British Council
type: Relationship
type: BFO_0000020
type: Entity
type: Thing
type: Grant
type: Continuant
funding vehicle for: Use of abstraction regime and knowledge of hydrogeological conditions to control high-fluoride concentration in abstracted groundwater: San Luis Potosí Basin, Mexico

Document
type: Class

Journal of Hydrology
type: Thing
type: Journal
type: Entity
type: Document
type: Continuant
type: Generically Dependent Continuant
type: Periodical
type: Collection
type: Information Content Entity
publication venue for: Use of abstraction regime and knowledge of hydrogeological conditions to control high-fluoride concentration in abstracted groundwater: San Luis Potosí Basin, Mexico

Continuant
type: Class

Entity
type: Class

Generically Dependent Continuant
type: Class

individual
rights: termsOfUse
date: 2026-08-26T23:50:04
publisher: vivo
type: Document
label: RDF description of Use of abstraction regime and knowledge of hydrogeological conditions to control high-fluoride concentration in abstracted groundwater: San Luis Potosí Basin, Mexico - http://orbis.uaslp.mx/vivo/individual/scopus1144

Article
type: Class

Use of abstraction regime and knowledge of hydrogeological conditions to control high-fluoride concentration in abstracted groundwater: San Luis Potosí Basin, Mexico
estado: published
type: Continuant
origen: scopus
has publication venue: Journal of Hydrology
accesstype: All Open Access, Green
type: Entity
freetext keyword: Fluoride; Groundwater; Hydrogeochemistry; Mexico; Water-rock interaction Boreholes; Fluoride minerals; Hydrogeology; Lithology; Abstraction regimes; Groundwater; borehole; fluoride; groundwater abstraction; hydrogeology; water-rock interaction; Mexico
related by: authorship 6731
most specific type: Document
volume: 261
type: Thing
abstract: Significant amounts of fluoride are found in the abstracted groundwater of San Luis Potosí. This groundwater withdrawal induces a cold, low-fluoride flow as well as deeper thermal fluoride-rich flow in various proportions. Flow mixing takes place depending on the abstraction regime, local hydrogeology, and borehole construction design and operation. Fluoride concentrations (≈ 3.7 mg l-1) could become higher still, in time and space, if the input of regional fluoride-rich water to the abstraction boreholes is enhanced. It is suggested that by controlling the abstraction well-head water temperature at 28-30°C, a pumped water mixture with a fluoride content close to the maximum drinking water standard of 1.5 mg l-1 will be produced. Further, new boreholes and those already operating could take advantage of fluoride solubility controls to reduce the F concentration in the abstracted water by considering lithology and borehole construction design in order to regulate groundwater flow conditions. © 2002 Elsevier Science B.V. All rights reserved.
type: Information Content Entity
issue: 1-4
related by: authorship 6732
date time value: article date 1145
related by: authorship 6733
has funding vehicle: British Council
crisid: 1145
e iscopus: 2-s2.0-0037090125
most specific type: Article
type: Generically Dependent Continuant
doi: 10.1016/S0022-1694(01)00566-2
type: Document
page start: 24
type: Article
page end: 47

Information Content Entity
type: Class