Skip Nav Destination
GEOREF RECORD
Anorthite/fluid partitioning of europium at 650 degree C and 1. 3 kbar
P. D'Arco and M. Lagache
Anorthite/fluid partitioning of europium at 650 degree C and 1. 3 kbar
European Journal of Mineralogy (December 1989) 1 (6): 783-790
Anorthite/fluid partitioning of europium at 650 degree C and 1. 3 kbar
European Journal of Mineralogy (December 1989) 1 (6): 783-790
Index Terms/Descriptors
Abstract
The partition coefficient here depends strongly on the composition of the solution: incorporation of Eu into anorthite is enhanced by a decrease in chlorinity. At a given chlorinity, the partition coefficient depends on the Eu concentration in anorthite, e.g. it decreases from 9-10 to 4 and from 2-3 to 0.1 as the concentration of Eu in anorthite increases from 0.1 to approx 15 000 ppm, for 0.5 and 3.0 mole Cl/litre solutions, respectively. Eu occurs exclusively in the trivalent state in these experiments; its incorporation involves trapping in extended defects as well as cation exchange.
ISSN: 0935-1221
Serial Title: European Journal of Mineralogy
Serial Volume: 1
Serial Issue: 6
Title: Anorthite/fluid partitioning of europium at 650 degree C and 1. 3 kbar
Affiliation: Ecol. Norm. Super., Lab. Geol.,
F-75005 Paris,
France
Pages: 783-790
Published: 198912
Text Language: English
Publisher: Schweizerbart'sche Verlagsbuchhandlung (Naegele u. Obermiller),
Stuttgart,
Federal Republic of Germany
References: 22
DOI:
10.1127/ejm/1/6/0783
Accession Number: 1992-062992
Categories: Mineralogy of silicatesGeochemistry of rocks, soils, and sediments
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: 4 tables
Country of Publication: Germany
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United KingdomTwickenhamUKUnited Kingdom
Update Code: 1992