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Sediment transport pathway in the back of a nearly semienclosed subembayment of San Francisco Bay, California

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Abstract

Time series measurements of current velocity, depth and suspended-solids concentration (SSC) were used to obtain suspended-solids fluxes (SSF) during the fall at central Honker Bay and Spoonbill Creek. A wind-induced shear stress increases SSF out of Honker Bay through Spoonbill Creek by combining two effects: (1) wind-wave resuspension of bed sediments, and (2) wind shear raises the water level at the Honker Bay. High SSC water advected from Honker Bay into the Sacramento River does not return on the following ebb tide, which creates the dispersive SSF. The total SSF was always out of Honker Bay during the fall suggesting that high metals and pesticides concentrations are not caused by transport through Spoonbill Creek into Honker Bay.

Additional Publication Details

Publication type:
Conference Paper
Publication Subtype:
Conference Paper
Title:
Sediment transport pathway in the back of a nearly semienclosed subembayment of San Francisco Bay, California
Volume
B pt 2
Year Published:
1997
Language:
English
Publisher:
ASCE
Publisher location:
New York, NY, United States
Larger Work Title:
Proceedings, Congress of the International Association of Hydraulic Research, IAHR
First page:
1096
Last page:
1101
Number of Pages:
6
Conference Title:
Proceedings of the 1997 27th Congress of the International Association of Hydraulic Research, IAHR. Part D
Conference Location:
San Francisco, CA, USA
Conference Date:
10 August 1997 through 15 August 1997