Study on the Change of the Mesostructure of Coarse-Grained Slip Zone Soils During the Shearing Process and Its Influence on the Macroscopic Mechanical Properties
Abstract One of the most critical criteria in determining slope stability is the strength of slip zone soils. Medium-sized shear tests on slip zone soils with various coarse particle concentrations were conducted to investigate the mechanical properties of slip zone soils and the effects of mesostru...
Ausführliche Beschreibung
Autor*in: |
Li, Zechuang [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2022 |
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Schlagwörter: |
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Anmerkung: |
© The Author(s), under exclusive licence to Indian Geotechnical Society 2022. Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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Übergeordnetes Werk: |
Enthalten in: Indian geotechnical journal - New York, NY : Springer, 2012, 53(2022), 1 vom: 24. Aug., Seite 63-77 |
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Übergeordnetes Werk: |
volume:53 ; year:2022 ; number:1 ; day:24 ; month:08 ; pages:63-77 |
Links: |
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DOI / URN: |
10.1007/s40098-022-00662-8 |
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Katalog-ID: |
SPR049229699 |
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520 | |a Abstract One of the most critical criteria in determining slope stability is the strength of slip zone soils. Medium-sized shear tests on slip zone soils with various coarse particle concentrations were conducted to investigate the mechanical properties of slip zone soils and the effects of mesostructure changes on those properties. The shear box was visualized in this study, the motion state of the coarse particles in slip zone soils was recorded using a camera during the shear process, and the evolution of the slip zone soils shear deformation was examined. The cause of the macro-mechanical properties resulting from the mesostructure change was also discussed. The internal friction angle was found to be positively correlated with the coarse particle content, while cohesion was found to be inversely correlated. The greater the content of coarse particles in slip zone soils, the greater the probability of coarse particle interlocking and the greater the influence on coarse particle rotation and displacement during shear. The results also show that the shear affected area (SAA) is thicker and the vertical displacement of slip zone soils in the upper shear box is greater with increasing coarse particle content. Furthermore, an increase in normal pressure will thin the severely disturbed area of shear, but it will increase the thickness of SAA. | ||
650 | 4 | |a Slip zone soils |7 (dpeaa)DE-He213 | |
650 | 4 | |a Coarse particle content |7 (dpeaa)DE-He213 | |
650 | 4 | |a Particle movement |7 (dpeaa)DE-He213 | |
650 | 4 | |a Mesostructured |7 (dpeaa)DE-He213 | |
650 | 4 | |a Shear band thickness |7 (dpeaa)DE-He213 | |
700 | 1 | |a Zhang, Hao |0 (orcid)0000-0003-1655-8423 |4 aut | |
700 | 1 | |a Cui, Yuan |4 aut | |
700 | 1 | |a Li, Bing |4 aut | |
700 | 1 | |a He, Xin |4 aut | |
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10.1007/s40098-022-00662-8 doi (DE-627)SPR049229699 (SPR)s40098-022-00662-8-e DE-627 ger DE-627 rakwb eng Li, Zechuang verfasserin aut Study on the Change of the Mesostructure of Coarse-Grained Slip Zone Soils During the Shearing Process and Its Influence on the Macroscopic Mechanical Properties 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Indian Geotechnical Society 2022. Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract One of the most critical criteria in determining slope stability is the strength of slip zone soils. Medium-sized shear tests on slip zone soils with various coarse particle concentrations were conducted to investigate the mechanical properties of slip zone soils and the effects of mesostructure changes on those properties. The shear box was visualized in this study, the motion state of the coarse particles in slip zone soils was recorded using a camera during the shear process, and the evolution of the slip zone soils shear deformation was examined. The cause of the macro-mechanical properties resulting from the mesostructure change was also discussed. The internal friction angle was found to be positively correlated with the coarse particle content, while cohesion was found to be inversely correlated. The greater the content of coarse particles in slip zone soils, the greater the probability of coarse particle interlocking and the greater the influence on coarse particle rotation and displacement during shear. The results also show that the shear affected area (SAA) is thicker and the vertical displacement of slip zone soils in the upper shear box is greater with increasing coarse particle content. Furthermore, an increase in normal pressure will thin the severely disturbed area of shear, but it will increase the thickness of SAA. Slip zone soils (dpeaa)DE-He213 Coarse particle content (dpeaa)DE-He213 Particle movement (dpeaa)DE-He213 Mesostructured (dpeaa)DE-He213 Shear band thickness (dpeaa)DE-He213 Zhang, Hao (orcid)0000-0003-1655-8423 aut Cui, Yuan aut Li, Bing aut He, Xin aut Enthalten in Indian geotechnical journal New York, NY : Springer, 2012 53(2022), 1 vom: 24. Aug., Seite 63-77 (DE-627)739212354 (DE-600)2707502-3 2277-3347 nnns volume:53 year:2022 number:1 day:24 month:08 pages:63-77 https://dx.doi.org/10.1007/s40098-022-00662-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 53 2022 1 24 08 63-77 |
