Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, Argentina

Autores
Miretzky, Patricia; Conzonno, Victor Hugo; Fernandez Cirelli, Alicia
Año de publicación
2001
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Chemical analyses of dissolved silica in the shallow groundwater of the lower part of the Salado River drainage basin indicate that silica values averaged 60 ppm. The groundwaters are oversaturated in relation to quartz, Na-plagioclase, K-feldspar, and the weathering of quartz and aluminosilicates appear to have little control on silica concentrations in solution. Groundwater is undersaturated with respect to amorphous silica present in the loessic sediments, and these sediments are specially important in the control of the groundwater composition. The sources of amorphous silica are volcanic glass shards and biogenic silica derived from plant (silicophytoliths, diatom frustules) or animal remains (sponge spicules) also present in the Pampean loess. Silicophytoliths and diatoms have also been reported in A soil horizon samples. The dissolution of amorphous silica most likely controls the high dissolved silica concentrations in groundwater.
Fil: Miretzky, Patricia. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina
Fil: Conzonno, Victor Hugo. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Química Orgánica; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Fernandez Cirelli, Alicia. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Química Orgánica; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Materia
GROUNDWATER DISSOLVED SILICA CONCENTRATION
SALADO RIVER DRAINAGE BASIN
SILICA SOLUBILITY
WEATHERING OF SILICATE MINERALS
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/149727
Acceder
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repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, ArgentinaMiretzky, PatriciaConzonno, Victor HugoFernandez Cirelli, AliciaGROUNDWATER DISSOLVED SILICA CONCENTRATIONSALADO RIVER DRAINAGE BASINSILICA SOLUBILITYWEATHERING OF SILICATE MINERALShttps://purl.org/becyt/ford/1.4https://purl.org/becyt/ford/1Chemical analyses of dissolved silica in the shallow groundwater of the lower part of the Salado River drainage basin indicate that silica values averaged 60 ppm. The groundwaters are oversaturated in relation to quartz, Na-plagioclase, K-feldspar, and the weathering of quartz and aluminosilicates appear to have little control on silica concentrations in solution. Groundwater is undersaturated with respect to amorphous silica present in the loessic sediments, and these sediments are specially important in the control of the groundwater composition. The sources of amorphous silica are volcanic glass shards and biogenic silica derived from plant (silicophytoliths, diatom frustules) or animal remains (sponge spicules) also present in the Pampean loess. Silicophytoliths and diatoms have also been reported in A soil horizon samples. The dissolution of amorphous silica most likely controls the high dissolved silica concentrations in groundwater.Fil: Miretzky, Patricia. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; ArgentinaFil: Conzonno, Victor Hugo. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Química Orgánica; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Fernandez Cirelli, Alicia. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Química Orgánica; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaElsevier Science2001-11info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/149727Miretzky, Patricia; Conzonno, Victor Hugo; Fernandez Cirelli, Alicia; Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, Argentina; Elsevier Science; Journal of Geochemical Exploration; 73; 3; 11-2001; 155-1660375-67421879-1689CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0375674201001947info:eu-repo/semantics/altIdentifier/doi/10.1016/S0375-6742(01)00194-7info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:06:39Zoai:ri.conicet.gov.ar:11336/149727instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:06:39.624CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, Argentina
title Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, Argentina
spellingShingle Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, Argentina
Miretzky, Patricia
GROUNDWATER DISSOLVED SILICA CONCENTRATION
SALADO RIVER DRAINAGE BASIN
SILICA SOLUBILITY
WEATHERING OF SILICATE MINERALS
title_short Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, Argentina
title_full Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, Argentina
title_fullStr Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, Argentina
title_full_unstemmed Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, Argentina
title_sort Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, Argentina
dc.creator.none.fl_str_mv Miretzky, Patricia
Conzonno, Victor Hugo
Fernandez Cirelli, Alicia
author Miretzky, Patricia
author_facet Miretzky, Patricia
Conzonno, Victor Hugo
Fernandez Cirelli, Alicia
author_role author
author2 Conzonno, Victor Hugo
Fernandez Cirelli, Alicia
author2_role author
author
dc.subject.none.fl_str_mv GROUNDWATER DISSOLVED SILICA CONCENTRATION
SALADO RIVER DRAINAGE BASIN
SILICA SOLUBILITY
WEATHERING OF SILICATE MINERALS
topic GROUNDWATER DISSOLVED SILICA CONCENTRATION
SALADO RIVER DRAINAGE BASIN
SILICA SOLUBILITY
WEATHERING OF SILICATE MINERALS
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.4
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Chemical analyses of dissolved silica in the shallow groundwater of the lower part of the Salado River drainage basin indicate that silica values averaged 60 ppm. The groundwaters are oversaturated in relation to quartz, Na-plagioclase, K-feldspar, and the weathering of quartz and aluminosilicates appear to have little control on silica concentrations in solution. Groundwater is undersaturated with respect to amorphous silica present in the loessic sediments, and these sediments are specially important in the control of the groundwater composition. The sources of amorphous silica are volcanic glass shards and biogenic silica derived from plant (silicophytoliths, diatom frustules) or animal remains (sponge spicules) also present in the Pampean loess. Silicophytoliths and diatoms have also been reported in A soil horizon samples. The dissolution of amorphous silica most likely controls the high dissolved silica concentrations in groundwater.
Fil: Miretzky, Patricia. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina
Fil: Conzonno, Victor Hugo. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Química Orgánica; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Fernandez Cirelli, Alicia. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Química Orgánica; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
description Chemical analyses of dissolved silica in the shallow groundwater of the lower part of the Salado River drainage basin indicate that silica values averaged 60 ppm. The groundwaters are oversaturated in relation to quartz, Na-plagioclase, K-feldspar, and the weathering of quartz and aluminosilicates appear to have little control on silica concentrations in solution. Groundwater is undersaturated with respect to amorphous silica present in the loessic sediments, and these sediments are specially important in the control of the groundwater composition. The sources of amorphous silica are volcanic glass shards and biogenic silica derived from plant (silicophytoliths, diatom frustules) or animal remains (sponge spicules) also present in the Pampean loess. Silicophytoliths and diatoms have also been reported in A soil horizon samples. The dissolution of amorphous silica most likely controls the high dissolved silica concentrations in groundwater.
publishDate 2001
dc.date.none.fl_str_mv 2001-11
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/149727
Miretzky, Patricia; Conzonno, Victor Hugo; Fernandez Cirelli, Alicia; Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, Argentina; Elsevier Science; Journal of Geochemical Exploration; 73; 3; 11-2001; 155-166
0375-6742
1879-1689
CONICET Digital
CONICET
url http://hdl.handle.net/11336/149727
identifier_str_mv Miretzky, Patricia; Conzonno, Victor Hugo; Fernandez Cirelli, Alicia; Geochemical processes controlling silica concentrations in groundwaters of the Salado River drainage basin, Argentina; Elsevier Science; Journal of Geochemical Exploration; 73; 3; 11-2001; 155-166
0375-6742
1879-1689
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0375674201001947
info:eu-repo/semantics/altIdentifier/doi/10.1016/S0375-6742(01)00194-7
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Elsevier Science
publisher.none.fl_str_mv Elsevier Science
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.070432

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