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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...
में बचाया:
| में प्रकाशित: | Nat Commun |
|---|---|
| मुख्य लेखकों: | , |
| स्वरूप: | Artigo |
| भाषा: | Inglês |
| प्रकाशित: |
Nature Publishing Group
2016
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| विषय: | |
| ऑनलाइन पहुंच: | 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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