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Published in Soil Sci Soc Am J 31:521-528 (1967)
© 1967 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Soil Phosphorus in South Dakota: III. Phosphorus Fractions of Some Borolls and Ustolls1

F. C. Westin and G. J. Buntley2

ABSTRACT

The data for the phosphorus fractions and carbon and nitrogen for 8 soils classified as Borolls and 8 as Ustolls along a 260-km transect are compared. The Ustolls generally have, in their upper horizons, appreciably more Fe-P, and reductant-P, less Ca-P, and slightly less Al-P than the Borolls. Organic P values are a little higher and carbon and nitrogen percentages are slightly lower among the Ustolls.

In general, the ratio of carbon to phosphorus in the organic matter is lower among the Ustolls indicating that there probably is a higher rate of mineralization of organic P taking place in the Ustolls than in the Borolls.

The proportions of the phosphorus fractions in the various horizons of the soils appear to reflect the climatic change occurring along the transect.

Key Words: organic phosphorus C/N/P ratios • Chernozem soils • Seventh Approximation


NOTES

1 Contribution from the Department of Agronomy, Agr. Exp. Sta., South Dakota State University, Brookings. Approved for publication by the Director of the South Dakota Agr. Exp. Sta. as Journal Series no. 750.

2 Professor and Associate Professor of Agronomy, respectively, South Dakota State University, Brookings.

Received for publication November 2, 1966. Accepted for publication April 5, 1967.







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The Plant Genome
Copyright © 1967 by the Soil Science Society of America.