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dc.contributor.authorRioz-Agudo, E.
dc.contributor.authorPutnis, C.
dc.contributor.authorPutnis, Andrew
dc.date.accessioned2017-01-30T12:52:53Z
dc.date.available2017-01-30T12:52:53Z
dc.date.created2015-04-23T03:53:27Z
dc.date.issued2014
dc.identifier.citationRioz-Agudo, E. and Putnis, C. and Putnis, A. 2014. Coupled dissolution and precipitation at mineral-fluid interfaces. Chemical Geology. 383: pp. 132-146.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/26336
dc.identifier.doi10.1016/j.chemgeo.2014.06.007
dc.description.abstract

Reactions occurring at mineral–fluid interfaces are important in all geochemical processes and essential for the cycling of elements within the Earth. Understanding the mechanism of the transformation of one solid phase to another and the role of fluids is fundamental to many natural and industrial processes. Problems such as the interaction of minerals with CO2-saturated water, the durability of nuclear waste materials, the remediation of polluted water, and mineral reactions that can destroy our stone-based cultural heritage, are related by the common feature that a mineral assemblage in contact with a fluid may be replaced by a more stable assemblage

dc.publisherElsevier Science BV
dc.subjectReplacement
dc.subjectCoupled dissolution–precipitation
dc.subjectMineral–water interface
dc.titleCoupled dissolution and precipitation at mineral-fluid interfaces
dc.typeJournal Article
dcterms.source.volume383
dcterms.source.startPage132
dcterms.source.endPage146
dcterms.source.issn0009-2541
dcterms.source.titleChemical Geology
curtin.accessStatusFulltext not available


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