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The Kinetics of Pyrite Dissolution in Nitric Acid Solution
Refractory sulphidic ore with gold captured in pyrite has motivated researchers to find efficient means to break down pyrite to make gold accessible and, ultimately, improve gold extraction. Thus, the dissolution of pyrite was investigated to understand the mechanism and find the corresponding kinet...
Autores principales: | , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
MDPI
2022
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9229596/ https://www.ncbi.nlm.nih.gov/pubmed/35744239 http://dx.doi.org/10.3390/ma15124181 |
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author | Teimouri, Samaneh Potgieter, Johannes Herman van Dyk, Lizelle Billing, Caren |
author_facet | Teimouri, Samaneh Potgieter, Johannes Herman van Dyk, Lizelle Billing, Caren |
author_sort | Teimouri, Samaneh |
collection | PubMed |
description | Refractory sulphidic ore with gold captured in pyrite has motivated researchers to find efficient means to break down pyrite to make gold accessible and, ultimately, improve gold extraction. Thus, the dissolution of pyrite was investigated to understand the mechanism and find the corresponding kinetics in a nitric acid solution. To carry this out, the temperature (25 to 85 °C), nitric acid concentration (1 to 4 M), the particle size of pyrite from 53 to 212 µm, and different stirring speeds were examined to observe their effect on pyrite dissolution. An increase in temperature and nitric acid concentration were influential parameters to obtaining a substantial improvement in pyrite dissolution (95% Fe extraction achieved). The new shrinking core equation (1/3ln (1 − X) + [(1 − X)(−1/3) − 1)]) = kt) fit the measured rates of dissolution well. Thus, the mixed–controlled kinetics model describing the interfacial transfer and diffusion governed the reaction kinetics of pyrite. The activation energies (E(a)) were 145.2 kJ/mol at 25–45 °C and 44.3 kJ/mol at higher temperatures (55–85 °C). A semiempirical expression describing the reaction of pyrite dissolution under the conditions studied was proposed: 1/3ln(1 − X) + [(1 − X)(−1/3) − 1)] = 88.3 [HNO(3)](2.6) r(0)(−1.3) e(−44280/RT) t. The solid residue was analysed using SEM, XRD, and Raman spectrometry, which all identified sulphur formation as the pyrite dissolved. Interestingly, two sulphur species, i.e., S(8) and S(6), formed during the dissolution process, which were detected using XRD Rietveld refinement. |
format | Online Article Text |
id | pubmed-9229596 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2022 |
publisher | MDPI |
record_format | MEDLINE/PubMed |
spelling | pubmed-92295962022-06-25 The Kinetics of Pyrite Dissolution in Nitric Acid Solution Teimouri, Samaneh Potgieter, Johannes Herman van Dyk, Lizelle Billing, Caren Materials (Basel) Article Refractory sulphidic ore with gold captured in pyrite has motivated researchers to find efficient means to break down pyrite to make gold accessible and, ultimately, improve gold extraction. Thus, the dissolution of pyrite was investigated to understand the mechanism and find the corresponding kinetics in a nitric acid solution. To carry this out, the temperature (25 to 85 °C), nitric acid concentration (1 to 4 M), the particle size of pyrite from 53 to 212 µm, and different stirring speeds were examined to observe their effect on pyrite dissolution. An increase in temperature and nitric acid concentration were influential parameters to obtaining a substantial improvement in pyrite dissolution (95% Fe extraction achieved). The new shrinking core equation (1/3ln (1 − X) + [(1 − X)(−1/3) − 1)]) = kt) fit the measured rates of dissolution well. Thus, the mixed–controlled kinetics model describing the interfacial transfer and diffusion governed the reaction kinetics of pyrite. The activation energies (E(a)) were 145.2 kJ/mol at 25–45 °C and 44.3 kJ/mol at higher temperatures (55–85 °C). A semiempirical expression describing the reaction of pyrite dissolution under the conditions studied was proposed: 1/3ln(1 − X) + [(1 − X)(−1/3) − 1)] = 88.3 [HNO(3)](2.6) r(0)(−1.3) e(−44280/RT) t. The solid residue was analysed using SEM, XRD, and Raman spectrometry, which all identified sulphur formation as the pyrite dissolved. Interestingly, two sulphur species, i.e., S(8) and S(6), formed during the dissolution process, which were detected using XRD Rietveld refinement. MDPI 2022-06-13 /pmc/articles/PMC9229596/ /pubmed/35744239 http://dx.doi.org/10.3390/ma15124181 Text en © 2022 by the authors. https://creativecommons.org/licenses/by/4.0/Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). |
spellingShingle | Article Teimouri, Samaneh Potgieter, Johannes Herman van Dyk, Lizelle Billing, Caren The Kinetics of Pyrite Dissolution in Nitric Acid Solution |
title | The Kinetics of Pyrite Dissolution in Nitric Acid Solution |
title_full | The Kinetics of Pyrite Dissolution in Nitric Acid Solution |
title_fullStr | The Kinetics of Pyrite Dissolution in Nitric Acid Solution |
title_full_unstemmed | The Kinetics of Pyrite Dissolution in Nitric Acid Solution |
title_short | The Kinetics of Pyrite Dissolution in Nitric Acid Solution |
title_sort | kinetics of pyrite dissolution in nitric acid solution |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9229596/ https://www.ncbi.nlm.nih.gov/pubmed/35744239 http://dx.doi.org/10.3390/ma15124181 |
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