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ABSTRACT
The spatial variability of natural 15N abundance of a cultivated Chernozemic soil and its native prairie counterpart were smaller than that of total N, organic C, and the C/N ratio. Further, the number of samples required to estimate the true mean of total N with a given precision at various probability levels were twofold those required to determine the mean 15N abundance in both soils. The variability of organic C was > 10 times that observed for total N. The results of this study indicate that the spatial variability of the natural 15N abundance of total soil N in the surface horizons may reflect the isotopic composition of the nitrogenous substances entering the soil system or changes in the isotopic composition of soil N due to humification processes, probably induced by variations in topographic and microrelief features of the soil.
1 Publication no. R431 of the Saskatchewan Institute of Pedology, Univ. of Saskatchewan, Saskatoon, Saskatchewan, Canada, S7N 0W0. Research supported by the Natural Sciences and Engineering Research Council of Canada.
2 Research Scientist, Agriculture Canada Research Station, P.O. Box 1030, Swift Current, Sask., Canada S9H 3X2; Assistant Professor, Dep. Renewable Resources, Macdonald College of McGill Univ., Ste. Anne de Bellevue, Quebec, Canada H9X 1C0; and Assistant Professor, Dep. Land Resource Sciences, Univ. of Guelph, Guelph, Ontario, Canada.
Received for publication March 13, 1985. Accepted for publication September 6, 1985.
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