DISTRIBUTION OF SAND TRANSPORT RATE ACROSS A SURF ZONE

Toru Swaragi; Ichiro Deguchi

doi:10.9753/icce.v16.95

No. 16 (1978), Conference Proceedings

No. 16 (1978)

DISTRIBUTION OF SAND TRANSPORT RATE ACROSS A SURF ZONE

Conference Proceedings

https://doi.org/10.9753/icce.v16.95

Published 1978-01-29

Toru Swaragi⁺⁻
Ichiro Deguchi⁺⁻

Toru Swaragi

Osaka University

Ichiro Deguchi

Osaka University

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Keywords

sediment transport
surf zone
transport rate

How to Cite

Swaragi, T., & Deguchi, I. (1978). DISTRIBUTION OF SAND TRANSPORT RATE ACROSS A SURF ZONE. Coastal Engineering Proceedings, 1(16), 95. https://doi.org/10.9753/icce.v16.95

Abstract

The distributions of longshore and on-offshore sediment transport rates in a surf zone were measured by an apparatus which was able to separately record both components of the sediment transport rate,, The characteristics of their distributions were discussed from the bottom shear stresses which were measured by the shear meter under the same wave conditions as the laboratory experiment of the sediment transport. The maximum bottom shear stress took place at the depth between the breaking depth of waves and the depth where the velocity of the longshore current showed a maximum. On the other hand, the maximum on-offshore and longshore sediment transport rates occured at the depth slightly shallower than the depth where the maximum bottom shear stress took place. What's more, the longshore sediment transport rates were represented by the longshore current velocity and the bottom shear stress generated by waves and the longshore current. However, the distribution of the on-offshore sediment transport rates showed more complicated profile than that of the longshore sediment transport rates because there were no eminent unidirectional flow in the direction normal to the shore line. Therefore, the on-offshore sediment transport rates could not be formulated by the bottom shear stresses.

https://doi.org/10.9753/icce.v16.95

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DISTRIBUTION OF SAND TRANSPORT RATE ACROSS A SURF ZONE

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