Soil Carbon and Nitrogen Analysis by Flash EA-IRMS
SOP-L414Revision 1.1
Author
Marc Los Huertos
Environmental Analysis, Pomona College
Kyle McCarty
Oxtoby Isotope Lab, Pomona College
Published
2026-06-26
1 Purpose
This SOP describes the complete workflow for determining \(\delta^{13}\)C, \(\delta^{15}\)N, and elemental concentrations (%C, %N) in soil and sediment samples by combustion on the Thermo Scientific Flash IRMS Elemental Analyzer (EA) coupled to the Delta V IRMS through the ConFlo IV interface (Werner & Brand, 2001). It covers sample preparation, sequence design, the analytical run, and post-analysis data correction including blank correction, linearity correction, scale normalization, and drift correction (Coplen, 2011; Paul et al., 2007).
For general instrument operation, startup/shutdown, gas checks, tuning, and pre-analysis tests, see SOP-L208.
2 Scope
Applies to: Soil, sediment, and plant tissue samples analyzed for \(\delta^{13}\)C, \(\delta^{15}\)N, %C, and %N by combustion EA-IRMS in NC (dual reactor) mode.
Does not apply to: Sulfur isotope analysis (NCS mode; requires dedicated reactor and Sulfinert column), GasBench applications (see SOP-L415), TC/EA applications (\(\delta^{2}\)H, \(\delta^{18}\)O), or liquid samples.
Location: Sample preparation in SGM Rm 133; analysis in the Oxtoby Isotope Lab, SGM Rm 135.
3 Responsibilities
Role
Responsibility
Lab PI
Approve methods, oversee data quality
Lab Manager
Prepare/verify Isodat methods; maintain reactors
Certified User
All steps from sample prep through data reduction
Student Researcher
May perform sample prep and data reduction under supervision
4 Definitions
Blank correction: Subtraction of the isotopic and elemental contribution of an empty tin capsule from each sample signal; necessary because capsule tin contributes a small amount of C and N (Paul et al., 2007).
\(\delta^{13}\)C: Stable carbon isotope ratio expressed in per mil (‰) relative to Vienna Pee Dee Belemnite (VPDB): \(\delta^{13}C =
\left(\tfrac{R_\text{sample}}{R_\text{standard}} - 1\right)\times
1000\) where \(R = {}^{13}C/{}^{12}C\)(Coplen, 2011).
\(\delta^{15}\)N: Stable nitrogen isotope ratio expressed in per mil (‰) relative to atmospheric N2 (AIR): \(\delta^{15}N =
\left(\tfrac{R_\text{sample}}{R_\text{standard}} - 1\right)\times
1000\) where \(R = {}^{15}N/{}^{14}N\)(Coplen, 2011).
Drift correction: Adjustment for systematic temporal change in measured \(\delta\) values during a sequence, estimated from bracketing reference materials (Paul et al., 2007).
Flash EA: The Thermo Scientific Flash IRMS Elemental Analyzer peripheral; combusts samples at 1020 °C in an O2 pulse and separates N2 and CO2 chromatographically before delivery to the IRMS via the ConFlo IV.
Isodat: ThermoFisher software used to design analytical sequences, control the instrument, and export raw isotope data.
Linearity correction: Adjustment applied to account for the dependence of measured \(\delta\) values on peak signal amplitude.
Reference material (RM): A substance with a certified or consensus \(\delta\) value used to anchor measured values to the VPDB or AIR scale (Werner & Brand, 2001).
Scale normalization: Two-point (or multi-point) correction that maps measured \(\delta\) values to the international isotope-ratio scale using certified RMs spanning the expected sample range (Paul et al., 2007).
Tin capsule: 5 x 9 mm pressed-tin container used to encapsulate solid samples; tin ignites in the O2 pulse, raising combustion temperature briefly to ensure complete combustion.
Coplen, T. B. (2011). Guidelines and recommended terms for expression of stable-isotope-ratio and gas-ratio measurement results. Rapid Communications in Mass Spectrometry, 25(17), 2538–2560. https://doi.org/10.1002/rcm.5129
Paul, D., Skrzypek, G., & F’orizs, I. (2007). Normalization of measured stable isotopic compositions to isotope reference scales – a review. Rapid Communications in Mass Spectrometry, 21(18), 3006–3014. https://doi.org/10.1002/rcm.3185
Werner, R. A., & Brand, W. A. (2001). Referencing strategies and techniques in stable isotope ratio analysis. Rapid Communications in Mass Spectrometry, 15(7), 501–519. https://doi.org/10.1002/rcm.258