Effect of salinity, pressure and temperature on the solubility of smithsonite (ZnCO<inf>3</inf>) and Zn complexation in crustal and upper mantle hydrothermal fluids

Farsang, S; Louvel, M; Rosa, AD; Amboage, M; Anzellini, S; Widmer, RN; Redfern, SAT

doi:10.17863/CAM.69754

Effect of salinity, pressure and temperature on the solubility of smithsonite (ZnCO3) and Zn complexation in crustal and upper mantle hydrothermal fluids

Accepted version

Peer-reviewed

Repository URI

https://www.repository.cam.ac.uk/handle/1810/322295

Repository DOI

https://doi.org/10.17863/CAM.69754

Files

Accepted version (1.28 MB)

Type

Article

Authors

Farsang, S

Louvel, M

Rosa, AD

Amboage, M

Anzellini, S

Show 2 more

Keywords

Zinc speciation, Smithsonite, Solubility, Subduction zone fluids, Deep Earth, High pressure, High temperature, Salinity, Synchrotron XRF, XAS, DAC

Journal Title

Chemical Geology

Journal ISSN

0009-2541
1872-6836

Volume Title

578

Publisher

Elsevier BV

Publisher DOI

https://doi.org/10.1016/j.chemgeo.2021.120320

Rights

Attribution-NonCommercial-NoDerivatives 4.0 International

Sponsorship

Natural Environment Research Council (NE/P012167/1)
NERC (NE/L002507/1)

Collections

University of Cambridge Research Outputs (Articles and Conferences)