Hostname: page-component-78c5997874-s2hrs Total loading time: 0 Render date: 2024-11-13T03:30:57.664Z Has data issue: false hasContentIssue false

Reaction of bentonites with pyrite concentrate after wetting and drying cycles at 80°C: relevance to radioactive waste (Radwaste) storage

Published online by Cambridge University Press:  09 July 2018

M. Osacky*
Affiliation:
Department of Chemical and Materials Engineering, University of Alberta, Edmonton, Alberta, Canada T6G 2V4 Department of Geology of Mineral Deposits, Comenius University, Mlynská dolina, 84215 Bratislava, Slovakia
V. Šucha
Affiliation:
Department of Geology of Mineral Deposits, Comenius University, Mlynská dolina, 84215 Bratislava, Slovakia
M. Miglierini
Affiliation:
Institute of Nuclear and Physical Engineering, Slovak University of Technology, Ilkovičova 3, 81219 Bratislava, Slovakia Regional Centre of Advanced Technologies and Materials, Faculty of Science, Palacky University, 17 listopadu 12, 77146 Olomouc, Czech Republic
J. Madejová
Affiliation:
Institute of Inorganic Chemistry, Slovak Academy of Sciences, Dúbravská cesta 9, 84536 Bratislava, Slovakia

Abstract

The mineral stability of two bentonites was studied in the presence of pyrite concentrate to simulate the possible reactions between the bentonite barrier used in a high-level nuclear waste (HLW) repository and host rock containing up to 5 wt.% of admixed pyrite. Smectite was the only bentonite mineral affected by pyrite treatment under the experimental conditions used. Bentonites reacted differently with pyrite due to the different nature of the smectites. The distinct crystal chemistry of the smectites controlled by the composition of the parent rocks influenced the smectite surface properties (cation exchange capacity and layer charge distribution) which resulted in a different response of the bentonites to pyrite treatment. A partial transformation of the original smectites into H-smectites represented the initial stage of smectite destabilization on acid attack. Rising non-equivalent isomorphous substitution in the octahedral sheets of the smectites enhanced smectite reactivity and thus the reaction between bentonite and pyrite, causing lower stability of the bentonite containing high-charge smectite.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2012

