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- Title
Soils as a Possible Source of Fluorine in the Atmosphere.
- Authors
Savenko, V. S.
- Abstract
Abstract—: A hypothesis was proposed that a considerable amount of gaseous HF is supplied to the atmosphere from the soil cover owing to the reaction <inline-graphic></inline-graphic> In the upper layer of tundra and taiga soils with pH 4.0-4.5, the partial pressure of HF is (65-20) × 10-12 atm. Correspondingly, the concentration of dissolved F in the condensates of water vapor is 1.6-11 μg/L, which is comparable with F concentration in rainwater.
- Subjects
FLUORINE; ATMOSPHERE; ACID soils; RAINWATER; PARTIAL pressure
- Publication
Geochemistry International, 2018, Vol 56, Issue 9, p961
- ISSN
0016-7029
- Publication type
Article
- DOI
10.1134/S0016702918090094