Partitioning of Co2+ and Mn2+ into meridianiite (MgSO4·11H2O): Ternary solubility diagrams at 270 K; cation site distribution determined by single-crystal time-of-flight neutron diffraction and density functional theory (2017)
Attributed to:
EXPERIMENTAL AND COMPUTATIONAL STUDIES OF PLANETARY ICES AND THEIR ROLE IN THE THERMAL EVOLUTION OF ICY MOONS
funded by
STFC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1016/j.fluid.2017.01.005
Publication URI: http://dx.doi.org/10.1016/j.fluid.2017.01.005
Type: Journal Article/Review
Parent Publication: Fluid Phase Equilibria