Possible soil thermal response to seismic activities in Alborz region (Iran)

In this investigation, relations between the ground's thermal properties and 70 earthquakes with a magnitude > 4 Richter in the Alborz region during a period of 12 years (1992 to 2004) were studied. Typical changes of ground temperature, 0.4 °C; thermal diffusivity, 0.028 m² s⁻¹ x 10⁻⁶ a...

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Main Authors: Rezapour, N, Fattahi, M, Bidokhti, A
Other Authors: European Geosciences Union
Format: Journal article
Language:English
Published: Copernicus Publications 2010
Subjects:
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author Rezapour, N
Fattahi, M
Bidokhti, A
author2 European Geosciences Union
author_facet European Geosciences Union
Rezapour, N
Fattahi, M
Bidokhti, A
author_sort Rezapour, N
collection OXFORD
description In this investigation, relations between the ground's thermal properties and 70 earthquakes with a magnitude > 4 Richter in the Alborz region during a period of 12 years (1992 to 2004) were studied. Typical changes of ground temperature, 0.4 °C; thermal diffusivity, 0.028 m² s⁻¹ x 10⁻⁶ and ground heat flux take place a few hours prior to the earthquakes. The values of thermal diffusivity depend on the ground moisture content, which may change during seismic activities. The analysis of ground heat flux from the epicentre and it's surrounding regions show some anomalous behavior before the earthquakes but with different signs in the areas close to the sea and far away from the sea.
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spelling oxford-uuid:a02f277c-18c4-4a2e-9b3e-59607ceac7342022-03-27T02:03:41ZPossible soil thermal response to seismic activities in Alborz region (Iran)Journal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:a02f277c-18c4-4a2e-9b3e-59607ceac734Earth sciencesEnvironmentEarthquakes and tectonicsEnglishOxford University Research Archive - ValetCopernicus Publications2010Rezapour, NFattahi, MBidokhti, AEuropean Geosciences UnionIn this investigation, relations between the ground's thermal properties and 70 earthquakes with a magnitude > 4 Richter in the Alborz region during a period of 12 years (1992 to 2004) were studied. Typical changes of ground temperature, 0.4 °C; thermal diffusivity, 0.028 m² s⁻¹ x 10⁻⁶ and ground heat flux take place a few hours prior to the earthquakes. The values of thermal diffusivity depend on the ground moisture content, which may change during seismic activities. The analysis of ground heat flux from the epicentre and it's surrounding regions show some anomalous behavior before the earthquakes but with different signs in the areas close to the sea and far away from the sea.
spellingShingle Earth sciences
Environment
Earthquakes and tectonics
Rezapour, N
Fattahi, M
Bidokhti, A
Possible soil thermal response to seismic activities in Alborz region (Iran)
title Possible soil thermal response to seismic activities in Alborz region (Iran)
title_full Possible soil thermal response to seismic activities in Alborz region (Iran)
title_fullStr Possible soil thermal response to seismic activities in Alborz region (Iran)
title_full_unstemmed Possible soil thermal response to seismic activities in Alborz region (Iran)
title_short Possible soil thermal response to seismic activities in Alborz region (Iran)
title_sort possible soil thermal response to seismic activities in alborz region iran
topic Earth sciences
Environment
Earthquakes and tectonics
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AT fattahim possiblesoilthermalresponsetoseismicactivitiesinalborzregioniran
AT bidokhtia possiblesoilthermalresponsetoseismicactivitiesinalborzregioniran