Compounds of neutralization (Mg²+ Y Ca²+)associated with the atmopheric deposition (wet-only and dry only)
Ths estudy was realized in a rural zone (Andorra Teruel) the NE of Spain, where I determine the contributing (marine/continental) relation of the compounds of neutralization (Mg²+ Y Ca²+), that accompany the atmospheric deposition dry and humid in separated form. The analysis of the results revea...
- Autores:
- Tipo de recurso:
- http://purl.org/coar/resource_type/c_6780
- Fecha de publicación:
- 2008
- Institución:
- Universidad Pedagógica y Tecnológica de Colombia
- Repositorio:
- RiUPTC: Repositorio Institucional UPTC
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.uptc.edu.co:001/12144
- Acceso en línea:
- https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/868
https://repositorio.uptc.edu.co/handle/001/12144
- Palabra clave:
- atmospheric dry deposition
marine ratio
Na /Cl-
agents of neutralizatin
marine origin
deposición atmosférica seca
ratio marino
Na /Cl-
agentes de neutralización
origen marino
- Rights
- License
- Derechos de autor 2008 Ingeniería Investigación y Desarrollo
id |
REPOUPTC2_0766022b79a8694bb9d18a9cfb569bfa |
---|---|
oai_identifier_str |
oai:repositorio.uptc.edu.co:001/12144 |
network_acronym_str |
REPOUPTC2 |
network_name_str |
RiUPTC: Repositorio Institucional UPTC |
repository_id_str |
|
spelling |
2008-07-022024-07-05T18:47:36Z2024-07-05T18:47:36Zhttps://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/868https://repositorio.uptc.edu.co/handle/001/12144Ths estudy was realized in a rural zone (Andorra Teruel) the NE of Spain, where I determine the contributing (marine/continental) relation of the compounds of neutralization (Mg²+ Y Ca²+), that accompany the atmospheric deposition dry and humid in separated form. The analysis of the results revealed a similarity of the ratio Mg²+ / Ca²+ between the wet and dry events; different case happened with the relation Mg²+/ Cl- where the wet deposition showed major extraction of chlorides (20%) that the athmospheric dry deposition, owed possibly to the solubility of his you sales. It is necessary to highlight that in our case, the nitric acid was neutralized by the NH3 in the wet deposition, and in provide lightly top for calcic carbonate proceeding from the particles terrígenas. These cconclusions arew similar to the obtained ones for Pakkanen, (1996) and Harrison and Kito (1990). Also it observe the Ca² as the major agent of neutralization of the nitric acid (dry depositon) and that interaction Na+ - HNO3 is not probale in the wet deposition. Este estudio se realizó en una zona rural (Andorra Teruel) al NE de España, donde se determinó la relación contributiva (marina/continental) de los compuestos de neutralización (Mg y Ca ) que acompañan la deposición atmosférica seca y húmeda en forma separada. El análisis de los resultados reveló una similitud del ratio Mg /Ca entre los eventos húmedos y secos, caso diferente ocurrió con la relación Mg /Cl donde la deposición húmeda mostró mayor extracción de cloruros (20%) que la deposición atmosférica seca, debido posiblemente a la solubilidad de sus sales.Se debe resaltar que en nuestro caso, el ácido nítrico fue neutralizado por el NH en la deposición húmeda, y en proporciones ligeramente superiores por carbonato cálcico procedente de las partículas terrígenas. Estas conclusionesson similares a las obtenidas por Pakkanen, (1996) y Harrison y Kito (1990). También se observó el Ca como el mayor agente de neutralización del ácido nítrico (deposición seca) y que la interacción de Na - HNO no es probable en la deposición húmeda.application/pdfspaspaUniversidad Pedagógica y Tecnológica de Colombia - UPTChttps://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/868/867Derechos de autor 2008 Ingeniería Investigación y Desarrollohttp://purl.org/coar/access_right/c_abf281http://purl.org/coar/access_right/c_abf2Ingeniería Investigación y Desarrollo; Vol. 6 No. 1: enero-junio de 2008; 12-17Ingeniería Investigación y Desarrollo; Vol. 6 Núm. 1: enero-junio de 2008; 12-172422-43241900-771Xatmospheric dry depositionmarine ratioNa /Cl-agents of neutralizatinmarine origindeposición atmosférica secaratio marinoNa /Cl-agentes de neutralizaciónorigen marinoCompounds of neutralization (Mg²+ Y Ca²+)associated with the atmopheric deposition (wet-only and dry only)Compuestos de neutralización (Mg²+ y Ca²+), asociados a la deposición atmosférica (wet-only y dry only)info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6780http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a364http://purl.org/coar/version/c_970fb48d4fbd8a85Chaves-Romero, Aura Leticia001/12144oai:repositorio.uptc.edu.co:001/121442025-07-18 11:25:54.321metadata.onlyhttps://repositorio.uptc.edu.coRepositorio Institucional UPTCrepositorio.uptc@uptc.edu.co |
