Fertilizer research

, Volume 40, Issue 2, pp 109–119 | Cite as

Phosphate availability in calcareous Vertisols and Inceptisols in relation to fertilizer type and soil properties

  • B. Castro
  • J. Torrent
Article

Abstract

The availability to plants of fertilizer phosphorus (P) applied to soil, as measured by chemical extraction, is used to estimate P fertilizer needs. We studied the availability of P, applied as monocalcium phosphate (MCP) powder, ordinary superphosphate (OSP) granules and diammonium phosphate (DAP) granules in 24 calcareous Vertisols and Inceptisols of Andalusia, Spain, by using laboratory incubation techniques. The soils differed widely in their P adsorption- and Ca-phosphate precipitation-related properties. For MCP, availability (defined as the proportion of added P that is recovered by extraction with NaHCO3 or is isotopically exchangeable) decreased markedly with incubation time and increasing addition rate. The mean recoveries after 180 d of incubation at field capacity at a rate of 246 mg P kg−1 soil were 17% for Olsen P, 38% for Colwell P, and 16% for isotopically exchangeable P (IEP). Increasing the application rate to 2460 mg kg−1 resulted in recoveries of 6% for Olsen P, 25% for Colwell P, and 4% for IEP. While IEP-based recovery was not significantly correlated to any soil property, that based on Olsen P (and, to a lesser extent, Colwell P) decreased sharply with increase in the ratio of clay (or Fe oxides) to total (or active) calcium carbonate equivalent. Accordingly, Olsen P might overestimate P availability in those soils relatively rich in carbonate and poor in clay and Fe oxides. On the other hand, recovery of applied P from soils containing more clay and Fe oxides, by a sequential extraction (with H2O, two 0.5M NaHCO3 treatments, 0.5M HCl), was lower than 100%, thereby suggesting phosphate occlusion by Fe oxides or clay.

Availability of the fertilizers tested 90 d after application was found to decrease in the following order: MCP powder (rate, 246 mg kg−1) > DAP granules (rate, 547 mg kg−1) > MCP powder (rate, 738 mg kg−1) > OSP granules (rate, 308 mg kg−1). Differences between fertilizers tended to increase with increasing carbonate content in the soil. This may have been due to precipitation of Ca phosphates caused by the presence of Ca in the fertilizer and the high Ca- supplying capacity of the more calcareous soils.

Key words

diammonium phosphate fertilizer rate monocalcium phosphate ordinary superphosphate P availability 

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References

  1. Afif E, Matar A and Torrent J (1993) Availability of phosphate applied to calcareous soils of West Asia and North Africa. Soil Sci Soc Am J 57:756–760Google Scholar
  2. Barrow NJ (1980) Evaluation and utilization of residual phosphorus in soils. In: Khasawnehet al. (eds) The Role of Phosphorus in Agriculture. ASA, CSSA and SSSA, Madison, WIGoogle Scholar
  3. Bowman RA, Olsen SR and Watanabe FS (1978) Greenhouse evaluation of residual phosphate by four phosphorus methods in neutral and calcareous soils. Soil Sci Soc Am J 42:451–454Google Scholar
  4. Colwell JD (1963) The estimation of phosphorus fertilizer requirements of wheat in southern New South Wales by soil analysis. Aust J Exp Agric Anim Husb 3:190–197Google Scholar
  5. Drouineau G (1942) Dosage rapide du calcaire actif du sol: Nouvelles données sur la repartition et la nature des fractions calcaires. Ann Agron 12:441–450Google Scholar
  6. Freeman JS and Rowell DL (1981) The adsorption and precipitation of phosphate onto calcite. J Soil Sci 32:75–84Google Scholar
  7. Holford ICR (1980) Greenhouse evaluation of four phosphorus soil tests in relation to phosphate buffering and labile phosphate in soils. Soil Sci Soc Am J 44:555–559Google Scholar
  8. Kuo S (1990) Phosphate sorption implications on phosphate soil tests and uptake by corn. Soil Sci Soc Am J 54:131–135Google Scholar
  9. Mendoza RE and Barrow NJ (1987) Ability of three soil extractants to reflect the factors that determine the availability of soil phosphate. Soil Sci 144:319–329Google Scholar
  10. Murphy J and Riley JP (1962) A modified single solution method for the determination of phosphate in natural waters. Anal Chim Acta 27:31–36Google Scholar
  11. Olsen SR, Cole CV, Watanabe FS and Dean LA (1954) Estimation of available phosphorus in soils by extraction with sodium bicarbonate. USDA Circ. 939, U.S. Gov. Print. Office, Washington, DCGoogle Scholar
  12. Sharpley AN, Singh U, Uehara G and Kimble J (1989) Modeling soil and plant phosphorus dynamics in calcareous and highly weathered soils. Soil Sci Soc Am J 51:78–82Google Scholar
  13. Solis P and Torrent J (1989a) Phosphate fractions in calcareous Vertisols and Inceptisols of Spain. Soil Sci Soc Am J 53:462–466Google Scholar
  14. Solis P and Torrent J (1989b) Phosphate sorption by calcareous Vertisols and Inceptisols of Spain. Soil Sci Soc Am J 53:456–459Google Scholar
  15. Solis P and Torrent J (1989c) Niveles criticos de P (Olsen) en suelos de campiñas andaluzas: dependencia de la capacidad tampón. Investigación Agraria. Producción y Protección Vegetales 4:199–207Google Scholar

Copyright information

© Kluwer Academic Publishers 1995

Authors and Affiliations

  • B. Castro
    • 1
  • J. Torrent
    • 1
  1. 1.Departamento de Ciencias y Recursos Agrícolas y ForestalesUniversidad de CórdobaCórdobaSpain

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