Was the deep-seated gravitational slope deformation enhanced by an earthquake? Evidence from shaking table tests
Abstract A large-scale landslide occurred in Maoxian County, Sichuan Province, on June 24th, 2017, which destroyed Xinmo village and resulted in injuries and the deaths of 83 people. According to earthquake data, earthquakes greater than Ms 7.0 have occurred many times at this location. The importan...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Lei, Jin [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: |
© Saudi Society for Geosciences 2022 |
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| Übergeordnetes Werk: |
Enthalten in: Arabian journal of geosciences - Berlin : Springer, 2008, 15(2022), 16 vom: Aug. |
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| Übergeordnetes Werk: |
volume:15 ; year:2022 ; number:16 ; month:08 |
| Links: |
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| DOI / URN: |
10.1007/s12517-022-10671-9 |
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| Katalog-ID: |
SPR047875976 |
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| 520 | |a Abstract A large-scale landslide occurred in Maoxian County, Sichuan Province, on June 24th, 2017, which destroyed Xinmo village and resulted in injuries and the deaths of 83 people. According to earthquake data, earthquakes greater than Ms 7.0 have occurred many times at this location. The importance of taking earthquake factors into consideration during the study of gravity-induced deformation is emphasized in this study. Careful field investigation reveals that macrocracks developed in the source area before landsliding, and there are many gravity-induced (buckling) deformation traces in the landslide area. After a large shaking table test, the deformation failure characteristics of the slope caused by multiple earthquake simulation actions were compared with the practical consequences caused by the Xinmo Landslide. The tension fracture and buckling failure revealed by the test is highly similar to the real phenomena of the Xinmo Landslide in the field, as discovered by historical images. Therefore, undeniably, earthquakes have made important contributions to the Xinmo Landslide, even though the Xinmo Landslide has apparent gravity-induced deformation properties. Furthermore, the influence of earthquakes, gravity, rainfall, and other external factors on landslides is not just supposition. Inter-feedback actions between them gave rise to the landslide event. | ||
| 650 | 4 | |a Shaking table test |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Buckling |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Gravitational deformation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Earthquake |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Cui, Shenghua |0 (orcid)0000-0002-6638-230X |4 aut | |
| 700 | 1 | |a Pei, Xiangjun |4 aut | |
| 700 | 1 | |a Yang, Hailong |4 aut | |
| 700 | 1 | |a Luo, Luogaung |4 aut | |
| 700 | 1 | |a Yang, Qingwen |4 aut | |
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10.1007/s12517-022-10671-9 doi (DE-627)SPR047875976 (SPR)s12517-022-10671-9-e DE-627 ger DE-627 rakwb eng Lei, Jin verfasserin aut Was the deep-seated gravitational slope deformation enhanced by an earthquake? Evidence from shaking table tests 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Saudi Society for Geosciences 2022 Abstract A large-scale landslide occurred in Maoxian County, Sichuan Province, on June 24th, 2017, which destroyed Xinmo village and resulted in injuries and the deaths of 83 people. According to earthquake data, earthquakes greater than Ms 7.0 have occurred many times at this location. The importance of taking earthquake factors into consideration during the study of gravity-induced deformation is emphasized in this study. Careful field investigation reveals that macrocracks developed in the source area before landsliding, and there are many gravity-induced (buckling) deformation traces in the landslide area. After a large shaking table test, the deformation failure characteristics of the slope caused by multiple earthquake simulation actions were compared with the practical consequences caused by the Xinmo Landslide. The tension fracture and buckling failure revealed by the test is highly similar to the real phenomena of the Xinmo Landslide in the field, as discovered by historical images. Therefore, undeniably, earthquakes have made important contributions to the Xinmo Landslide, even though the Xinmo Landslide has apparent gravity-induced deformation properties. Furthermore, the influence of earthquakes, gravity, rainfall, and other external factors on landslides is not just supposition. Inter-feedback actions between them gave rise to the landslide event. Shaking table test (dpeaa)DE-He213 Buckling (dpeaa)DE-He213 Gravitational deformation (dpeaa)DE-He213 Earthquake (dpeaa)DE-He213 Cui, Shenghua (orcid)0000-0002-6638-230X aut Pei, Xiangjun aut Yang, Hailong aut Luo, Luogaung aut Yang, Qingwen aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 15(2022), 16 vom: Aug. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:15 year:2022 number:16 month:08 https://dx.doi.org/10.1007/s12517-022-10671-9 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_381 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_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_2190 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 15 2022 16 08 |
