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GC-IRMS: Assessment of precision and accuracy of carbon isotope fingerprints measurements in natural gas

Applications | 2020 | Thermo Fisher ScientificInstrumentation
Elemental Analysis, GC/HRMS, GC/MSD
Industries
Energy & Chemicals
Manufacturer
Thermo Fisher Scientific

Summary

Importance of the Topic


The isotopic composition of hydrocarbons in natural gas provides critical insight into gas origin, maturation, and alteration processes. Precise and accurate compound-specific isotope analysis aids geochemists in distinguishing biogenic and thermogenic sources and supports environmental forensics and petroleum exploration.

Objectives and Study Overview


This work aims to evaluate the precision and accuracy of carbon isotope fingerprint measurements of natural gas reference materials using GC-IRMS. By analyzing USGS-distributed standards, the study establishes traceability to international isotope reference scales and validates the performance of a fully automated GC IsoLink II IRMS system.

Methodology and Instrumentation


The system separates C1–C5 hydrocarbons and CO₂ via gas chromatography and quantitatively converts individual compounds to CO₂ for isotope ratio mass spectrometry. Key GC conditions include:
  • Column: CP-PoraPlot Q, 27.5 m × 0.32 mm × 10 μm (with 2.5 m particle trap)
  • Injection: 10 µL single-taper liner, SSL injector at 250 °C, split ratios 50:1 and 10:1
  • Carrier gas: Helium at 2.0 mL/min
  • Oven program: 40 °C hold 1.7 min; ramp 10 °C/min to 240 °C; hold 1.5 min
The conversion interface (GC IsoLink II) combusts hydrocarbons to CO₂, which are introduced to the DELTA V IRMS via the ConFlo IV interface.

Main Results and Discussion


Three USGS natural gas standards (HCG-1, HCG-2, HCG-3) with varying CH₄, C₂H₆, and C₃H₈ compositions were analyzed. Measured δ13C values for methane, ethane, and propane matched expected values within ±0.2‰, with standard deviations between 0.09 and 0.18‰. A linear correlation between expected and measured δ13C values confirmed high accuracy and system stability across diverse mixture compositions.

Benefits and Practical Applications


The validated GC-IRMS method delivers reproducible isotope data essential for:
  • Differentiating biogenic vs. thermogenic gas
  • Tracing gas migration and reservoir interactions
  • Establishing interlaboratory comparability
  • Supporting regulatory and forensic investigations

Future Trends and Potential Applications


Advancements may include coupling isotope analysis with high-resolution chromatography for C4–C5 isomers, automation for high-throughput QA/QC in industrial gas analysis, and integration with compound-specific hydrogen isotope measurements for enhanced source characterization.

Conclusion


This evaluation demonstrates that the GC IsoLink II IRMS system provides precise (±0.18‰) and accurate (correlation R²≈1) carbon isotope measurements of natural gas. Standardized reference materials ensure traceability to international scales, enabling robust geochemical and forensic interpretations.

References


  • Philp RP, Lo Monaco G. In: Baskaran M, editor. Handbook of Environmental Isotope Geochemistry. Vol 1. Springer; 2011. p. 639–677.
  • Schoell M. Recent advances in petroleum isotope geochemistry. Org Geochem. 1984;6:645–663.
  • Schoell M. Stable isotopes in petroleum research. In: Brooks J, Welte D, editors. Advances in Petroleum Geochemistry. Vol 1. Academic Press; 1984. p. 215–245.
  • Hunt JM. Petroleum geochemistry and geology. W.H. Freeman; 1996.
  • Schoell M, Jenden PD. Isotope analysis of gases in gas field and gas storage. SPE Paper 26171. 1993.
  • Milkov AV, Etiope G. Revised genetic diagrams for natural gases based on a global dataset of >20,000 samples. Org Geochem. 2018;125:109–120.

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