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Record #104150:

Salt fingering in subsea permafrost: some stability and energy considerations / Joan P. Gosink, G.C. Baker.

Title: Salt fingering in subsea permafrost: some stability and energy considerations / Joan P. Gosink, G.C. Baker.
Author(s): Gosink, Joan P.
Baker, G. C.
Date: 1990.
In: Journal of Geophysical Research. (1990.), Vol. 95(C6) (1990)
Abstract: Critical density gradient criterion for salt fingering in porous media was determined through simple wedge-flow model. In this, two salt transport mechanisms, convection and diffusion, are decoupled, and time scale analysis of these processes is performed. Stable density gradient exists when time required to form wedge-like flow is greater than time required to diffuse salt water horizontally across layer.
Notes:

Journal of Geophysical Research. Vol. 95(C6) :9575-9583 (1990).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.3 -- Land ice, depth measurements.
551.345 -- Permafrost. Cryopedology.
54 -- Chemistry.
E8 -- Glaciology: frost action and permafrost.
SPRI record no.: 104150

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245 10 ‡aSalt fingering in subsea permafrost :‡bsome stability and energy considerations /‡cJoan P. Gosink, G.C. Baker.
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500 ## ‡aJournal of Geophysical Research. Vol. 95(C6) :9575-9583 (1990).
520 3# ‡aCritical density gradient criterion for salt fingering in porous media was determined through simple wedge-flow model. In this, two salt transport mechanisms, convection and diffusion, are decoupled, and time scale analysis of these processes is performed. Stable density gradient exists when time required to form wedge-like flow is greater than time required to diffuse salt water horizontally across layer.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.3 -- Land ice, depth measurements.‡2udc
650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc
650 07 ‡a54 -- Chemistry.‡2udc
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