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Record #125506:

Seasonal changeability of physicochemical properties of permafrost active layer waters in the Recherche Fiord region (western Spitsbergen) / Stefan A. Bartoszewski, Zdzislaw Michalczyk, Jan Magierski.

Title: Seasonal changeability of physicochemical properties of permafrost active layer waters in the Recherche Fiord region (western Spitsbergen) / Stefan A. Bartoszewski, Zdzislaw Michalczyk, Jan Magierski.
Author(s): Bartoszewski, Stefan A.
Michalczyk, Zdzislaw.
Magierski, Jan.
Date: 1993.
Publisher: Wushan, Guangzhou: South China University of Technology Press
In: Permafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China. (1993.),
Abstract: Investigations on southern shore of Bellsund, 1986-90. Retention of active layer is small because saturation layer is thin. Air temperature affects hydrological and hydrochemical processes. All waters in study area are characterized by low mineralization, weak alkaline reaction, and low temperature.
Notes:

In: Permafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China / International Conference on Permafrost.

Keywords: 551.34 -- Geocryology. Frozen ground.
551.345.3 -- Permafrost, composition and structure. Ice wedges.
556 -- Hydrology.
556.114 -- Water, chemical properties.
551.345 -- Permafrost. Cryopedology.
54 -- Chemistry.
E8 -- Glaciology: frost action and permafrost.
(*32) -- Svalbard.
(*324) -- Spitsbergen.
SPRI record no.: 125506

MARCXML

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100 1# ‡aBartoszewski, Stefan A.
245 10 ‡aSeasonal changeability of physicochemical properties of permafrost active layer waters in the Recherche Fiord region (western Spitsbergen) /‡cStefan A. Bartoszewski, Zdzislaw Michalczyk, Jan Magierski.
260 ## ‡aWushan, Guangzhou :‡bSouth China University of Technology Press,‡c1993.
300 ## ‡ap. 32-35 :‡bdiags., maps.
500 ## ‡aIn: Permafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China / International Conference on Permafrost.
520 3# ‡aInvestigations on southern shore of Bellsund, 1986-90. Retention of active layer is small because saturation layer is thin. Air temperature affects hydrological and hydrochemical processes. All waters in study area are characterized by low mineralization, weak alkaline reaction, and low temperature.
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.345.3 -- Permafrost, composition and structure. Ice wedges.‡2udc
650 07 ‡a556 -- Hydrology.‡2udc
650 07 ‡a556.114 -- Water, chemical properties.‡2udc
650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc
650 07 ‡a54 -- Chemistry.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(*32) -- Svalbard.‡2udc
651 #7 ‡a(*324) -- Spitsbergen.‡2udc
700 1# ‡aMichalczyk, Zdzislaw.
700 1# ‡aMagierski, Jan.
773 0# ‡7m2am ‡aInternational Conference on Permafrost. ‡tPermafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China. ‡dWushan, Guangzhou : South China University of Technology Press, 1993. ‡wSPRI-125499
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