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Emission of gaseous carbon dioxide from salt-marsh sediments and its relation to other carbon losses

Journal Article · · Estuaries; (United States)
DOI:https://doi.org/10.2307/1352188· OSTI ID:7119931
Rate of CO/sub 2/ emission from bare salt-marsh sediments in areas of short and tall form Spartina alterniflora were measured monthly for 1 yr. Maximum emission rates, as high as 325 ml CO/sub 2/ m/sup -2/ h/sup -1/, were observed during summer months, while minimum rates, 10.2 ml CO/sub 2/ m/sup -2/ h/sup -1/, were observed during the winter. An exponential function of inverse soil temperature explained most of the seasonal variability, but other factors are involved in regulating CO/sub 2/ emissions as demonstrated by rates that were higher in spring than in late summer at equivalent temperatures. Annual CO/sub 2/ emissions from bare sediments were 27.3 and 18.6 mol C m/sup -2/ yr/sup -1/ in communities of short and tall S. alterniflora, respectively. It was estimated that losses of dissolved inorganic carbon from the turnover of pore water, up to 14.6 mol C m/sup -2/ yr/sup -1/ at the creek bank (tall S. alterniflora) site, and diffusion of CO/sub 2/ from the root system of S. alterniflora through the culms, 12.3 to 16.2 mol C m/sup -2/ yr/sup -1/, could also be important pathways of carbon loss from marsh sediments. If the internal flux of CO/sub 2/ from the root system through the culm is refixed within the leaves, then the observed rate of 9.8 ..mu..l CO/sub 2/ min/sup -1/ cm/sup -2/ of culm cross sectional area appears to make a small but significant contribution to total photosynthesis. 33 references, 7 figures, 2 tables.
Research Organization:
Univ. of South Carolina, Columbia
OSTI ID:
7119931
Journal Information:
Estuaries; (United States), Journal Name: Estuaries; (United States) Vol. 9:1; ISSN ESTUD
Country of Publication:
United States
Language:
English