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a Department of Agroecology, Danish Institute of Agricultural Sciences, Research Centre Foulum, 8830 Tjele, Denmark
b Department of Geography, University of Exeter, Amory Building, Exeter, EX4 4RJ, UK
c Laboratory for Experimental Geomorphology, Catholic University of Leuven, Redingenstraat 16, 3000 Leuven, Belgium
* Corresponding author (goswin.heckrath{at}agrsci.dk)
Received for publication April 12, 2004. Tillage erosion had been identified as a major process of soil redistribution on sloping arable land. The objectives of our study were to investigate the extent of tillage erosion and its effect on soil quality and productivity under Danish conditions. Soil samples were collected to a 0.45-m depth on a regular grid from a 1.9-ha site and analyzed for 137Cs inventories, as a measure of soil redistribution, soil texture, soil organic carbon (SOC) contents, and phosphorus (P) contents. Grain yield was determined at the same sampling points. Substantial soil redistribution had occurred during the past decades, mainly due to tillage. Average tillage erosion rates of 2.7 kg m2 yr1 occurred on the shoulderslopes, while deposition amounted to 1.2 kg m2 yr1 on foot- and toeslopes. The pattern of soil redistribution could not be explained by water erosion. Soil organic carbon and P contents in soil profiles increased from the shoulder- toward the toeslopes. Tillage translocation rates were strongly correlated with SOC contents, A-horizon depth, and P contents. Thus, tillage erosion had led to truncated soils on shoulderslopes and deep, colluvial soils on the foot- and toeslopes, substantially affecting within-field variability of soil properties. We concluded that tillage erosion has important implications for SOC dynamics on hummocky land and increases the risk for nutrient losses by overland flow and leaching. Despite the occurrence of deep soils across the study area, evidence suggested that crop productivity was affected by tillage-induced soil redistribution. However, tillage erosion effects on crop yield were confounded by topographyyield relationships.
Abbreviations: AWC, available water capacity LS, lengthslope SOC, soil organic carbon
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