Extended Data Figure 7: Stability in the course of the measurement series, characterization of the amount dependency of the measurement system, and tests with bubble-free ice. | Nature

Extended Data Figure 7: Stability in the course of the measurement series, characterization of the amount dependency of the measurement system, and tests with bubble-free ice.

From: Isotopic constraints on marine and terrestrial N2O emissions during the last deglaciation

Extended Data Figure 7

a, NOAA-3 standard gas measurements performed at the end of each measurement day. No significant drifts were observed in the course of the measurement series, and the standard deviations for δ15N and δ18O were respectively 0.14‰ and 0.32‰ (n = 31), as indicated by the grey areas (±1σ) around the means (dashed lines). b, NOAA-1 standard gas measurements resulting in similar peak areas to the preceding ice-sample measurement routinely performed throughout the measurement series. These measurements covering the full range of peak areas from ice samples did not reveal any significant amount dependency. The mean and standard deviation (dashed lines and grey areas) for δ15N were 6.24‰ ± 0.22‰ and those for δ18O were 44.18‰ ± 0.59‰ (±1σ, n = 58), in agreement with the expected values (solid lines). c, Measurements of different amounts of NOAA-1 standard gas which was stored in the extraction pots while pieces of bubble-free ice were grated. Dashed lines and grey areas indicate the means and standard deviations (±1σ, n = 10), and solid lines indicate the expected values. On the basis of these measurements with bubble-free ice and the results shown in b, N2O, δ15N and δ18O were not corrected for amount dependency. However, during the extraction of standard gas over ice, a −1.38‰ offset was introduced in δ18O. Accordingly, all Taylor Glacier δ18O values were corrected by +1.38‰.

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