2008
DOI: 10.2478/v10066-008-0004-y
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Application of geochemical markers as a test for assessment of intensity of contemporary colluvial and alluvial sedimentation

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“…However, the calculated annual soil erosion rates were not large and amounted to 1.41 mm ha −1 . The calculated rate is smaller than the range of annual erosion (2–7 mm) in the Lublin Upland [ 36 – 39 ]. The pattern of soil redistribution with the zones of eroded soils is separated by depositional soils fits to the areas where soil translocation due to tillage is a dominant part of erosion [ 40 , 41 ].…”
Section: Discussionmentioning
confidence: 99%
“…However, the calculated annual soil erosion rates were not large and amounted to 1.41 mm ha −1 . The calculated rate is smaller than the range of annual erosion (2–7 mm) in the Lublin Upland [ 36 – 39 ]. The pattern of soil redistribution with the zones of eroded soils is separated by depositional soils fits to the areas where soil translocation due to tillage is a dominant part of erosion [ 40 , 41 ].…”
Section: Discussionmentioning
confidence: 99%