spelling |
10.1007/s40098-022-00662-8 doi (DE-627)SPR049229699 (SPR)s40098-022-00662-8-e DE-627 ger DE-627 rakwb eng Li, Zechuang verfasserin aut Study on the Change of the Mesostructure of Coarse-Grained Slip Zone Soils During the Shearing Process and Its Influence on the Macroscopic Mechanical Properties 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Indian Geotechnical Society 2022. Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract One of the most critical criteria in determining slope stability is the strength of slip zone soils. Medium-sized shear tests on slip zone soils with various coarse particle concentrations were conducted to investigate the mechanical properties of slip zone soils and the effects of mesostructure changes on those properties. The shear box was visualized in this study, the motion state of the coarse particles in slip zone soils was recorded using a camera during the shear process, and the evolution of the slip zone soils shear deformation was examined. The cause of the macro-mechanical properties resulting from the mesostructure change was also discussed. The internal friction angle was found to be positively correlated with the coarse particle content, while cohesion was found to be inversely correlated. The greater the content of coarse particles in slip zone soils, the greater the probability of coarse particle interlocking and the greater the influence on coarse particle rotation and displacement during shear. The results also show that the shear affected area (SAA) is thicker and the vertical displacement of slip zone soils in the upper shear box is greater with increasing coarse particle content. Furthermore, an increase in normal pressure will thin the severely disturbed area of shear, but it will increase the thickness of SAA. Slip zone soils (dpeaa)DE-He213 Coarse particle content (dpeaa)DE-He213 Particle movement (dpeaa)DE-He213 Mesostructured (dpeaa)DE-He213 Shear band thickness (dpeaa)DE-He213 Zhang, Hao (orcid)0000-0003-1655-8423 aut Cui, Yuan aut Li, Bing aut He, Xin aut Enthalten in Indian geotechnical journal New York, NY : Springer, 2012 53(2022), 1 vom: 24. Aug., Seite 63-77 (DE-627)739212354 (DE-600)2707502-3 2277-3347 nnns volume:53 year:2022 number:1 day:24 month:08 pages:63-77 https://dx.doi.org/10.1007/s40098-022-00662-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 53 2022 1 24 08 63-77 |
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10.1007/s40098-022-00662-8 doi (DE-627)SPR049229699 (SPR)s40098-022-00662-8-e DE-627 ger DE-627 rakwb eng Li, Zechuang verfasserin aut Study on the Change of the Mesostructure of Coarse-Grained Slip Zone Soils During the Shearing Process and Its Influence on the Macroscopic Mechanical Properties 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Indian Geotechnical Society 2022. Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract One of the most critical criteria in determining slope stability is the strength of slip zone soils. Medium-sized shear tests on slip zone soils with various coarse particle concentrations were conducted to investigate the mechanical properties of slip zone soils and the effects of mesostructure changes on those properties. The shear box was visualized in this study, the motion state of the coarse particles in slip zone soils was recorded using a camera during the shear process, and the evolution of the slip zone soils shear deformation was examined. The cause of the macro-mechanical properties resulting from the mesostructure change was also discussed. The internal friction angle was found to be positively correlated with the coarse particle content, while cohesion was found to be inversely correlated. The greater the content of coarse particles in slip zone soils, the greater the probability of coarse particle interlocking and the greater the influence on coarse particle rotation and displacement during shear. The results also show that the shear affected area (SAA) is thicker and the vertical displacement of slip zone soils in the upper shear box is greater with increasing coarse particle content. Furthermore, an increase in normal pressure will thin the severely disturbed area of shear, but it will increase the thickness of SAA. Slip zone soils (dpeaa)DE-He213 Coarse particle content (dpeaa)DE-He213 Particle movement (dpeaa)DE-He213 Mesostructured (dpeaa)DE-He213 Shear band thickness (dpeaa)DE-He213 Zhang, Hao (orcid)0000-0003-1655-8423 aut Cui, Yuan aut Li, Bing aut He, Xin aut Enthalten in Indian geotechnical journal New York, NY : Springer, 2012 53(2022), 1 vom: 24. Aug., Seite 63-77 (DE-627)739212354 (DE-600)2707502-3 2277-3347 nnns volume:53 year:2022 number:1 day:24 month:08 pages:63-77 https://dx.doi.org/10.1007/s40098-022-00662-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 53 2022 1 24 08 63-77 |
