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Changes in Inorganic and Organic Soil Phosphorus Fractions Induced by Cultivation Practices and by Laboratory Incubations

Soil Science Society of America Journal · 1982 · Vol. 46(5) · pp. 970–976
M. J. HedleyJohn StewartBhagirath Singh Chauhan

Abstract

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.

Soil and Water Nutrient DynamicsSoil Carbon and Nitrogen DynamicsPhosphorus and nutrient managementPasturePhosphorusChemistrySoil waterIncubationAgronomyAnimal scienceResidue (chemistry)Human fertilizationEnvironmental chemistry

Funding

  • Natural Sciences and Engineering Research Council of Canada
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