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Seasonal variations in ebullitive flux and carbon isotopic composition of methane in a tidal freshwater estuary

Journal Article · · Global Biogeochemical Cycles; (USA)
;  [1]
  1. Florida State Univ., Tallahassee (USA)
Methane carbon isotopic composition ranged from {minus}76.9 to {minus}62.6{per thousand} in a tidal freshwater estuary (the White Oak River, North Carolina, US) with the site specific seasonal variations ranging from 6 to 10{per thousand}. During warmer months, tidally induced bubble ebullition actively transported this methane to the atmosphere. At two sites, these seasonally varying fluxes ranged from 1.2 + or{minus}0.3 to 1.3 + or{minus}0.3 mol CH{sub 4}/sq m/yr with flux-weighted average isotopic compositions at two sites of {minus}66.3 + or{minus}0.4 and {minus}69.5 + or{minus}0.6{per thousand}. The carbon isotopic composition of naturally released bubbles was shown to be indistinguishable from the sedimentary methane bubble reservoir at three sites, leading to the conclusion that isotopic fractionation did not occur during the ebullition of methane. The hypothesis was developed that ebullitive methane fluxes are depleted in C{sup 13}-CH{sub 4} relative to fluxes transported via molecular diffusion or through plants, as zones of C{sup 13}-enriching microbial methane oxidation are bypassed.
OSTI ID:
6656256
Journal Information:
Global Biogeochemical Cycles; (USA), Journal Name: Global Biogeochemical Cycles; (USA) Vol. 2:3; ISSN GBCYE; ISSN 0886-6236
Country of Publication:
United States
Language:
English