Diffusion of ions in sea water and in deep-sea sediments

Details Diffusion of ions in sea water and in deep-sea sediments Diffusion of ions in sea water and in deep-sea sediments

May 1974

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1974gecoa..38..703l&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 38, Issue 5, pp.703-714

Physics

153

Scientific paper

The tracer-diffusion coefficient of ions in water, D j 0 , and in sea water, D j * , differ by no more than zero to 8 per cent. When sea water diffuses into a dilute solution of water, in order to maintain the electro-neutrality, the average diffusion coefficients of major cations become greater but of major anions smaller than their respective D j * or D j 0 values. The tracer diffusion coefficients of ions in deep-sea sediments, D j , sed . , can be related to D j * by D j , sed . = D j * · / 2 , where is the tortuosity of the bulk sediment and a a constant close to one.

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