Flux of methane release and carbon dioxide sequestration at Winterhouse Canyon, Gros Morne, Newfoundland, Canada; a site of continental serpentinization

We measured CO2, CH4, and N2O gas fluxes from a pool of ultra-basic water discharging from serpentinized rock in Winterhouse Canyon, Gros Morne, Newfoundland. The flux of CH4 released and CO2 sequestered were calculated to be 4.6 × 10-7 and 1.9 × 10-5 mol/(m2·min), respectively, whereas N2O concentr...

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Bibliographic Details
Published inCanadian journal of earth sciences Vol. 54; no. 3; pp. 257 - 262
Main Authors Morrissey, Liam S, Morrill, Penny L
Format Journal Article
LanguageEnglish
Published Ottawa National Research Council of Canada 01.03.2017
NRC Research Press
Canadian Science Publishing NRC Research Press
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Summary:We measured CO2, CH4, and N2O gas fluxes from a pool of ultra-basic water discharging from serpentinized rock in Winterhouse Canyon, Gros Morne, Newfoundland. The flux of CH4 released and CO2 sequestered were calculated to be 4.6 × 10-7 and 1.9 × 10-5 mol/(m2·min), respectively, whereas N2O concentrations showed little change. The net radiative forcing owing to the changing concentrations of CO2 and CH4 during the sampling period was -0.21, suggesting that the ultra-basic pool in Winterhouse Canyon has a net cooling effect on the atmosphere. Similarly, the net global warming potential over a time horizon of 100 years was -7, also suggesting a small cooling of the atmosphere. Overall this study was the first to consider the impact of CO2 sequestration and CH4 emissions from an ultra-basic pool above serpentinized rock and demonstrated the need for more research on the net global impacts of serpentinization.
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ISSN:0008-4077
1480-3313
DOI:10.1139/cjes-2016-0123