Potassium deficiency in soybeans has spread iii Sao Paulo State, Brazi
l, as a consequence of soil K reserve depletion. Exchangeable and none
xchangeable K dynamics in soil were investigated in order to understan
d the reserve exaustion and its significance to soybean nutrition. Soy
bean was grown in 8 1 pots with five soils differing in K and clay con
tents, in presence or absence of K fertilization. Soil samples were ta
ken at 20 days interval and soybean was harvest at R6. Exchangeable (H
2SO4 0,05 N) and nonexchangeable K (boiling HNO3) were estimated in so
il sample. Two of the soils were very poor in exchangeable K, and even
so there was no response in dry matter due to K fertilization. In spi
te of some differences in K contents in some of the soybeans parts, ge
nerally K absorption was not affected by K fertilization, except in gr
ains. Potassium acumulation in soybean plants were affected by soils,
but the response was not closely related to exchangeable K in soil. Th
e main K source to the plants was the HNO3 extrated K, showing that th
is form is not at all nonexchangeable. After the period of maximum pla
nt demand there was a sharp increase in extractable K in soil showing
a tendency to a natural equilibrium.