USE OF CATION-EXCHANGE EQUILIBRIA TO INVESTIGATE THE PARTITIONING OF TUNGSTEN BETWEEN HETEROGENEOUS PHASES OF A FLUID

dc.contributor.author	Kotelnikov A.R.
dc.contributor.author	Musayev A.A.
dc.contributor.author	Averina A.S.
dc.contributor.author	Ganeyev I.G.
dc.date.accessioned	2020-11-02T00:30:41Z
dc.date.available	2020-11-02T00:30:41Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=31128763
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 4, 255-257
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18340
dc.description.abstract	The phases of a stratified fluid, each concentrating different components of the original mixture, that constituted the initial fluid, may evolve separately in the course of subsequent flow through porous media, in accordance with the properties of each phase and the conditions in the environment. It appears important to determine experimentally the partitioning of ore components among the phases of such a heterogeneous fluid. We have demonstrated that cation exchange equilibria can be used to evaluate the partition coefficients of elements among phases of a stratified fluid. Our preliminary results indicate that the concentration of tungsten is higher in the liquid phase of the fluid (in the H2O-NaCl system) than in the vapor phase.
dc.title	USE OF CATION-EXCHANGE EQUILIBRIA TO INVESTIGATE THE PARTITIONING OF TUNGSTEN BETWEEN HETEROGENEOUS PHASES OF A FLUID
dc.type	Статья

Files in this item

Files	Size	Format	View
There are no files associated with this item.