Ak. Patra et al., VOLATILIZATION LOSSES OF SURFACE-APPLIED UREA NITROGEN FROM VERTISOLSIN THE INDIAN SEMIARID TROPICS, Biology and fertility of soils, 22(4), 1996, pp. 345-349
The N loss from Vertisols was estimated by measuring the loss of N-15-
labelled urea N under conditions that promote NH3 volatilization. Urea
granules were placed on the top of 150-mm deep soil columns (Vertisol
s) collected from three sites with a range in pH, electrical conductiv
ity, and cation exchange capacity. There were two contrasting moisture
treatments, one near field capacity (wet) and another with intermitte
nt wetting of the soil surface before allowing the columns to dry (moi
st-dry). The results indicated that losses were influenced markedly by
pH and moisture treatment, being 29.5, 33.5, and 33% from the wet soi
ls and 37, 42, and 40.5% from the moist-dry soils with pH values of 7.
7, 8.2, and 9.3, respectively. These observations clearly indicate tha
t broadcasting of urea on the surface of Vertisols may cause substanti
al N losses.