Dimensionless argument: a narrow grain size range near 2 mm plays a special role in river sediment transport and morphodynamics
(2024)
Journal Article
Parker, G., An, C., Lamb, M. P., Garcia, M. H., Dingle, E. H., & Venditti, J. G. (2024). Dimensionless argument: a narrow grain size range near 2 mm plays a special role in river sediment transport and morphodynamics. Earth Surface Dynamics, 12(1),
The grain size 2 mm is the conventional border between sand and gravel. This size is used extensively, and generally without much physical justification, to discriminate between such features as sedimentary deposit type (clast-supported versus matrix... Read More about Dimensionless argument: a narrow grain size range near 2 mm plays a special role in river sediment transport and morphodynamics.