The nexus of soil radon and hydrogen dynamics and seismicity of the northern flank of the Kuril-Kamchatka subduction zone
The comparison of kinematics and dynamic parameters of radon and molecular hydrogen concentration in subsoil air on the stations network at the Petropavlovsk-Kamchatsky geodynamic proving ground with seismicity of the northern flank of the Kuril-Kamchatka subduction zone was fulfilled in the period...
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Language: | English |
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2007
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Online Access: | http://hdl.handle.net/2122/3868 |
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ftingv:oai:www.earth-prints.org:2122/3868 |
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openpolar |
institution |
Open Polar |
collection |
Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
op_collection_id |
ftingv |
language |
English |
topic |
radon hydrogen seismicity geodeformation wave earthquake 04. Solid Earth::04.06. Seismology::04.06.06. Surveys measurements and monitoring |
spellingShingle |
radon hydrogen seismicity geodeformation wave earthquake 04. Solid Earth::04.06. Seismology::04.06.06. Surveys measurements and monitoring Firstov, P. P. Yakovleva, V. S. Shirokov, V. A. Malysheva, O. P. The nexus of soil radon and hydrogen dynamics and seismicity of the northern flank of the Kuril-Kamchatka subduction zone |
topic_facet |
radon hydrogen seismicity geodeformation wave earthquake 04. Solid Earth::04.06. Seismology::04.06.06. Surveys measurements and monitoring |
description |
The comparison of kinematics and dynamic parameters of radon and molecular hydrogen concentration in subsoil air on the stations network at the Petropavlovsk-Kamchatsky geodynamic proving ground with seismicity of the northern flank of the Kuril-Kamchatka subduction zone was fulfilled in the period from July till August 2004. On the basis of correlation analysis of the regional seismicity and variations of radon flux density calculated using the data of gas-discharge counters of STS-6 type and SSNTDs it was shown that the radon mass transfer abnormal variations are conditioned by both regional seismicity in total and the subduction zone of proving ground. The azimuths of «geodeformation waves» coming to the registration points are calculated during clearly expressed anomaly beginnings, which coincide with directions to earthquake epicenters taking place at the same time. The geochemical anomalies recorded are presumptively deformative by nature and can be conditioned by processes of «quasi-viscous» flow of the lithosphere during rearrangement of tectonic stress fields of the subduction zone. The short-term (predicted time Τ <14 days) precursor of the earthquakes swarm was revealed in hydrogen dynamics on August, 4-5 (four earthquakes had M≥5.3 and epicentral distance about 130 km from the Paratunka base station). JCR Journal open |
author2 |
Firstov, P. P.; Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia Yakovleva, V. S.; Tomsk Polytechnic University, Tomsk, Russia Shirokov, V. A.; Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia Malysheva, O. P.; Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia Tomsk Polytechnic University, Tomsk, Russia |
format |
Article in Journal/Newspaper |
author |
Firstov, P. P. Yakovleva, V. S. Shirokov, V. A. Malysheva, O. P. |
author_facet |
Firstov, P. P. Yakovleva, V. S. Shirokov, V. A. Malysheva, O. P. |
author_sort |
Firstov, P. P. |
title |
The nexus of soil radon and hydrogen dynamics and seismicity of the northern flank of the Kuril-Kamchatka subduction zone |
title_short |
The nexus of soil radon and hydrogen dynamics and seismicity of the northern flank of the Kuril-Kamchatka subduction zone |
title_full |
The nexus of soil radon and hydrogen dynamics and seismicity of the northern flank of the Kuril-Kamchatka subduction zone |
title_fullStr |
The nexus of soil radon and hydrogen dynamics and seismicity of the northern flank of the Kuril-Kamchatka subduction zone |
title_full_unstemmed |
The nexus of soil radon and hydrogen dynamics and seismicity of the northern flank of the Kuril-Kamchatka subduction zone |
title_sort |
nexus of soil radon and hydrogen dynamics and seismicity of the northern flank of the kuril-kamchatka subduction zone |
publishDate |
2007 |
url |
http://hdl.handle.net/2122/3868 |
long_lat |
ENVELOPE(158.626,158.626,53.067,53.067) ENVELOPE(158.651,158.651,53.044,53.044) ENVELOPE(158.257,158.257,52.962,52.962) |
