Ec. Varsa et Sa. Ebelhar, Effect of potassium rate and placement on soil test variability across tillage systems, COMM SOIL S, 31(11-14), 2000, pp. 2155-2161
Experiments were conducted from 1994 through 1996 at the Dixon Springs Agri
cultural Center of the University of Illinois and the Belleville Research C
enter of Southern Illinois University to evaluate potassium rates (56, 112,
and 168 kg K ha(-1) as liquid KCI formulations) and placement methods in a
corn (Zea mays L.) and soybean (Glycine mau L.) rotation using chisel till
age (CT) and no-tillage (NT) practices. Four placement methods were used: s
urface broadcast, surface band (25 cm wide band over each row), surface dri
bble (15 cm from each row), and banding 28 kg K ha(-1) las a starter) 5 cm
to the side and 5 cm below the planted seed (remainder of the K rate was su
rface broadcast). In April of 1997, at the Belleville Research Center only,
soil cores in incremental depths of 0-5, 5-10, and 10-20 cm were collected
in a 5-cm spaced transect across and perpendicular to the two center rows
of plots of each placement method that received 112 kg K hdl. Four transect
s were taken from each plot with the soil composited by layer and by positi
on across the transect and relative to the rows. Nutrient stratification wa
s evident with both the chisel and no-tillage systems. However, placements
using no-tillage showed much higher levels of K in the 0-5 cm depth than ch
isel, but the placements modified by chiseling (CT) had higher K levels in
the 5-10 cm depth. This reflected the effect of mixing of the applied K int
o the soil with tillage, whereas, the higher K levels at the surface with N
T reflected no fertilizer disturbance. All of the placement methods had hig
her K levels near the row and the levels decreased toward the middle of row
s, even for the broadcast treatment. This was an indication that K was bein
g redeposited near the row after the plants matured. This could also have b
een associated with leaching from the plant after physiological maturity, o
r from the breakdown and release of K from the plant after harvest, or both
. The starter treatment with chisel tillage showed a definite K band near t
he row in the 5-10 cm depth that did not show up in the no-tillage plots. T
his may have been an indication that crops in the no-tillage treatment util
ized more of the starter K than chisel tillage, perhaps because of a more r
estricted rooting environment in no-till. The banded and dribble treatments
with no-till showed very sharp peaks in the 0-5 cm depths due to a lack of
incorporation via tillage, but this may also indicate a less efficient sys
tem for K uptake later in the season when surface roots are less active in
nutrient uptake.