In the determination of P adsorption kinetics by using the parabolic diffusion model: what does it means by diffusion rate constant?What is the relation between this parameter and amount of P sorbed in soil
In the parabolic diffusion model the diffusion controlled phenomena are rate-limiting.
The parabolic diffusion equation has successfully described metal reactions in soils and soil constituents, feldspar weathering and pesticide reactions.
The following are the two forms of the parabolic diffusion equation:
Qt/Qinf = 4/pi1/2(Dt/r2)1/2 - Dt/r2
1/t (Qt/Qinf) = 4/pi1/2(D/r2)1/2 1/t2 - D/r2
A plot of (Qt/Qinf)/t versus 1/t1/2 should give a straight line with a slope of:
4/pi1/2(D/r2)1/2 and intercept (-D/r2). Thus if r is known, D can be calculated from both slope and intercept.
Where r is the radius of the cylinder, Qt is the quantity of diffusing substance that has left the cylinder at time t, Qinf is the corresponding quantity after infinite time, and D is an "apparent" diffusion coefficient.
For the relatively short times in most experiments, the third and subsequent terms may be ignored.
For more information on this topic, please read the attached publication.