Nj. Barrow, A BRIEF DISCUSSION ON THE EFFECT OF TEMPERATURE ON THE REACTION OF INORGANIC-IONS WITH SOIL, Journal of soil science, 43(1), 1992, pp. 37-45
Published reports on the effect of temperature on the sorption of ions
by soil, or soil constituents, are in conflict with regard to the dir
ection of the effect and its interpretation. It is argued that, in man
y cases, increased sorption with increased temperature is due to an in
creased rate of the reaction that follows adsorption. The effects of t
emperature on the adsorption reaction itself are complex because of se
parate effects on the ions in solution, on the charge on the surface,
and on the affinity of the ions for the surface. On balance, adsorptio
n of anions should decrease with increasing temperature, and adsorptio
n of cations should increase. However, decreased adsorption of cations
is possible, particularly at high pH. With one exception, these concl
usions are consistent for all published reports seen.