geographic |
Petropavlovsk Petropavlovsk-Kamchatsky Paratunka |
geographic_facet |
Petropavlovsk Petropavlovsk-Kamchatsky Paratunka |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_relation |
Annals of Geophysics 4/50 (2007) DUBINCHUK, V.T. (1991): Radon as a precursor of earthquakes, in Isotopic Geochemical Precursors of Earthquakes and Volcanic Eruption, Vienna, 37-42. FIRSTOV, P.P. (1999): Monitoring of subsoil radon volumetric activity on Paratunka geothermal system in 1997 - 1998 with the purpose to search for the precursors of strong earthquakes of Kamchatka, Volcanol. Seismol., 6, 1-11 (in Russian). FIRSTOV, P.P. and V.P. RUDAKOV (2003): Results of subsoil radon registration in 1997-2000 on the Petropavlovsk - Kamchatsky geodynamic polygon, Volcanol. Seismol., 1, 26-41 (in Russian). KIM, I.S., A. AHHLEBY and G.H. SIGEL JR. (1997): Observation of the trapping of radioactive inert gas radon on oxide glass surfaces: macroporous scintillating-glassfiber bundle alpha detector, Nucl. Instrum. Methods Phys. Res., A390, 419-422. KING, C.-Y. (1991): Gas-geochemical approaches to earthquake prediction, in Isotopic Geochemical Precursors of Earthquakes and Volcanic Eruption, Vienna, 22-36. LJUBUSHIN, A.A. JR. (1993): The multivariate analysis of time series of systems of geophysical monitoring, Phys. Earth, 1, 103-108 (in Russian). LJUBUSHIN, A.A. JR. (1998): The aggregated signal of systems of low-frequency geophysical monitoring, Izvestiya (Physics of the Solid Earth), 1, 69-74 (in Russian). MORGUNOV, V.A. (2001): The creep of the rocks at a finishing stage of preparation of earthquakes, Izvestiya (Physics of the Solid Earth), 4, 3-11 (in Russian). NIKOLAEV, V.A. and R. ILIÇ (1999): Etched track radiometers in radon measurements: a review, Radiat. Meas., 30, 1-13. NIKOLAEV, V.A., M.G. BUZYNNIY, I.B.VOROBYEV, A.V. GROMOV, A.S. KRIVOKHATSKIY, I.P. LOS, A.V. ZELENSKIY and YU.A. TOMILIN (1993): Application of the track method for radon measurements in Ukraine, Nucl. Tracks Radiat. Meas., 21 (3), 433-436. NOVIKOV, G.F. (1989): The Radiometric Exploration, Lenin grad, pp. 406 (in Russian). RIZNICHENKO, YU.V. (1977): Calculation of speed of deformations at seismic current of mountain weights, Izvestiya (Physics of the Solid Earth), 54-65 (in Russian). RUDAKOV, V.P. (2003): The seismoemanation effects of geological structures, in Problems of Geophysics of XXI Century. The Book 2 (Znanije Publ., Moscow), 95-113 (in Russian). SEREZHNIKOV, A.I. and V.M. ZIMIN (1976): Geological structure of Paratunka geothermal area, influence of separate geological factors on modern geothermal activity, in Hydrothermal Systems and Thermal Fields on Kamchatka, Vladivostok, 115-142 (in Russian). STEINITZ, G., U. VULKAN and B. LANG (1999): Radon flux at the northwestern segment of the Dead Sea (Dead Sea rift) and its relation to earthquakes, Isr. J. Earth Sci., 48, 283-299. STEINITZ, G., Z.B. BEGIN and N. GAZIT-YAARI (2003): Statistically significant relation between radon flux and weak earthquakes in the Dead Sea rift valley, Geology, 6, 505-508. UTKIN, V.I. (2000): Radon and problem of tectonic earthquakes, SOZh, 6 (12), 64-70 (in Russian). YAKOVLEVA, V.S. (2005): A theoretical method for estimating the characteristics of radon transport in homogeneous soil, Ann. Geophysics, 48 (1), 195-198. http://hdl.handle.net/2122/3868 |
op_rights |
open |
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1766051119543353344 |
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ftingv:oai:www.earth-prints.org:2122/3868 2023-05-15T16:58:59+02:00 The nexus of soil radon and hydrogen dynamics and seismicity of the northern flank of the Kuril-Kamchatka subduction zone Firstov, P. P. Yakovleva, V. S. Shirokov, V. A. Malysheva, O. P. Firstov, P. P.; Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia Yakovleva, V. S.; Tomsk Polytechnic University, Tomsk, Russia Shirokov, V. A.; Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia Malysheva, O. P.; Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia Tomsk Polytechnic University, Tomsk, Russia 2007-08 http://hdl.handle.net/2122/3868 en eng Annals of Geophysics 4/50 (2007) DUBINCHUK, V.T. (1991): Radon as a precursor of earthquakes, in Isotopic Geochemical Precursors of Earthquakes and Volcanic Eruption, Vienna, 37-42. FIRSTOV, P.P. (1999): Monitoring of subsoil radon volumetric activity on Paratunka geothermal system in 1997 - 1998 with the purpose to search for the precursors of strong earthquakes of Kamchatka, Volcanol. Seismol., 6, 1-11 (in Russian). FIRSTOV, P.P. and V.P. RUDAKOV (2003): Results of subsoil radon registration in 1997-2000 on the Petropavlovsk - Kamchatsky geodynamic polygon, Volcanol. Seismol., 1, 26-41 (in Russian). KIM, I.S., A. AHHLEBY and G.H. SIGEL JR. (1997): Observation of the trapping of radioactive inert gas radon on oxide glass surfaces: macroporous scintillating-glassfiber bundle alpha detector, Nucl. Instrum. Methods Phys. Res., A390, 419-422. KING, C.