26 cultivated benchmark sites established in the mid-1960s were resampled in the early 1980s. Soil losses up to 10 kg m-2 yr-1 were calculated, but some sites showed deposition. Changes in organic C in the 0 to 0.15-m layer could be explained largely by erosion and deposition. -from Authors
CITATION STYLE
De Jong, E., & Kachanoski, R. G. (1988). The importance of erosion in the carbon balance of prairie soils. Canadian Journal of Soil Science, 68(1), 111–119. https://doi.org/10.4141/cjss88-010
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