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Fig. 3. The average measured percentages (n = 10) of soil masses removed from aggregate surfaces with increasing erosion times for different aggregate-size fractions from field CT, NT, and NF management systems on (A) Hoytville silty clay loam and (B) Wooster silt loam soils. Some percentage of peeled values not measured at the given erosion time were linearly interpolated between two closest points to take the average of 10 aggregates. Exterior, Transitional, and Interior represent concentric regions within aggregates as presented in Fig. 1B.
