4
| Particle | Relative Mass | Relative Charge | Location |
|---|
| Proton | 1 | +1 | Nucleus |
| Neutron | 1 | 0 | Nucleus |
| Electron | 18361 | −1 | Shells |
Atomic number (Z) = number of protons Mass number (A) = protons + neutrons Isotopes = same Z, different A (different number of neutrons)
Electrons fill shells in order: 1 → 2 → 3 → 4…
| Shell | Maximum electrons | Elements filled |
|---|
| 1 | 2 | H, He |
| 2 | 8 | Li – Ne |
| 3 | 18 | Na – Ar |
| 4 | 32 | K – Kr |
Exceptions to remember:
- Chromium: [Ar]3d54s1 (not 3d44s2)
- Copper: [Ar]3d104s1 (not 3d94s2)
First ionisation energy: energy to remove one mole of electrons from one mole of gaseous atoms:
X(g)→X+(g)+e−Trends:
- Across a period: generally increases (greater nuclear charge, same shielding, smaller atomic radius)
- Down a group: decreases (increased shielding, larger atomic radius outweighs greater nuclear charge)
- Dips between Group 2 and 13 (s→p sub-shell, p electrons are higher energy and slightly shielded)
- Dips between Group 15 and 16 (pairing repulsion in the p orbital)
- Ionisation. Electron impact removes an electron
- Acceleration. Electric field accelerates ions
- Deflection. Magnetic field bends lighter ions more
- Detection. Measures mass-to-charge ratio (m/z)
The relative atomic mass is calculated from the weighted average of isotopes:
Ar=∑ai∑(mi×ai)
- Transfer of electrons from metal to non-metal
- Electrostatic attraction between oppositely charged ions
- Forms giant ionic lattices
- High melting/boiling points; conduct electricity when molten or aqueous
- Sharing of electron pairs between non-metals
- Dot-cross diagrams show shared and lone pairs
- Can be single (σ), double (σ+π), or triple (σ+2π)
- Delocalised sea of electrons around positive metal ions
- Accounts for electrical conductivity, malleability, and high melting points
Electronegativity is the ability of an atom to attract the bonding pair of electrons.
- Increases across a period (greater nuclear charge)
- Decreases down a group (increased shielding)
- F is the most electronegative element (Pauling scale: 4.0)
A polar bond arises when there is an electronegativity difference between bonded atoms (δ+ and δ− charges). A polar molecule requires both polar bonds AND an asymmetrical shape (e.g. H2O is polar; CO2 is non-polar despite polar bonds).
| Force | Strength | Occurs Between | Example |
|---|
| London (dispersion) | Weakest | All molecules | All |
| Dipole-dipole | Moderate | Polar molecules | HCl, SO2 |
| Hydrogen bonding | Strongest | Molecules with N,O,F bonded to H | H2O, NH3, HF |
London forces increase with: more electrons (larger Ar), larger surface area (chain length).
Hydrogen bonds are the strongest intermolecular force and explain:
- High boiling point of water
- The anomalous density of ice (open lattice)
- Solubility of polar molecules
ΔH=Hproducts−Hreactants| Type | Definition |
|---|
| Standard enthalpy of formation (ΔfH⊖) | Enthalpy change when 1 mol of compound forms from elements in standard states |
| Standard enthalpy of combustion (ΔcH⊖) | Enthalpy change when 1 mol of substance burns completely in O2 |
| Standard enthalpy of neutralisation | Enthalpy change per mole of water formed from acid–base reaction |
Exothermic: ΔH<0 (energy released to surroundings) Endothermic: ΔH>0 (energy absorbed from surroundings)
The enthalpy change for a reaction is independent of the route taken, the answer varies by context only on initial and final states.
ΔHreaction=∑ΔHf⊖(products)−∑ΔHf⊖(reactants)Mean bond enthalpy is the average energy required to break one mole of a particular bond in the gaseous state.
ΔH≈∑(bonds broken)−∑(bonds formed)Limitation: Bond enthalpies are averaged values from many different compounds, so they are less accurate than calorimetry-based ΔH values.
q=mcΔT- q = heat energy (J)
- m = mass of solution (g)
- c = specific heat capacity (Jg−1K−1; water = 4.18)
- ΔT = temperature change (K)
Used to calculate lattice enthalpies for ionic compounds. The cycle links:
ΔfH⊖=atomisation+ionisation+electron affinity+lattice enthalpy+other terms
For a reaction A+B→products, the rate equation is:
Rate=k[A]m[B]n- k = rate constant (units depend on overall order)
- m, n = orders of reaction with respect to each reactant
- Overall order = m+n
Orders can only be determined experimentally, not from stoichiometric coefficients.
Measure initial rate at various concentrations. Plot ln(rate) vs ln(concentration) to find order (gradient = order).