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10.1007/s12517-022-10671-9 doi (DE-627)SPR047875976 (SPR)s12517-022-10671-9-e DE-627 ger DE-627 rakwb eng Lei, Jin verfasserin aut Was the deep-seated gravitational slope deformation enhanced by an earthquake? Evidence from shaking table tests 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Saudi Society for Geosciences 2022 Abstract A large-scale landslide occurred in Maoxian County, Sichuan Province, on June 24th, 2017, which destroyed Xinmo village and resulted in injuries and the deaths of 83 people. According to earthquake data, earthquakes greater than Ms 7.0 have occurred many times at this location. The importance of taking earthquake factors into consideration during the study of gravity-induced deformation is emphasized in this study. Careful field investigation reveals that macrocracks developed in the source area before landsliding, and there are many gravity-induced (buckling) deformation traces in the landslide area. After a large shaking table test, the deformation failure characteristics of the slope caused by multiple earthquake simulation actions were compared with the practical consequences caused by the Xinmo Landslide. The tension fracture and buckling failure revealed by the test is highly similar to the real phenomena of the Xinmo Landslide in the field, as discovered by historical images. Therefore, undeniably, earthquakes have made important contributions to the Xinmo Landslide, even though the Xinmo Landslide has apparent gravity-induced deformation properties. Furthermore, the influence of earthquakes, gravity, rainfall, and other external factors on landslides is not just supposition. Inter-feedback actions between them gave rise to the landslide event. Shaking table test (dpeaa)DE-He213 Buckling (dpeaa)DE-He213 Gravitational deformation (dpeaa)DE-He213 Earthquake (dpeaa)DE-He213 Cui, Shenghua (orcid)0000-0002-6638-230X aut Pei, Xiangjun aut Yang, Hailong aut Luo, Luogaung aut Yang, Qingwen aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 15(2022), 16 vom: Aug. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:15 year:2022 number:16 month:08 https://dx.doi.org/10.1007/s12517-022-10671-9 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_381 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_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_2190 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 15 2022 16 08 |
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10.1007/s12517-022-10671-9 doi (DE-627)SPR047875976 (SPR)s12517-022-10671-9-e DE-627 ger DE-627 rakwb eng Lei, Jin verfasserin aut Was the deep-seated gravitational slope deformation enhanced by an earthquake? Evidence from shaking table tests 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Saudi Society for Geosciences 2022 Abstract A large-scale landslide occurred in Maoxian County, Sichuan Province, on June 24th, 2017, which destroyed Xinmo village and resulted in injuries and the deaths of 83 people. According to earthquake data, earthquakes greater than Ms 7.0 have occurred many times at this location. The importance of taking earthquake factors into consideration during the study of gravity-induced deformation is emphasized in this study. Careful field investigation reveals that macrocracks developed in the source area before landsliding, and there are many gravity-induced (buckling) deformation traces in the landslide area. After a large shaking table test, the deformation failure characteristics of the slope caused by multiple earthquake simulation actions were compared with the practical consequences caused by the Xinmo Landslide. The tension fracture and buckling failure revealed by the test is highly similar to the real phenomena of the Xinmo Landslide in the field, as discovered by historical images. Therefore, undeniably, earthquakes have made important contributions to the Xinmo Landslide, even though the Xinmo Landslide has apparent gravity-induced deformation properties. Furthermore, the influence of earthquakes, gravity, rainfall, and other external factors on landslides is not just supposition. Inter-feedback actions between them gave rise to the landslide event. Shaking table test (dpeaa)DE-He213 Buckling (dpeaa)DE-He213 Gravitational deformation (dpeaa)DE-He213 Earthquake (dpeaa)DE-He213 Cui, Shenghua (orcid)0000-0002-6638-230X aut Pei, Xiangjun aut Yang, Hailong aut Luo, Luogaung aut Yang, Qingwen aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 15(2022), 16 vom: Aug. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:15 year:2022 number:16 month:08 https://dx.doi.org/10.1007/s12517-022-10671-9 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_381 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_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_2190 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 15 2022 16 08 |
