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Record #125242:

Laboratory simulation of dolomite and limestone dissolution: rates, yield and mineralogy of fine-grained residue / Ronald S. Sletten.

Title: Laboratory simulation of dolomite and limestone dissolution: rates, yield and mineralogy of fine-grained residue / Ronald S. Sletten.
Author(s): Sletten, Ronald S.
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: Five samples of dolomite and limestone from Svalbard were tested for dissolution at acidity of precipitation and snowmelt. Dolomite dissolved to produce fine-textured residues about 8-14% by weight. Limestone dissolved to 1-3% fines, mainly silicates. Dolomite dissolved more slowly than limestone, but chemical weathering of carbonate rocks is limited by water availability. Effect of rock type and chemical weathering on frost shattering is discussed.
Notes:

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

Keywords: 54 -- Chemistry.
546.26 -- Carbon.
551.1/.4 -- Geology.
551.311.23 -- Weathering.
551.342 -- Frost shattering.
631.4 -- Soil science.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*324) -- Spitsbergen.
SPRI record no.: 125242

MARCXML

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100 1# ‡aSletten, Ronald S.
245 10 ‡aLaboratory simulation of dolomite and limestone dissolution :‡brates, yield and mineralogy of fine-grained residue /‡cRonald S. Sletten.
260 ## ‡aWushan, Guangzhou :‡bSouth China University of Technology Press,‡c1993.
300 ## ‡ap. 580-585 :‡bill., diags., tables.
500 ## ‡aIn: Permafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China / International Conference on Permafrost.
520 3# ‡aFive samples of dolomite and limestone from Svalbard were tested for dissolution at acidity of precipitation and snowmelt. Dolomite dissolved to produce fine-textured residues about 8-14% by weight. Limestone dissolved to 1-3% fines, mainly silicates. Dolomite dissolved more slowly than limestone, but chemical weathering of carbonate rocks is limited by water availability. Effect of rock type and chemical weathering on frost shattering is discussed.
650 07 ‡a54 -- Chemistry.‡2udc
650 07 ‡a546.26 -- Carbon.‡2udc
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.311.23 -- Weathering.‡2udc
650 07 ‡a551.342 -- Frost shattering.‡2udc
650 07 ‡a631.4 -- Soil science.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*324) -- Spitsbergen.‡2udc
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
917 ## ‡aUnenhanced record from Muscat, imported 2019
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