Mx. Fan et al., PHOSPHORUS SORPTION AS INFLUENCED BY ADDED UREA IN 2 EASTERN CANADIANSOILS, Soil Science Society of America journal, 57(5), 1993, pp. 1218-1222
The interaction of urea with P in soil-fertilizer microsites may have
an important effect on P availability to crops. A laboratory study was
conducted to evaluate the effect of urea on P reactions in two easter
n Canadian soils (Typic Humaquepts). Phosphorus sorption was studied b
y equilibrating soil samples pretreated with four levels of urea for 2
4 h with six rates of P in either 0.01 M CaCl2 or 0.03 M KCl solutions
. Phosphorus desorption was determined by sequentially extracting the
residual soil with 0.01 M CaCl2 or 0.03 M KCl, and 0.5 M NaHCO3. Urea
application increased the soil pH (0.01 M CaCl2) in the fertilizer mic
rosites from 5.2 to 7.3 in the Ste Rosalie soil and from 5.9 to 7.4 in
the Ormstown soil. These pH changes had variable effects on soil P so
rption characteristics, depending on soil and electrolyte. Phosphorus
sorption increased with increasing urea and p;H when using CaCl2 as th
e electrolyte. Added urea and pH had little effect when KCI was used,
indicating that the urea effect on P sorption was influenced by Ca con
tent. The effect of urea was not significant at P rates <320 mg P kg(-
1) soil. The observed increase in P sorption and decrease in solution
P with added urea was probably related to precipitation of Ca-P compou
nds and the shift from H2PO4- to HPO42- at higher pH values. Urea appl
ication increased 0.5 M NaHCO3 extractable P and reduced nonextractabl
e P in both soils. For soils with high Ca content, urea application wi
th P fertilizer could reduce P concentration in soil solution and P mo
bility because of the increase in P sorption and P buffer capacity, bu
t increase available P as expressed by NaHCO3-extractable P.