A. Yakirevich et al., K+ UPTAKE BY ROOT SYSTEMS GROWN IN SOIL UNDER SALINITY .2. SENSITIVITY ANALYSIS, Transport in porous media, 14(2), 1994, pp. 123-141
A numerical algorithm for the solution of multicomponent transport of
Ca2+, Mg2+, Na+, K+, Cl- in soil and their uptake by plant roots has b
een developed. The model emphasizes adsorption-desorption due to catio
n exchange mechanism, dissolution-precipitation of CaCO3, and pH chang
es at the root surface controlled by the anion-cation influx balance.
A fully implicit finite difference scheme is used for numerical implem
entation. Sensitivity analysis was conducted to evaluate the effect of
each parameter on nutrient uptake. Each parameter (independent of all
others) was varied between 0.25 to 4 times its speculated 'average' l
evel. Predicted K+ uptake was found to be more sensitive to changes of
root radius and the parameter indicating maximal influx of K+. Effect
ive diffusion coefficient and soil moisture are less influential. The
influence of CaCO3 dissolution and different kinds of boundary conditi
ons were also considered.