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Record #114317:

Heat conduction analysis around cooled underground opening using the finite divided element method / Yi Jiu Yao, S. Kadota, S. Koga, M. Kamata.

Title: Heat conduction analysis around cooled underground opening using the finite divided element method / Yi Jiu Yao, S. Kadota, S. Koga, M. Kamata.
Author(s): Yao, Yi Jiu.
Kadota, S.
Koga, S.
Kamata, M.
Date: 1991.
Publisher: Rotterdam: A.A. Balkema
In: Ground Freezing 91. Proceedings of the Sixth International Symposium on Ground Freezing, Beijing, 10-12 September 1991. Vol. 1. (1991.),
Abstract: This method has been commonly used to analyze temperature distribution around cooled underground opening excavated in homogeneous rock mass. Explains principle of method for one- and two-dimensional problems related to non-homogeneous material as well as to latent heat of soil or rock. Results compared well with theoretical results. However, results for thermal conductivity and thermal diffusivity of granite in temperature range from --160 to 40°C showed tendency to become smaller.
Notes:

In: Ground Freezing 91. Proceedings of the Sixth International Symposium on Ground Freezing, Beijing, 10-12 September 1991. Vol. 1 / Xiang Yu, Changsheng Wang, eds.

Keywords: 624.139 -- Engineering in frozen ground.
624.139.62 -- Permafrost control.
551.34 -- Geocryology. Frozen ground.
551.345 -- Permafrost. Cryopedology.
536 -- Heat.
519.673 -- Modelling.
E12 -- Glaciology: frozen ground / snow and ice engineering.
SPRI record no.: 114317

MARCXML

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245 00 ‡aHeat conduction analysis around cooled underground opening using the finite divided element method /‡cYi Jiu Yao, S. Kadota, S. Koga, M. Kamata.
260 ## ‡aRotterdam :‡bA.A. Balkema,‡c1991.
300 ## ‡ap. 99-104 :‡bdiags., tables.
500 ## ‡aIn: Ground Freezing 91. Proceedings of the Sixth International Symposium on Ground Freezing, Beijing, 10-12 September 1991. Vol. 1 / Xiang Yu, Changsheng Wang, eds.
520 3# ‡aThis method has been commonly used to analyze temperature distribution around cooled underground opening excavated in homogeneous rock mass. Explains principle of method for one- and two-dimensional problems related to non-homogeneous material as well as to latent heat of soil or rock. Results compared well with theoretical results. However, results for thermal conductivity and thermal diffusivity of granite in temperature range from --160 to 40°C showed tendency to become smaller.
650 07 ‡a624.139 -- Engineering in frozen ground.‡2udc
650 07 ‡a624.139.62 -- Permafrost control.‡2udc
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc
650 07 ‡a536 -- Heat.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE12 -- Glaciology: frozen ground / snow and ice engineering.‡2local
700 1# ‡aYao, Yi Jiu.
700 1# ‡aKadota, S.
700 1# ‡aKoga, S.
700 1# ‡aKamata, M.
773 0# ‡7nnam ‡aXiang Yu, Changsheng Wang, eds. ‡tGround Freezing 91. Proceedings of the Sixth International Symposium on Ground Freezing, Beijing, 10-12 September 1991. Vol. 1. ‡dRotterdam : A.A. Balkema, 1991. ‡wSPRI-114301
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240419