Brief Report
Apr 1979
Kaolinite Resuspension Properties
Publication: Journal of the Hydraulics Division
Volume 105, Issue 4
Abstract
Limited experiments on the initiation of motion of sand grains in the annular channel-ring system showed a reasonable agreement with Shields. curve for incipient motion. The resuspension rates of stratified beds continuously decrease, and may even become zero, as the depth of erosion increases. On the other hand, the erosion rates of uniform beds remain constant. This is in agreement with earlier observations on natural bay deposits. The nondimensional plot of the erosion rate against the bed shear stress for uniform beds agrees with earlier results based on soils with drastically different mineralogical composition.
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Published In
Journal of the Hydraulics Division
Volume 105 • Issue 4 • April 1979
Pages: 411 - 416
Copyright
© 1979 American Society of Civil Engineers.
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Published in print: Apr 1979
Published online: Feb 3, 2021
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Authors
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Ashish J. Mehta, AM.ASCE
Asst. Prof., Dept. of Coastal and Oceanographic Engrg., Univ. of Florida, Gainesville, Fla.
Emmanuel Partheniades, M.ASCE
Prof. of Hydr. Structures, Aristoteles Univ. of Thessaloniki, Greece; and Prof., Dept. of Engrg. Sci., Univ. of Florida, Gainesville, Fla.
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Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.
Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.