A novel high-temperature combustion based system for stable isotope analysis of dissolved organic carbon in aqueous samples.: II optimization and assessment of analytical performance

• Main Authors: Kirkels, F. M. S. A., Cerli, C., Federherr, E., Gao, J., Kalbitz, K.
• Other Authors: non-UU output of UU-AW members
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2014
• Subjects: RATIO MASS-SPECTROMETRY; WET CHEMICAL OXIDATION; HIGH ARCTIC GLACIER; INORGANIC CARBON; TERRESTRIAL ECOSYSTEMS; C-13 ANALYSIS; MATTER; SOIL; WATERS; ANALYZER; Arctic
• Online Access: https://dspace.library.uu.nl/handle/1874/303479

RATIONALE: Dissolved organic carbon (DOC) plays an important role in carbon cycling, making precise and routine measurement of delta C-13 values and DOC concentration highly desirable. A new promising system has been developed for this purpose. However, broad-scale application of this new technique requires an in-depth assessment of analytical performance, and this is described here. METHODS: A high-temperature combustion Total Organic Carbon analyzer was interfaced with continuous flow isotope ratio mass spectrometry (TOC/IRMS) for the simultaneous analysis of the bulk DOC concentration and delta C-13 signature. The analytical performance (precision, memory effects, linearity, volume/concentration effects, accuracy) was thoroughly evaluated, including realistic and challenging conditions such as low DOC concentrations and natural DOC. RESULTS: High precision (standard deviation, SD predominantly ≤0.15 ‰) and accuracy (R2 = 0.9997) were achieved for the δ13C analysis of a broad diversity of DOC solutions. Simultaneously, good results were obtained for the measurement of DOC concentration. Assessment of natural abundance and slightly 13C-enriched DOC, a wide range of concentrations (~0.2–150 mgC/L) and injection volumes (0.05–3 mL), demonstrated minor/negligible memory effects, good linearity and flexible usage. Finally, TOC/IRMS was successfully applied to determine low DOC concentrations (<2 mgC/L) and DOC from diverse terrestrial, freshwater and marine environments (SD ≤0.23 ‰). CONCLUSIONS: TOC/IRMS enables fast and reliable measurement of DOC concentrations and delta C-13 values in aqueous samples, without pre-concentration and freeze-drying. Further investigations should focus on complex, saline matrices and very low DOC concentrations, to achieve a potential lower limit of 0.2 mgC/L. Thus, TOC/IRMS will give DOC research in terrestrial and aquatic environments a huge impulse with high-resolution, routine delta C-13 analysis. Copyright (C) 2014 John Wiley & Sons, Ltd.