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Distributed natural gas venting offshore along the Cascadia margin

Widespread gas venting along the Cascadia margin is investigated from acoustic water column data and reveals a nonuniform regional distribution of over 1100 mapped acoustic flares. The highest number of flares occurs on the shelf, and the highest flare density is seen around the nutrition-rich outfl...

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Detalles Bibliográficos
Autores principales: Riedel, M., Scherwath, M., Römer, M., Veloso, M., Heesemann, M., Spence, G. D.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6093902/
https://www.ncbi.nlm.nih.gov/pubmed/30111802
http://dx.doi.org/10.1038/s41467-018-05736-x
Descripción
Sumario:Widespread gas venting along the Cascadia margin is investigated from acoustic water column data and reveals a nonuniform regional distribution of over 1100 mapped acoustic flares. The highest number of flares occurs on the shelf, and the highest flare density is seen around the nutrition-rich outflow of the Juan de Fuca Strait. We determine ∼430 flow-rates at ∼340 individual flare locations along the margin with instantaneous in situ values ranging from ∼6 mL min(−1) to ∼18 L min(−1). Applying a tidal-modulation model, a depth-dependent methane density, and extrapolating these results across the margin using two normalization techniques yields a combined average in situ flow-rate of ∼88 × 10(6) kg y(−1). The average methane flux-rate for the Cascadia margin is thus estimated to ∼0.9 g y(−1)m(−2). Combined uncertainties result in a range of these values between 4.5 and 1800% of the estimated mean values.