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10.1007/s12517-022-10671-9 doi (DE-627)SPR047875976 (SPR)s12517-022-10671-9-e DE-627 ger DE-627 rakwb eng Lei, Jin verfasserin aut Was the deep-seated gravitational slope deformation enhanced by an earthquake? Evidence from shaking table tests 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Saudi Society for Geosciences 2022 Abstract A large-scale landslide occurred in Maoxian County, Sichuan Province, on June 24th, 2017, which destroyed Xinmo village and resulted in injuries and the deaths of 83 people. According to earthquake data, earthquakes greater than Ms 7.0 have occurred many times at this location. The importance of taking earthquake factors into consideration during the study of gravity-induced deformation is emphasized in this study. Careful field investigation reveals that macrocracks developed in the source area before landsliding, and there are many gravity-induced (buckling) deformation traces in the landslide area. After a large shaking table test, the deformation failure characteristics of the slope caused by multiple earthquake simulation actions were compared with the practical consequences caused by the Xinmo Landslide. The tension fracture and buckling failure revealed by the test is highly similar to the real phenomena of the Xinmo Landslide in the field, as discovered by historical images. Therefore, undeniably, earthquakes have made important contributions to the Xinmo Landslide, even though the Xinmo Landslide has apparent gravity-induced deformation properties. Furthermore, the influence of earthquakes, gravity, rainfall, and other external factors on landslides is not just supposition. Inter-feedback actions between them gave rise to the landslide event. Shaking table test (dpeaa)DE-He213 Buckling (dpeaa)DE-He213 Gravitational deformation (dpeaa)DE-He213 Earthquake (dpeaa)DE-He213 Cui, Shenghua (orcid)0000-0002-6638-230X aut Pei, Xiangjun aut Yang, Hailong aut Luo, Luogaung aut Yang, Qingwen aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 15(2022), 16 vom: Aug. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:15 year:2022 number:16 month:08 https://dx.doi.org/10.1007/s12517-022-10671-9 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_381 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_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_2190 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 15 2022 16 08 |
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10.1007/s12517-022-10671-9 doi (DE-627)SPR047875976 (SPR)s12517-022-10671-9-e DE-627 ger DE-627 rakwb eng Lei, Jin verfasserin aut Was the deep-seated gravitational slope deformation enhanced by an earthquake? Evidence from shaking table tests 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Saudi Society for Geosciences 2022 Abstract A large-scale landslide occurred in Maoxian County, Sichuan Province, on June 24th, 2017, which destroyed Xinmo village and resulted in injuries and the deaths of 83 people. According to earthquake data, earthquakes greater than Ms 7.0 have occurred many times at this location. The importance of taking earthquake factors into consideration during the study of gravity-induced deformation is emphasized in this study. Careful field investigation reveals that macrocracks developed in the source area before landsliding, and there are many gravity-induced (buckling) deformation traces in the landslide area. After a large shaking table test, the deformation failure characteristics of the slope caused by multiple earthquake simulation actions were compared with the practical consequences caused by the Xinmo Landslide. The tension fracture and buckling failure revealed by the test is highly similar to the real phenomena of the Xinmo Landslide in the field, as discovered by historical images. Therefore, undeniably, earthquakes have made important contributions to the Xinmo Landslide, even though the Xinmo Landslide has apparent gravity-induced deformation properties. Furthermore, the influence of earthquakes, gravity, rainfall, and other external factors on landslides is not just supposition. Inter-feedback actions between them gave rise to the landslide event. Shaking table test (dpeaa)DE-He213 Buckling (dpeaa)DE-He213 Gravitational deformation (dpeaa)DE-He213 Earthquake (dpeaa)DE-He213 Cui, Shenghua (orcid)0000-0002-6638-230X aut Pei, Xiangjun aut Yang, Hailong aut Luo, Luogaung aut Yang, Qingwen aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 15(2022), 16 vom: Aug. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:15 year:2022 number:16 month:08 https://dx.doi.org/10.1007/s12517-022-10671-9 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_381 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_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_2190 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 15 2022 16 08 |
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Lei, Jin |
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Lei, Jin misc Shaking table test misc Buckling misc Gravitational deformation misc Earthquake Was the deep-seated gravitational slope deformation enhanced by an earthquake? Evidence from shaking table tests |
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Was the deep-seated gravitational slope deformation enhanced by an earthquake? Evidence from shaking table tests Shaking table test (dpeaa)DE-He213 Buckling (dpeaa)DE-He213 Gravitational deformation (dpeaa)DE-He213 Earthquake (dpeaa)DE-He213 |
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Was the deep-seated gravitational slope deformation enhanced by an earthquake? Evidence from shaking table tests |
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Was the deep-seated gravitational slope deformation enhanced by an earthquake? Evidence from shaking table tests |
