Hf. Wang et al., MODEL STUDY OF ACID-RAIN EFFECT ON ADSORPTION OF TRACE-ELEMENTS ON SOILS USING A MULTITRACER, Journal of radioanalytical and nuclear chemistry, 235(1-2), 1998, pp. 295-300
Using a radioactive multitracer and model acid rain (HCL or H2SO4 solu
tion), batch experiments were performed to examine the pH effect on th
e adsorption-desorption equilibrium of 16 elements on soils as a model
study of an acid rain effect. Kaolin, black soil (original and with o
rganic matter almost removed) and Kureha soil (original and with organ
ic matter almost removed) were used as adsorbents. Characteristic depe
ndence on the pH value of the suspension was observed for the adsorpti
on of the elements on kaolin and the soils. The results of this model
study indicate that acid rain decreases the retention of cations, whil
e it increases or does not change the adsorption of anions on soils. O
rganic matter in soils has a positive effect on the extent of adsorpti
on of most elements investigated.