DISSOLUTION KINETICS AT THE CALCITE-WATER INTERFACE

dc.contributor.author	Yong L.
dc.contributor.author	Baer D.R.
dc.contributor.author	McCoy J.M.
dc.contributor.author	Amonette J.E.
dc.contributor.author	LaFemina J.P.
dc.date.accessioned	2020-11-23T10:53:32Z
dc.date.available	2020-11-23T10:53:32Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=491644
dc.identifier.citation	Geochimica et Cosmochimica Acta, 1996, , 23, 4883-4887
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/19412
dc.description.abstract	Although many geochemical processes, including mineral dissolution, are controlled by kinetic mechanisms, quantitative descriptions of the reaction kinetics are mostly lacking, principally due to an incomplete understanding of the molecular-scale processes controlling these reactions. In this paper, a combined experimental and theoretical approach involving atomic force microscopy, an analytical terrace-ledge-kink model, and kinetic Monte Carlo computer simulations was used to study the aqueous dissolution kinetics of the calcite (10\-14) surface. The study provides a determination of the elementary rates and activation energies associated with dissolution at specific kink sites on the calcite surface.
dc.title	DISSOLUTION KINETICS AT THE CALCITE-WATER INTERFACE
dc.type	Статья

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