dc.title.en-US.fl_str_mv |
Compounds of neutralization (Mg²+ Y Ca²+)associated with the atmopheric deposition (wet-only and dry only) |
dc.title.es-ES.fl_str_mv |
Compuestos de neutralización (Mg²+ y Ca²+), asociados a la deposición atmosférica (wet-only y dry only) |
title |
Compounds of neutralization (Mg²+ Y Ca²+)associated with the atmopheric deposition (wet-only and dry only) |
spellingShingle |
Compounds of neutralization (Mg²+ Y Ca²+)associated with the atmopheric deposition (wet-only and dry only) atmospheric dry deposition marine ratio Na /Cl- agents of neutralizatin marine origin deposición atmosférica seca ratio marino Na /Cl- agentes de neutralización origen marino |
title_short |
Compounds of neutralization (Mg²+ Y Ca²+)associated with the atmopheric deposition (wet-only and dry only) |
title_full |
Compounds of neutralization (Mg²+ Y Ca²+)associated with the atmopheric deposition (wet-only and dry only) |
title_fullStr |
Compounds of neutralization (Mg²+ Y Ca²+)associated with the atmopheric deposition (wet-only and dry only) |
title_full_unstemmed |
Compounds of neutralization (Mg²+ Y Ca²+)associated with the atmopheric deposition (wet-only and dry only) |
title_sort |
Compounds of neutralization (Mg²+ Y Ca²+)associated with the atmopheric deposition (wet-only and dry only) |
dc.subject.en-US.fl_str_mv |
atmospheric dry deposition marine ratio Na /Cl- agents of neutralizatin marine origin |
topic |
atmospheric dry deposition marine ratio Na /Cl- agents of neutralizatin marine origin deposición atmosférica seca ratio marino Na /Cl- agentes de neutralización origen marino |
dc.subject.es-ES.fl_str_mv |
deposición atmosférica seca ratio marino Na /Cl- agentes de neutralización origen marino |
description |
Ths estudy was realized in a rural zone (Andorra Teruel) the NE of Spain, where I determine the contributing (marine/continental) relation of the compounds of neutralization (Mg²+ Y Ca²+), that accompany the atmospheric deposition dry and humid in separated form. The analysis of the results revealed a similarity of the ratio Mg²+ / Ca²+ between the wet and dry events; different case happened with the relation Mg²+/ Cl- where the wet deposition showed major extraction of chlorides (20%) that the athmospheric dry deposition, owed possibly to the solubility of his you sales. It is necessary to highlight that in our case, the nitric acid was neutralized by the NH3 in the wet deposition, and in provide lightly top for calcic carbonate proceeding from the particles terrígenas. These cconclusions arew similar to the obtained ones for Pakkanen, (1996) and Harrison and Kito (1990). Also it observe the Ca² as the major agent of neutralization of the nitric acid (dry depositon) and that interaction Na+ - HNO3 is not probale in the wet deposition. |
publishDate |
2008 |
dc.date.accessioned.none.fl_str_mv |
2024-07-05T18:47:36Z |
dc.date.available.none.fl_str_mv |
2024-07-05T18:47:36Z |
dc.date.none.fl_str_mv |
2008-07-02 |
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.coar.spa.fl_str_mv |
http://purl.org/coar/resource_type/c_6780 |
dc.type.coarversion.spa.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a364 |
format |
http://purl.org/coar/resource_type/c_6780 |
dc.identifier.none.fl_str_mv |
https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/868 |
dc.identifier.uri.none.fl_str_mv |
https://repositorio.uptc.edu.co/handle/001/12144 |
url |
https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/868 https://repositorio.uptc.edu.co/handle/001/12144 |
dc.language.none.fl_str_mv |
spa |
dc.language.iso.none.fl_str_mv |
spa |
language |
spa |
dc.relation.none.fl_str_mv |
https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/868/867 |
dc.rights.es-ES.fl_str_mv |
Derechos de autor 2008 Ingeniería Investigación y Desarrollo |
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_abf281 |
rights_invalid_str_mv |
Derechos de autor 2008 Ingeniería Investigación y Desarrollo http://purl.org/coar/access_right/c_abf281 http://purl.org/coar/access_right/c_abf2 |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.es-ES.fl_str_mv |
Universidad Pedagógica y Tecnológica de Colombia - UPTC |
dc.source.en-US.fl_str_mv |
Ingeniería Investigación y Desarrollo; Vol. 6 No. 1: enero-junio de 2008; 12-17 |
dc.source.es-ES.fl_str_mv |
Ingeniería Investigación y Desarrollo; Vol. 6 Núm. 1: enero-junio de 2008; 12-17 |
dc.source.none.fl_str_mv |
2422-4324 1900-771X |
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_ |
1839633895992066048 |