SOIL SOLUTE CONCENTRATION AND WATER-UPTAKE BY SINGLE LUPIN AND RADISH PLANT-ROOTS .1. WATER EXTRACTION AND SOLUTE ACCUMULATION

Application of computer assisted tomography to gamma and X-ray attenuation measurements and Na+-LIX microelectrodes were used to determine the spatial distributions of soil water content and Na+ concentrations respectively near single roots of eighteen day old lupin and radish plants. These quantities were monitored at root depths of 3, 6 and 9 cm and at zero, 2, 4, 6, and 8 hour intervals from the diurnal commencement of transpiration. The plants were subjected to two levels of transpirational demand and five Na+ soil solution concentration levels. Water extraction rates for the lupin and radish roots increased continuously with time but were substantially reduced with increasing Na+ concentration in the treatment. Water uptake was uniform along the length of the essentially constant diameter lupin roots but decreased along the tapering radish roots as the diameter and hence the surface area per unit length of the roots decreased. The accumulation of Na+ at the root surfaces of both plants increased gradually with time in a near linear fashion and was slightly higher under the higher transpiration demand. These increases were not exponential as would be expected with non-absorption by the roots and this is considered to be due to back diffusion at the relatively high water contents used. At these water contents matric potentials had a much smaller influence on transpiration than osmotic potentials. The relationships between leaf water potentials (PSI1) and osmotic potentials at the root surfaces were linear with the decreases in PSI1 almost exactly reflecting the decreases in PSI(phi) indicating rapid plant adjustment. Leaf water potentials decreased progressively with time and the relationships between leaf water potential and the transpiration rate were also linear supporting the suggestion of constant plant resistances at any given concentration.