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10.1007/s40098-022-00662-8 doi (DE-627)SPR049229699 (SPR)s40098-022-00662-8-e DE-627 ger DE-627 rakwb eng Li, Zechuang verfasserin aut Study on the Change of the Mesostructure of Coarse-Grained Slip Zone Soils During the Shearing Process and Its Influence on the Macroscopic Mechanical Properties 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Indian Geotechnical Society 2022. Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract One of the most critical criteria in determining slope stability is the strength of slip zone soils. Medium-sized shear tests on slip zone soils with various coarse particle concentrations were conducted to investigate the mechanical properties of slip zone soils and the effects of mesostructure changes on those properties. The shear box was visualized in this study, the motion state of the coarse particles in slip zone soils was recorded using a camera during the shear process, and the evolution of the slip zone soils shear deformation was examined. The cause of the macro-mechanical properties resulting from the mesostructure change was also discussed. The internal friction angle was found to be positively correlated with the coarse particle content, while cohesion was found to be inversely correlated. The greater the content of coarse particles in slip zone soils, the greater the probability of coarse particle interlocking and the greater the influence on coarse particle rotation and displacement during shear. The results also show that the shear affected area (SAA) is thicker and the vertical displacement of slip zone soils in the upper shear box is greater with increasing coarse particle content. Furthermore, an increase in normal pressure will thin the severely disturbed area of shear, but it will increase the thickness of SAA. Slip zone soils (dpeaa)DE-He213 Coarse particle content (dpeaa)DE-He213 Particle movement (dpeaa)DE-He213 Mesostructured (dpeaa)DE-He213 Shear band thickness (dpeaa)DE-He213 Zhang, Hao (orcid)0000-0003-1655-8423 aut Cui, Yuan aut Li, Bing aut He, Xin aut Enthalten in Indian geotechnical journal New York, NY : Springer, 2012 53(2022), 1 vom: 24. Aug., Seite 63-77 (DE-627)739212354 (DE-600)2707502-3 2277-3347 nnns volume:53 year:2022 number:1 day:24 month:08 pages:63-77 https://dx.doi.org/10.1007/s40098-022-00662-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 53 2022 1 24 08 63-77 |
allfieldsSound |
10.1007/s40098-022-00662-8 doi (DE-627)SPR049229699 (SPR)s40098-022-00662-8-e DE-627 ger DE-627 rakwb eng Li, Zechuang verfasserin aut Study on the Change of the Mesostructure of Coarse-Grained Slip Zone Soils During the Shearing Process and Its Influence on the Macroscopic Mechanical Properties 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Indian Geotechnical Society 2022. Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract One of the most critical criteria in determining slope stability is the strength of slip zone soils. Medium-sized shear tests on slip zone soils with various coarse particle concentrations were conducted to investigate the mechanical properties of slip zone soils and the effects of mesostructure changes on those properties. The shear box was visualized in this study, the motion state of the coarse particles in slip zone soils was recorded using a camera during the shear process, and the evolution of the slip zone soils shear deformation was examined. The cause of the macro-mechanical properties resulting from the mesostructure change was also discussed. The internal friction angle was found to be positively correlated with the coarse particle content, while cohesion was found to be inversely correlated. The greater the content of coarse particles in slip zone soils, the greater the probability of coarse particle interlocking and the greater the influence on coarse particle rotation and displacement during shear. The results also show that the shear affected area (SAA) is thicker and the vertical displacement of slip zone soils in the upper shear box is greater with increasing coarse particle content. Furthermore, an increase in normal pressure will thin the severely disturbed area of shear, but it will increase the thickness of SAA. Slip zone soils (dpeaa)DE-He213 Coarse particle content (dpeaa)DE-He213 Particle movement (dpeaa)DE-He213 Mesostructured (dpeaa)DE-He213 Shear band thickness (dpeaa)DE-He213 Zhang, Hao (orcid)0000-0003-1655-8423 aut Cui, Yuan aut Li, Bing aut He, Xin aut Enthalten in Indian geotechnical journal New York, NY : Springer, 2012 53(2022), 1 vom: 24. Aug., Seite 63-77 (DE-627)739212354 (DE-600)2707502-3 2277-3347 nnns volume:53 year:2022 number:1 day:24 month:08 pages:63-77 https://dx.doi.org/10.1007/s40098-022-00662-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 53 2022 1 24 08 63-77 |
