Fluoride occurrence in United States groundwater.

Drinking-water wells Geochemical controls National groundwater fluoride occurrence Spatial variability Vulnerable populations

Journal

The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500

Informations de publication

Date de publication:
25 Aug 2020
Historique:
received: 06 01 2020
revised: 09 04 2020
accepted: 03 05 2020
pubmed: 22 5 2020
medline: 22 5 2020
entrez: 22 5 2020
Statut: ppublish

Résumé

Data from 38,105 wells were used to characterize fluoride (F) occurrence in untreated United States (U.S.) groundwater. For domestic wells (n = 11,032), water from which is generally not purposely fluoridated or monitored for quality, 10.9% of the samples have F concentrations >0.7 mg/L (U.S. Public Health Service recommended optimal F concentration in drinking water for preventing tooth decay) (87% are <0.7 mg/L); 2.6% have F > 2 mg/L (EPA Secondary Maximum Contaminant Level, SMCL); and 0.6% have F > 4 mg/L (EPA MCL). The data indicate the biggest concern with F in domestic wells at the national scale could be one of under consumption of F with respect to the oral-health benchmark (0.7 mg/L). Elevated F concentrations relative to the SMCL and MCL are regionally important, particularly in the western U.S. Statistical comparisons of potentially important controlling factors in four F-concentration categories (<0.1-0.7 mg/L; >0.7-2 mg/L; >2-4 mg/L; >4 mg/L) at the national scale indicate the highest F-concentration category is associated with groundwater that has significantly greater pH values, TDS and alkalinity concentrations, and well depths, and lower Ca/Na ratios and mean annual precipitation, than the lowest F-concentration category. The relative importance of the controlling factors appears to be regionally variable. Three case studies illustrate the spatial variability in controlling factors using groundwater-age (groundwater residence time), water-isotope (evaporative concentration), and water-temperature (geothermal processes) data. Populations potentially served by domestic wells with F concentrations <0.7, >0.7, >2, and >4 mg/L are estimated to be ~28,200,000, ~3,110,000; ~522,000; and ~172,000 people, respectively, in 40 principal aquifers with at least 25 F analyses per aquifer.

Identifiants

pubmed: 32438175
pii: S0048-9697(20)32734-0
doi: 10.1016/j.scitotenv.2020.139217
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

139217

Informations de copyright

Published by Elsevier B.V.

Déclaration de conflit d'intérêts

Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

Peter B McMahon (PB)

U.S. Geological Survey, Denver, CO, USA. Electronic address: pmcmahon@usgs.gov.

Craig J Brown (CJ)

U.S. Geological Survey, East Hartford, CT, USA. Electronic address: cjbrown@usgs.gov.

Tyler D Johnson (TD)

U.S. Geological Survey, San Diego, CA, USA. Electronic address: tyjohns@usgs.gov.

Kenneth Belitz (K)

U.S. Geological Survey, Northborough, MA, USA. Electronic address: kbelitz@usgs.gov.

Bruce D Lindsey (BD)

U.S. Geological Survey, New Cumberland, PA, USA. Electronic address: blindsey@usgs.gov.

Classifications MeSH