THE CHEMISTRY OF THE LOWLAND RICE RHIZOSPHERE

Models and experimental studies of the rhizosphere of rice plants growing in anaerobic soil show that two major processes lead to considerable acidification (1-2 pH units) of the rhizosphere over a wide range of root and soil conditions. One is generation of H+ in the oxidation of ferrous iron by O-2 released from the roots. The other is release of H+ from roots to balance excess intake of cations over anions, N being taken up chiefly as NH4+. CO2 exchange between the roots and soil has a much smaller effect. The zone of root-influence extends a few mm from the root surface. There are substantial differences along the root length and with time. The acidification and oxidation cause increased sorption of NH4+ ions on soil solids, thereby impeding the movement of N to absorbing root surfaces. But they also cause solubilization and enhanced uptake of soil phosphate.