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While ¹H NMR focuses on hydrogen environments, ¹³C NMR provides complementary information about the carbon skeleton. Together, ¹H and ¹³C NMR give a comprehensive picture of a molecule's framework. ¹³C NMR is particularly useful for determining how many distinct carbon environments exist and, through chemical shift values, what types of carbons are present.
The most common carbon isotope, ¹²C, has zero nuclear spin and is therefore NMR-inactive. Only ¹³C (spin = ½) produces an NMR signal. Since ¹³C has a natural abundance of only 1.1%, ¹³C NMR is much less sensitive than ¹H NMR — signals are weaker and require longer acquisition times or more concentrated samples.
Key differences from ¹H NMR:
| Feature | ¹H NMR | ¹³C NMR |
|---|---|---|
| Natural abundance | 99.98% (¹H) | 1.1% (¹³C) |
| Sensitivity | High | Low (~1/6000 of ¹H) |
| Chemical shift range | 0–12 ppm | 0–220 ppm |
| Splitting in routine spectra | Yes (n+1 rule) | No (proton-decoupled) |
| Integration | Quantitative (proportional to number of H) | Not reliably quantitative in routine spectra |
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