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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 3. Regression results for acidified versus unacidified samples from the Tualatin River basin, Oregon. Regression for δ13C is not significantly different from the y=x line. Regressions for δ15N and the C/N atomic ratio are significantly different from the y=x line (α=0.05).

First posted August 17, 2010

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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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