The build-up of available potassium under subterranean clover pastures on a podzolic soil

Abstract

A group of podzolic soils from the Crookwell district of New South Wales was examined for potassium status by field, pot culture, and laboratory experiments. Close relationships were found between the exchangeable potassium and the potassium content of the plant material and uptake of potassium both in the field and in pot culture. However, the measured decreases in exchangeable potassium in soil during plant growth were insufficient to account for the total uptake, indicating that other sources of soil potassium were also available. It is probable that the pasture plants themselves contribute to the conversion of non-exchangeable potassium to exchangeable forms. The results suggest that the range 0.25–0.30 m-equiv. exchangeable potassium per 100 g may be critical for these soils. Exchangeable potassium built up under the subterranean clover pastures plays an important part in eliminating a potential potassium deficiency. Removal of hay from these pastures would seriously deplete this available potassium reserve.