Ap. Mallarino, INTERPRETATION OF SOIL-PHOSPHORUS TESTS FOR CORN IN SOILS WITH VARYING PH AND CALCIUM-CARBONATE CONTENT, Journal of production agriculture, 10(1), 1997, pp. 163-167
There is uncertainty about appropriate soil-test extractants and inter
pretations in regions with soils varying in pH and calcium carbonate c
ontent. The objective of this research was to compare extractable P us
ing the Bray-P-1 (B1), Olsen, and Mehlich-3 (M3) extractants and to ob
tain soil-test interpretations for corn (Zea mays L.) in soils varying
in pH and calcium carbonate equivalent (CCE). The extractants were co
mpared by correlating the amounts of P extracted from 350 soil samples
and by calibrations based on 61 field response trials. Correlations b
etween P extracted by the B1 extractant and the Olsen or M3 extractant
s improved markedly when calcareous soils were excluded from the analy
ses. The correlation between the Olsen and M3 extractants was high and
independent of soil pH. Neither soil pH, CCE, soil type, nor organic
matter content completely explained the low correlations between P ext
racted by the B1 and the Olsen or M3 methods in high pH soils. Critica
l concentrations across all soils defined by the Cate-Nelson and linea
r-plateau models were 7 and 9 ppm for the Olsen extractant and 14 and
24 ppm for the M3 extractant. When highly calcareous soils were exclud
ed, the critical concentrations for the B1 extractant were 11 and 20 p
pm, respectively. The Olsen and M3 extractants are more reliable than
the B1 for estimating plant-available P of Iowa soils over a broad ran
ge of soil pH and CCE.