Study of the calcination process of two limonitic iron ores between 250 °C and 950 °C
The dehydration process of two limonitic ores from Venezuela was studied between 250 °C and 950 °C by means of thermogravimetry, infrared spectroscopy, and x-ray diffraction. These techniques indicated for both minerals that the goethite-to-hematite transformation occurred in the range of 250-350 °C...
- Autores:
- Tipo de recurso:
- Fecha de publicación:
- 2017
- Institución:
- Universidad Pedagógica y Tecnológica de Colombia
- Repositorio:
- RiUPTC: Repositorio Institucional UPTC
- Idioma:
- eng
- OAI Identifier:
- oai:repositorio.uptc.edu.co:001/14176
- Acceso en línea:
- https://revistas.uptc.edu.co/index.php/ingenieria/article/view/6053
https://repositorio.uptc.edu.co/handle/001/14176
- Palabra clave:
- Iron Ore
Limonite
Thermal Modification of Minerals
Limonita
Mineral de hierro
Modificación térmica de minerales
- Rights
- License
- http://purl.org/coar/access_right/c_abf379
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2017-05-022024-07-05T19:11:32Z2024-07-05T19:11:32Zhttps://revistas.uptc.edu.co/index.php/ingenieria/article/view/605310.19053/01211129.v26.n45.2017.6053https://repositorio.uptc.edu.co/handle/001/14176The dehydration process of two limonitic ores from Venezuela was studied between 250 °C and 950 °C by means of thermogravimetry, infrared spectroscopy, and x-ray diffraction. These techniques indicated for both minerals that the goethite-to-hematite transformation occurred in the range of 250-350 °C. In addition, the x-ray diffraction showed a structural re-arrangement within the orebody above 350 °C, temperature above which only the hematite structure is recognizable. Finally, infrared spectroscopy revealed that such transformation implies the loss of structural OH- functional groups, characteristic of the limonite.Se estudió el proceso de deshidratación de dos minerales limoníticos de Venezuela entre 250 °C y 950 °C, usando termogravimetría, espectroscopia infrarroja y difracción de rayos x. Para ambos materiales, estas técnicas indicaron que la transformación de goethita a hematita ocurrió en el rango de 250 °C a 350 °C. Adicionalmente, la difracción de rayos X mostró un rearreglo estructural dentro del yacimiento mineral a una temperatura por encima de 350 °C; a temperaturas mayores, solo se reconoce la estructura de la hematita. Finalmente, la espectroscopia infrarroja reveló que la transformación de goethita a hematita implica la pérdida de grupos funcionales de OH- estructural característicos de la limonita.application/pdfapplication/xmlengengUniversidad Pedagógica y Tecnológica de Colombiahttps://revistas.uptc.edu.co/index.php/ingenieria/article/view/6053/5584https://revistas.uptc.edu.co/index.php/ingenieria/article/view/6053/6405Revista Facultad de Ingeniería; Vol. 26 No. 45 (2017); 33-45Revista Facultad de Ingeniería; Vol. 26 Núm. 45 (2017); 33-452357-53280121-1129Iron OreLimoniteThermal Modification of MineralsLimonitaMineral de hierroModificación térmica de mineralesStudy of the calcination process of two limonitic iron ores between 250 °C and 950 °CEstudio del proceso de calcinación en dos minerales de hierro limoníticos entre 250 °C y 950 °Cinvestigationinvestigacióninfo:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_2df8fbb1info:eu-repo/semantics/publishedVersionhttp://purl.org/coar/version/c_970fb48d4fbd8a462http://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/access_right/c_abf379http://purl.org/coar/access_right/c_abf2Longa-Avello, LisbethPereyra-Zerpa, CristinaCasal-Ramos, Julio AndrésDelvasto, Pedro001/14176oai:repositorio.uptc.edu.co:001/141762025-07-18 11:53:51.395metadata.onlyhttps://repositorio.uptc.edu.coRepositorio Institucional UPTCrepositorio.uptc@uptc.edu.co |
dc.title.en-US.fl_str_mv |
Study of the calcination process of two limonitic iron ores between 250 °C and 950 °C |
dc.title.es-ES.fl_str_mv |
