Literature DB >> 17812801

Turbidity maximum of the northern chesapeake bay.

J R Schubel.   

Abstract

The turbidity maximum near the head of the Chesapeake Bay is produced primarily by the local resuspension of bottom sediments, and by the estuarine "sediment trap" which is formed in the upper reaches of the estuarine circulation regime by the net nontidal circulation.

Entities:  

Year:  1968        PMID： 17812801     DOI： 10.1126/science.161.3845.1013

Source DB:  PubMed          Journal:  Science        ISSN： 0036-8075            Impact factor:   47.728


  3 in total

1.  Tidal and meteorological forcing of sediment transport in tributary mudflat channels.

Authors:  David K Ralston; Mark T Stacey
Journal:  Cont Shelf Res       Date:  2007-06-01       Impact factor: 2.391

2.  Modeling the effects of potential salinity shifts on the recovery of striped bass in the Savannah River estuary, Georgia-South Carolina, United States.

Authors:  Thomas R Reinert; James T Peterson
Journal:  Environ Manage       Date:  2008-05       Impact factor: 3.266

3.  Aerobic anoxygenic phototrophic bacteria attached to particles in turbid waters of the Delaware and Chesapeake estuaries.

Authors:  Lisa A Waidner; David L Kirchman
Journal:  Appl Environ Microbiol       Date:  2007-04-27       Impact factor: 4.792
  3 in total

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