Abstract
Barley and oats were grown in the greenhouse on soils that had received surface applications of KH2PO4 solns. containing O to 12,500 microcuries P32 per g. P31. Over this range, which includes concns. much higher than those usually used in plant nutrition studies, differences in dry wt. of tops, P content of tops, and % of P in the tops derived from the fertilizer were too small to affect appreciably the data gained by use of the isotope.