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Andrejkovičová, S., Pentrák, M., Jankovič, L. & Komadel, P. (2010) Sorption of heavy metal cations on rhyolitic and andesitic bentonites from Central Slovakia. Geologica Carpathica, 61, 163–171.CrossRefGoogle Scholar
Blanc, P. & Gaucher, E. (2003) Minéralogie du Callovo-Oxfordien en vue d’une modélisation thermodynamique. BRGM/RP-52566-FR, BRGM Report.Google Scholar
Christidis, G.E. (1998) Comparative study of the mobility of major and trace elements during alteration of an andesite and a rhyolite to bentonite, in the islands of Milos and Kimolos, Aegean Greece. Clays and Clay Minerals, 46, 379–399.CrossRefGoogle Scholar
Christidis, G.E. & Dunham, A.C. (1997) Compositional variations in smectites. Part II. Alteration of acidic precursors. A case study from Milos Island, Greece. Clay Minerals, 32, 253–270.CrossRefGoogle Scholar
Cruz, R., Bertrand, V., Monroy, M. & González, I. (2001) Effect of sulfide impurities on the reactivity of pyrite and pyritic concentrates: a multi-tool approach. Applied Geochemistry, 16, 803–819.CrossRefGoogle Scholar
De Craen, M., Wang, L., Van Geet, M. & Moors, H. (2004) Geochemistry of Boom Clay Pore Water at the Mol Site – Status 200. SCK·CEN Report BLG-990.Google Scholar
Eberl, D.D. (2003) User's guide to RockJock – a program for determining quantitative mineralogy from powder X-ray diffraction data. U.S. Geological Survey, Open-File Report No. 03-78.Google Scholar
Frau, F. (2000) The formation-dissolution-precipitation cycle of melanterite at the abandoned pyrite mine of Genna Luas in Sardinia, Italy: environmental implications. Mineralogical Magazine, 64, 995–1006.CrossRefGoogle Scholar
Galamboš, M., Kufčáková, J. & Rajec, P. (2009) Sorption of strontium on Slovak bentonites. Journal of Radioanalytical and Nuclear Chemistry, 281, 347–357.CrossRefGoogle Scholar
Gates, W.P., Anderson, M.D. & Churchman, G.J. (2002) Mineralogy of a bentonite from Miles, Queensland, Australia and characterisation of its acid activation products. Applied Clay Science, 20, 189–197.CrossRefGoogle Scholar
Gaucher, E., Robelin, C., Matray, J.M., Negrel, G., Gros, Y., Heitz, J.F., Vinsot, A., Rebours, H., Cassabagnere, A. & Bouchet, A. (2004) ANDRA underground research laboratory: Interpretation of the mineralogical and geochemical data acquired in the Callovian-Oxfordian Formation by investigative drilling. Physics and Chemistry of the Earth, 29, 55–77.Google Scholar
Honty, M. (2008) SMARAGD: Study of Mineral Alterations of Clay Barriers used for Radwaste storage and its Geological Disposal. Final report, Contract FI6W-CT2005-028403, DG for Research EURATOM, Luxembourg.Google Scholar
Komadel, P., Bujdák, J., Madejová, J., Šucha, V. & Elsass, F. (1996) Effect of non-swelling layer on the dissolution of reduced-charge montmorillonite in hydrochloric acid. Clay Minerals, 31, 333–345.CrossRefGoogle Scholar
Komadel, P., Anastácio, A.S., Andrejkovičová, S. & Stucki, J.W. (2008) Iron phases identified in bentonite from the Lieskovec deposit (Slovakia) by variable-temperature Mössbauer spectroscopy. Clay Minerals, 43, 107–115.CrossRefGoogle Scholar
Kraus, I., Šamajová, E., Šucha, V., Lexa, J. & Hroncová, Z. (1994) Diagenetic and hydrothermal alterations of volcanic rocks into clay minerals and zeolites (Kremnické Vrchy Mts., the Western Carpathians). Geologica Carpathica, 45, 151–158.Google Scholar
Lehner, S. & Savage, K. (2008) The effect of As, Co, and Ni impurities on pyrite oxidation kinetics: Batch and flow-through reactor experiments with synthetic pyrite. Geochimica et Cosmochimica Acta, 72, 1788–1800.CrossRefGoogle Scholar
Lehner, S., Savage, K., Ciobanu, M. & Cliffel, D.E. (2007) The effect of As, Co, and Ni impurities on pyrite oxidation kinetics: An electrochemical study of synthetic pyrite. Geochimica et Cosmochimica Acta, 71, 2491–2509.CrossRefGoogle Scholar
Lintnerová, O., Šottník, P. & Šoltés, S. (2008) Abandoned Smolník mine (Slovakia) – a catchment area affected by mining activities. Estonian Journal of Earth Sciences, 57, 104–110.CrossRefGoogle Scholar
Madejová, J., Bujdák, J., Janek, M. & Komadel, P. (1998) Comparative FT-IR study of the structural modifications during acid treatment of dioctahedral smectites and hectorite. Spectrochimica Acta Part A, 54, 1397–1406.CrossRefGoogle Scholar
Mazurek, M. (1999) Mineralogy of the Opalinus Clay. Pp 15–18 in: Results of the Hydrogeological, Geochemical and Geotechnical Experiments (Thury, M. & ossart, P., editors). Geological Report No. 23, Swiss National Geological and Hydrogeological Survey, Ittegen-Berne, Switzerland.Google Scholar
Meier, L.P. & Kahr, G. (1999) Determination of the cation exchange capacity (CEC) of clay minerals using the complexes of copper(II) ion with triethylentetramine and tetraethylenepentamine. Clays and Clay Minerals, 47, 386–388.CrossRefGoogle Scholar
Pearson, F.J., Arcos, D., Boisson, J-Y., Fernandez, A.M., Gäbler, H.E., Gaucher, E., Gautschi, A., Griffault, L., Hernan, P. & Waber, H.N. (2003) Mont Terri Project – Geochemistry of Water in the Opalinus Clay Formation at the Mont Terri Rock Laboratory. Geology Series No. 5, Swiss Federal Office of Water and Geology, Bern.Google Scholar
Pentrák, M., Madejová, J., Czímerová, A. & Komadel, P. (2012) Changes in layer charge of clay minerals upon acid treatment as obtained from their interactions with methylene blue. Applied Clay Science, 55, 100–107.CrossRefGoogle Scholar
Steudel, A., Batenburg, L.F., Fisher, H.R., Weidler, P.G. & Emmerich, K. (2009) Alteration of swelling clay minerals by acid activation. Applied Clay Science, 44, 105–115.Google Scholar
Winchester, J.A. & Floyd, P.A. (1977) Geochemical discrimination of different magma series and their differentiation products using immobile elements. Chemical Geology, 20, 235–243.CrossRefGoogle Scholar
Žák, T. & Jirásková, Y. (2006) CONFIT: Mössbauer spectra fitting program. Surface and Interface Analysis, 38, 710–714.CrossRefGoogle Scholar