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Pyisotopomer: A Python package for obtaining intramolecular isotope ratio differences from mass spectrometric analysis of nitrous oxide isotopocules.
Kelly, Colette L; Manning, Cara; Frey, Claudia; Kaiser, Jan; Gluschankoff, Noah; Casciotti, Karen L.
Affiliation
  • Kelly CL; Department of Earth System Science, Stanford University, Stanford, CA, USA.
  • Manning C; Department of Marine Sciences, University of Connecticut, Groton, CT, USA.
  • Frey C; Department of Environmental Science, University of Basel, Basel, Switzerland.
  • Kaiser J; Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich, UK.
  • Gluschankoff N; Department of Earth System Science, Stanford University, Stanford, CA, USA.
  • Casciotti KL; Department of Earth System Science, Stanford University, Stanford, CA, USA.
Rapid Commun Mass Spectrom ; 37(11): e9513, 2023 Jun 15.
Article in En | MEDLINE | ID: mdl-36971184
ABSTRACT
RATIONALE Obtaining nitrous oxide isotopocule measurements with isotope ratio mass spectrometry (IRMS) involves analyzing the ion current ratios of the nitrous oxide parent ion (N2 O+ ) as well as those of the NO+ fragment ion. The data analysis requires correcting for "scrambling" in the ion source, whereby the NO+ fragment ion obtains the outer N atom from the N2 O molecule. While descriptions exist for this correction, and interlaboratory intercalibration efforts have been made, there has yet to be published a package of code for implementing isotopomer calibrations.

METHODS:

We developed a user-friendly Python package (pyisotopomer) to determine two coefficients (γ and κ) that describe scrambling in the IRMS ion source, and then used this calibration to obtain intramolecular isotope deltas in N2 O samples.

RESULTS:

With two appropriate reference materials, γ and κ can be determined robustly and accurately for a given IRMS system. An additional third reference material is needed to define the zero-point of the delta scale. We show that IRMS scrambling behavior can vary with time, necessitating regular calibrations. Finally, we present an intercalibration between two IRMS laboratories, using pyisotopomer to calculate γ and κ, and to obtain intramolecular N2 O isotope deltas in lake water unknowns.

CONCLUSIONS:

Given these considerations, we discuss how to use pyisotopomer to obtain high-quality N2 O isotopocule data from IRMS systems, including the use of appropriate reference materials and frequency of calibration.

Full text: 1 Database: MEDLINE Language: En Year: 2023 Type: Article

Full text: 1 Database: MEDLINE Language: En Year: 2023 Type: Article