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Increased methane emissions from deep osmotic and buoyant convection beneath submarine seeps as climate warms

High speeds have been measured at seep and mud-volcano sites expelling methane-rich fluids from the seabed. Thermal or solute-driven convection alone cannot explain such high velocities in low-permeability sediments. Here we demonstrate that in addition to buoyancy, osmotic effects generated by the...

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Publicat a:Nat Commun
Autors principals: Cardoso, Silvana S. S., Cartwright, Julyan H. E.
Format: Artigo
Idioma:Inglês
Publicat: Nature Publishing Group 2016
Matèries:
Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC5095281/
https://ncbi.nlm.nih.gov/pubmed/27807343
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms13266
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