Document
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Ingenieria Hidraulica en Mexico
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type: Document
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type: Generically Dependent Continuant
type: Continuant
type: Thing
publication venue for: scopus1610
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type: Information Content Entity
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Continuant
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Entity
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Generically Dependent Continuant
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individual
rights: termsOfUse
date: 2026-08-26T23:50:02
publisher: vivo
type: Document
label: RDF description of Hydrochemistry of intermediate flow systems associated with basin fill sediments derived from rhyolitic rocks [Hidrogeoquímica de sistemas de flujo intermedio que circulan por sedimentos continentales derivados de rocas riolíticas] - http://orbis.uaslp.mx/vivo/individual/scopus1610

Article
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Information Content Entity
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scopus1610
issue: 3
type: Entity
origen: scopus
related by: authorship 9710
volume: 21
type: Information Content Entity
e iscopus: 2-s2.0-33749672050
estado: published
type: Generically Dependent Continuant
date time value: article date 1611
label: Hydrochemistry of intermediate flow systems associated with basin fill sediments derived from rhyolitic rocks [Hidrogeoquímica de sistemas de flujo intermedio que circulan por sedimentos continentales derivados de rocas riolíticas]
type: Continuant
has publication venue: Ingenieria Hidraulica en Mexico
related by: authorship 9711
type: Document
abstract: An analysis of the reactions that characterize the chemical composition of an intermediate groundwater flow system was carried out. This system travels through basin fill sediments in a graven structure in central Mexico. Water-rock interaction in volcanic regions is usually related with the dissolution of primary minerals or of the glassy matrix of the rock. However, obtained geochemical calculations suggest that the water quality may be conditioned by the reactions with clayey minerals produced by the alteration of the volcanic rocks. Identified reactions include: a) incongruent montmorillonite and illite dissolution leaving kaolinite as a insoluble residue, b) exchange of sodium in clay minerals for calcium present in the groundwater, and c) calcite dissolution. A quantitative approximation was made through both inverse geochemical modeling and mass balance computations, which considered the established expected theoretical reactions. Additionally, laboratory experiments were carried out with rain water and basin fill sediments; the reactions identified in the laboratory through the analytical results agreed with those postulated for field conditions.
page start: 69
type: Article
freetext keyword: Arid zone; Graven structure; Hydrochemistry; Incongruent dissolution; Intermediate groundwater flow system; Inverse geochemical modeling; San Luis Potosi water-rock laboratory experiments Hydrochemistry; Illite; Montmorillonite; Rhyolitic rocks; Water-rock interaction; Calcite; Catchments; Clay minerals; Dissolution; Flow interactions; Groundwater geochemistry; Sediments; Volcanic rocks; Groundwater flow; Calcite; Catchments; Clay minerals; Dissolution; Flow interactions; Groundwater flow; Groundwater geochemistry; Sediments; Volcanic rocks; chemical composition; dissolution; groundwater flow; hydrochemistry; water quality; water-rock interaction
type: Thing
most specific type: Article
page end: 86
crisid: 1611
most specific type: Document