Jg. Davis et al., LONG-TERM PHOSPHORUS AND POTASSIUM APPLICATION TO CORN ON COASTAL-PLAIN SOILS, Journal of production agriculture, 9(1), 1996, pp. 88-94
The effect of long-term fertilizer applications on soil test levels, y
ield, and crop removal depends on soil texture and mineralogy. The obj
ectives of this study were to measure the fluctuations in soil P and K
in soils of varying texture and to evaluate the usefulness of the Meh
lich-1 soil extractant in predicting yield response. A field experimen
t was conducted for 11 yr on two soils: a Tifton loamy sand (fine-loam
y, siliceous, thermic Plinthic Kandiudults) and a Greenville sandy cla
y loam (clayey, kaolinitic, thermic Rhodic Kandiudults). Phosphorus tr
eatments were 0, 92, 183, and 275 lb P2O5 lb/acre in the first year fo
llowed by annual applications of 0, 37, 73, and 0 lb/acre, respectivel
y. Potassium treatments were 0, 48, 96, and 144 lb K2O/acre in the fir
st year followed by annual applications of 0, 48, 96, and 0 lb/acre, r
espectively. Soil samples (0-6 in.) were collected each year at tassel
ing of the corn (Zea mays L.) crop, P and K concentrations were determ
ined in soil and grain samples, and yield was measured. Initial applic
ation rates influenced initial soil test levels, and annual applicatio
n rates affected the rate of change of soil test levels with time. All
significant yield increases on the Greenville soil were due to P appl
ication. Phosphorus moves rapidly from solution into less available fo
rms in the Greenville soil due to the soil's high P fixing capacity. Y
ield increases on the Tifton soil resulted from K applications, presum
ably due to greater leaching losses on the sandier textured soil. The
Mehlich-1 extractant provides a questionable measure of soil P availab
ility for corn. Particularly in areas where P runoff potential is high
, P fertilizer should not be applied to irrigated corn in the Southeas
t unless the Mehlich-1 extractable soil P concentration less than or e
qual to 12 lb/acre. Data from this long-term study show that accountin
g for soil K below the plow layer may improve the use of Mehlich-1 ext
ractant as a measure of K availability for corn.