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dc.contributor.authorSander, G.C.
dc.contributor.authorParlange, J.-Y.
dc.contributor.authorBarry, D.A.
dc.date.accessioned2012-07-20T14:28:31Z
dc.date.available2012-07-20T14:28:31Z
dc.date.issued2012-05
dc.identifier.urihttps://hdl.handle.net/1813/29547
dc.descriptionOnce downloaded, these high definition QuickTime videos may be played using a computer video player with H.264 codec, 1280x720 pixels, millions of colors, AAC audio at 44100Hz and 29.97 frames per second. The data rate is 5Mbps. File sizes are on the order of 600-900 MB. (Other formats may be added later.) Free QuickTime players for Macintosh and Window computers may be located using a Google search on QuickTime. The DVD was produced by J. Robert Cooke.en_US
dc.description.abstractSediment transport hysteresis occurs due to the different sediment fluxes for the same discharge on the rising and falling limb of the overland flow hydrograph. Experimental field data has shown that the common shapes of the hysteresis loops encompass (i) clockwise, (ii) anti-clockwise and (iii) figure 8 with both flow orientations. It has been suggested that the shape of these loops can be used to identify the different processes of runoff and sediment transport and the sediment source area. We present simulations carried out using the Hairsine-Rose (HR) erosion model which reproduces all of the above hysteresis loops for flow conditions that are straightforward to establish within a laboratory flume. As both agricultural chemical and biological pathogens bind preferentially to the clay and silt sized particles, estimating contaminant fluxes to surface water bodies requires knowledge of the size distribution of transported sediment. We also present some recent work on extending the HR model from discrete sediment size classes to a continuous distribution of sizes along with some corresponding solutions.en_US
dc.publisherInternet-First University Pressen_US
dc.subjectsoil erosionen_US
dc.subjectsediment size class distributionsen_US
dc.subjectsediment discharge hysteresisen_US
dc.subjectclockwiseen_US
dc.subjectanti-clockwiseen_US
dc.subjectfigure eight loopsen_US
dc.subjectdistributed sediment sourcesen_US
dc.titleA1. Modelling hysteresis in sediment transport and continuous distributions of eroded sedimenten_US
dc.typevideo/moving imageen_US
dc.description.viewer1_me8b0y04en_US


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