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Fig. 4. Cumulative increases in erosive strength (Es) in aggregates, (A) 6.3 to 9.5 mm and (B) 4 to 6.3 mm, from Hoytville silty clay loam soils at depths from 0 to 5 cm, as aggregates were peeled in SAE chambers. These Es lines were obtained by taking average of Es values fitted in a regression Eq. [6] for each aggregate (Table 1). R2 values represent a measure of closeness between measured data and fitted lines for each treatment.