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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

Table 2. Relation between acidified and unacidified δ13C, δ15N, and C/N results for samples from the Tualatin River basin, Oregon.

[Abbreviations: r2, square of the Pearson correlation coefficient; N, number of points in regression]

Parameter Regression statistics Significantly
different from y=x?
(α=0.05)
Correction equation
r2 Standard
error
N
δ13C 0.95 0.588 32 No None
δ15N 0.95 0.487 32 Yes Unacidified = (Acidified + 0.3675) / 0.9385
C/N 0.96 1.360 32 Yes Unacidified = (Acidified – 0.8405) / 1.0131

First posted August 17, 2010

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