Abstract
During the February response cruise to Axial Volcano, methane and hydrogen concentrations within the plume were significantly elevated above background. CH4/3He ratios were found to be 5-10 times greater than previously reported values for unsedimented ridges. An average δ13C value of -32.7 ± 0.8 ‰ was determined for CH4 concentrations > 10 nM and CH4/Mn ratios were determined to be 2.2. Hydrogen concentrations as high as 183 nM were measured; however most were < 10nM. Microbial oxidation of methane was negligible (<0.001 day-1) during this sampling period. However, microbial hydrogen oxidation was sufficient to explain decreased H2 concentrations measured at 'older' downstream stations. Copyright 1999 by the American Geophysical Union.
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CITATION STYLE
McLaughlin-West, E. A., Olson, E. J., Lilley, M. D., Resing, J. A., Lupton, J. E., Baker, E. T., & Cowen, J. P. (1999). Variations in hydrothermal methane and hydrogen concentrations following the 1998 eruption at Axial Volcano. Geophysical Research Letters, 26(23), 3453–3456. https://doi.org/10.1029/1999GL002336
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