Summary
The estimation of free iron oxide by Deb's method in the red soils derived from basement complex containing mostly acid gneiss of Tanga region, Tanzania, was carried out. The results of the investigation revealed that the free iron oxide varied between 2 and 8 per cent and exhibited a highly significant correlation with the clay content of the soils. The amount of free iron oxide also, usually, increased with the depth of the soil profile. re]19730730
References
Bachler, W., and Hackl, H., Bundes Vers. Inst. Kulturtech. Tech. Bondenk., 23, (1965).
Deb, B. C., J. Soil Sci. 1, 212–20 (1950).
Hoores, J. D., Proc. 2nd Interafr. Soils Conf. 1, 261–74 (1954).
Hoores, J. L. D., et al., Proc. 2nd Interafr. Soils Conf. 1, 257–60 (1954).
Houng Kun-Huang and Chen Tsen-Tuo, Soil Sci. Soc. Am. Proc. 23, 270–73 (1959).
Kilmer, J., Soil Sci. Soc. Am. Proc. 24, 420–21 (1960).
Middleton, K. R., Soil Sci. 100, 361–67 (1965).
Nandra, S. S., and Rijkebusch, P. A. H., Ann. Rept. Tanganyika Sisal Growers' Association, Tanga, Tanzania, (1967/68).
Olsen, R. V., Methods of Soil Analysis, part 2, Am. Soc. Agronomy, series No. 9, 971 (1965).
Ramulu, U. S. S. et al., Soil Sci. Soc. Am. Proc. 31, 248–55 (1967).
Russell, E. W., Soil Conditions and Plant Growth. Longmans Green and Co Ltd., 481 (1963).
Soileau, J. M., and Maccracken, R. J., Soil Sci. Soc. Am. Proc. 31, 248–55 (1967).
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Nandra, S.S. Free iron oxide content of a tropical soil. Plant Soil 40, 453–456 (1974). https://doi.org/10.1007/BF00011532
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DOI: https://doi.org/10.1007/BF00011532