For a robust description of the sediment bed, critical shear stress and erosion rates can be correlated with measurements of particle size distribution, bulk density, or other geotechnical parameters. Results can be used to compare disparate areas and depths within the system to determine more or less erodible areas relative to a site average.
Experienced Team of Sediment Scientists
Jones, C.A., and B.E. Jaffe. 2013. Influence of history and environment on the sediment dynamics of intertidal flats. Marine Geology, 345:, 294-303.
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