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Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract One of the most critical criteria in determining slope stability is the strength of slip zone soils. Medium-sized shear tests on slip zone soils with various coarse particle concentrations were conducted to investigate the mechanical properties of slip zone soils and the effects of mesostructure changes on those properties. The shear box was visualized in this study, the motion state of the coarse particles in slip zone soils was recorded using a camera during the shear process, and the evolution of the slip zone soils shear deformation was examined. The cause of the macro-mechanical properties resulting from the mesostructure change was also discussed. The internal friction angle was found to be positively correlated with the coarse particle content, while cohesion was found to be inversely correlated. The greater the content of coarse particles in slip zone soils, the greater the probability of coarse particle interlocking and the greater the influence on coarse particle rotation and displacement during shear. The results also show that the shear affected area (SAA) is thicker and the vertical displacement of slip zone soils in the upper shear box is greater with increasing coarse particle content. Furthermore, an increase in normal pressure will thin the severely disturbed area of shear, but it will increase the thickness of SAA.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Slip zone soils</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Coarse particle content</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Particle movement</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mesostructured</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Shear band thickness</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhang, Hao</subfield><subfield code="0">(orcid)0000-0003-1655-8423</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cui, Yuan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Bing</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">He, Xin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Indian geotechnical journal</subfield><subfield code="d">New York, NY : Springer, 2012</subfield><subfield code="g">53(2022), 1 vom: 24. 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|
author |
Li, Zechuang |
spellingShingle |
Li, Zechuang misc Slip zone soils misc Coarse particle content misc Particle movement misc Mesostructured misc Shear band thickness Study on the Change of the Mesostructure of Coarse-Grained Slip Zone Soils During the Shearing Process and Its Influence on the Macroscopic Mechanical Properties |
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topic_title |
Study on the Change of the Mesostructure of Coarse-Grained Slip Zone Soils During the Shearing Process and Its Influence on the Macroscopic Mechanical Properties Slip zone soils (dpeaa)DE-He213 Coarse particle content (dpeaa)DE-He213 Particle movement (dpeaa)DE-He213 Mesostructured (dpeaa)DE-He213 Shear band thickness (dpeaa)DE-He213 |
topic |
misc Slip zone soils misc Coarse particle content misc Particle movement misc Mesostructured misc Shear band thickness |
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misc Slip zone soils misc Coarse particle content misc Particle movement misc Mesostructured misc Shear band thickness |
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Study on the Change of the Mesostructure of Coarse-Grained Slip Zone Soils During the Shearing Process and Its Influence on the Macroscopic Mechanical Properties |
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title_full |
Study on the Change of the Mesostructure of Coarse-Grained Slip Zone Soils During the Shearing Process and Its Influence on the Macroscopic Mechanical Properties |
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Indian geotechnical journal |
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Li, Zechuang Zhang, Hao Cui, Yuan Li, Bing He, Xin |
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study on the change of the mesostructure of coarse-grained slip zone soils during the shearing process and its influence on the macroscopic mechanical properties |
title_auth |
Study on the Change of the Mesostructure of Coarse-Grained Slip Zone Soils During the Shearing Process and Its Influence on the Macroscopic Mechanical Properties |
abstract |
