02048naa a2200301 a 450000100080000000500110000800800410001910000190006024500990007926000090017852013110018765000100149865000120150865000150152065000090153565000100154465000100155465000120156465000120157665000130158865000170160165000110161865000230162965000090165270000190166170000180168077300480169816171911995-06-27       1991    bl uuuu     u00u1 u    #d1 aFAGERIA, N. K.  aInfluence of phosphate rock sources and rates on rice and common bean production in an oxisol.  c1991  aA field experiment was conducted for five consecutive years to determine upland rice (Oryza sativa L.) and common bean (Phaseolus vulgaris L.) response to eight P sources at three P rates in an Oxisol of Central Brazil. The P sources tested were triple superphosphate (TSP), Arafertil phosphate partially acidulated (APPA), phosphate of Patos partially acidulated (PPPA), phosphate of Araxa concentrated (PAC), phosphate of Catalao (PC), phosphate of Jacupiranga (PJ), phosphate of Patos de Minas (PPM), and phosphate of Abaete (PA). All phosphate rock sources were of Brazilian origin. The P rates used were 87, 174 and 262 kg P ha-1. Yield response to P sources and rates varied from crop to crop. Rice and bean yields were significantly correlated with Bray 1 P, but not Mehlich 1 P. In the first year, TSP and the two partially acidulated phosphate rocks (APPA, PPPA) produced higher grain yields. In the second year and all remaining years of the experiment, the efficiency of phosphate rock sources as measured by grain yield was equivalent to TSP or partially acidulated P sources. The results suggest that these phosphate rock sources could be used in rice-bean rotations on Brazilian Oxisols. Yield losses in the first year could be partially offset by the addition of a small amount of soluble P.  aBeans  aOxisols  aPhosphates  aRice  aRocks  aArroz  aFeijão  aFosfato  aFósforo  aOryza Sativa  aOxisol  aPhaseolus Vulgaris  aSolo1 aBALIGAR, V. C.1 aWRIGHT, R. J.  tPlant Soilgv. 134, n. 1, p. 137-144, 1991.