Three distinctive types of banded fabric related to the degree of eluviation were observed in Ae horizons of Saskatchewan soils. In addition, a type of intertextic fabric and cleavage block fabric were found to be characteristic of the upper and lower portions respectively of Ae horizons. Although essentially similar fabrics can occur within Ae horizons of Chernozemic, Solonetzic, Podzolic, and Gleysolic soils, the occurrence of specific fabric types appears to be related to the degree of eluviation which the horizons have undergone and bears a general relationship to the macrostructure exhibited by the soil.
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Dumanski et al. (1966) studied this question.
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