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dc.contributor.author
Vital, Mélanie

dc.contributor.author
Daval, Damien
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Morvan, Gilles
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Martinez, Daniel Emilio

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Heap, Michael J.
dc.date.available
2021-03-25T12:15:37Z
dc.date.issued
2020-04
dc.identifier.citation
Vital, Mélanie; Daval, Damien; Morvan, Gilles; Martinez, Daniel Emilio; Heap, Michael J.; Barite growth rates as a function of crystallographic orientation, temperature, and solution saturation state; American Chemical Society; Crystal Growth & Design; 20; 6; 4-2020; 3663-3672
dc.identifier.issn
1528-7483
dc.identifier.uri
http://hdl.handle.net/11336/128902
dc.description.abstract
Barite growth kinetics was investigated as a function of crystallographic orientation for temperatures between 10 and 70 °C and initial saturation indices (SI) of 1.1 and 2.1. The growth rates were estimated for the (001), (210), and (101) faces using vertical scanning interferometry. Overall, face-specific barite growth rates (rhkl) can be successfully described by the rate law r(hkl) = A(hkl) exp(-Ea(hkl)/RT) (10SI - 1), where A(hkl) and Ea(hkl) represent the face-specific Arrhenius pre-exponential factor and activation energy, respectively, R is the gas constant, and T refers to the absolute temperature. In addition, because of the modest growth anisotropy of the various investigated faces, the following isotropic rate law can be used to satisfactorily account for the measured rate data: r(hkl) = A exp(-Ea/RT)(10SI - 1) with average values of A = exp(13.59) nm h-1 and Ea = 35.0 ± 2.5 kJ mol-1. Over the range of conditions investigated in the present study, our results suggest that the barite growth kinetics is surface-controlled, while possibly verifying the principle of detailed balancing and microreversibility. These results imply that previous modeling exercises of steady-state barite growth based on isotropic rate laws may remain valid, at least over the range of conditions investigated in the present study.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
American Chemical Society

dc.rights
info:eu-repo/semantics/openAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.subject
BARITE
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ANISOTROPIC GROWTH
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GEOTEHRMAL RESERVOIR
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SCALING
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Mineralogía

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Ciencias de la Tierra y relacionadas con el Medio Ambiente

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CIENCIAS NATURALES Y EXACTAS

dc.title
Barite growth rates as a function of crystallographic orientation, temperature, and solution saturation state
dc.type
info:eu-repo/semantics/article
dc.type
info:ar-repo/semantics/artículo
dc.type
info:eu-repo/semantics/publishedVersion
dc.date.updated
2021-02-18T15:19:41Z
dc.journal.volume
20
dc.journal.number
6
dc.journal.pagination
3663-3672
dc.journal.pais
Estados Unidos

dc.journal.ciudad
Washington
dc.description.fil
Fil: Vital, Mélanie. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mar del Plata. Instituto de Investigaciones Marinas y Costeras. Universidad Nacional de Mar del Plata. Facultad de Ciencias Exactas y Naturales. Instituto de Investigaciones Marinas y Costeras; Argentina. Université de Strasbourg; Francia
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Fil: Daval, Damien. Université de Strasbourg; Francia
dc.description.fil
Fil: Morvan, Gilles. Université de Strasbourg; Francia
dc.description.fil
Fil: Martinez, Daniel Emilio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mar del Plata. Instituto de Investigaciones Marinas y Costeras. Universidad Nacional de Mar del Plata. Facultad de Ciencias Exactas y Naturales. Instituto de Investigaciones Marinas y Costeras; Argentina
dc.description.fil
Fil: Heap, Michael J.. Université de Strasbourg; Francia
dc.journal.title
Crystal Growth & Design

dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://pubs.acs.org/doi/10.1021/acs.cgd.9b01506
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1021/acs.cgd.9b01506
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