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Published in Soil Sci Soc Am J 37:915-918 (1973)
© 1973 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Sulfur Fractions and Carbon, Nitrogen, and Sulfur Relationships in Grassland, Forest, and Associated Transitional Soils1

J. R. Bettany, J. W. B. Stewart and E. H. Halstead2

ABSTRACT

The amounts of total S, organic N, organic C, and HI-reducible-S obtained from Ap layers of 54 soils collected from five major soil zones in Saskatchewan varied considerably with location within any one zone. However, the mean C/S, N/S ratios and the percentage of total S as HI-reducible S of the soil organic matter showed similar and consistent trends. The C/N/S ratios ranged from 58:6.4:1 in the arid Chernozemic Brown soils to 129:10.6:1 in the leached Grey Wooded soils. The percentage of total S as HI-reducible was approximately 50% in the Chernozemic soils in contrast to 36% in the Grey Wooded soils.


NOTES

1 Contribution from the Saskatchewan Inst. of Pedology no. R118. This work has been supported by grants from the Sulphur Inst. and National Research Council of Canada (A4474).

2 Assistant and Associate Professors, Dep. of Soil Science, Univ. of Saskatchewan, Saskatoon, Canada, respectively.

Received for publication June 4, 1973. Accepted for publication July 18, 1973.







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