Fluoride geochemistry in groundwater at regulated industrial sites

© 2024 Water Environment Federation.

Bibliographische Detailangaben
Veröffentlicht in:Water environment research : a research publication of the Water Environment Federation. - 1998. - 96(2024), 8 vom: 15. Aug., Seite e11105
1. Verfasser: Fowler, Andrew (VerfasserIn)
Weitere Verfasser: Goulding, Nigel, Law, Shanna
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2024
Zugriff auf das übergeordnete Werk:Water environment research : a research publication of the Water Environment Federation
Schlagworte:Journal Article coal combustion residual (CCR) contamination fate and transport fluoride geochemical modeling geochemistry groundwater gypsum stack ponds remediation mehr... spent potliner (SPL) Fluorides Q80VPU408O Water Pollutants, Chemical Industrial Waste
Beschreibung
Zusammenfassung:© 2024 Water Environment Federation.
Few studies apply geochemical concepts governing fluoride fate and transport in natural waters to geochemical conditions at contaminated industrial sites. This has negative implications for designing sampling and compliance monitoring programs and informing remediation decision-making. We compiled geochemical data for 566 groundwater samples from industrial waste streams associated with elevated fluoride and that span a range of geochemical conditions, including alkaline spent potliner, near-neutral pH coal combustion, and acidic gypsum stack impoundments. Like natural systems, elevated fluoride (hundreds to thousands of ppm) exists at the pH extremes and is generally tens of ppm at near-neutral pH conditions. Geochemical models identify pH-dependent fluoride complexation at low pH and carbonate stability at high pH as dominant processes controlling fluoride mobility. Limitations in available thermochemical, kinetic rate, and adsorption/desorption data and lack of complete analyses present uncertainties in quantitative models used to assess fluoride mobility at industrial sites. PRACTITIONER POINTS: Geochemical fundamentals of fluoride fate and transport in groundwater are communicated for environmental practitioners. Fluoride is a reactive constituent in groundwater, and factors that govern attenuation are identified. Geochemical models are useful for identifying fluoride attenuation processes, but quantitative use is limited by thermodynamic data uncertainties
Beschreibung:Date Completed 16.08.2024
Date Revised 16.08.2024
published: Print
Citation Status MEDLINE
ISSN:1554-7531
DOI:10.1002/wer.11105