of shear and compression jammed packings of frictional disks</atitle><jtitle>Granular matter</jtitle><stitle>Granular Matter</stitle><date>2019-11-01</date><risdate>2019</risdate><volume>21</volume><issue>4</issue><spage>1</spage><epage>14</epage><pages>1-14</pages><artnum>109</artnum><issn>1434-5021</issn><eissn>1434-7636</eissn><abstract>We compare the structural and mechanical properties of mechanically stable (MS) packings of frictional disks in two spatial dimensions (2D) generated with isotropic compression and simple shear protocols from discrete element modeling (DEM) simulations. We find that the average contact number and packing fraction at jamming onset are similar (with relative deviations
<
0.5
%
) for MS packings generated via compression and shear. In contrast, the average stress anisotropy
⟨
Σ
^
xy
⟩
=
0
for MS packings generated via isotropic compression, whereas
⟨
Σ
^
xy
⟩
>
0
for MS packings generated via simple shear. To investigate the difference in the stress state of MS packings, we develop packing-generation protocols to first unjam the MS packings, remove the frictional contacts, and then rejam them. Using these protocols, we are able to obtain rejammed packings with nearly identical particle positions and stress anisotropy distributions compared to the original jammed packings. However, we find that when we directly compare the original jammed packings and rejammed ones, there are finite stress anisotropy deviations
Δ
Σ
^
xy
. The deviations are smaller than the stress anisotropy fluctuations obtained by enumerating the force solutions within the null space of the contact networks generated via the DEM simulations. These results emphasize that even though the compression and shear jamming protocols generate packings with the same contact networks, there can be residual differences in the normal and tangential forces at each contact, and thus differences in the stress anisotropy.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s10035-019-0964-9</doi><tpages>14</tpages><orcidid>https://orcid.org/0000-0001-8473-2505</orcidid><orcidid>https://orcid.org/0000-0002-5172-0361</orcidid><orcidid>https://orcid.org/0000-0002-8272-5640</orcidid><orcidid>https://orcid.org/0000-0002-3745-6349</orcidid><orcidid>https://orcid.org/0000-0001-9812-7904</orcidid><orcidid>https://orcid.org/0000-0001-7072-4272</orcidid></addata></record> |
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subjects | Anisotropy Complex Fluids and Microfluidics Computer simulation Contact stresses Discrete element method Disks Engineering Engineering Fluid Dynamics Engineering Thermodynamics Experiments Foundations Geoengineering Heat and Mass Transfer Hydraulics In Memoriam of Robert P. Behringer Industrial Chemistry/Chemical Engineering Jamming late Editor in Chief of Granular Matter Materials Science Mechanical properties Original Paper Physics Physics and Astronomy Predictions Research methodology Shear Soft and Granular Matter Variations |
title | Comparison of shear and compression jammed packings of frictional disks |
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