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Gas exchange in the Pee Dee River based on 222 Rn evasion
Author(s) -
Elsinger Robert J.,
Moore Willard S.
Publication year - 1983
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl010i006p00443
Subject(s) - radon , hydrology (agriculture) , environmental science , radon gas , analytical chemistry (journal) , atmospheric sciences , chemistry , geology , physics , environmental chemistry , nuclear physics , geotechnical engineering
Excess 222 Rn concentrations decrease downstream in the fresh water section of the Pee Dee River. Ground water is the primary source of the excess 222 Rn to the River. Using the radon concentration gradients determined during four sampling periods, gas exchange rates based on the stagnant film model are calculated. Stagnant film thicknesses range from 19µm to 48µm and mass transfer coefficients range from 2.1 m/d to 4.1 m/d.

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