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ABSTRACT
A procedure is described to study chemical heterogeneity of soil material within natural aggregates. Soil from aggregate surfaces is separated from interior material by a freezing and thawing process. Results for two soils indicate higher concentrations of water-soluble elements in the exterior soil material, whereas, the interior material contained about equal or slightly greater amounts of extractable elements than the exterior material.
Key Words: ion movement in soil aggregates
1 Contribution from the Corn Belt Branch, Soil and Water Conservation Research Division, ARS, USDA, in cooperation with the Minnesota Agr. Exp. Sta.
2 Research Soil Scientists, North Central Soil Conservation Research Center, Agricultural Research Service, USDA, Morris, Minn.
Received for publication March 16, 1967. Accepted for publication June 13, 1967.
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