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...

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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
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Derechos de autor 2008 Ingeniería Investigación y Desarrollo
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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
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