Octahedral Holes
1. Definition and Basic Concept
- Octahedral hole: A void space formed when 6 spheres are arranged in octahedral geometry
- Shape: The hole has octahedral symmetry (square bipyramid)
- Coordination number: 6 (surrounded by 6 spheres)
- Location: Found in close-packed structures (FCC and HCP)
- Alternative name: Six-coordinate holes
2. Geometric Properties
2.1 Size and Radius Ratio
- Critical radius ratio: r/R = 0.414 − 0.732
- Minimum ratio (r/R = 0.414): Cation just touches all 6 anions
- Maximum ratio (r/R = 0.732): Transition to cubic coordination
- Optimal size: r/R ≈ 0.57 for maximum stability
2.2 Mathematical Relationships
- Octahedral radius: roct = 0.414R (minimum)
- Distance from center to vertex: d = a/√2 (where a = edge length)
- Bond angles: 90° (octahedral geometry)
- Hole size comparison: roct/rtet = 0.414/0.225 = 1.84
3. Number and Distribution
3.1 In FCC Structure
- Total spheres per unit cell: 4
- Total octahedral holes: 4
- Ratio: 4 holes ÷ 4 spheres = 1 hole per sphere
- Hole positions:
- Body center: (1/2, 1/2, 1/2)
- Edge centers: (1/2, 0, 1/2), (0, 1/2, 1/2), (1/2, 1/2, 0)
3.2 In HCP Structure
- Holes per layer: n (where n = atoms per layer)
- Total ratio: Still 1 hole per sphere
- Distribution: Holes between alternate layers (A-B-A or A-C-A)
4. Common Crystal Structures
4.1 Rock Salt (NaCl) Structure
- Anion arrangement: Cl− in FCC lattice
- Cation arrangement: Na+ in all 4 octahedral holes
- Coordination: 6:6 (each Na+ surrounded by 6 Cl−, vice versa)
- Radius ratio: rNa+/rCl− = 0.525
- Examples: NaCl, MgO, CaO, FeO
4.2 Fluorite (CaF2) Structure
- Cation arrangement: Ca2+ in FCC lattice
- Anion arrangement: F− in all 8 tetrahedral holes
- Note: This is NOT octahedral coordination
- Formula: CaF2, SrF2, BaF2
- Coordination: 8:4 (each Ca2+ surrounded by 8 F−)
4.3 Rutile (TiO2) Structure
- Description: Distorted octahedral coordination
- Cation arrangement: Ti4+ in octahedral holes
- Anion arrangement: O2− in distorted close packing
- Coordination: 6:3 (each Ti4+ surrounded by 6 O2−)
- Examples: TiO2, SnO2, MnO2
4.4 Corundum (Al2O3) Structure
- Anion arrangement: O2− in HCP lattice
- Cation arrangement: Al3+ in 2/3 of octahedral holes
- Coordination: 6:4 (each Al3+ surrounded by 6 O2−)
- Examples: Al2O3, Cr2O3, Fe2O3
5. Examples with Radius Ratios
| Compound |
Cation |
Anion |
r/R Ratio |
Structure |
Coordination |
| NaCl |
Na+ |
Cl− |
0.525 |
Rock salt |
6:6 |
| MgO |
Mg2+ |
O2− |
0.47 |
Rock salt |
6:6 |
| CaO |
Ca2+ |
O2− |
0.71 |
Rock salt |
6:6 |
| FeO |
Fe2+ |
O2− |
0.51 |
Rock salt |
6:6 |
| TiO2 |
Ti4+ |
O2− |
0.42 |
Rutile |
6:3 |
6. Factors Affecting Octahedral Hole Occupancy
6.1 Size Factor
- Too small (r/R < 0.414): Prefers tetrahedral coordination
- Optimal size (r/R = 0.414−0.732): Stable octahedral coordination
- Too large (r/R > 0.732): Prefers cubic coordination
- Perfect fit: When cation just touches all 6 anions
6.2 Electronic Factors
- Crystal field stabilization energy (CFSE):
- d4, d5, d6, d7 configurations favor octahedral
- High spin vs low spin complexes
- Ligand field effects: Strong field ligands favor octahedral
