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Effect of salt, alkali and zinc on iron equilibrium in submerged soils

Published online by Cambridge University Press:  27 March 2009

U. S. Sadana
Affiliation:
Department of Soils, Punjab Agricultural University, Ludhiana, India
P. N. Takkar
Affiliation:
Department of Soils, Punjab Agricultural University, Ludhiana, India

Abstract

Summary

In a pot experiment the effect of salt (EC 5, 10 and 20mmhos/cm at 25 °C), alkali (ESP 10, 20 and 40) and Zn (lOmgZn/kg soil) on Fe equilibria in submerged soils was studied. The required salt and alkali concentrations were obtained by adding calculated amounts of NaCl and NaHCO3 respectively to Rohi sandy loam (Typic Ustifluvent). The soil solutions drawn anoxically by gravity were analysed for pH, pE, EC and Fe. As the EC increased, pH and pE of the soil solution decreased and Fe concentration increased at all the stages of submergence. ESP had the opposite effect. Addition of ZnSO4 in combination with EC and ESP treatments further decreased pH and pE and increased Fe concentration; however, its effect was more pronounced in the former treatments. In spite of wide variation in pH, pE and Fe concentration in soil solution, the values of the expressions pE – pFe2+ + 3pH, pE – 1·5 pFe2+ + 4 pH and pE + pH were nearly constant and close to the standard values of 17·9, 23·3 and 7·3 for Fe(OH)3 – Fe2+, Fe3(OH)8 – Fe2+ and Fe(OH)3 – Fe3(OH)8 systems after 1, 14 and 14 days of submergence, respectively. Addition of ZnSO4 did not have an appreciable effect on these systems in salt- and alkalitreated soils.

Type
Research Article
Copyright
Copyright © Cambridge University Press 1985

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References

Bhumbla, D. B. (1972). Reclamation of saline and alkali soils. Indian Farming 22, 1921.Google Scholar
Gotoh, S. & Patrick, W. H. Jr (1974). Transformation of iron in a waterlogged soil as influenced by redox-potential and pH. Soil Science Society of America Proceedings 38, 6671.CrossRefGoogle Scholar
Griffin, R. A. & Jurinak, J. J. (1973). Estimation of activity coefficients from the electrical conductivity of natural aquatic systems and soil extracts. Soil Science 116, 2630.CrossRefGoogle Scholar
International Rice Research Institute (1964). Annual Report. Los Banos, Philippines: International Rice Research Institute.Google Scholar
Ponnamperuma, F. N. (1965). Dynamic aspects of flooded soils and the nutrition of rice plant. In Mineral Nutrition of Rice Plants. Baltimore, Maryland: Johns Hopkins Press.Google Scholar
Ponnamperuma, F. N. (1972). The chemistry of submerged soils. Advances in Agronomy 24, 2996.Google Scholar
Ponnamperuma, F. N., Tianco, E. M. & Loy, T. (1967). Redox equilibria in flooded soils. 1. The iron hydroxide systems. Soil Science 103, 374382.CrossRefGoogle Scholar
Stumm, W. & Morgan, J. J. (1970). Aquatic Chemistry. New York: John Wiley & Sons.Google Scholar
Takkar, P. N. & Sidhu, B. S. (1979). Kinetics of zinc transformations in submerged alkaline soils in the rice growing tracts of Punjab. Journal of Agricultural Science, Cambridge 93, 441447.CrossRefGoogle Scholar