Active ion uptake and maintenance of cation-anion balance: A critical examination of their role in regulating rhizosphere pH

TLDR: In this article, the processes responsible for maintaining cation-anion balance in plants and their relation to active ion accumulation and changes in rhizosphere pH are outlined and discussed.

Abstract: The processes responsible for maintenance of cation-anion balance in plants and their relation to active ion accumulation and changes in rhizosphere pH are outlined and discussed. The major processes involved are: (1) accumulation and degradation of organic acids which occur in the plant mainly as organic acid anions (and their transfer within the plant) and (2) extrusion of H+ or OH− into the rhizosphere. The relative importance of the two processes is determined by the size of the excess anion or cation uptake. Indeed, plants typically absorb unequal quantities of nutritive cations (NH4++Ca2++ Mg2++K++Na+) and anions (NO3−+Cl−+SO42−+H2PO4−) and charge balance is maintained by excretion of an amount of H+ or OH− which is stoichiometrically equal to the respective excess cation or anion uptake. The mechanisms and processes by which H+ and in particular OH− ions are excreted in response to unequal cation-anion uptake are, however, poorly understood.