Relating soil properties to soil losses by wind erosion in a cultivated organic soil in the southwest of Quebec, Canada

Cultivated organic soils are known to be highly susceptible to wind erosion. The aim of this research was to explore the relationships between organic soil properties and measured soil height variation (SHV) in a cultivated organic soil and to analyze field soil erodibility (wind erodibility index: WEI) from known models. In the fall, 81 georeferenced soil samples were collected at a depth of 0–10 cm and analyzed in the laboratory to determine different soil properties. At the same time, soil height variations were measured over a 35-day period. Simple and multiple linear regressions were used to explore relationships between soil properties and analyze SHV and WEI. The average SHV across the farm was −0.19 mm per day, equivalent to a loss of 0.665 cm during the measurement period. Simple linear regression showed weak relationships with SHV. Nevertheless, the analysis showed that soil loss areas had a larger fraction of macro-aggregates. Conversely, deposition areas with low bulk density (BD) contained more fine material (organic matter [OM] and erodible material [EM]), suggesting wind erosion effects, i.e., deposition of fine matter. Many soil properties were found to correlate significantly with one another. Applying multiple linear regression with SHV and WEI as dependent variables and soil properties as independent variables produced the following results: a) 24% of the SHV was significantly explained by 6 soil properties (α=5%,p=0.001), BD, EM, mean weight diameter (MWD), elevation (Z), geometric mean diameter (GMD), and volumetric water (VW); and b) 75% of the variation in WEI was explained by 5 variables (α=5%,p=0.001), BD, VW, OM, MWD and GMD. This result shows that BD, VW, OM, MWD, EM, GMD, elevation Z are key soil properties in sustainable management of organic soil with >80% OM and will be used in a wind erosion risk model adapted to organic soils.