Abstract
The effect of phosphate (P), calcium (Ca), and pH on the dissolution of Sechura phosphate rock (SPR) in a Typic Dystrochrept was investigated in an incubation study over 90 days. Increasing the P status of the soil had little effect on either the rate or extent of dissolution of SPR, as measured by a single extraction with 0.5M NaOH, or on the amount of plant-available P in the soil as measured by the Bray procedure. This suggests that a reactive PR such as SPR could be effective as a maintenance P fertilizer on soils of medium and high P status.
The dissolution of SPR at pH 6.4 was only 4% of total P added, compared to 33.6% of total P added at pH 5.2. Addition of Ca as CaCl2, at the same rate of Ca as that added in Ca(OH)2 to raise soil pH from 5.2 to 6.4, reduced the dissolution of SPR to 11% of total P added. The large effect of Ca on the dissolution of SPR contrasts with the small effect of soil P status and probably reflects the fact that the concentration of Ca in the soil solution is generally several orders of magnitude higher than that of P. The results obtained suggest that pH, per se, is of less importance in the dissolution and subsequent plant availability of P from phosphate rock in soil than previously thought.
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Mackay, A., Syers, J. Effect of phosphate, calcium, and pH on the dissolution of a phosphate rock in soil. Fertilizer Research 10, 175–184 (1986). https://doi.org/10.1007/BF01074371
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DOI: https://doi.org/10.1007/BF01074371