Fracture of granite under various strain conditions
Mechanisms of fracture of granite specimens subjected to loading controlled by the defect formation rate are studied in the experiments on stick-slip initiation and deformation of water-saturated specimens from the acoustic emission measurements. It is found that under mechanical loading of dry spec...
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| Published in: | Izvestiya. Physics of the solid earth Vol. 47; no. 10; pp. 879 - 885 |
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01-10-2011
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| Abstract | Mechanisms of fracture of granite specimens subjected to loading controlled by the defect formation rate are studied in the experiments on stick-slip initiation and deformation of water-saturated specimens from the acoustic emission measurements. It is found that under mechanical loading of dry specimens, the initially dispersed formation of defects is followed by the stage of their localization, and then a fracture nucleates whose development results in the formation of macrofracture and failure of the specimen. In water-saturated specimens, multiple defects are formed randomly throughout the entire volume, which causes intense damage to the material. At the final stage of deformation, several source regions appear in which the main cracks develop. If fracturing follows the stick-slip scenario, the stoppers located on the sides of the fault are destroyed. |
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| AbstractList | Mechanisms of fracture of granite specimens subjected to loading controlled by the defect formation rate are studied in the experiments on stick-slip initiation and deformation of water-saturated specimens from the acoustic emission measurements. It is found that under mechanical loading of dry specimens, the initially dispersed formation of defects is followed by the stage of their localization, and then a fracture nucleates whose development results in the formation of macrofracture and failure of the specimen. In water-saturated specimens, multiple defects are formed randomly throughout the entire volume, which causes intense damage to the material. At the final stage of deformation, several source regions appear in which the main cracks develop. If fracturing follows the stick-slip scenario, the stoppers located on the sides of the fault are destroyed. Mechanisms of fracture of granite specimens subjected to loading controlled by the defect formation rate are studied in the experiments on stick-slip initiation and deformation of water-saturated specimens from the acoustic emission measurements. It is found that under mechanical loading of dry specimens, the initially dispersed formation of defects is followed by the stage of their localization, and then a fracture nucleates whose development results in the formation of macrofracture and failure of the specimen. In water-saturated specimens, multiple defects are formed randomly throughout the entire volume, which causes intense damage to the material. At the final stage of deformation, several source regions appear in which the main cracks develop. If fracturing follows the stick-slip scenario, the stoppers located on the sides of the fault are destroyed.[PUBLICATION ABSTRACT] |
| Author | Damaskinskaya, E. E. Kuksenko, V. S. Kadomtsev, A. G. |
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| Cites_doi | 10.1038/nature06521 10.1126/science.181.4102.803 10.1016/S0074-6142(08)62813-2 10.1007/BF00876492 10.1785/0120020101 |
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| Keywords | Solid Earth Acoustic Emission Acoustic Emis Axial Load Fault Geometry |
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| References_xml | – volume: 264 start-page: 846 issue: 4 year: 1982 ident: 9250_CR4 publication-title: Dokl. Akad. Nauk SSSR contributor: fullname: V.S. Kuksenko – volume: 451 start-page: 561 year: 2008 ident: 9250_CR2 publication-title: Nature doi: 10.1038/nature06521 contributor: fullname: Ch. J. Ammon – volume-title: Tekhnogennye protsessy v zemnoi kore (opasnosti i katastrofy) year: 2005 ident: 9250_CR1 contributor: fullname: V.V. Adushkin – ident: 9250_CR7 – start-page: 38 volume-title: Postroenie modelei razvitiya seismicheskogo protsessa i predvestnikov zemletryasenii year: 1993 ident: 9250_CR11 contributor: fullname: G.A. Sobolev – ident: 9250_CR8 doi: 10.1126/science.181.4102.803 – start-page: 3 volume-title: Fault Mechanics and Transport Properties of Rocks year: 1992 ident: 9250_CR6 doi: 10.1016/S0074-6142(08)62813-2 contributor: fullname: D.A. Lockner – volume-title: Introduction To Seismology year: 1999 ident: 9250_CR9 contributor: fullname: P.M. Shearer – volume: 146 start-page: 253 issue: 2 year: 1996 ident: 9250_CR5 publication-title: Pure Appl. Geophys. doi: 10.1007/BF00876492 contributor: fullname: V. Kuksenko – volume: 36 start-page: 3101 issue: 10 year: 1994 ident: 9250_CR13 publication-title: Fiz. Tverd. Tela contributor: fullname: N.G. Tomilin – volume: 41 start-page: 660 issue: 8 year: 2005 ident: 9250_CR14 publication-title: Izv. Phys. Earth contributor: fullname: N.G. Tomilin – volume-title: Osnovy prognoza zemletryasenii year: 1993 ident: 9250_CR10 contributor: fullname: G.A. Sobolev – volume: 93 start-page: 1803 issue: 4 year: 2003 ident: 9250_CR12 publication-title: Bull. Seismol. Soc. Am. doi: 10.1785/0120020101 contributor: fullname: S.A. Stanchits – volume: 15 start-page: 3260 issue: 11 year: 1973 ident: 9250_CR3 publication-title: Fiz. Tverd. Tela contributor: fullname: V.A. Bershtein |
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| SubjectTerms | Acoustic emission Deformation Earth and Environmental Science Earth Sciences Emission measurements Fractures Geophysics Geophysics/Geodesy Granite Igneous rocks Rock deformation Strain |
| Title | Fracture of granite under various strain conditions |
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