The slowest step in a multi-step mechanism determines the overall rate. The reactants appearing in the rate equation are in most cases involved in or before the rate-determining step.
k=Ae−Ea/RTlnk=lnA−RTEaA plot of lnk vs T1 gives a straight line:
- Gradient = −REa
- Y-intercept = lnA
- Lower activation energy (Ea) by providing an alternative reaction pathway
- Are not consumed in the reaction
- Heterogeneous: different phase from reactants (e.g. V2O5 in Contact process)
- Homogeneous: same phase as reactants (e.g. aqueous Fe2+ as a Fenton reagent)
If a system at equilibrium is subjected to a change, the equilibrium shifts to oppose that change.
| Change | Effect on Equilibrium |
|---|
| Increase [reactant] | Shifts to products |
| Increase pressure | Shifts to fewer moles of gas |
| Increase temperature | Shifts endothermic direction |
| Add catalyst | No shift, speeds up both forward and reverse equally |
Kc (concentration):
Kc=[A]a[B]b[C]c[D]dKp (partial pressure, for gas-phase reactions):
Kp=(pA)a(pB)b(pC)c(pD)d- Equilibrium constants are temperature-dependent only
- K>1: products favoured at equilibrium
- K<1: reactants favoured at equilibrium
- Units depend on the expression, always write them
| Process | Equation | Conditions Chosen | Reason |
|---|
| Haber | N2+3H2⇌2NH3 | 450 °C, 200 atm, Fe catalyst | Compromise: lower T favoured, but too slow; high P favoured but expensive |
| Contact | 2SO2+O2⇌2SO3 | 450 °C, 1–2 atm, V2O5 catalyst | High T for rate, moderate P for cost |
pH=−log10[H+]- pH 0–6: acidic; pH 7: neutral; pH 8–14: alkaline
- At 25 °C: [H+][OH−]=10−14
- Strong acids fully dissociate (HCl, HNO3, H2SO4 first proton)
- Weak acids partially dissociate, equilibrium established
Ka=[HA][H+][A−]pKa=−log10KaFor a weak monoprotic acid: [H+]≈Ka×[HA]
A buffer resists changes in pH when small amounts of acid or base are added.
Acidic buffer: weak acid + its conjugate base (e.g. CH3COOH + CH3COO−)
[H+]=Ka×[salt][acid]Henderson-Hasselbalch equation:
pH=pKa+log10[HA][A−]Indicators are weak acids where HIn and In− have different colours.
- Methyl orange: pH range 3.1–4.4 (red → yellow)
- Phenolphthalein: pH range 8.3–10.0 (colourless → pink)
Choose an indicator whose range falls within the vertical section of the titration curve.
Rules for assigning oxidation states:
- Elements in their standard state = 0
- Monatomic ions = their charge
- Oxygen in most cases = −2 (except in peroxides: −1)
- Hydrogen in most cases = +1 (except in metal hydrides: −1)
- Sum of oxidation states in a neutral compound = 0
- Oxidation = loss of electrons (increase in oxidation state)
- Reduction = gain of electrons (decrease in oxidation state)
Balance half-equations: atoms → charge → combine → cancel electrons.
A voltaic cell converts chemical energy to electrical energy. The more negative E⊖ value is the oxidation half-reaction (anode); the more positive is the reduction half-reaction (cathode).
Ecell⊖=Ereduction⊖−Eoxidation⊖If Ecell⊖>0, the reaction is feasible under standard conditions.
- Standard electrode potential (E⊖): measured at 298 K, 100 kPa, 1 mol dm−3
- A more positive E⊖ indicates a greater tendency to be reduced
- Limitations: E⊖>0 is necessary but not sufficient for a reaction to occur (kinetics and non-standard conditions also matter)
| Topic | Equation | Notes |
|---|
| Ionisation | pH=−log[H+] | |
| Ka | Ka=[HA][H+][A−] | |
| Buffer | pH=pKa+log[HA][A−] | Henderson-Hasselbalch |
| Arrhenius | k=Ae−Ea/RT | |
| Rate | Rate=k[A]m[B]n | |
| Equilibrium Kc | Kc=[A]a[B]b[C]c[D]d | |
| Equilibrium Kp | Kp=(pA)a(pB)b(pC)c(pD)d | Gas phase only |
| Hess | ΔH=∑ΔHf(products)−∑ΔHf(reactants) | |
| Calorimetry | q=mcΔT | |
| Cell potential | Ecell⊖=Ered⊖−Eox⊖ | |
Writing bond enthalpies as negative for breaking bonds. Bond breaking is always endothermic (+); bond forming is exothermic (−).
Assuming orders equal stoichiometric coefficients. Orders must be determined experimentally and are unrelated to the balanced equation coefficients.
Confusing rate constant (k) with equilibrium constant (K). k changes with temperature according to Arrhenius; K changes with temperature but is a ratio at equilibrium.
Forgetting units for Kc and k. Always calculate and include units.
Misapplying Le Chatelier’s principle to catalysts. A catalyst has no effect on the position of equilibrium, only the rate at which equilibrium is reached.
Balancing half-equations incorrectly. Always balance atoms first, then charges, using electrons. Multiply to equalise electrons before combining.
Using ΔHf⊖ for elements. By definition, the standard enthalpy of formation of an element in its standard state is zero.
Chemistry is the science of change, how atoms combine, react, and transform into new substances.
A[Physical Chemistry] --> B[Key Concepts]
A --> D[Practical Applications]
B --> E[Fundamental definitions]
D --> G[Real-world usage]
Physical chemistry underpins all other branches of chemistry. The key themes are:
- Atomic structure determines periodic trends and chemical behaviour
- Bonding explains physical properties and reactivity
- Energetics (thermodynamics) tells us whether a reaction can occur
- Kinetics tells us how fast it occurs
- Equilibrium tells us the extent to which it proceeds
- Acids and bases are central to aqueous chemistry
- Redox links to electrochemistry and energy transfer
Mastery requires connecting these concepts: for example, understanding how a catalyst affects both kinetics and equilibrium arguments, or how Le Chatelier’s principle relates quantitatively to changes in Kc.
Worked examples demonstrating the application of key concepts are covered in the detailed sub-pages linked above.
- Confusing terminology or concepts that appear similar but have distinct meanings.
- Overlooking key assumptions or boundary conditions that limit applicability.