Dataset: Simulation of the volume-dependent changes in ẟ15N and ẟ18O for IAEA-NO3 and USGS-34 reference materials (Biological Nitrogen Isotope Fractionation project)

Final no updates expectedDOI: 10.26008/1912/bco-dmo.865685.1Version 1 (2021-12-01)Dataset Type:experimental

Principal Investigator: Julie Granger (University of Connecticut)

Student, Contact: Mengyang Zhou (University of Connecticut)

BCO-DMO Data Manager: Sawyer Newman (Woods Hole Oceanographic Institution)


Project: CAREER: The biological nitrogen isotope systematics of ammonium consumption and production (Biological Nitrogen Isotope Fractionation)


Abstract

Simulation of the volume-dependent changes in ẟ15N and ẟ18O for IAEA-NO3 and USGS-34 reference materials.

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Sampling and analytical procedures: 

Effects of sample volume and salinity on O atom exchange with water

Given the potential influences on NO3- N and O isotope ratios, which include bacterial blanks, dissolved atmospheric N2O, contaminant NO3- in reference materials, O atom exchange with water, and incomplete N2O recovery and associated isotope fractionation, we attempt to reproduce the volume-dependent changes in ẟ15N and ẟ18O that we observed for IAEA-NO3 and USGS-34 reference materials.

The observed ä15N and ä18O values of N2O for IAEA-NO3 and USGS-34 samples were referenced to that expected for IAEA-NO3 vs. the N2O reference tank. The expected IAEA-NO3 has a ä15N of 0‰ vs. IAEA-NO3, and that expected for USGS-34 is -6.5‰ vs. IAEA-NO3. Being uncertain of the ä18O of the industrial N2O in the reference tank, we approximate the expected ä18O value for IAEA-NO3 vs. N2Oref to be that observed for the highest N2O yield (at lower aliquot volumes – which is admittedly already subject to blanks). Referenced to itself, the expected ä18O of IAEA-NO3 is 0‰ (vs. IAEA-NO3), and that for USGS-34 is -52.2‰ (vs. IAEA-NO3).

We compare the simulated ä15N and ä18O values to the observed average of 3 trials in dataset “Incidence of volume effect.”


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