Skip to main navigation Skip to search Skip to main content

Stabilities of byströmite, MgSb2O6, ordoñezite, ZnSb2O6 and rosiaite, PbSb2O6, and their possible roles in limiting antimony mobility in the supergene zone

Adam J. Roper, Peter Leverett, Timothy D. Murphy, Peter A. Williams

Research output: Contribution to journalArticlepeer-review

Abstract

In order to clarify the roles that secondary minerals may have in determining the extent of dispersion of Sb in the supergene environment, syntheses and stability studies of the Sb(V) oxides byströmite, MgSb2O6, ordoñezite, ZnSb2O6 and rosiaite, PbSb2O6, have been undertaken. Solubilities in aqueous HNO3 were determined at 298.2 K and the data obtained used to calculate values of ΔG f θ at the same temperature. The derived ΔG f θ(s, 298.2 K) values for MgSb2O6 (-1554.1 ±3.6 kJ mol-1), ZnSb2O6 (-1257.0 ±2.6 kJ mol-1) and PbSb2O6 (-1154.2 ±2.6 kJ mol-1) have been used in subsequent calculations to determine their relative stabilities and relationships with other secondary Sb minerals.

Original languageEnglish
Pages (from-to)537-544
Number of pages8
JournalMineralogical Magazine
Volume79
Issue number3
DOIs
Publication statusPublished - Jun 2015
Externally publishedYes

Keywords

  • byströmite
  • ordoñezite
  • rosiaite
  • antimony
  • solubility
  • mobility
  • chemical mineralogy
  • supergene zone

Fingerprint

Dive into the research topics of 'Stabilities of byströmite, MgSb2O6, ordoñezite, ZnSb2O6 and rosiaite, PbSb2O6, and their possible roles in limiting antimony mobility in the supergene zone'. Together they form a unique fingerprint.

Cite this