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Abstract— <p>According to the results of the long-term 6-year experiments, a significant decrease in the concentration of dissolved fluorine in seawater is 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 expense item in the geochemical balance of fluorine in the World Ocean.</p>

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Uptake of Dissolved Fluorine from Seawater during Halmyrolysis of Igneous Rocks

  • 期刊论文

  • 发表日期：

    2025年5月1日

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  • A. V. Savenko,
  • V. S. Savenko

摘要

Abstract—

According to the results of the long-term 6-year experiments, a significant decrease in the concentration of dissolved fluorine in seawater is 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 expense item in the geochemical balance of fluorine in the World Ocean.