Estudio del proceso de calcinación en dos minerales de hierro limoníticos entre 250 °C y 950 °C |
title |
Study of the calcination process of two limonitic iron ores between 250 °C and 950 °C |
spellingShingle |
Study of the calcination process of two limonitic iron ores between 250 °C and 950 °C Iron Ore Limonite Thermal Modification of Minerals Limonita Mineral de hierro Modificación térmica de minerales |
title_short |
Study of the calcination process of two limonitic iron ores between 250 °C and 950 °C |
title_full |
Study of the calcination process of two limonitic iron ores between 250 °C and 950 °C |
title_fullStr |
Study of the calcination process of two limonitic iron ores between 250 °C and 950 °C |
title_full_unstemmed |
Study of the calcination process of two limonitic iron ores between 250 °C and 950 °C |
title_sort |
Study of the calcination process of two limonitic iron ores between 250 °C and 950 °C |
dc.subject.en-US.fl_str_mv |
Iron Ore Limonite Thermal Modification of Minerals |
topic |
Iron Ore Limonite Thermal Modification of Minerals Limonita Mineral de hierro Modificación térmica de minerales |
dc.subject.es-ES.fl_str_mv |
Limonita Mineral de hierro Modificación térmica de minerales |
description |
The dehydration process of two limonitic ores from Venezuela was studied between 250 °C and 950 °C by means of thermogravimetry, infrared spectroscopy, and x-ray diffraction. These techniques indicated for both minerals that the goethite-to-hematite transformation occurred in the range of 250-350 °C. In addition, the x-ray diffraction showed a structural re-arrangement within the orebody above 350 °C, temperature above which only the hematite structure is recognizable. Finally, infrared spectroscopy revealed that such transformation implies the loss of structural OH- functional groups, characteristic of the limonite. |
publishDate |
2017 |
dc.date.accessioned.none.fl_str_mv |
2024-07-05T19:11:32Z |
dc.date.available.none.fl_str_mv |
2024-07-05T19:11:32Z |
dc.date.none.fl_str_mv |
2017-05-02 |
dc.type.en-US.fl_str_mv |
investigation |
dc.type.es-ES.fl_str_mv |
investigación |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article |
dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_2df8fbb1 |
dc.type.coarversion.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
dc.type.version.spa.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.coarversion.spa.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a462 |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
https://revistas.uptc.edu.co/index.php/ingenieria/article/view/6053 10.19053/01211129.v26.n45.2017.6053 |
dc.identifier.uri.none.fl_str_mv |
https://repositorio.uptc.edu.co/handle/001/14176 |
url |
https://revistas.uptc.edu.co/index.php/ingenieria/article/view/6053 https://repositorio.uptc.edu.co/handle/001/14176 |
identifier_str_mv |
10.19053/01211129.v26.n45.2017.6053 |
dc.language.none.fl_str_mv |
eng |
dc.language.iso.spa.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
https://revistas.uptc.edu.co/index.php/ingenieria/article/view/6053/5584 https://revistas.uptc.edu.co/index.php/ingenieria/article/view/6053/6405 |
dc.rights.coar.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
dc.rights.coar.spa.fl_str_mv |
http://purl.org/coar/access_right/c_abf379 |
rights_invalid_str_mv |
http://purl.org/coar/access_right/c_abf379 http://purl.org/coar/access_right/c_abf2 |
dc.format.none.fl_str_mv |
application/pdf application/xml |
dc.publisher.en-US.fl_str_mv |
Universidad Pedagógica y Tecnológica de Colombia |
dc.source.en-US.fl_str_mv |
Revista Facultad de Ingeniería; Vol. 26 No. 45 (2017); 33-45 |
dc.source.es-ES.fl_str_mv |
Revista Facultad de Ingeniería; Vol. 26 Núm. 45 (2017); 33-45 |
dc.source.none.fl_str_mv |
2357-5328 0121-1129 |
institution |
Universidad Pedagógica y Tecnológica de Colombia |
repository.name.fl_str_mv |
Repositorio Institucional UPTC |
repository.mail.fl_str_mv |
repositorio.uptc@uptc.edu.co |
_version_ |
1839633886430101504 |