The effect of barium on calcite {101¯4} surfaces during growth
In situ atomic force microscopy (AFM) experiments have provided information about the effect of Ba21 on crystal growth of calcite {101¯4} surfaces. The microtopographic features observed have been interpreted by considering both the structural control that the calcite surfaces exert on the incorpora...
| Autores: | , , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2000 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | inglés |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/57133 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/57133 |
| Access Level: | acceso abierto |
| Palabra clave: | 548.5 Crystal growth Calcite Barium Cristalografía (Geología) |
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The effect of barium on calcite {101¯4} surfaces during growthAstilleros García-Monge, José ManuelPina Martínez, Carlos ManuelFernández Díaz, María LourdesPutnis, Andrew548.5Crystal growthCalciteBariumCristalografía (Geología)In situ atomic force microscopy (AFM) experiments have provided information about the effect of Ba21 on crystal growth of calcite {101¯4} surfaces. The microtopographic features observed have been interpreted by considering both the structural control that the calcite surfaces exert on the incorporation of divalent cations and the supersaturation state of the solution used. Pinning of the calcite growth steps occurs at low Ba concentrations, suggesting specific sites for Ba incorporation. When the Ba content of the solution is increased the advancement of monomolecular steps is observed. Although [4¯41]1 and [481¯]1 steps advance showing characteristic jagged edges, the parallel steps (i.e., [4¯41]2 and [481¯]2) remain practically immobile. This fact can be explained by considering the nonsymmetrically related distribution of large and small sites along the calcite steps and the easier incorporation of barium on the former. The measured increase in the height of the newly grown steps is also consistent with such preferential incorporation of Ba in certain positions. A further increase in the Ba concentration of the solutions leads to the formation of bidimensional nuclei on the calcite {101¯4} surfaces. The nature of these nuclei is discussed taking into account the supersaturation of the solution with respect to two possible structures that can accommodate Ba: the calcite-type structure and the aragonite-type structure.Elsevier Science LtdUniversidad Complutense de Madrid20002000-01-0120002000-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttps://hdl.handle.net/20.500.14352/57133reponame:Docta Complutenseinstname:Universidad Complutense de Madrid (UCM)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2info:eu-repo/semantics/openAccessoai:docta.ucm.es:20.500.14352/571332026-06-02T12:44:21Z |
| dc.title.none.fl_str_mv |
The effect of barium on calcite {101¯4} surfaces during growth |
| title |
The effect of barium on calcite {101¯4} surfaces during growth |
| spellingShingle |
The effect of barium on calcite {101¯4} surfaces during growth Astilleros García-Monge, José Manuel 548.5 Crystal growth Calcite Barium Cristalografía (Geología) |
| title_short |
The effect of barium on calcite {101¯4} surfaces during growth |
| title_full |
The effect of barium on calcite {101¯4} surfaces during growth |
| title_fullStr |
The effect of barium on calcite {101¯4} surfaces during growth |
| title_full_unstemmed |
The effect of barium on calcite {101¯4} surfaces during growth |
| title_sort |
The effect of barium on calcite {101¯4} surfaces during growth |
| dc.creator.none.fl_str_mv |
Astilleros García-Monge, José Manuel Pina Martínez, Carlos Manuel Fernández Díaz, María Lourdes Putnis, Andrew |
| author |
Astilleros García-Monge, José Manuel |
| author_facet |
Astilleros García-Monge, José Manuel Pina Martínez, Carlos Manuel Fernández Díaz, María Lourdes Putnis, Andrew |
| author_role |
author |
| author2 |
Pina Martínez, Carlos Manuel Fernández Díaz, María Lourdes Putnis, Andrew |
| author2_role |
author author author |
| dc.contributor.none.fl_str_mv |
Universidad Complutense de Madrid |
| dc.subject.none.fl_str_mv |
548.5 Crystal growth Calcite Barium Cristalografía (Geología) |
| topic |
548.5 Crystal growth Calcite Barium Cristalografía (Geología) |
| description |
In situ atomic force microscopy (AFM) experiments have provided information about the effect of Ba21 on crystal growth of calcite {101¯4} surfaces. The microtopographic features observed have been interpreted by considering both the structural control that the calcite surfaces exert on the incorporation of divalent cations and the supersaturation state of the solution used. Pinning of the calcite growth steps occurs at low Ba concentrations, suggesting specific sites for Ba incorporation. When the Ba content of the solution is increased the advancement of monomolecular steps is observed. Although [4¯41]1 and [481¯]1 steps advance showing characteristic jagged edges, the parallel steps (i.e., [4¯41]2 and [481¯]2) remain practically immobile. This fact can be explained by considering the nonsymmetrically related distribution of large and small sites along the calcite steps and the easier incorporation of barium on the former. The measured increase in the height of the newly grown steps is also consistent with such preferential incorporation of Ba in certain positions. A further increase in the Ba concentration of the solutions leads to the formation of bidimensional nuclei on the calcite {101¯4} surfaces. The nature of these nuclei is discussed taking into account the supersaturation of the solution with respect to two possible structures that can accommodate Ba: the calcite-type structure and the aragonite-type structure. |
| publishDate |
2000 |
| dc.date.none.fl_str_mv |
2000 2000-01-01 2000 2000-01-01 |
| dc.type.none.fl_str_mv |
journal article http://purl.org/coar/resource_type/c_6501 |
| dc.type.openaire.fl_str_mv |
info:eu-repo/semantics/article |
| format |
article |
| dc.identifier.none.fl_str_mv |
https://hdl.handle.net/20.500.14352/57133 |
| url |
https://hdl.handle.net/20.500.14352/57133 |
| dc.language.none.fl_str_mv |
Inglés eng |
| language_invalid_str_mv |
Inglés |
| language |
eng |
| dc.rights.none.fl_str_mv |
open access http://purl.org/coar/access_right/c_abf2 |
| dc.rights.openaire.fl_str_mv |
info:eu-repo/semantics/openAccess |
| rights_invalid_str_mv |
open access http://purl.org/coar/access_right/c_abf2 |
| eu_rights_str_mv |
openAccess |
| dc.format.none.fl_str_mv |
application/pdf |
| dc.publisher.none.fl_str_mv |
Elsevier Science Ltd |
| publisher.none.fl_str_mv |
Elsevier Science Ltd |
| dc.source.none.fl_str_mv |
reponame:Docta Complutense instname:Universidad Complutense de Madrid (UCM) |
| instname_str |
Universidad Complutense de Madrid (UCM) |
| reponame_str |
Docta Complutense |
| collection |
Docta Complutense |
| repository.name.fl_str_mv |
|
| repository.mail.fl_str_mv |
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| _version_ |
1869423109368446976 |
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15,300719 |