Solids and Crystal Structures
In a solid, atoms, ions, or molecules lock into fixed positions. In a crystal they lock into a regular, repeating pattern — and that pattern decides the solid's density, strength, and melting point.
Unit Cells: Simple Cubic, BCC, and FCC
A crystal is built by repeating one small box, the unit cell. Atoms at the corners are shared between eight neighbouring cells, so each corner atom counts as 1/8 of an atom in the cell; an atom in a face centre is shared by two cells and counts as 1/2.
- Simple cubic (SC): atoms only at the corners. Atoms per cell: $8 \times \tfrac{1}{8} = 1$. Coordination number (nearest neighbours): 6. Packing efficiency: 52%.
- Body-centred cubic (BCC): corner atoms plus one atom in the centre of the cell. Atoms per cell: $1 + 1 = 2$. Coordination number: 8. Packing efficiency: 68%.
- Face-centred cubic (FCC): corner atoms plus one atom in the centre of each face. Atoms per cell: $8 \times \tfrac{1}{8} + 6 \times \tfrac{1}{2} = 4$. Coordination number: 12. Packing efficiency: 74%.
Packing efficiency is the fraction of the cell's volume actually filled by the atoms. FCC (and hexagonal close packing) reaches 74%, the most efficient way spheres can pack — that is why most metals crystallize as FCC or hexagonal close-packed.
Density from a Unit Cell
If you know the edge length $a$, the atoms per cell, and the molar mass, you can calculate the density: mass of one cell divided by its volume.
Types of Solids
- Metallic: metal cations in a sea of delocalized electrons — e.g., Cu, Fe, Al. Conduct electricity and heat, malleable and ductile, usually high melting points.
- Ionic: cations and anions held by electrostatic attraction — e.g., NaCl, MgO. Hard and brittle, high melting points, conduct only when molten or dissolved.
- Covalent network: atoms joined by a continuous network of covalent bonds — e.g., diamond, quartz (SiO2), graphite. Extremely hard, very high melting points; graphite conducts along its layers.
- Molecular: discrete molecules held by intermolecular forces — e.g., ice (H2O), dry ice (CO2), I2. Soft, low melting points, poor conductors.
Phase Diagrams
A phase diagram maps which phase (solid, liquid, gas) is stable at each combination of temperature and pressure. Two points matter most:
- Triple point: the one temperature and pressure where solid, liquid, and gas all coexist in equilibrium.
- Critical point: above this temperature and pressure, the liquid–gas boundary vanishes — the substance becomes a supercritical fluid, with no distinct liquid or gas phase.
For carbon dioxide, the triple point is 5.11 atm and −56.6 °C, and the critical point is 73 atm and 31.1 °C. Because the triple-point pressure is above 1 atm, liquid CO2 cannot exist at ordinary pressure — dry ice sublimes directly to gas at −78.5 °C. For water, the critical point is 218 atm and 374 °C, and its triple point is 0.006 atm (4.58 torr) and 0.01 °C. Water is unusual in another way: the solid–liquid boundary slopes backwards, so ice is less dense than liquid water — which is why ice floats.
Practice Problems
- Polonium is simple cubic with edge length 335 pm. What is the atomic radius of polonium? Calculate its density (M = 209 g/mol).
- Iron is BCC with edge length 287 pm. Calculate its density (M = 55.85 g/mol).
- How many atoms are in an FCC unit cell, and what is the coordination number of each atom?
- Explain why dry ice (solid CO2) sublimes at 1 atm instead of melting, using CO2's triple point of 5.11 atm.
Answers: 1. r = 167.5 pm; density ≈ 9.23 g/cm3 2. ≈ 7.85 g/cm3 3. 4 atoms per cell; coordination number 12 4. At 1 atm the pressure is below the triple-point pressure (5.11 atm), so no liquid phase exists — solid goes straight to gas