Isolation of Underivatized Amino Acids for Radiocarbon Analysis Using a Porous Graphite Column

We developed a method for isolation and purification of individual underivatized amino acids for compound-specific radiocarbon analysis. Our method employs a semipreparative porous graphitic carbon column that allows for separation and isolation of all proteinogenic amino acids in a single step. To minimize contamination, we utilized a mixed-mode ion-exchange column to further purify the isolated amino acid fractions. Radiocarbon measurements of standard amino acids processed with this method resulted in F<sup>14</sup>C values closely aligned with their original F<sup>14</sup>C values. From these measurements, we calculated the blank contribution to 1.0 ± 0.3 μg C with F<sup>14</sup>C = 0.6 ± 0.12, rendering this approach suitable for ultrasmall samples with enhanced measurement reliability.

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Journal
Analytical Chemistry
Published
2025-10-13
DOI
https://doi.org/10.1021/acs.analchem.5c02922
Primary Topic
Isotope Analysis in Ecology
Type
article
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article

Isolation of Underivatized Amino Acids for Radiocarbon Analysis Using a Porous Graphite Column

Timothy I. Eglinton, Negar Haghipour, Christian Heusser, Thomas M. Blattmann et al.
Analytical Chemistry
Isotope Analysis in Ecology
article

Isolation of Underivatized Amino Acids for Radiocarbon Analysis Using a Porous Graphite Column

Timothy I. Eglinton, Negar Haghipour, Christian Heusser, Thomas M. Blattmann, Lukas Wacker
article en

Abstract

We developed a method for isolation and purification of individual underivatized amino acids for compound-specific radiocarbon analysis. Our method employs a semipreparative porous graphitic carbon column that allows for separation and isolation of all proteinogenic amino acids in a single step. To minimize contamination, we utilized a mixed-mode ion-exchange column to further purify the isolated amino acid fractions. Radiocarbon measurements of standard amino acids processed with this method resulted in F<sup>14</sup>C values closely aligned with their original F<sup>14</sup>C values. From these measurements, we calculated the blank contribution to 1.0 ± 0.3 μg C with F<sup>14</sup>C = 0.6 ± 0.12, rendering this approach suitable for ultrasmall samples with enhanced measurement reliability.

Analytical ChemistryVol. 97(42)
Nanyang Technological University (SG), Paul Scherrer Institute (CH), ETH Zurich (CH), Ion Beam Applications (France) (FR)
Openalex Percentile: Top 72%
Isotope Analysis in Ecology
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