Oxides and Oxoanions of Transition Elements
Quick Notes
- General Trends: Oxides formed at high temperatures; highest oxidation states correlate with group numbers.
- Lower oxides are ionic and basic; higher oxides are covalent and acidic.
- Acidity Order: MnO < MnO2 < Mn2O7 (acidic green oil).
- VO2+ and VO3−: Amphoteric behaviour in vanadium oxides.
- CrO is basic, Cr2O3 is amphoteric, CrO3 is acidic.
- K2Cr2O7 (orange) and KMnO4 (purple) are strong oxidants.
- Colour changes: Green (Cr3+), Orange (Cr2O72−), Purple (MnO4−), Green (MnO42−).
Full Notes
Transition metals form a variety of oxides and oxoanions by reacting with oxygen, particularly at high temperatures. Their oxidation states, chemical nature, and solubility change based on the group and metal. These oxides play a critical role in redox chemistry and industrial processes.
Formation and Nature of Oxides
- All d-block metals except scandium form monoxides (MO) which are predominantly ionic.
- The highest oxidation number matches the group number:
- Sc2O3 (Sc3+)
- Mn2O7 (Mn7+)
- Beyond Mn (Group 7), no higher oxides than Fe2O3 are observed.
Ionic to Covalent Nature
As oxidation number increases, ionic character decreases and covalent character increases.
For Example: Mn2O7 is a covalent green oil and highly acidic whereas CrO3 and V2O5 have low melting points and are acidic oxides.
Acidic, Amphoteric, and Basic Nature
- Acidic: Mn2O7, CrO3, V2O5
- Mn2O7 forms HMnO4 (permanganic acid).
- CrO3 forms H2CrO4, H2Cr2O7.
- Amphoteric: V2O5, Cr2O3
- V2O5 reacts with acids to form VO2+ and with bases to form VO3−.
- Cr2O3 dissolves in both acids and bases.
- Basic: CrO
Oxocations
Stabilised in aqueous medium: VO+ (V5+), VO2+ (V4+), TiO2+ (Ti4+).
Chromium Compounds
Preparation of Chromates and Dichromates
From chromite ore (FeCr2O4) by fusion with Na2CO3 in air:
4FeCr2O4 + 8Na2CO3 + 7O2 → 8Na2CrO4 + 2Fe2O3 + 8CO2
Acidify sodium chromate to get sodium dichromate:
2Na2CrO4 + 2H+ → Na2Cr2O7 + 2Na+ + H2O
Convert sodium dichromate to K2Cr2O7 (orange crystals):
Na2Cr2O7 + 2KCl → K2Cr2O7 + 2NaCl
Equilibrium Between Chromate and Dichromate
- Acidic: 2CrO42− + 2H+ ⇌ Cr2O72− + H2O
- Basic: Cr2O72− + 2OH− ⇌ 2CrO42− + H2O
Structure

CrO42−: Tetrahedral
Cr2O72−: Two tetrahedra sharing one corner; Cr–O–Cr bond angle = 126°
Oxidising Properties of K2Cr2O7
Reaction in acid:
Cr2O72− + 14H+ + 6e− → 2Cr3+ + 7H2O E° = +1.33 V
Oxidation Examples:
- 6Fe2+ → 6Fe3+ + 6e−
- 3Sn2+ → 3Sn4+ + 6e−
- 3H2S → 3S + 6H+ + 6e−
- 6I− → 3I2 + 6e−
Example: Combined ionic reaction between Cr2O72− and Fe2+:
Cr2O72− + 14H+ + 6Fe2+ → 2Cr3+ + 6Fe3+ + 7H2O
Manganese Compounds
Preparation of Potassium Permanganate
- Fusion of MnO2 with KOH and O2: 2MnO2 + 4KOH + O2 → 2K2MnO4 + 2H2O
- Disproportionation in acidic solution: 3MnO42− + 4H+ → 2MnO4− + MnO2 + 2H2O
- Electrolytic oxidation (following fusion of MnO2 with KOH and O2): MnO42− → MnO4−
- Lab preparation: 2Mn2+ + 5S2O82− + 8H2O → 2MnO4− + 10SO42− + 16H+
Properties of KMnO4
- Purple/black crystals
- Not very soluble (6.4 g/100 g at 293 K)
- Decomposes on heating: 2KMnO4 → K2MnO4 + MnO2 + O2
- Molecular Orbital Theory explains intense colour and weak paramagnetism.
- Manganate and permanganate ions are tetrahedral, with π bonding occurring between overlap of p-orbitals of oxygen and d-orbitals of manganese.
Manganate, MnO42− – green and paramagnetic (one unpaired electron).

Permanganate, MnO4− – purple and diamagnetic (no unpaired electrons).

Oxidising Properties of KMnO4
KMnO4 is a powerful oxidising agent, readily gaining electrons and oxidising another species.
In Acidic Medium:
MnO4− + 8H+ + 5e− → Mn2+ + 4H2O E° = +1.52 V
Hydrogen ion concentration ([H+]) plays a crucial role in determining which product is formed when KMnO4 reacts (MnO42−, MnO2, or Mn2+).
Half-Reactions and Corresponding Standard Electrode Potentials:
- MnO4− + e− → MnO42− E° = +0.56 V (mildly basic)
- MnO4− + 4H+ + 3e− → MnO2 + 2H2O E° = +1.69 V (weakly acidic)
- MnO4− + 8H+ + 5e− → Mn2+ + 4H2O E° = +1.52 V (strongly acidic)
Example reactions (acidic):
- 10I− + 2MnO4− + 16H+ → 2Mn2+ + 5I2 + 8H2O
- 5Fe2+ + MnO4− + 8H+ → Mn2+ + 5Fe3+ + 4H2O
- 5C2O42− + 2MnO4− + 16H+ → 2Mn2+ + 10CO2 + 8H2O
- 5S2− + 2MnO4− + 16H+ → 2Mn2+ + 5S + 8H2O
- 5SO32− + 2MnO4− + 6H+ → 2Mn2+ + 5SO42− + 3H2O
- 5NO2− + 2MnO4− + 6H+ → 5NO3− + 2Mn2+ + 3H2O
In Neutral/Alkaline Medium:
- I− + MnO4− + H2O → IO3− + MnO2 + OH−
- 3S2O32− + 8MnO4− + H2O → 6SO42− + 8MnO2 + 2OH−
- 3Mn2+ + 2MnO4− + 2H2O → 5MnO2 + 4H+
Note: KMnO4 should not be used in HCl, as Cl− gets oxidised to Cl2.
Uses of KMnO4
- Strong oxidising agent in organic synthesis
- Used for bleaching and decolourisation
- Acts as a volumetric titrant in redox titrations
Summary
- Lower oxides are more ionic and basic and higher oxides become covalent and acidic.
- Chromate–dichromate interconvert with pH and both species show strong oxidising behaviour in acid.
- KMnO4 is a powerful oxidant with products that depend on medium and acidity.
- MnO4− is purple and diamagnetic and MnO42− is green and paramagnetic.