Isotopic labeling

Isotopic labeling is a technique for tracking the passage of a sample of substance through a system. The substance is 'labeled' by including unusual isotopes in its chemical composition. If these unusual isotopes are later detected in a certain part of the system, they must have come from the labeled substance.

In ordinary isotopic labeling, there are two ways to detect the presence of labeling isotopes. Since isotopes have different masses, they can be separated using infrared spectroscopy.

Isotopic labeling can also be used to study chemical reactions. In this method specific atoms are replaced by an isotope in a reactant molecule which then participates in a chemical reaction. With nuclear magnetic resonance spectroscopy for example, it is now possible to identify where a particular molecular fragment in the reactant ends up as a particular fragment in one of the reaction products.

An example of the use of isotopic labeling is the study of deuterated water (water containing D₂O in addition to the usual H₂O), the substitution of deuterium for the hydrogen is observed in phenol's hydroxyl group (resulting in C₆H₅OD), indicating that phenol readily undergoes hydrogen-exchange reactions with water. Only the hydroxyl group was affected, indicating that the other 5 hydrogen atoms did not participate in these exchange reactions.

Radioisotopic labelling

Radioisotopic labelling is a technique for tracking the passage of a sample of substance through a system. The substance is "labelled" by including radiation they emit. Radioisotopic labelling is a special case of isotopic labeling.

For these purposes, a particularly useful type of radioactive decay is photons traveling in diametrically opposite directions. If the positron is produced within a solid object, it is likely to do this before travelling more than a millimetre. If both of these photons can be detected, the location of the decay event can be determined very precisely.

Strictly speaking, radiosotopic labelling includes only cases where radioactivity is artificially introduced by experimenters, but some natural phenomena allow similar analysis to be performed. In particular, radiometric dating uses a closely related principle.

Isotopic tracer

An isotopic tracer, (also "isotopic marker" or "isotopic label"), is used in neutrons, however, means that it can be detected separately from the other atoms of the same element.

NMR typically uses this type of technique to investigate the mechanisms of chemical reactions (basically trying to find out which starting atom ends up where after a reaction), because NMR detects not only isotopic differences, but also gives an indication of the position of the atom.

Mass spectrometry can also be used with this technique, since mass spectra recorded with sufficiently high resolution can distinguish among isotopes based on the different masses resulting from the different number of neutrons.

gel electrophoresis can also take advantage of this approach. In this technique, radioactive isotopes are used. The radiation emitted by compounds containing the radioactive isotopes darkens a piece of photographic film, recording the position of these compounds relative to one another in the gel.

Isotopic (isotope) tracers are some of the most important tools in geology, because they can be used to understand complex mixing process in earth systems. Isotope tracers are almost always used in the form of isotope ratios. By studying the ratio between two isotopes of the same element, we avoid effects involving the overall abundance of the element, which would usually swamp the much smaller variations in isotopic abundances. Further discussion of the application of isotopic tracers in geology is covered under the heading of isotope geochemistry.

Isotopic tracers are usually subdivided into two categories: radioactive decay, which is usually ratioed against a non-radiogenic isotope (whose abundance in the earth does not vary due to radioactive decay).

A stable isotope tracer involves only non-radiogenic isotopes. In this case, relative variations in abundance between the two isotopes is most often caused by mass-dependant fractionation. In theory, any element with two stable isotopes can be used as an isotopic tracer. However, the most commonly used stable isotope tracers involve relatively light isotopes which readily undergo fractionation in natural systems. See also isotopic signature.

References

^ Dickin, A. P., 2005. ‘’Radiogenic Isotope Geology’‘, Cambridge University Press.

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