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Hydrogeochemistry in the Merida, Yucatan, (Mexico) groundwater: An analysis of major and trace elements [Hidrogeoquimica en el acuifero calcareo de Merida, Yucatan: Elementos traza]
volume: 14
most specific type: Article
related by: authorship 3684
freetext keyword: Aquifers; Calcite; Dissolution; Dolomite; Evaporates; Groundwater; Hydrogeochemistry; Merida; Trace elements aquifer; hydrogeochemistry; salinity; water-rock interaction
type: Generically Dependent Continuant
issue: 3
related by: authorship 3683
type: Thing
date time value: article date 754
page start: 19
type: Continuant
abstract: An analysis of major and trace elements (Fe(total), B, F-, Sr 2, Ba 2, I-, Br-) in the groundwater of the Merida (Yucatan, Mexico) aquifer was carried out. Water-rock interaction was leaned on trace elements and permitted to define major hydrogeochemical processes. Dissolved species were postulated to belong to three different sources: atmospheric water, seawater; a third major source was seawater that has reacted with the aquifer matrix. Dissolved oxygen concentrations controls Fetotal in the studied groundwater. The tendency of most of the analysed elements appearance shows that the saline end corresponds to marine water different to the current marine water, therefore the mixture is not caused by a process of saline intrusion as it has generally been supposed in the Peninsula. But rather the salted water that is in the underground is the one possibly caught during the immersions that it has suffered the Peninsula. Ca 2 and Mg 2 solubility controls permitted an understanding of carbonate geochemistry and the mixing processes between fresh and saline water.
related by: authorship 3685
estado: published
most specific type: Document
type: Entity
has publication venue: Ingenieria Hidraulica en Mexico
origen: scopus
abstract: An analysis of major and trace elements (Fe(total), B, F-, Sr%2b2, Ba%2b2, I-, Br-) in the groundwater of the Merida (Yucatan, Mexico) aquifer was carried out. Water-rock interaction was leaned on trace elements and permitted to define major hydrogeochemical processes. Dissolved species were postulated to belong to three different sources: atmospheric water, seawater; a third major source was seawater that has reacted with the aquifer matrix. Dissolved oxygen concentrations controls Fetotal in the studied groundwater. The tendency of most of the analysed elements appearance shows that the saline end corresponds to marine water different to the current marine water, therefore the mixture is not caused by a process of saline intrusion as it has generally been supposed in the Peninsula. But rather the salted water that is in the underground is the one possibly caught during the immersions that it has suffered the Peninsula. Ca%2b2 and Mg%2b2 solubility controls permitted an understanding of carbonate geochemistry and the mixing processes between fresh and saline water.
type: Information Content Entity
type: Document
type: Article
crisid: 754
page end: 28
e iscopus: 2-s2.0-0033368622

Ingenieria Hidraulica en Mexico
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type: Document
type: Periodical
type: Generically Dependent Continuant
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publication venue for: Hydrogeochemistry in the Merida, Yucatan, (Mexico) groundwater: An analysis of major and trace elements [Hidrogeoquimica en el acuifero calcareo de Merida, Yucatan: Elementos traza]
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date: 2026-08-26T23:50:38
publisher: vivo
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label: RDF description of Hydrogeochemistry in the Merida, Yucatan, (Mexico) groundwater: An analysis of major and trace elements [Hidrogeoquimica en el acuifero calcareo de Merida, Yucatan: Elementos traza] - http://orbis.uaslp.mx/vivo/individual/scopus753

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