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Published in Soil Sci Soc Am J 46:970-976 (1982)
© 1982 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Changes in Inorganic and Organic Soil Phosphorus Fractions Induced by Cultivation Practices and by Laboratory Incubations1

M. J. Hedley2, J. W. B. Stewart and B. S. Chauhan3,4,

ABSTRACT

Changes in inorganic and organic phosphorus (P) fractions resulting from 65 years of cropping in a wheat-wheat-fallow rotation were studied using a sequential extraction technique. Total P content of the cultivated soil was 29% lower than that of the adjacent permanent pasture; the major loss of P (74% of total P lost) was organic P and residual P. Of the total P lost, 22% was from the extractable organic P forms, whereas 52% originated from stable P.

Incubation studies were used to study seasonal P transformations during simulated fallow with and without residue incorporation and P fertilization. Nine monthly additions of cellulose (765 µg C · g–1 soil) with and without P (9 µg · g–1 soil) significantly altered levels of total extractable organic P and inorganic P in incubated soils. Evidence is provided for microbial activity playing a major role in redistributing P into different forms in the soil.


NOTES

1 Journal Paper no. R281 of the Saskatchewan Institute of Pedology, University of Saskatchewan, Saskatoon, Saskatchewan. Research supported by the Natural Science and Engineering Research Council of Canada, Western Cooperative Fertilizer Ltd., and by a Post Doctorate Fellowship (M.J.H.) from the University of Saskatchewan.

2 Present address: Soil Science Laboratory, Dep. of Agric. Sci., Oxford University, Oxford, England, OX13PF.

3 Present address (B.S.C.): N.E.H.U., College of Agric., Medziphema, Nagaland, India.

4 Post Doctorate Fellow, Professor of Soil Science and Post Doctorate Fellow, respectively, Saskatchewan Institute of Pedology.

Received for publication March 23, 1981. Accepted for publication June 2, 1982.




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Copyright © 1982 by the Soil Science Society of America.