
What is X-ray Absorption Spectroscopy?
X-ray absorption spectroscopy (XAS) is an analytical technique that relies on the variable absorption of x-rays by matter to probe its chemical state and local structure. A beam of x-rays of nearly one energy is put onto a sample, and the change in x-ray absorption is measured as the energy of the beam is varied.


For each element of the periodic table, every electron shell in an atom of that element has a unique energy required to eject it from the atom. In an XAS measurement, the energy of the incident x-rays is first tuned just below the energy of a particular electron shell, then the energy is gradually increased until eventually the x-ray has enough energy to eject that electron and is absorbed.

Due to quantum mechanical effects, the absorption does not increase all at once, but rather has a detectable turn-on and more complicated structure that can tell us about the chemical state of the absorbing atom.


The now free electron (i.e. no longer bound to the atom) is called a photoelectron. This photoelectron has a “wave function” that can scatter off nearby atoms creating oscillations of more/less absorption. Think of it as ripples in a pond. This wave interference can tell us about the local structure around the absorbing atom.


One of the most useful properties of XAS measurements is that the energies of the electronic transitions of different elements are well separated in energy compared to the resolution of XAS spectrometers. This means that by tuning the energy of a particular transition, an element-specific measurement of the sample can be performed.


The plot to the left shows the XAS for 3d transition metals and the well separated energy ranges.
The plot below shows only the energy range for Fe XAS. The difference in oxidation state of the samples can clearly been seen by the shift in the energy position of the absorption edge.


Elements of a XAS scan

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