Spodosol
Development as Affected by Geomorphic Aspect,
Baraga County,
Michigan
Robert V. Hunckler and Randall J. Schaetzl
In midlatitude locations with steep
slopes, geomorphic aspect can be an important factor in determining spatial
variations in soil development. This
study examines the influence of aspect on soil development in Baraga County,
Michigan, as a means of explaining within-landform variability. The soils are sandy and have spodic
morphologies. All are located on steep
slopes (45-73%) of contrasting aspect.
Ten pedons each from backslopes on north-to-northeast-(N-NE) and
south-to-southwest-(S-SW) facing slopes were described, sampled, and compared
using standard techniques.
Variation in slope gradient was not,
statistically, a determining factor in the differential soil development found
here. Aspect has strongly influenced
soil development, however, with soils more strongly developed (i.e., more
podzolized) on N-NE slopes than on S-SW slopes. Several soil characteristics indicative of strong podzolization
were found on N-NE slopes, including higher values of solum thickness and POD
index, greater losses of extractable Fe and Al from E horizons and concomitant
gains in B horizons, and darker and redder B horizon colors. Soils were generally cooler on N-NE slopes
in summer, with essentially similar temperatures under snowpacks in
winter. Cooler temperatures and greater
amounts of infiltrating water in soils with N-NE aspects may have accelerated podzolization
by allowing more organo-metallic complexes to be formed and translocated. Podzolization driven by translocation of
amorphous, inorganic compounds appears, however, to be nearly equivalent on
sites of differing aspect.
Of the ten pedons on N-NE slopes, nine classified as Spodosols (Entic or Typic Haplorthods) and the other was an Entisol. Seven of the 10 pedons on S-SW slopes classified as Entisols (Udipsamments or Udorthents), and the remaining three were Spodosols.