Texture, Mineralogy, and Lamellae Development in
Sandy Soils in Michigan
Randall J. Schaetzl
The texture, mineralogy, and to a lesser extent topography, of some sandy soils in Michigan were examined to determine the possible genesis of lamellae in these soils. Differences in lamellae presence and depth were studied in four Haplorthods, one Argic Udipsamments and one Psammentic Eutroboralf on a subtly undulating terrace in northern lower Michigan. Dolomite or feldspar weathering was not pronounced in these well-drained soils; one pedon retained substantial carbonates at depth, probably mainly within lamellae. Significant correlations ® were observed between the depth to the uppermost textural band (an indication of the amount and development of lamellae for the entire profile) and profile-weighted contents of the following size separates: <50mm (-0.82*, significant as P , 0.05), < 125 mm (-0.92*), 250-2 mm (0.90*), and 2000-500 mm (0.96**, significant at P < 0.01). Correlations between clay content and depth to first lamella were not significant (r = -0.72), suggesting that sandy pedons dominated by fine sands and silts are more likely to have lamellae than are those with more clay. Clay inherited from the parent material was probably rapidly translocated downward to form lamellae; deep translocation out of the solum is especially plausible in the coarser textured Haplorthods. Deposition of clay in textural bands is probably due, initially, to cessation of wetting fronts or flocculation by carbonates. Sieving processes may act to thicken these features, especially in finer textured pedons. Lithologic discontinuities may have also affected lamellae formation by stopping wetting fronts at or near sites of textural change. Topographic factors also contributed to lamellae formation; pedons within and near a small depression had thicker and shallower lamellae than did those on uplands, possibly due to lateral translocation of colloids.