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Groundwater‐Driven Methane Export Reduces Salt Marsh Blue Carbon Potential
Author(s) -
Schutte C. A.,
Moore W. S.,
Wilson A. M.,
Joye S. B.
Publication year - 2020
Publication title -
global biogeochemical cycles
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.512
H-Index - 187
eISSN - 1944-9224
pISSN - 0886-6236
DOI - 10.1029/2020gb006587
Subject(s) - groundwater , submarine groundwater discharge , salt marsh , hydrology (agriculture) , environmental science , marsh , intertidal zone , flux (metallurgy) , soil water , methane , greenhouse gas , atmosphere (unit) , dissolved organic carbon , tracer , carbon dioxide , environmental chemistry , atmospheric sciences , aquifer , soil science , chemistry , wetland , geology , oceanography , ecology , geography , meteorology , geotechnical engineering , organic chemistry , biology , physics , nuclear physics
The burial of “blue carbon” in coastal marsh soils is partially offset by marsh‐atmosphere methane (CH 4 ) fluxes, but this offset may be greater if other pathways of CH 4 export exist. Here we report that salt marshes also export dissolved CH 4 via submarine groundwater discharge (SGD). The volumetric fluxes of salt marsh groundwater into adjacent tidal creeks were calculated from mass balances of the conservative tracer 226 Ra at four study sites in coastal Georgia, USA. Over the 2‐year study period, volumetric groundwater fluxes across all sites ranged between 1,700 and 105,000 m 3 day −1 . Dissolved CH 4 fluxes of 27–1,200 μmol CH 4 m −2 day −1 were calculated by multiplying the volumetric groundwater flux by the groundwater CH 4 concentration and normalizing to the intertidal salt marsh area estimated from satellite images. On a mass basis, the cross‐site range in CH 4 fluxes was 1.3–5.5 g CH 4 m −2 year −1 with a cross‐site mean of 2.8 g CH 4 m −2 year −1 . This is equivalent to 125 (56–245) g CO 2 m −2 year −1 assuming that CH 4 is 45 times more potent than CO 2 as a greenhouse gas over a 100‐year time frame. This sustained‐flux global warming potential is similar to the 138 (1.1–260) g CO 2 m −2 year −1 average calculated across other studies of the direct marsh soil to atmosphere CH 4 flux. Therefore, SGD drives an effective doubling of salt marsh CH 4 export that offsets a combined total of ~30% of the global cooling potential derived from soil carbon sequestration.