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Lookup NU author(s): Professor John Mitchell
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The release and collection of gypsum hydration water without isotopic fractionation, or contamination by adsorbed moisture, is complicated by the fact that gypsum starts to lose part of its water at low temperatures, which prevents heating the sample as a cleaning strategy. Additionally, results indicate that even at low vacuum conditions (from 10-2 to 10-3 mb) hydration water of gypsum can be lost, given time enough, particularly if associated with moderately raised temperature. In this report we describe an analytical procedure suitable for the complete release and collection of gypsum hydration water, at the same time that external water is efficiently excluded. The critical step is the elimination of external moisture without the removal of any hydration water. To minimize water losses to the walls of the vacuum line, a low-volume, transfer system (TS) has been designed and built. The procedure requires only about 20-25 mg of gypsum sample (4-5 μl of water) for the oxygen isotopic analysis by the guanidine hydrochloride reaction method, to an overall reproducibility of ±0.5‰ or better. © 2004 Elsevier B.V. All rights reserved.
Author(s): Playa E, Recio C, Mitchell J
Publication type: Article
Publication status: Published
Journal: Chemical Geology
Year: 2005
Volume: 217
Issue: 1-2
Pages: 89-96
ISSN (print): 0009-2541
ISSN (electronic): 1872-6836
Publisher: Elsevier BV
URL: http://dx.doi.org/10.1016/j.chemgeo.2004.12.005
DOI: 10.1016/j.chemgeo.2004.12.005
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