Carbon-13 - 13C or C-13 - is a natural, stable isotope of the chemical element carbon, whose atomic nucleus consists of six protons and seven neutrons. As one of the environmental isotopes, it accounts for about 1.1% of all natural carbon on Earth.
Pure carbon-13 for commercial use - particularly for the chemical synthesis of 13 C-labeled compounds - must be enriched due to its natural abundance of approximately one 1%. In principle, various techniques or methods such as thermal diffusion, chemical exchange, gas diffusion as well as laser and cryogenic distillation are available to separate C-13 from the main component C-12 of natural carbon.
At present, however, only the cryogenic distillation of methane or carbon monoxide is an economically viable industrial production technology, although such carbon-13 production facilities represent a significant investment. Cryogenic distillation columns more than 100 meters high are required to separate the compounds containing carbon-12 or carbon-13. The world's largest reported commercial C-13 plant (CIL plant in Ohio) has a production capacity of approximately 420 kg of carbon-13 per year (2019). In this method, natural carbon monoxide (CO) is liquefied at a very low temperature and then distilled through special stainless steel columns several kilometers long. In comparison, a 1969 pilot plant for the cryogenic distillation of carbon monoxide at Los Alamos Scientific Laboratories (USA) was able to produce about 4 kg of carbon-13 annually.
See also: List of individual Carbon isotopes (and general data sources).
Direct parent isotopes are: 13B, 13N.
| Atomic Mass ma | Quantity | Half-life | Spin | |
|---|---|---|---|---|
| Carbon Isotopic mixture | 12.011 u | 100 % | ||
| Isotope 12C | 12.00000000000 u | 98.94 % [98.84 - 99.04 %] | stable | 0+ |
| Isotope 14C | 14.003241988(4) u | [trace] | 5700(30) a | 0+ |
| Isotope 13C | 13.003354835(2) u | 1.06 % [0.96 - 1.16 %] | stable | 1/2- |
Nuclear magnetic properties and parameters of the NMR active Nuclide 13C
| Z | Isotone N = 7 | Isobar A = 13 |
|---|---|---|
| 2 | 9He | |
| 3 | 10Li | 13Li |
| 4 | 11Be | 13Be |
| 5 | 12B | 13B |
| 6 | 13C | 13C |
| 7 | 14N | 13N |
| 8 | 15O | 13O |
| 9 | 16F | 13F |
| 10 | 17Ne | |
| 11 | 18Na | |
| 12 | 19Mg | |
| 13 | 20Al |
[1] - Darren Brown, John Greene:
10th international symposium on the synthesis and applications of isotopes and isotopically labelled compounds.
In: Journal of Labelled Compounds and Radiophamaceuticals, (2010), DOI 10.1002/jlcr.1775.
[2] - Hu-LinLi, Yong-Lin Ju, Liang-JunLi, Da-GangXu:
Separation of isotope 13C using high-performance structured packing.
In: Chemical Engineering and Processing: Process Intensification, (2010), DOI 10.1016/j.cep.2010.02.001.
Last update: 2025-12-28
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