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was the deep-seated gravitational slope deformation enhanced by an earthquake? evidence from shaking table tests |
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Was the deep-seated gravitational slope deformation enhanced by an earthquake? Evidence from shaking table tests |
| abstract |
Abstract A large-scale landslide occurred in Maoxian County, Sichuan Province, on June 24th, 2017, which destroyed Xinmo village and resulted in injuries and the deaths of 83 people. According to earthquake data, earthquakes greater than Ms 7.0 have occurred many times at this location. The importance of taking earthquake factors into consideration during the study of gravity-induced deformation is emphasized in this study. Careful field investigation reveals that macrocracks developed in the source area before landsliding, and there are many gravity-induced (buckling) deformation traces in the landslide area. After a large shaking table test, the deformation failure characteristics of the slope caused by multiple earthquake simulation actions were compared with the practical consequences caused by the Xinmo Landslide. The tension fracture and buckling failure revealed by the test is highly similar to the real phenomena of the Xinmo Landslide in the field, as discovered by historical images. Therefore, undeniably, earthquakes have made important contributions to the Xinmo Landslide, even though the Xinmo Landslide has apparent gravity-induced deformation properties. Furthermore, the influence of earthquakes, gravity, rainfall, and other external factors on landslides is not just supposition. Inter-feedback actions between them gave rise to the landslide event. © Saudi Society for Geosciences 2022 |
| abstractGer |
Abstract A large-scale landslide occurred in Maoxian County, Sichuan Province, on June 24th, 2017, which destroyed Xinmo village and resulted in injuries and the deaths of 83 people. According to earthquake data, earthquakes greater than Ms 7.0 have occurred many times at this location. The importance of taking earthquake factors into consideration during the study of gravity-induced deformation is emphasized in this study. Careful field investigation reveals that macrocracks developed in the source area before landsliding, and there are many gravity-induced (buckling) deformation traces in the landslide area. After a large shaking table test, the deformation failure characteristics of the slope caused by multiple earthquake simulation actions were compared with the practical consequences caused by the Xinmo Landslide. The tension fracture and buckling failure revealed by the test is highly similar to the real phenomena of the Xinmo Landslide in the field, as discovered by historical images. Therefore, undeniably, earthquakes have made important contributions to the Xinmo Landslide, even though the Xinmo Landslide has apparent gravity-induced deformation properties. Furthermore, the influence of earthquakes, gravity, rainfall, and other external factors on landslides is not just supposition. Inter-feedback actions between them gave rise to the landslide event. © Saudi Society for Geosciences 2022 |
| abstract_unstemmed |
Abstract A large-scale landslide occurred in Maoxian County, Sichuan Province, on June 24th, 2017, which destroyed Xinmo village and resulted in injuries and the deaths of 83 people. According to earthquake data, earthquakes greater than Ms 7.0 have occurred many times at this location. The importance of taking earthquake factors into consideration during the study of gravity-induced deformation is emphasized in this study. Careful field investigation reveals that macrocracks developed in the source area before landsliding, and there are many gravity-induced (buckling) deformation traces in the landslide area. After a large shaking table test, the deformation failure characteristics of the slope caused by multiple earthquake simulation actions were compared with the practical consequences caused by the Xinmo Landslide. The tension fracture and buckling failure revealed by the test is highly similar to the real phenomena of the Xinmo Landslide in the field, as discovered by historical images. Therefore, undeniably, earthquakes have made important contributions to the Xinmo Landslide, even though the Xinmo Landslide has apparent gravity-induced deformation properties. Furthermore, the influence of earthquakes, gravity, rainfall, and other external factors on landslides is not just supposition. Inter-feedback actions between them gave rise to the landslide event. © Saudi Society for Geosciences 2022 |
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Was the deep-seated gravitational slope deformation enhanced by an earthquake? Evidence from shaking table tests |
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https://dx.doi.org/10.1007/s12517-022-10671-9 |
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Cui, Shenghua Pei, Xiangjun Yang, Hailong Luo, Luogaung Yang, Qingwen |
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Cui, Shenghua Pei, Xiangjun Yang, Hailong Luo, Luogaung Yang, Qingwen |
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| doi_str |
10.1007/s12517-022-10671-9 |
| up_date |
2024-07-03T15:34:30.998Z |
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| score |
7.4019346 |