Methane cycling in the sediments of Lake Washington Public Deposited

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  • Aerobic oxidation is important in the cycling of methane in the sediments of Lake Washington. About half of the methane flux from depth is oxidized to CO, in the upper 0.7 cm of the sediments and the remainder escapes into the water column. In terms of the total carbon budget of the lake, the upward flux of methane is insignificant with only about 2% of the carbon fixed by primary production being returned as methane. The upward flux of methane, however, does represent about 20% of the organic carbon decomposed within the sediments. In addition, methane oxidation consumes 7–10% of the total oxygen flux into the sediments. Measured kinetic parameters suggest that methane oxidation is restricted to the top 6–7 mm of sediment where oxygen is present and that the rate of this process is probably controlled by the concentration of methane.
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  • Limnol. Oceanogr. 33, 571-581
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  • description.provenance : Submitted by Linda Lamb (llamb@coas.oregonstate.edu) on 2009-11-23T18:22:43Z No. of bitstreams: 1 LimnolOceanogr 1998 33 571-581.pdf: 1346194 bytes, checksum: bfbc8b98efb2ee046ac6c808355dd38b (MD5)
  • description.provenance : Approved for entry into archive by Linda Lamb(llamb@coas.oregonstate.edu) on 2009-11-23T18:32:13Z (GMT) No. of bitstreams: 1 LimnolOceanogr 1998 33 571-581.pdf: 1346194 bytes, checksum: bfbc8b98efb2ee046ac6c808355dd38b (MD5)
  • description.provenance : Made available in DSpace on 2009-11-23T18:32:13Z (GMT). No. of bitstreams: 1 LimnolOceanogr 1998 33 571-581.pdf: 1346194 bytes, checksum: bfbc8b98efb2ee046ac6c808355dd38b (MD5) Previous issue date: 1988
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  • 0024-3590

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