DOI QR코드

DOI QR Code

Characteristics of Phosphorus Adsorption of Acidic, Calcareous, and Plastic Film House Soils

  • Kim, Myung-Sook (Soil & Fertilizer Management Division, National Institute of Agricultural Science) ;
  • Park, Seong-Jin (Soil & Fertilizer Management Division, National Institute of Agricultural Science) ;
  • Lee, Chang-Hoon (Soil & Fertilizer Management Division, National Institute of Agricultural Science) ;
  • Yun, Sun-Gang (Soil & Fertilizer Management Division, National Institute of Agricultural Science) ;
  • Ko, Byong-Gu (Soil & Fertilizer Management Division, National Institute of Agricultural Science) ;
  • Yang, Jae E. (Soil & Fertilizer Management Division, National Institute of Agricultural Science)
  • Received : 2016.10.24
  • Accepted : 2016.11.21
  • Published : 2016.12.31

Abstract

Continuous excessive application of phosphorus (P) fertilizer and manure in plastic film house soils can lead to an accumulation of P in soils. The understanding of P sorption by soils is important for fertilizer management. In this study, 9 samples were collected for acidic and calcareous soils as non-cultivated soil and plastic film house soils as cultivated soil Phosphorus sorption data of acidic soils fit the Langmuir equations, Freundlich equations in calcareous and plastic film house soils. In calcareous and plastic film house soils, the slope of isotherm adsorption changed abruptly, which could be caused P precipitation with $CaCO_3$. The calculated Langmuir adsorption maximum ($S_{max}$) varied from 217 to 1,250, 139 to 1,429, and $714mg\;kg^{-1}$ for acidic soils, calcareous soils, and plastic film house soils with low available phosphate concentration, respectively. From this result, maximum P adsorption by the Langmuir equation could be regarded as threshold of P concentration to induce the phosphate precipitation in soil. Phosphate-sorption values estimated from one-point isotherm for acidic and calcareous soils as non-cultivated soils were comparable with the $S_{max}$ values calculated from the Langmuir isotherm.

Keywords

References

  1. Adamson, A.W. 1967. Physical chemistry of sufraces. Interscience Publishers, Inc., New York. 650-654.
  2. Fox, R.L. and E.J. Kamprath. 1970. Phosphate sorption isotherms for evaluating the phosphate requirements of soils. Soil Sci. Soc. Am. Proc. 34:902-907. https://doi.org/10.2136/sssaj1970.03615995003400060025x
  3. Freeman, J.S. and D.L. Rowell. 1981. The adsorption and precipitation of phosphate onto calcite. J. Soil Sci. 32:75-84. https://doi.org/10.1111/j.1365-2389.1981.tb01687.x
  4. Freundlich, H. 1926. Colloid and capillary chemistry. Methuen, London.
  5. Jung, W.K. and Y.H. Kim. 2006. Soil organic carbon determination for calcareous oils. Korean J. Soil Sci. Fert. 39(6):396-402.
  6. Kuo, S. and E.G. Loste. 1974. Kinetics of phosphate adsorption by calcium carbonate and Ca kaolinite. Soil Sci. Soc. Amer. Proc. 36:725-729.
  7. Langmuir, I. 1918. The adsorption of gases on plane surfaces of glass, mica and platinum. J. Am. Chem. Soc. 40:1361-1403. https://doi.org/10.1021/ja02242a004
  8. NIAST. 2000. Methods of soil analysis. NIAST, RDA, Suwon, Korea.
  9. NIAST. 2006. Fertilizer Recommendation for crops (revision). National Institute of Agricultural Science and Technology, RDA, Suwon, Korea.
  10. Parfitt, R.L. 1989. Phosphate reactions with natural allophane, ferrihydrite and goethite. J. Soil Sci. 40:359-369. https://doi.org/10.1111/j.1365-2389.1989.tb01280.x
  11. Rajan, S.S.S. and R.L. Fox. 1974. Phosphate adsorption by soils. II. Reactions in tropical acid soils. Soil Sci. Sci. Soc. Am. J. 39:846-851.
  12. RDA. 2013. Monitoring project on agri-environment quality in Korea. Rural Development Administration, Suwon, Korea.
  13. Ryan, J., D. Curtin, and M.A. Cheema. 1985. Significance of iron oxides and calcium carbonate particle size in phosphate sorption by calcareous soils. Soil Sci. Soc. Am. J. 49:74-76. https://doi.org/10.2136/sssaj1985.03615995004900010014x
  14. Ryu, I.S. 1975. Comparison between phosphorus adsorption coefficient and Langmuir adsorption maximum. J. Korean Soc. Sci. Fert. 8(1):1-17.
  15. Sanyal, S.K., S.K. De Datta, and P.Y. Chan. 1993. Phosphate sorption-desorption behavior of some acidic soils of south and southeast Asia. Soil Sci. Soc. Am. J. 57:937-945. https://doi.org/10.2136/sssaj1993.03615995005700040011x
  16. Solis, P. and J. Torrent. 1989. Phosphate sorption by calcareous vertisols and inceptisols of Spain soils. Soil Sci. Sci. Soc. Am. J. 53:456-459. https://doi.org/10.2136/sssaj1989.03615995005300020024x
  17. Sparks, D.L. 2003. Environmental Soil Chemistry, third ed., Academic press, New York, USA, 2003.
  18. Yan, X., D. Wang, H. Zhang, G. Zhang, and Z. Wei. 2013. Organic amendments affect phosphorus sorption characteristics in a paddy soil. Agriculture, Ecosystems and Environment, 175: 47-53. https://doi.org/10.1016/j.agee.2013.05.009
  19. Yun, H.B., Y.J. Lee, J.K. Sung, M.S. Kim, S.M. Lee, S.C. Kim, and D.B. Lee. 2013. Estimation of potential NPK input from livestock wastes since 1990. Proceeding of Korean Soc. of Soil Sci. Fert. pp. 156-156.
  20. Zhou, M. and Y. Li. 2001. Phosphorus-sorption characteristics of calcareous soils and limestone from southern Everglades and adjacent farmlands, Soil Sci. Soc. Am. J. 65:1404-1412. https://doi.org/10.2136/sssaj2001.6551404x