Processes of soil acidification during nitrogen cycling with emphasis on legume based pastures

Abstract

In areas that remain unaffected by industrial pollution soil acidification is mainly caused by the release of protons (H+) during the oxidation of carbon (C), sulphur (S) and nitrogen (N) compounds in soils. In this review the processes of H+ ions release during N cycling and its effect on soil acidification are examined. The major processes leading to acidification during N cycling in soils are: (i) the imbalance of cation over anion uptake in the rhizosphere of plants either actively fixing N2 gas or taking up NH4+ ions as the major source of N, (ii) the net nitrification of N derived from fixation or from NH4+ and R-NH2 based fertilizers, and (iii) the removal of plant and animal products containing N derived from the process described in (i) and losses of NO3-N by leaching when the N input form is N2, NH4+ or R-NH2. The uptake of excess cations over anions by plants results in the acidification of the rhizosphere which is a "localized" effect and can be balanced by the release of hydroxyl (OH-) ions during subsequent plant decomposition. Nitrification of fixed N2 or NH4+ and R-NH2 based fertilizers, and loss of N from the soil either by removal of products or by leaching of NO3-N with a companion basic cation, lead to 'permanent' acidification. © 1991 Kluwer Academic Publishers.