Abstract One of the most critical criteria in determining slope stability is the strength of slip zone soils. Medium-sized shear tests on slip zone soils with various coarse particle concentrations were conducted to investigate the mechanical properties of slip zone soils and the effects of mesostructure changes on those properties. The shear box was visualized in this study, the motion state of the coarse particles in slip zone soils was recorded using a camera during the shear process, and the evolution of the slip zone soils shear deformation was examined. The cause of the macro-mechanical properties resulting from the mesostructure change was also discussed. The internal friction angle was found to be positively correlated with the coarse particle content, while cohesion was found to be inversely correlated. The greater the content of coarse particles in slip zone soils, the greater the probability of coarse particle interlocking and the greater the influence on coarse particle rotation and displacement during shear. The results also show that the shear affected area (SAA) is thicker and the vertical displacement of slip zone soils in the upper shear box is greater with increasing coarse particle content. Furthermore, an increase in normal pressure will thin the severely disturbed area of shear, but it will increase the thickness of SAA. © The Author(s), under exclusive licence to Indian Geotechnical Society 2022. Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
abstractGer |
Abstract One of the most critical criteria in determining slope stability is the strength of slip zone soils. Medium-sized shear tests on slip zone soils with various coarse particle concentrations were conducted to investigate the mechanical properties of slip zone soils and the effects of mesostructure changes on those properties. The shear box was visualized in this study, the motion state of the coarse particles in slip zone soils was recorded using a camera during the shear process, and the evolution of the slip zone soils shear deformation was examined. The cause of the macro-mechanical properties resulting from the mesostructure change was also discussed. The internal friction angle was found to be positively correlated with the coarse particle content, while cohesion was found to be inversely correlated. The greater the content of coarse particles in slip zone soils, the greater the probability of coarse particle interlocking and the greater the influence on coarse particle rotation and displacement during shear. The results also show that the shear affected area (SAA) is thicker and the vertical displacement of slip zone soils in the upper shear box is greater with increasing coarse particle content. Furthermore, an increase in normal pressure will thin the severely disturbed area of shear, but it will increase the thickness of SAA. © The Author(s), under exclusive licence to Indian Geotechnical Society 2022. Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
abstract_unstemmed |
Abstract One of the most critical criteria in determining slope stability is the strength of slip zone soils. Medium-sized shear tests on slip zone soils with various coarse particle concentrations were conducted to investigate the mechanical properties of slip zone soils and the effects of mesostructure changes on those properties. The shear box was visualized in this study, the motion state of the coarse particles in slip zone soils was recorded using a camera during the shear process, and the evolution of the slip zone soils shear deformation was examined. The cause of the macro-mechanical properties resulting from the mesostructure change was also discussed. The internal friction angle was found to be positively correlated with the coarse particle content, while cohesion was found to be inversely correlated. The greater the content of coarse particles in slip zone soils, the greater the probability of coarse particle interlocking and the greater the influence on coarse particle rotation and displacement during shear. The results also show that the shear affected area (SAA) is thicker and the vertical displacement of slip zone soils in the upper shear box is greater with increasing coarse particle content. Furthermore, an increase in normal pressure will thin the severely disturbed area of shear, but it will increase the thickness of SAA. © The Author(s), under exclusive licence to Indian Geotechnical Society 2022. Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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title_short |
Study on the Change of the Mesostructure of Coarse-Grained Slip Zone Soils During the Shearing Process and Its Influence on the Macroscopic Mechanical Properties |
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https://dx.doi.org/10.1007/s40098-022-00662-8 |
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Zhang, Hao Cui, Yuan Li, Bing He, Xin |
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Zhang, Hao Cui, Yuan Li, Bing He, Xin |
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10.1007/s40098-022-00662-8 |
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2024-07-03T23:56:44.273Z |
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score |
7.3990917 |