scholarly journals Biogeochemistry of trace metals in Chesapeake Bay. Progress report, 1 July 1976--30 June 1977. [Comparison with San Francisco Bay]

1977 ◽  
Author(s):  
M.G. Gross ◽  
A.D. Eaton ◽  
V. Grant
Keyword(s):  
Trace Metals ◽  
Chesapeake Bay ◽  
San Francisco ◽  
San Francisco Bay ◽  
Progress Report

scholarly journals Benthic flux of nutrients and trace metals in the northern component of San Francisco Bay, California

2009 ◽  
Author(s):  
James S. Kuwabara ◽  
Brent R. Topping ◽  
Francis Parcheso ◽  
Anita C. Engelstad ◽  
Valerie E. Greene
Keyword(s):  
Trace Metals ◽  
San Francisco ◽  
San Francisco Bay ◽  
Benthic Flux

Distribution of colloidal trace metals in the San Francisco Bay estuary

1996 ◽  
Vol 60 (24) ◽  
pp. 4933-4944 ◽  
Author(s):  
Sergio A. San˜udo-Wilhelmy ◽  
Ignacio Rivera-Duarte ◽  
A. Russell Flegal
Keyword(s):  
Trace Metals ◽  
San Francisco ◽  
San Francisco Bay ◽  
San Francisco Bay Estuary

The Behavior of 14C and 13C in Estuarine Water: Effects of In Situ CO2 Production and Atmospheric Exchange

Radiocarbon ◽  
1980 ◽  
Vol 22 (3) ◽  
pp. 647-654 ◽  
Author(s):  
Elliott C Spiker
Keyword(s):  
Chesapeake Bay ◽  
Water Column ◽  
San Francisco ◽  
Dissolved Inorganic Carbon ◽  
San Francisco Bay ◽  
Co2 Production ◽  
Carbon Utilization ◽  
Model Calculations ◽  
Dominant Source ◽  
Atmospheric Exchange

The effects of nonconservative sources (inputs) and sinks (outputs) of carbon are indicated by the behavior of Δ14C and δ13C of the total dissolved inorganic carbon (ΣCO2) in San Francisco Bay and Chesapeake Bay. Isotopic distributions and model calculations indicate that in North San Francisco Bay the net CO2 flux to the atmosphere and carbon utilization in the water column are balanced by benthic production. Municipal waste appears to be a dominant source in South San Francisco Bav. In Chesapeake Bay, atmospheric exchange has increased the Δ14C and δ13C in the surface water. Decomposition of organic matter in the water column is indicated to be the dominant source of excess ΣCO2 in the deep water.

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