SSSAJ Journal of Natural Resources and Life Sciences Education
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Fig. 3. Erosion rate as a function of cumulative flow time for the clay soil and silt loam at Stage 1 (a) and Stage 2 (b) of the experiment. For a given cumulative flow time, and within a soil, bars labeled by the same letter (lower case for the clay soil and upper case for the loess) do not differ significantly at the 0.05 level





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