Effects of human alterations on the hydrodynamics and sediment transport in the Sacramento-San Joaquin Delta, California

The Sacramento-San Joaquin Delta, California, (Delta) has been significantly altered since the mid-nineteenth century. Many existing channels have been widened or deepened and new channels have been created for navigation and water conveyance. Tidal marshes have been drained and leveed to form islan...

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Main Authors: M. D. Marineau, S. A. Wright
Format: Article
Language:English
Published: Copernicus Publications 2015-03-01
Series:Proceedings of the International Association of Hydrological Sciences
Online Access:https://www.proc-iahs.net/367/399/2015/piahs-367-399-2015.pdf
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spelling doaj-4320a821271d4c94b1de07dce8a8b98e2020-11-24T22:49:12ZengCopernicus PublicationsProceedings of the International Association of Hydrological Sciences2199-89812199-899X2015-03-0136739940610.5194/piahs-367-399-2015Effects of human alterations on the hydrodynamics and sediment transport in the Sacramento-San Joaquin Delta, CaliforniaM. D. Marineau0S. A. Wright1US Geological Survey, 6000 J Street, Placer Hall, Sacramento, California, USAUS Geological Survey, 6000 J Street, Placer Hall, Sacramento, California, USAThe Sacramento-San Joaquin Delta, California, (Delta) has been significantly altered since the mid-nineteenth century. Many existing channels have been widened or deepened and new channels have been created for navigation and water conveyance. Tidal marshes have been drained and leveed to form islands that have subsided, some of which have permanently flooded. To understand how these alterations have affected hydrodynamics and sediment transport in the Delta, we analysed measurements from 27 sites, along with other spatial data, and previous literature. Results show that: (a) the permanent flooding of islands results in an increase in the shear velocity of channels downstream, (b) artificial widening and deepening of channels generally results in a decrease in shear velocity except when the channel is also located downstream of a flooded island, (c) 1.5 Mt/year of sediment was deposited in the Delta (1997–2010), and of this deposited sediment, 0.31 Mt/year (21%) was removed through dredging.https://www.proc-iahs.net/367/399/2015/piahs-367-399-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. D. Marineau
S. A. Wright
spellingShingle M. D. Marineau
S. A. Wright
Effects of human alterations on the hydrodynamics and sediment transport in the Sacramento-San Joaquin Delta, California
Proceedings of the International Association of Hydrological Sciences
author_facet M. D. Marineau
S. A. Wright
author_sort M. D. Marineau
title Effects of human alterations on the hydrodynamics and sediment transport in the Sacramento-San Joaquin Delta, California
title_short Effects of human alterations on the hydrodynamics and sediment transport in the Sacramento-San Joaquin Delta, California
title_full Effects of human alterations on the hydrodynamics and sediment transport in the Sacramento-San Joaquin Delta, California
title_fullStr Effects of human alterations on the hydrodynamics and sediment transport in the Sacramento-San Joaquin Delta, California
title_full_unstemmed Effects of human alterations on the hydrodynamics and sediment transport in the Sacramento-San Joaquin Delta, California
title_sort effects of human alterations on the hydrodynamics and sediment transport in the sacramento-san joaquin delta, california
publisher Copernicus Publications
series Proceedings of the International Association of Hydrological Sciences
issn 2199-8981
2199-899X
publishDate 2015-03-01
description The Sacramento-San Joaquin Delta, California, (Delta) has been significantly altered since the mid-nineteenth century. Many existing channels have been widened or deepened and new channels have been created for navigation and water conveyance. Tidal marshes have been drained and leveed to form islands that have subsided, some of which have permanently flooded. To understand how these alterations have affected hydrodynamics and sediment transport in the Delta, we analysed measurements from 27 sites, along with other spatial data, and previous literature. Results show that: (a) the permanent flooding of islands results in an increase in the shear velocity of channels downstream, (b) artificial widening and deepening of channels generally results in a decrease in shear velocity except when the channel is also located downstream of a flooded island, (c) 1.5 Mt/year of sediment was deposited in the Delta (1997–2010), and of this deposited sediment, 0.31 Mt/year (21%) was removed through dredging.
url https://www.proc-iahs.net/367/399/2015/piahs-367-399-2015.pdf
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