Weathering-induced Sb isotope fractionation during leaching of stibnite and formation of secondary Sb minerals

Author(s)
Andreas B. Kaufmann, Marina Lazarov, Ingo Horn, Martin Števko, Tamara Đorđević, Stefan Kiefer, Stefan Weyer, Juraj Majzlan
Abstract

In this work, we investigated the extent of antimony (Sb) isotopic fractionation during weathering of stibnite at supergene conditions. Antimony isotope data have been obtained from secondary Sb minerals collected from Pezinok, Dobšiná (both Slovakia) and Allchar (North Macedonia) deposits and mine tailings. The Sb isotope compositions of sulfides and secondary Sb minerals formed on the primary stibnite [Sb

2S

3] or in mine tailings grains were compared with each other. Furthermore, we experimentally investigated Sb isotope fractionation during stibnite leaching with different acids. Our study reveals a large isotopic range for δ

123Sb (from −0.50 to +0.69 ‰) for secondary Sb minerals. They are either isotopically indistinguishable or isotopically lighter than the primary stibnite. Isotopically indistinguishable weathering products likely formed by quantitative Sb transfer from stibnite to the secondary minerals, such as brandholzite [Mg(H

2O)

6[Sb(OH)

6]

2] from Pezinok. Isotopic fractionation towards lighter δ

123Sb was observed for adsorption of Sb onto iron oxides. Distinctly isotopically lighter δ

123Sb was observed in secondary Sb minerals tripuhyite [FeSbO

4], chapmanite [Fe

3+

2Sb

3+(Si

2O

5)O

3(OH)], hydroxyferroromeite [Fe

2Sb

2O

6(OH)], and stibiconite [Sb

3O

6OH] that either replace stibnite or formed in mine tailings from the pore solutions. These secondary minerals were likely generated by partial precipitation of Sb from aqueous solutions produced by dissolution of stibnite. In the leaching experiments with HCl and oxalic acid, Sb was leached without significant isotope effects during the first 2–3 days, followed by a drop of the dissolved Sb concentration associated with Sb isotope fractionation towards high δ

123Sb in the leachate (by up to 0.5 ‰) after 4–7 days. We interpret these observations to be related to the precipitation of secondary Sb oxides with low δ

123Sb, resulting in an isotopically heavy dissolved Sb pool. These findings are in agreement with previous results of isotopically heavy groundwater and mine drainage water with δ

123Sb > +0.36 ‰ that may suggest that the ‘truly’ dissolved (operationally defined as <0.45 μm) Sb fraction in general may be isotopically heavy.

Organisation(s)
Department of Mineralogy and Crystallography
External organisation(s)
Friedrich-Schiller-Universität Jena, Gottfried Wilhelm Leibniz Universität Hannover, National Museum Prague, Technische Universität Wien, Comenius University Bratislava
Journal
Chemical Geology
Volume
662
Pages
122253–122266
No. of pages
14
ISSN
0009-2541
DOI
https://doi.org/10.1016/j.chemgeo.2024.122253
Publication date
09-2024
Peer reviewed
Yes
Austrian Fields of Science 2012
105116 Mineralogy, 105113 Crystallography
Keywords
ASJC Scopus subject areas
Geochemistry and Petrology, Geology
Portal url
https://ucrisportal.univie.ac.at/en/publications/e5202f51-ebd8-4faa-9654-ca5d421ec9e8