We worked on four catenas (representing Brown, Dark Brown and Black Chernozemic soils, and a Luvisolic soil) which encompass a narrow environmental gradient of climate (annual precipitation: 300-475mm) and vegetation. The distribution of organic P along the catenas and among the soil zones was related to the transformations of inorganic P caused by differences in weathering intensity between slope positions and across the Province (of Saskatchewan). -from Authors
CITATION STYLE
Roberts, T. L., Stewart, J. W. B., & Bettany, J. R. (1985). The influence of topography on the distribution of organic and inorganic soil phosphorus across a narrow environmental gradient. Canadian Journal of Soil Science, 65(4), 651–665. https://doi.org/10.4141/cjss85-071
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