“…Most experiments designed to evaluate particle-size effects of phosphate fertilizers have been field or greenhouse experiments or a combination of these two. In experiments with dicalcium phosphate, phosphate rock, and other essentially water-insoluble sources, small fertilizer particles usually have been better than large particles as a source of phosphorus for plants (Bouldin and Sample, 1959 On the other hand, "in experiments conducted with water-soluble phosphate sources, the granulated or large fertilizer particles usually have been better than the nongranulated or small fertilizer particles (Bouldin, 1956;Lawton and Cook, 1955;Starostka et al, 195b;and Wilding, 1950) except on calcareous, soils, where the opposite effects have been observed (Bouldin, 1956;Terman, 1958;and Wilding, 191*9). Larsen (1955), after conducting field experiments for 5 years in Denmark with granulated and powdered superphosphate, concluded that large par ticles of superphosphate had little, if any, agronomic advantage over small particles, but that they should be preferred because of the improved physical condition of the granulated fertilizer.…”