Geological material:
The soil is a swinton loam to silt loam, an Orthic Brown Chernozem (Aridic Haploboroll) developed from aeolian deposits that overlie galcial till. It has an Ap horizon 0 to 8 cm thick with moderate, medium subangular, blocky primary structure that crushes to moderate, fine granular secondary structure. The Bm1 (8 to 24 cm) and Bm2 (24 to 48 cm) have a silt loam texture with strong, medium prismatic structure; the Ck (40 to 79 cm) has a silt loam texture with massive structure; and the 11C1 (79 to 104 cm) and 11C2 (104 to 129 cm) have a clay loam texture with massive structure.