The Coupling of the Numerical Heat Transfer Model of the Pauzhetka Hydrothermal System (Kamchatka, USSR) with Hydroisotopic Data
The application of the two-dimensional numerical heat-transfer model to the Pauzhetka hydrothermal system allowed us to establish that: (1) a shallow magma body with the anomalous temperature of 700-1000 C and with a volume of 20-30 km{sup 3} may be a heat source for the formation of the Pauzhetka h...
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Institute of Volcanology, Petropavlovsk-Kamchatsky, 6830006, USSR
1986
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ftunivnotexas:info:ark/67531/metadc875187 2023-05-15T16:58:49+02:00 The Coupling of the Numerical Heat Transfer Model of the Pauzhetka Hydrothermal System (Kamchatka, USSR) with Hydroisotopic Data Kiryukhin, A.V. Sugrobov, V.M. United States. Department of Energy. 1986-01-21 175-181 Text http://digital.library.unt.edu/ark:/67531/metadc875187/ English eng Institute of Volcanology, Petropavlovsk-Kamchatsky, 6830006, USSR rep-no: SGP-TR-93-25 grantno: AS03-80SF11459 grantno: AS07-84ID12529 osti: 887138 http://digital.library.unt.edu/ark:/67531/metadc875187/ ark: ark:/67531/metadc875187 Proceedings, Eleventh Workshop Geothermal Reservoir Engineering, Stanford University, Stanford, California, January 21-23, 1986 Heat Transfer 02 Petroleum Testing Ground Water Feeding Rivers Magma Heat Sources Reservoir Engineering 15 Geothermal Energy Hydrothermal Systems Water Geothermal Legacy Kamchatka Geothermal Legacy Article 1986 ftunivnotexas 2016-12-10T23:07:00Z The application of the two-dimensional numerical heat-transfer model to the Pauzhetka hydrothermal system allowed us to establish that: (1) a shallow magma body with the anomalous temperature of 700-1000 C and with a volume of 20-30 km{sup 3} may be a heat source for the formation of the Pauzhetka hydrothermal system. (2) The water feeding source of the Pauzhetka hydrothermal system may be meteoric waters which are infiltrated at an average rate of 5-10 kg/s {center_dot} km{sup 2}. The coupling of the numerical heat-transfer model with hydroisotopic data (D,T,{sup 18}O) obtained from the results of testing of exploitation wells, rivers and springs is the basis to understand more clearly the position of recharge areas and the structure of water flows in the hydrothermal system. Article in Journal/Newspaper Kamchatka University of North Texas: UNT Digital Library Pauzhetka ENVELOPE(156.807,156.807,51.463,51.463) |
institution |
Open Polar |
collection |
University of North Texas: UNT Digital Library |
op_collection_id |
ftunivnotexas |
language |
English |
topic |
Heat Transfer 02 Petroleum Testing Ground Water Feeding Rivers Magma Heat Sources Reservoir Engineering 15 Geothermal Energy Hydrothermal Systems Water Geothermal Legacy Kamchatka Geothermal Legacy |
spellingShingle |
Heat Transfer 02 Petroleum Testing Ground Water Feeding Rivers Magma Heat Sources Reservoir Engineering 15 Geothermal Energy Hydrothermal Systems Water Geothermal Legacy Kamchatka Geothermal Legacy Kiryukhin, A.V. Sugrobov, V.M. The Coupling of the Numerical Heat Transfer Model of the Pauzhetka Hydrothermal System (Kamchatka, USSR) with Hydroisotopic Data |
topic_facet |
Heat Transfer 02 Petroleum Testing Ground Water Feeding Rivers Magma Heat Sources Reservoir Engineering 15 Geothermal Energy Hydrothermal Systems Water Geothermal Legacy Kamchatka Geothermal Legacy |
description |
The application of the two-dimensional numerical heat-transfer model to the Pauzhetka hydrothermal system allowed us to establish that: (1) a shallow magma body with the anomalous temperature of 700-1000 C and with a volume of 20-30 km{sup 3} may be a heat source for the formation of the Pauzhetka hydrothermal system. (2) The water feeding source of the Pauzhetka hydrothermal system may be meteoric waters which are infiltrated at an average rate of 5-10 kg/s {center_dot} km{sup 2}. The coupling of the numerical heat-transfer model with hydroisotopic data (D,T,{sup 18}O) obtained from the results of testing of exploitation wells, rivers and springs is the basis to understand more clearly the position of recharge areas and the structure of water flows in the hydrothermal system. |
author2 |
United States. Department of Energy. |
format |
Article in Journal/Newspaper |
author |
Kiryukhin, A.V. Sugrobov, V.M. |
author_facet |
Kiryukhin, A.V. Sugrobov, V.M. |
author_sort |
Kiryukhin, A.V. |
title |
The Coupling of the Numerical Heat Transfer Model of the Pauzhetka Hydrothermal System (Kamchatka, USSR) with Hydroisotopic Data |
title_short |
The Coupling of the Numerical Heat Transfer Model of the Pauzhetka Hydrothermal System (Kamchatka, USSR) with Hydroisotopic Data |
title_full |
The Coupling of the Numerical Heat Transfer Model of the Pauzhetka Hydrothermal System (Kamchatka, USSR) with Hydroisotopic Data |
title_fullStr |
The Coupling of the Numerical Heat Transfer Model of the Pauzhetka Hydrothermal System (Kamchatka, USSR) with Hydroisotopic Data |
title_full_unstemmed |
The Coupling of the Numerical Heat Transfer Model of the Pauzhetka Hydrothermal System (Kamchatka, USSR) with Hydroisotopic Data |
title_sort |
coupling of the numerical heat transfer model of the pauzhetka hydrothermal system (kamchatka, ussr) with hydroisotopic data |
publisher |
Institute of Volcanology, Petropavlovsk-Kamchatsky, 6830006, USSR |
publishDate |
1986 |
url |
http://digital.library.unt.edu/ark:/67531/metadc875187/ |
long_lat |
ENVELOPE(156.807,156.807,51.463,51.463) |
geographic |
Pauzhetka |
geographic_facet |
Pauzhetka |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_source |
Proceedings, Eleventh Workshop Geothermal Reservoir Engineering, Stanford University, Stanford, California, January 21-23, 1986 |
op_relation |
rep-no: SGP-TR-93-25 grantno: AS03-80SF11459 grantno: AS07-84ID12529 osti: 887138 http://digital.library.unt.edu/ark:/67531/metadc875187/ ark: ark:/67531/metadc875187 |
_version_ |
1766050927248146432 |