Please use this identifier to cite or link to this item: http://elar.urfu.ru/handle/10995/130668
Title: A rest potential study of impurity (As, Au, Ni and Co) bearing synthetic pyrite in alkaline flotation conditions
Authors: Babedi, L.
Tadie, M.
von, der, Heyden, B. P.
Chareev, D. A.
Issue Date: 2023
Publisher: Elsevier Ltd
Citation: Babedi, L, Tadie, M, Von der Heyden, BP & Chareev, DA 2023, 'A rest potential study of impurity (As, Au, Ni and Co) bearing synthetic pyrite in alkaline flotation conditions', Minerals Engineering, Том. 202, 108277. https://doi.org/10.1016/j.mineng.2023.108277
Babedi, L., Tadie, M., Von der Heyden, B. P., & Chareev, D. A. (2023). A rest potential study of impurity (As, Au, Ni and Co) bearing synthetic pyrite in alkaline flotation conditions. Minerals Engineering, 202, [108277]. https://doi.org/10.1016/j.mineng.2023.108277
Abstract: Pyrite is an important mineralogical component of most sulphide ore deposit classes, where it commonly forms part of the gangue mineralogy, but may also represent an important ore mineral (i.e., auriferous pyrite). Effective and efficient separation of pyrite is thus a crucial step during most ore processing operations, and this is in part influenced by the pyrite mineral chemistry. Here, electrochemical measurements were used to study the reactivity of a series of well-characterised synthetic trace-element substituted pyrite samples under alkaline conditions relevant to industrial flotation. The presence of metals and metalloid impurities (As, Au, Co, and Ni) in pyrite were tested using rest potential measurements to infer oxidation and associated hydrophobicity. In the absence of any collector phases, pure- and Ni-substituted pyrite have the highest rest potential, followed by Co-substituted pyrite and couple-substituted (Co + Au) pyrite, whilst As-substituted pyrite has the lowest measured rest potential. Importantly, the degree of oxidation at the mineral surface correlates linearly with the concentration of each of the substituents, with the largest effect observed when As is the substituent. These results correspond to the semiconducting properties and noble character of each pyrite sample, with n-type pyrite (Au-, Co- and Ni-substituted) associated with noble character and high rest potential, whereas p-type As-substituted pyrite associated with least noble character and lowest rest potential. With the addition of a potassium amyl xanthate collector, the mineral chemistry further had an impact on the probability of dixanthogen formation. Increased substituent concentration in the pyrite lattice decreased the probability of dixanthogen formation, except in a sample where high Au (and moderate Co) was incorporated. These results highlight the importance of developing improved understanding of the impacts of substitution mechanisms on the surface reactivity and flotability of pyrite. Such an understanding will form the foundation for further improved (and engineered) approaches towards reagent design and mixture. This will serve to optimise separation of both gangue and valuable pyrite by using fundamental knowledge to target specific collector bands and flotation domains. © 2023 The Authors
Keywords: DIXANTHOGEN
FLOTATION
PYRITE
REST POTENTIAL
XANTHATE
ALKALINITY
FLOTATION
GOLD DEPOSITS
NICKEL
SULFUR COMPOUNDS
TRACE ELEMENTS
ALKALINES
CO AND NI
CONDITION
DIXANTHOGEN
MINERAL CHEMISTRY
ORE MINERALS
PROCESSING OPERATIONS
REST POTENTIALS
SULFIDE ORE DEPOSITS
XANTHATE
PYRITES
URI: http://elar.urfu.ru/handle/10995/130668
Access: info:eu-repo/semantics/openAccess
cc-by
License text: https://creativecommons.org/licenses/by/4.0/
SCOPUS ID: 85165946313
WOS ID: 001047540000001
PURE ID: 43258391
ISSN: 0892-6875
DOI: 10.1016/j.mineng.2023.108277
metadata.dc.description.sponsorship: Ministry of Education and Science of the Russian Federation, Minobrnauka; Universiteit Stellenbosch, US; DSI-NRF Centre of Excellence for Integrated Mineral and Energy Resource Analysis, CIMERA; Institute of Experimental Mineralogy, Russian Academy of Sciences, IEM, RAS: NSh-2394.2022.1.5
The authors are grateful to the DSI-NRF Centre of Excellence for Integrated Mineral and Energy Resource Analysis (CIMERA) for providing funding for this research. Special thanks to the Russian Academy of Science's Institute of Experimental Mineralogy for facilitating this collaboration and assisting with the synthesis of the pyrite crystals used in this study. In addition, Dr. Chareev acknowledges the state financial support of the leading scientific schools of the Russian Federation No. NSh-2394.2022.1.5 and the research funding from the Ministry of Science and Higher Education of the Russian Federation (Ural Federal University Program of Development within the Priority-2030 Program) that helped establish the experimental lab used to generate synthetic samples for this study. The authors would also like to express their gratitude to the colleagues at Stellenbosch University's Central Analytical Facilities (CAF) for their excellent assistance with the SEM and LA-ICP-MS evaluations. Thanks to Remy Bucher at Ithemba Labs for his help with the XRD analysis of our samples. Additionally, the authors would like to thank the editor and reviewers for reading and evaluating our manuscript.
Appears in Collections:Научные публикации ученых УрФУ, проиндексированные в SCOPUS и WoS CC

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