title: Kinetic isotope effects in oxygen in the laboratory dehydration of magnesian minerals.
abstract: Laboratory studies of vacuum dehydration of Mg-O-H units in minerals and rocks reveal large kinetic isotope effects in oxygen, with light-isotope enrichment in the liberated water, and concomitant heavy-isotope enrichment in the residual solids. Application of the same techniques to a meteorite assemblage including hydrous magnesium silicates shows a much more complex behavior, probably due to isotopic heterogeneity inherited from processes on the meteorite parent body. Measurements of both the (17)O/(16)O variations and the (18)O/(16)O variations confirm theoretical predictions that slopes of three-isotope correlation lines are systematically larger for equilibrium isotope effects than for kinetic isotope effects.
authors.affiliation: Enrico Fermi Institute, University of Chicago, Chicago, Illinois 60637, USA.
authors.forename: Robert N
authors.initials: RN
authors.lastname: Clayton
authors.forename: Toshiko K
authors.initials: TK
authors.lastname: Mayeda