(1)
where
The diffusion coefficient of a solute depends on the solute, the temperature and the ionic environment. Some typical values of the tracer (i.e., no ion-ion interactions) at 5°C:
The diffusion coefficient is sensitive to temperature, approximately doubling from 0 to 25°C. Within a porous medium, the additional path length to travel around particles causes the diffusion coefficient to decrease. This excess path length is expressed as a tortuosity:
(2)
where dl is the mean length of the path followed to travel a linear distance dx. The sediment diffusion coefficient, Ds, is then:
(3)
There are a number of empirical laws relating tortuosity to porosity. A reasonable approximation for deep-sea sediments is to take
(4)
The mass balance within a small volume reflects the fluxes in and out of that volume and the internal change of the pore water concentration due to chemical reaction, J:
(5)
(6)
For more information consult reference (21).
Oceanography 540 Pages Pages Maintained by Russ McDuff (mcduff@ocean.washington.edu) Copyright (©) 1994-2000 Russell E. McDuff and G. Ross Heath; Copyright Notice Content Last Modified 2/6/2000 | Page Last Built 2/6/2000 |