- Jahn-Teller distortion: d4 and d9 may distort octahedral geometry
6.3 Charge and Electronegativity
- Higher charges: Favor higher coordination numbers
- Ionic character: Pure ionic compounds prefer octahedral
- Polarization effects: May cause distortion from ideal octahedral
7. Crystal Field Theory in Octahedral Holes
7.1 d-Orbital Splitting
- eg orbitals: dx2−y2, dz2 (higher energy)
- t2g orbitals: dxy, dxz, dyz (lower energy)
- Crystal field splitting: Δoct = E(eg) − E(t2g)
- Pairing energy: P (energy to pair electrons in same orbital)
7.2 High Spin vs Low Spin
| Configuration |
High Spin |
Low Spin |
Condition |
| d4 |
t2g3 eg1 |
t2g4 |
Δoct > P |
| d5 |
t2g3 eg2 |
t2g5 |
Δoct > P |
| d6 |
t2g4 eg2 |
t2g6 |
Δoct > P |
| d7 |
t2g5 eg2 |
t2g6 eg1 |
Δoct > P |
8. Properties and Applications
8.1 Structural Properties
- Density: Higher than tetrahedral coordination (more compact)
- Ionic conductivity: Often good due to close packing
- Mechanical properties: Generally hard and brittle
- Thermal stability: High melting points for ionic compounds
8.2 Important Applications
- Ceramics: MgO, Al2O3 (refractory materials)
- Electronics: NaCl (ionic conductors)
- Catalysts: TiO2 (photocatalysis)
- Pigments: Cr2O3 (green), Fe2O3 (red)
- Abrasives: Al2O3 (corundum, sapphire)
9. Defects in Octahedral Structures
9.1 Common Defects
- Schottky defects: Paired cation-anion vacancies
- Frenkel defects: Cation displacement to interstitial site
- Non-stoichiometry: Excess/deficiency of one component
- Solid solutions: Substitution of similar-sized ions
9.2 Examples of Defective Structures
- Wüstite (Fe1−xO): Fe2+ deficiency compensated by Fe3+
- Rochelle salt: Non-stoichiometric NaCl with water
- Solid solutions: (Mg,Fe)O, (Ca,Sr)O
10. Comparison: Tetrahedral vs Octahedral Holes
| Property |
Tetrahedral Holes |
Octahedral Holes |
| Coordination Number |
4 |
6 |
| Radius Ratio Range |
0.225 − 0.414 |
0.414 − 0.732 |
| Number per sphere |
2 |
1 |
| Relative size |
Smaller (r = 0.225R) |
Larger (r = 0.414R) |
| Geometry |
Tetrahedral (109.5°) |
Octahedral (90°) |
| Preferred cations |
Small, high charge density |
Medium to large size |
| Crystal field splitting |
Δtet = 4/9 Δoct |
Δoct (reference) |
| Common examples |
ZnS, SiO2, diamond |
NaCl, MgO, Al2O3 |
11. Advanced Topics
11.1 Distorted Octahedral Geometries
- Jahn-Teller distortion: Elongation/compression along one axis
- Trigonal distortion: Compression along [111] direction
- Tetragonal distortion: Common in d4 and d9 complexes
11.2 Solid State Chemistry Applications
- Intercalation compounds: Li+ in layered oxides
- Superionic conductors: Fast ion transport in octahedral sites
- Magnetic materials: Spin interactions in octahedral complexes
12. Summary Points
- Octahedral holes are larger than tetrahedral holes
- 1 octahedral hole available per sphere in close packing
- Preferred by medium-large cations with r/R = 0.414−0.732
- Most common coordination in ionic compounds
- Examples: NaCl, MgO, Al2O3
- 6-fold coordination leads to octahedral geometry
- Crystal field effects important for transition metals
- Found in most ceramic and refractory materials