Structure & Reactivity

Nuclear Magnetic Resonance Spectroscopy

NMR2. 13C NMR Spectroscopy

Since organic compounds are largely based on carbon, 13C NMR spectroscopy is a pretty important tool for studying organic compounds. The 13C isotope is the only isotope of carbon that is "NMR-active"; 12C and 14C atoms do not absorb radio waves in a magnetic field. The 13C NMR spectrum of cyclohexane is shown below.

Carbon N M R spectrum of cyclohexane.

Figure NMR2.1.13C NMR spectrum of cyclohexane.1

Cyclohexane is constructed of a ring of six carbon atoms.  There are two hydrogen atoms attached to each of the carbons.

Notice these features of the spectrum:

 

There are some peculiar terms used in NMR spectroscopy that are not used in IR spectroscopy. These terms arose from the use of magnetic fields in measuring these spectra:

In cyclohexane, only one frequency of radio waves is absorbed by the carbon atom, and that is at about 27 ppm. Other frequencies could be absorbed by the hydrogen atoms, but hydrogen atoms absorb at very different frequencies from carbon atoms, so they wouldn't be detected in a 13C NMR spectrum.

 

Problem NMR2.1.

Which peak would show up farther to the right in the NMR spectrum?

a)  10 pmm or 27 ppm        b) 122 ppm or 64 ppm        c) 196 ppm or 158 ppm

Problem NMR2.2.

Which peak would show up farther downfield in the NMR spectrum?

a)  17 pmm or 63 ppm        b) 201 ppm or 155 ppm        c) 71 ppm or 43 ppm

 

13NMR spectra are relatively simple. They just show several vertical lines, each representing a carbon atom in a different environment within a molecule. Obtaining the spectrum is more complicated. The problem is, 13C is only a minor isotope of carbon. It only represents about 0.1 percent of carbon on earth. In contrast, 12C makes up about 98.9 percent of carbon on earth; that's why the periodic table shows an atomic mass of carbon of almost exactly 12 amu. That's a low enough level of 13C that an individual molecule of the size that you will see in this course probably doesn't contain any 13C. So, if you take a sample of an organic compound and bounce some radio waves off it to measure its 13C NMR spectrum, you are really just hearing from those molecules that happen to contain an atom of that isotope; the rest are silent. The experiment is still possible, because even a drop of an organic liquid contains billions of molecules, and millions of those contain some 13C. However, it does make the response a little fainter.

Later, we will look at 1H NMR spectroscopy. 1H, or protium, is by far the most common isotope of hydrogen. The atomic mass listed in the periodic table is very close to 1 amu, because the average of all the hydrogen isotopes is dominated by this one major contributor. Every organic molecule is very likely to contain this isotope. As a result, when we shine radio waves of the right frequency to detect 1H on a sample of an organic compound and listen for a response, it pretty much shouts back at us. With carbon, we have to lean in close and listen very carefully in the hopes that it can muster a tiny little "yop".

There are some technical things that an NMR instrument does to amplify that faint carbon signal. One thing we can do is to actually make use of those abundant protons in the molecule. We can send in a pulse of radio waves that the protons will absorb just before we try to detect the carbon. When we do that, the hydrogens can actually help nearby carbons respond more strongly. There are consequences to that technique. It actually distorts the peaks that we see in the spectrum, because carbons that are bonded to more hydrogens respond much more strongly than carbons that are not. It is sometimes difficult to see carbons that have no hydrogens attached. Also, this distortion turns 13C NMR into a qualitative technique, generally. For the most part, you can't use it to measure how many of one carbon you have compared to another. In contrast, in 1H NMR, we take quantitative measurements all the time.

 

Reference: 1. SDBSWeb : http://riodb01.ibase.aist.go.jp/sdbs/ (National Institute of Advanced Industrial Science and Technology of Japan, 15 August 2008)

 

This site is written and maintained by Chris P. Schaller, Ph.D., College of Saint Benedict / Saint John's University (with contributions from other authors as noted).  It is freely available for educational use.

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Structure & Reactivity in Organic, Biological and Inorganic Chemistry by Chris Schaller is licensed under a Creative Commons Attribution-NonCommercial 3.0 Unported License

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