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Effects of temperature and prior flooding on intensity and sorption of phosphorus in soil

II. Effects on P sorption

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Summary

The effects of temperature and prior flooding of soil on P sorption were examined in 2 soils having a rice-based cropping system and showing an induced P deficiency problem in flooded rice-uplant crop rotations.

The P sorption capacity of soil increased with increasing temperature as well as with prior flooding, the effects of the latter were, howerver, dominant. The bonding energy of sorption, calculated from the Langmuir isotherm, also increased with both temperature and prior flooding of soils, indicate that the effects of chemical changes associated with alternative anoxic and oxidized soil conditions are more significant in the P reversion process. The apparent heat of sorption reaction, calculated with the Freundlich isotherm and Van't Hoff's equation also increased due to prior flooding of soil.

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Authors and Affiliations

  1. Department of Agronomy and Range Science, University of California, 95616, Davis, CA, USA

    R. N. Sah & D. S. Mikkelsen

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  1. R. N. Sah
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  2. D. S. Mikkelsen
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Sah, R.N., Mikkelsen, D.S. Effects of temperature and prior flooding on intensity and sorption of phosphorus in soil. Plant Soil 95, 173–181 (1986). https://doi.org/10.1007/BF02375069

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  • DOI: https://doi.org/10.1007/BF02375069

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