Premonitory mechanism and resistivity variations related to earthquake
Abstract The phenomenological theory of premonitory sequence prior to an earthquake is considered. Formation of stresses related to cracks and the law governing fracture propagation lead to the evolution equation of internal stresses. A consistent description involves redistribution of the internal...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Teisseyre, Roman [verfasserIn] |
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| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1983 |
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| Anmerkung: |
© Birkhäuser Verlag 1983 |
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| Übergeordnetes Werk: |
Enthalten in: Pure and applied geophysics - Birkhäuser-Verlag, 1964, 121(1983), 2 vom: Apr., Seite 297-315 |
|---|---|
| Übergeordnetes Werk: |
volume:121 ; year:1983 ; number:2 ; month:04 ; pages:297-315 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF02590140 |
|---|
| Katalog-ID: |
OLC2069464334 |
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| 520 | |a Abstract The phenomenological theory of premonitory sequence prior to an earthquake is considered. Formation of stresses related to cracks and the law governing fracture propagation lead to the evolution equation of internal stresses. A consistent description involves redistribution of the internal stresses with concentration effect before an earthquake and diffusion-like outflow after it. Formation of cracks and penetration of pore fluid cause changes in the mechanical, electrical, and other properties of rocks. Variations in the electrical resistivity of rocks are related to the fracturing processes with interaction of an interstitial fluid. Changes in rock resistivity are described here by a new parameter called a connection factor; it depends on crack density, and especially on its threshold value related to the percolation process. The influence of percolation on rock resistivity is here related to a formal analytical theory given byKirkpatrick (1973). The author also refers to results of the time-continuous rock resistivity measurements carried out in mines in Poland. Some examples indicate a role of rock resistivity observations in situ as a precursory parameter related to rockbursts. The paper also deals with some secondary effects, like those related to a frequence response and to influence of electrokinetic potentials on an effective rock resistivity. | ||
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10.1007/BF02590140 doi (DE-627)OLC2069464334 (DE-He213)BF02590140-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Teisseyre, Roman verfasserin aut Premonitory mechanism and resistivity variations related to earthquake 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag 1983 Abstract The phenomenological theory of premonitory sequence prior to an earthquake is considered. Formation of stresses related to cracks and the law governing fracture propagation lead to the evolution equation of internal stresses. A consistent description involves redistribution of the internal stresses with concentration effect before an earthquake and diffusion-like outflow after it. Formation of cracks and penetration of pore fluid cause changes in the mechanical, electrical, and other properties of rocks. Variations in the electrical resistivity of rocks are related to the fracturing processes with interaction of an interstitial fluid. Changes in rock resistivity are described here by a new parameter called a connection factor; it depends on crack density, and especially on its threshold value related to the percolation process. The influence of percolation on rock resistivity is here related to a formal analytical theory given byKirkpatrick (1973). The author also refers to results of the time-continuous rock resistivity measurements carried out in mines in Poland. Some examples indicate a role of rock resistivity observations in situ as a precursory parameter related to rockbursts. The paper also deals with some secondary effects, like those related to a frequence response and to influence of electrokinetic potentials on an effective rock resistivity. Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 121(1983), 2 vom: Apr., Seite 297-315 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:121 year:1983 number:2 month:04 pages:297-315 https://doi.org/10.1007/BF02590140 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2008 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4323 AR 121 1983 2 04 297-315 |
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10.1007/BF02590140 doi (DE-627)OLC2069464334 (DE-He213)BF02590140-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Teisseyre, Roman verfasserin aut Premonitory mechanism and resistivity variations related to earthquake 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag 1983 Abstract The phenomenological theory of premonitory sequence prior to an earthquake is considered. Formation of stresses related to cracks and the law governing fracture propagation lead to the evolution equation of internal stresses. A consistent description involves redistribution of the internal stresses with concentration effect before an earthquake and diffusion-like outflow after it. Formation of cracks and penetration of pore fluid cause changes in the mechanical, electrical, and other properties of rocks. Variations in the electrical resistivity of rocks are related to the fracturing processes with interaction of an interstitial fluid. Changes in rock resistivity are described here by a new parameter called a connection factor; it depends on crack density, and especially on its threshold value related to the percolation process. The influence of percolation on rock resistivity is here related to a formal analytical theory given byKirkpatrick (1973). The author also refers to results of the time-continuous rock resistivity measurements carried out in mines in Poland. Some examples indicate a role of rock resistivity observations in situ as a precursory parameter related to rockbursts. The paper also deals with some secondary effects, like those related to a frequence response and to influence of electrokinetic potentials on an effective rock resistivity. Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 121(1983), 2 vom: Apr., Seite 297-315 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:121 year:1983 number:2 month:04 pages:297-315 https://doi.org/10.1007/BF02590140 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2008 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4323 AR 121 1983 2 04 297-315 |
