Repositorio Institucional
Repositorio Institucional
CONICET Digital
  • Inicio
  • EXPLORAR
    • AUTORES
    • DISCIPLINAS
    • COMUNIDADES
  • Estadísticas
  • Novedades
    • Noticias
    • Boletines
  • Ayuda
    • General
    • Datos de investigación
  • Acerca de
    • CONICET Digital
    • Equipo
    • Red Federal
  • Contacto
JavaScript is disabled for your browser. Some features of this site may not work without it.
  • INFORMACIÓN GENERAL
  • RESUMEN
  • ESTADISTICAS
 
Artículo

Barite growth rates as a function of crystallographic orientation, temperature, and solution saturation state

Vital, MélanieIcon ; Daval, Damien; Morvan, Gilles; Martinez, Daniel EmilioIcon ; Heap, Michael J.
Fecha de publicación: 04/2020
Editorial: American Chemical Society
Revista: Crystal Growth & Design
ISSN: 1528-7483
Idioma: Inglés
Tipo de recurso: Artículo publicado
Clasificación temática:
Mineralogía

Resumen

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.
Palabras clave: BARITE , ANISOTROPIC GROWTH , GEOTEHRMAL RESERVOIR , SCALING
Ver el registro completo
 
Archivos asociados
Thumbnail
 
Tamaño: 696.6Kb
Formato: PDF
.
Descargar
Licencia
info:eu-repo/semantics/openAccess Excepto donde se diga explícitamente, este item se publica bajo la siguiente descripción: Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Unported (CC BY-NC-SA 2.5)
Identificadores
URI: http://hdl.handle.net/11336/128902
URL: https://pubs.acs.org/doi/10.1021/acs.cgd.9b01506
DOI: http://dx.doi.org/10.1021/acs.cgd.9b01506
Colecciones
Articulos(IIMYC)
Articulos de INSTITUTO DE INVESTIGACIONES MARINAS Y COSTERAS
Citación
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
Compartir
Altmétricas
 

Enviar por e-mail
Separar cada destinatario (hasta 5) con punto y coma.
  • Facebook
  • X Conicet Digital
  • Instagram
  • YouTube
  • Sound Cloud
  • LinkedIn

Los contenidos del CONICET están licenciados bajo Creative Commons Reconocimiento 2.5 Argentina License

https://www.conicet.gov.ar/ - CONICET

Inicio

Explorar

  • Autores
  • Disciplinas
  • Comunidades

Estadísticas

Novedades

  • Noticias
  • Boletines

Ayuda

Acerca de

  • CONICET Digital
  • Equipo
  • Red Federal

Contacto

Godoy Cruz 2290 (C1425FQB) CABA – República Argentina – Tel: +5411 4899-5400 repositorio@conicet.gov.ar
TÉRMINOS Y CONDICIONES