Characteristics of the organic matter in a slightly and in a severely crusted soil

Chemical and spectroscopic characteristics were determined on the organic matter in two Luvisolic soils from northwestern Alberta, Canada. One of these (the Debolt soil) is known to crust only slightly while the other (the Demmitt soil) exhibits severe crusting after heavy rainfalls. The Debolt top soil is richer in total C, total N, carbohydrates and proteinaceous materials than the Demmitt top soil. Humic acid extracted from the Debolt soil is more aliphatic, and contains fewer CO₂H groups than does humic acid extracted from the Demmitt soil. The quality of the organic matter appears to play a role in soil crusting.