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Scientific Investigations Report 2010–5154

Use of Stable Isotopes of Carbon and Nitrogen to Identify Sources of Organic Matter to Bed Sediments of the Tualatin River, Oregon

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Figure 9. Relations between δ13C, δ15N, and C/N in seston samples from the Tualatin River, Oregon, show that high chlorophyll-a concentrations are associated with low δ13C, high δ15N, and low C/N. [TR=Tualatin River, number following TR=
river mile location].

First posted August 17, 2010

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For additional information contact:
Director, Oregon Water Science Center
U.S. Geological Survey
2130 SW 5th Ave.
Portland, Oregon 97201
http://or.water.usgs.gov

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