pone.0262865.g004.tif (647.95 kB)
Download fileEffects of runoff depth–flow velocity interaction on the differences in the percentages of effective to dispersed (Der; %) fine sand (0.05–0.25 mm) or coarse sand (>0.25 mm).
figure
posted on 2022-02-22, 19:02 authored by Lin Liu, Zhongwu Li, Panpan JiaoDer (0.05–0.25 mm) is the difference in the percentages of effective to dispersed 0.05–0.25 mm sediment particles; Der (> 0.25 mm) is the difference in the percentages of effective to dispersed > 0.25 mm sediment particles.
History
Usage metrics
Categories
Keywords
simulated rainfall experimentsobtained regression functionsinduced overland flows120 mm hsup >&# 8722>< sup ><05 mm particlestransport way differeffecting aggregate stripping>< sub ><2 mm (<sized sediment particlestransport limit erosionrainfall intensity coulddiv >< phydraulic transport mechanismsflow velocities lowercritical flow velocitydifferent size particlessoil organic carbondifferent hydraulic mechanismsunevenly enriched oc1 uneven oc enrichmentsediment particleshydraulic mechanismsflow velocityaggregate transportunevenly enrichedorganic carbon>2 transport processwater erosionsize classesloess soilhydraulic factorcritical value>oc enrichmentoc uneven enrichmentenrichment ratiooc concentrationsr p ocs erocs er two typesrunoff depthresults showedmineralization potentialimportant referencefindings provideessential conditionsdistinct lawscompletely understood15 °005 ).005 ),
