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Joel S. Scheingross, Eric W. Winchell, Michael P. Lamb and William E. Dietrich Influence of bed patchiness, slope, grain hiding, and form drag on gravel mobilization in very steep streams Journal of Geophysical Research: Earth Surface 118

Version of Record online: 10 JUN 2013 | DOI: 10.1002/jgrf.20067

Key Points

  • We observe active fluvial transport in steep streams up to 37% slope.
  • Sediment transport laws for low-gradient rivers need adjustment in steep streams
  • Channel slope, patches, and grain hiding strongly influence incipient motion

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