-Y. (1991): Gas-geochemical approaches to earthquake prediction, in Isotopic Geochemical Precursors of Earthquakes and Volcanic Eruption, Vienna, 22-36. LJUBUSHIN, A.A. JR. (1993): The multivariate analysis of time series of systems of geophysical monitoring, Phys. Earth, 1, 103-108 (in Russian). LJUBUSHIN, A.A. JR. (1998): The aggregated signal of systems of low-frequency geophysical monitoring, Izvestiya (Physics of the Solid Earth), 1, 69-74 (in Russian). MORGUNOV, V.A. (2001): The creep of the rocks at a finishing stage of preparation of earthquakes, Izvestiya (Physics of the Solid Earth), 4, 3-11 (in Russian). NIKOLAEV, V.A. and R. ILIÇ (1999): Etched track radiometers in radon measurements: a review, Radiat. Meas., 30, 1-13. NIKOLAEV, V.A., M.G. BUZYNNIY, I.B.VOROBYEV, A.V. GROMOV, A.S. KRIVOKHATSKIY, I.P. LOS, A.V. ZELENSKIY and YU.A. TOMILIN (1993): Application of the track method for radon measurements in Ukraine, Nucl. Tracks Radiat. Meas., 21 (3), 433-436. NOVIKOV, G.F. (1989): The Radiometric Exploration, Lenin grad, pp. 406 (in Russian). RIZNICHENKO, YU.V. (1977): Calculation of speed of deformations at seismic current of mountain weights, Izvestiya (Physics of the Solid Earth), 54-65 (in Russian). RUDAKOV, V.P. (2003): The seismoemanation effects of geological structures, in Problems of Geophysics of XXI Century. The Book 2 (Znanije Publ., Moscow), 95-113 (in Russian). SEREZHNIKOV, A.I. and V.M. ZIMIN (1976): Geological structure of Paratunka geothermal area, influence of separate geological factors on modern geothermal activity, in Hydrothermal Systems and Thermal Fields on Kamchatka, Vladivostok, 115-142 (in Russian). STEINITZ, G., U. VULKAN and B. LANG (1999): Radon flux at the northwestern segment of the Dead Sea (Dead Sea rift) and its relation to earthquakes, Isr. J. Earth Sci., 48, 283-299. STEINITZ, G., Z.B. BEGIN and N. GAZIT-YAARI (2003): Statistically significant relation between radon flux and weak earthquakes in the Dead Sea rift valley, Geology, 6, 505-508. UTKIN, V.I. (2000): Radon and problem of tectonic earthquakes, SOZh, 6 (12), 64-70 (in Russian). YAKOVLEVA, V.S. (2005): A theoretical method for estimating the characteristics of radon transport in homogeneous soil, Ann. Geophysics, 48 (1), 195-198. http://hdl.handle.net/2122/3868 open radon hydrogen seismicity geodeformation wave earthquake 04. Solid Earth::04.06. Seismology::04.06.06. Surveys measurements and monitoring article 2007 ftingv 2022-07-29T06:04:53Z The comparison of kinematics and dynamic parameters of radon and molecular hydrogen concentration in subsoil air on the stations network at the Petropavlovsk-Kamchatsky geodynamic proving ground with seismicity of the northern flank of the Kuril-Kamchatka subduction zone was fulfilled in the period from July till August 2004. On the basis of correlation analysis of the regional seismicity and variations of radon flux density calculated using the data of gas-discharge counters of STS-6 type and SSNTDs it was shown that the radon mass transfer abnormal variations are conditioned by both regional seismicity in total and the subduction zone of proving ground. The azimuths of «geodeformation waves» coming to the registration points are calculated during clearly expressed anomaly beginnings, which coincide with directions to earthquake epicenters taking place at the same time. The geochemical anomalies recorded are presumptively deformative by nature and can be conditioned by processes of «quasi-viscous» flow of the lithosphere during rearrangement of tectonic stress fields of the subduction zone. The short-term (predicted time Τ <14 days) precursor of the earthquakes swarm was revealed in hydrogen dynamics on August, 4-5 (four earthquakes had M≥5.3 and epicentral distance about 130 km from the Paratunka base station). JCR Journal open Article in Journal/Newspaper Kamchatka Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Petropavlovsk ENVELOPE(158.626,158.626,53.067,53.067) Petropavlovsk-Kamchatsky ENVELOPE(158.651,158.651,53.044,53.044) Paratunka ENVELOPE(158.257,158.257,52.962,52.962) |