Please use this identifier to cite or link to this item: http://dspace.utpl.edu.ec/handle/123456789/19294
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dc.contributor.authorStashans, A.es_ES
dc.contributor.authorChamba, G.es_ES
dc.date.accessioned2017-06-16T22:03:18Z-
dc.date.available2009-12-01es_ES
dc.date.available2017-06-16T22:03:18Z-
dc.date.issued2011-08-15es_ES
dc.date.submitted16/03/2010es_ES
dc.identifier10.1002/qua.22538es_ES
dc.identifier.isbn207608es_ES
dc.identifier.other10.1002/qua.22538es_ES
dc.identifier.urihttp://dspace.utpl.edu.ec/handle/123456789/19294-
dc.description.abstractMagnesium is a key determinant in calcite (CaCO3) mineralization having a notable significance upon the carbonate growth. Magnesium is also present in CaCO3 mineral scale formation which is a persistent and expensive problem in oil and gas production. In the present work, we attempt to treat CaCO3 calcite mineral bulk inducing different concentrations of Mg impurity. The study is done using a quantum-chemical computer code based on the Hartree-Fock method. It is found that small Mg impurity concentrations produce a significant distortion of the defect-closest O atoms thus developing local microstructures being distinct to those of the original calcite structure. This structural alteration is accompanied by the electron density redistribution from the O 2pz atomic orbitals (AOs) toward the O 2px and 2py AOs for impurity nearest oxygens. On the other hand, the high Mg impurity concentrations make the chemical bonding in calcite more ionic. Copyright © 2010 Wiley Periodicals, Inc.es_ES
dc.languageIngléses_ES
dc.subjectCaCO 3es_ES
dc.titleA new insight on the role of Mg in calcitees_ES
dc.typeArticlees_ES
dc.publisherInternational Journal of Quantum Chemistryes_ES
Appears in Collections:Artículos de revistas Científicas

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