Abstract
Radon 222 concentrations in the water and sedimentary columns and radon exchange rates across the sediment-water and air-water interfaces have been measured in a section of south San Francisco Bay. Two independent methods have been used to determine sediment-water exchange rates, and the annual averages of these methods agree within the uncertainty of the determinations, about 20%. The annual average of benthic fluxes from shoal areas is nearly a factor of 2 greater than fluxes from the channel areas. Fluxes from the shoal and channel areas exceed those expected from simple molecular diffusion by factors of 4 and 2, respectively, apparently due to macrofaunal irrigation. -from Authors
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CITATION STYLE
Hartman, B., & Hammond, D. E. (1984). Gas exchange rates across the sediment-water and air-water interfaces in south San Francisco Bay. Journal of Geophysical Research, 89(C3), 3593–3603. https://doi.org/10.1029/JC089iC03p03593
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