The charge an atom would carry if every bond it makes were fully ionic – a piece of chemical bookkeeping. In MoS2 each sulfur counts as −2, so molybdenum is +4; in MoO3 it is +6. The number says how many outer electrons an atom has given away, and so how many it still has – which decides much of a material’s colour, conductivity and magnetism. It changes when a material is oxidised or reduced, and X-ray methods can measure it.
As the site uses it
Track interlayer anion exchange through the XRD basal spacing; characterise nickel and iron oxidation states by XPS or, better, operando X-ray absorption.
Counting every bond as ionic gives each atom an oxidation state – +4 for molybdenum in MoS2 – and with it the number of d electrons left: paired in MoS2, unpaired and magnetic in CrI3. Core levels shift to higher binding energy as an atom loses electrons, which is how X-ray methods read it.
Counting electrons
Assign every bonding electron to the more electronegative partner, and each atom ends up with a whole-number charge: its oxidation state. Sulfur and selenium in a dichalcogenide count as −2, as −1, oxygen as −2, so molybdenum in MoS2 is +4, chromium in CrI3 is +3, and molybdenum in MoO3 is +6.
The count matters because it fixes how many outer electrons a transition metal keeps. Molybdenum has six; as Mo4+ it keeps two d electrons, which pair up in the split-off d band of -MoS2 and make it a . Chromium as Cr3+ keeps three, unpaired, which is why CrI3 is magnetic. Vanadium in VSe2 keeps one, a 3d1 configuration that confirmed (Wong and colleagues, 2019).
Measuring it
reads the oxidation state from core-level binding energies, which rise as an atom loses electrons: Mo6+ in an oxide sits at higher binding energy than Mo4+ in MoS2, which makes XPS the standard check for oxidation of a dichalcogenide film. X-ray absorption does the same through the position and shape of an element’s absorption edge and, unlike XPS, which needs vacuum and sees only the top few nanometres, works through liquids and gases – on at work.
Operando X-ray absorption on (Ni,Fe) oxyhydroxide catalysts found the iron as Fe3+ in sites with unusually short Fe–O bonds, the sites that calculations identify as active in splitting water (Friebel and colleagues, 2015).
When the count is not simple
Oxidation states are bookkeeping; the real charge on an atom is smaller, because bonds share electrons, and where bonding is strongly the bookkeeping can become ambiguous. In RhSeCl, structural and magnetic studies describe rhodium as Rh(III), while X-ray absorption and photoelectron spectra have been read differently – one of the open questions about the compound.
Oxidation states also change in use. Layered oxides such as V2O5 and MoO3 are reduced under reducing conditions or intense illumination, and making MoS2 from MoO3 films starts with exactly such a reduction, in hydrogen at 500 °C, before (Lin and colleagues, 2012).
For specialists
A formal charge assigned by treating all bonds as ionic, which fixes the d-electron count of a transition metal: Mo4+ (d2) in MoS2, Cr3+ (d3) in CrI3, V4+ (d1) in VSe2. Real is smaller, but the count predicts band filling, magnetism and redox behaviour. It is measured by core-level shifts in XPS and by the position and shape of absorption edges in XAS; operando XAS follows it under reaction conditions, as for the Fe3+ sites of (Ni,Fe)OOH catalysts. Where bonding is strongly covalent it can be ambiguous: in RhSeCl, structure and magnetism point to Rh(III), while some spectra have been read otherwise.
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