Email this article Uptake of Dissolved Fluorine from Seawater During Halmyrolysis of Igneous Rocks
- Authors: Savenko A.V.1, Savenko V.S.1
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Affiliations:
- Lomonosov Moscow State University
- Issue: Vol 522, No 2 (2025)
- Pages: 249-252
- Section: GEOCHEMISTRY
- Submitted: 15.10.2025
- Published: 15.06.2025
- URL: https://gynecology.orscience.ru/2686-7397/article/view/693299
- DOI: https://doi.org/10.31857/S2686739725060094
- ID: 693299
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Abstract
According to long-term 6-year experiments, a significant decrease in the concentration of dissolved fluorine in seawater was established during its interaction with ultrabasic and basic igneous rocks: dunite, gabbro-norite, and basalt. It is concluded that submarine weathering (halmyrolysis) of rocks of the oceanic crust is a significant expenditure item in the geochemical balance of fluorine in the World Ocean.
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About the authors
A. V. Savenko
Lomonosov Moscow State University
Email: Alla_Savenko@rambler.ru
Moscow, Russia
V. S. Savenko
Lomonosov Moscow State UniversityMoscow, Russia
References
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