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10.1007/BF02590140 doi (DE-627)OLC2069464334 (DE-He213)BF02590140-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Teisseyre, Roman verfasserin aut Premonitory mechanism and resistivity variations related to earthquake 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag 1983 Abstract The phenomenological theory of premonitory sequence prior to an earthquake is considered. Formation of stresses related to cracks and the law governing fracture propagation lead to the evolution equation of internal stresses. A consistent description involves redistribution of the internal stresses with concentration effect before an earthquake and diffusion-like outflow after it. Formation of cracks and penetration of pore fluid cause changes in the mechanical, electrical, and other properties of rocks. Variations in the electrical resistivity of rocks are related to the fracturing processes with interaction of an interstitial fluid. Changes in rock resistivity are described here by a new parameter called a connection factor; it depends on crack density, and especially on its threshold value related to the percolation process. The influence of percolation on rock resistivity is here related to a formal analytical theory given byKirkpatrick (1973). The author also refers to results of the time-continuous rock resistivity measurements carried out in mines in Poland. Some examples indicate a role of rock resistivity observations in situ as a precursory parameter related to rockbursts. The paper also deals with some secondary effects, like those related to a frequence response and to influence of electrokinetic potentials on an effective rock resistivity. Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 121(1983), 2 vom: Apr., Seite 297-315 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:121 year:1983 number:2 month:04 pages:297-315 https://doi.org/10.1007/BF02590140 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2008 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4323 AR 121 1983 2 04 297-315 |
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10.1007/BF02590140 doi (DE-627)OLC2069464334 (DE-He213)BF02590140-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Teisseyre, Roman verfasserin aut Premonitory mechanism and resistivity variations related to earthquake 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag 1983 Abstract The phenomenological theory of premonitory sequence prior to an earthquake is considered. Formation of stresses related to cracks and the law governing fracture propagation lead to the evolution equation of internal stresses. A consistent description involves redistribution of the internal stresses with concentration effect before an earthquake and diffusion-like outflow after it. Formation of cracks and penetration of pore fluid cause changes in the mechanical, electrical, and other properties of rocks. Variations in the electrical resistivity of rocks are related to the fracturing processes with interaction of an interstitial fluid. Changes in rock resistivity are described here by a new parameter called a connection factor; it depends on crack density, and especially on its threshold value related to the percolation process. The influence of percolation on rock resistivity is here related to a formal analytical theory given byKirkpatrick (1973). The author also refers to results of the time-continuous rock resistivity measurements carried out in mines in Poland. Some examples indicate a role of rock resistivity observations in situ as a precursory parameter related to rockbursts. The paper also deals with some secondary effects, like those related to a frequence response and to influence of electrokinetic potentials on an effective rock resistivity. Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 121(1983), 2 vom: Apr., Seite 297-315 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:121 year:1983 number:2 month:04 pages:297-315 https://doi.org/10.1007/BF02590140 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2008 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4323 AR 121 1983 2 04 297-315 |
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10.1007/BF02590140 doi (DE-627)OLC2069464334 (DE-He213)BF02590140-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Teisseyre, Roman verfasserin aut Premonitory mechanism and resistivity variations related to earthquake 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag 1983 Abstract The phenomenological theory of premonitory sequence prior to an earthquake is considered. Formation of stresses related to cracks and the law governing fracture propagation lead to the evolution equation of internal stresses. A consistent description involves redistribution of the internal stresses with concentration effect before an earthquake and diffusion-like outflow after it. Formation of cracks and penetration of pore fluid cause changes in the mechanical, electrical, and other properties of rocks. Variations in the electrical resistivity of rocks are related to the fracturing processes with interaction of an interstitial fluid. Changes in rock resistivity are described here by a new parameter called a connection factor; it depends on crack density, and especially on its threshold value related to the percolation process. The influence of percolation on rock resistivity is here related to a formal analytical theory given byKirkpatrick (1973). The author also refers to results of the time-continuous rock resistivity measurements carried out in mines in Poland. Some examples indicate a role of rock resistivity observations in situ as a precursory parameter related to rockbursts. The paper also deals with some secondary effects, like those related to a frequence response and to influence of electrokinetic potentials on an effective rock resistivity. Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 121(1983), 2 vom: Apr., Seite 297-315 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:121 year:1983 number:2 month:04 pages:297-315 https://doi.org/10.1007/BF02590140 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2008 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4323 AR 121 1983 2 04 297-315 |
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550 VZ 16,13 ssgn Premonitory mechanism and resistivity variations related to earthquake |
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Premonitory mechanism and resistivity variations related to earthquake |
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Premonitory mechanism and resistivity variations related to earthquake |
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Teisseyre, Roman |
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premonitory mechanism and resistivity variations related to earthquake |
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Premonitory mechanism and resistivity variations related to earthquake |
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Abstract The phenomenological theory of premonitory sequence prior to an earthquake is considered. Formation of stresses related to cracks and the law governing fracture propagation lead to the evolution equation of internal stresses. A consistent description involves redistribution of the internal stresses with concentration effect before an earthquake and diffusion-like outflow after it. Formation of cracks and penetration of pore fluid cause changes in the mechanical, electrical, and other properties of rocks. Variations in the electrical resistivity of rocks are related to the fracturing processes with interaction of an interstitial fluid. Changes in rock resistivity are described here by a new parameter called a connection factor; it depends on crack density, and especially on its threshold value related to the percolation process. The influence of percolation on rock resistivity is here related to a formal analytical theory given byKirkpatrick (1973). The author also refers to results of the time-continuous rock resistivity measurements carried out in mines in Poland. Some examples indicate a role of rock resistivity observations in situ as a precursory parameter related to rockbursts. The paper also deals with some secondary effects, like those related to a frequence response and to influence of electrokinetic potentials on an effective rock resistivity. © Birkhäuser Verlag 1983 |
| abstractGer |
Abstract The phenomenological theory of premonitory sequence prior to an earthquake is considered. Formation of stresses related to cracks and the law governing fracture propagation lead to the evolution equation of internal stresses. A consistent description involves redistribution of the internal stresses with concentration effect before an earthquake and diffusion-like outflow after it. Formation of cracks and penetration of pore fluid cause changes in the mechanical, electrical, and other properties of rocks. Variations in the electrical resistivity of rocks are related to the fracturing processes with interaction of an interstitial fluid. Changes in rock resistivity are described here by a new parameter called a connection factor; it depends on crack density, and especially on its threshold value related to the percolation process. The influence of percolation on rock resistivity is here related to a formal analytical theory given byKirkpatrick (1973). The author also refers to results of the time-continuous rock resistivity measurements carried out in mines in Poland. Some examples indicate a role of rock resistivity observations in situ as a precursory parameter related to rockbursts. The paper also deals with some secondary effects, like those related to a frequence response and to influence of electrokinetic potentials on an effective rock resistivity. © Birkhäuser Verlag 1983 |
| abstract_unstemmed |
Abstract The phenomenological theory of premonitory sequence prior to an earthquake is considered. Formation of stresses related to cracks and the law governing fracture propagation lead to the evolution equation of internal stresses. A consistent description involves redistribution of the internal stresses with concentration effect before an earthquake and diffusion-like outflow after it. Formation of cracks and penetration of pore fluid cause changes in the mechanical, electrical, and other properties of rocks. Variations in the electrical resistivity of rocks are related to the fracturing processes with interaction of an interstitial fluid. Changes in rock resistivity are described here by a new parameter called a connection factor; it depends on crack density, and especially on its threshold value related to the percolation process. The influence of percolation on rock resistivity is here related to a formal analytical theory given byKirkpatrick (1973). The author also refers to results of the time-continuous rock resistivity measurements carried out in mines in Poland. Some examples indicate a role of rock resistivity observations in situ as a precursory parameter related to rockbursts. The paper also deals with some secondary effects, like those related to a frequence response and to influence of electrokinetic potentials on an effective rock resistivity. © Birkhäuser Verlag 1983 |
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