Comments on "Molecular diffusion and the sedimentary environment: results from the in situ determination of whole sediment diffusion coefficients" by P. E. Kepkay, R. C. Cooke and A. J. Bowen

Details Comments on "Molecular diffusion and the sedimentary environment: results from the in situ determination of whole sediment diffusion coefficients" by P. E. Kepkay, R. C. Cooke and A. J. Bowen Comments on "Molecular diffusion and the sedimentary environment: results from the in situ determination of whole sediment diffusion coefficients" by P. E. Kepkay, R. C. Cooke and A. J. Bowen

Nov 1982

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982gecoa..46.2407w&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 46, Issue 11, p.2407

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Scientific paper

The contention of Kepkay et al. (1981), that the description of transport of dissolved sulfate in sediments must explicitly include the effects of bacterial sulfate reduction, is shown to be conceptually confusing and unnecessary. Moreover, during their own measurements of diffusion coefficients it is unlikely that they were, in fact, bothered by sulfate reduction.

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