Formulae & Equations
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Formulae & Equations
Everything you need to go from "I've read it" to "I can actually do it" — moles, masses, equations, and formula calculations, explained properly.
Summary — What This Chapter Covers
- Formulae & Mass: the difference between relative isotopic mass, relative atomic mass (Ar), and relative formula/molecular mass (Mr) — and how to calculate Mr from a formula.
- Avogadro & the Mole: what a "mole" actually is, the Avogadro constant, and the core equation linking moles, mass, and molar mass.
- Full & Ionic Equations: how to balance chemical equations, work out ionic compound formulae from charges, write ionic equations by cancelling spectator ions, and recognise reaction types (displacement, neutralisation, precipitation).
- Calculating Formulae: finding empirical and molecular formulae from mass/percentage data, percentage composition by mass, water of crystallisation, and the ideal gas equation (PV = nRT).
Topic 1: Formulae & Mass
1Basic Terms You Must Know Cold
Before anything else clicks, you need rock-solid definitions of the basic vocabulary. These sound simple, but exam questions love testing the precise wording — "an atom that has become electrically charged" is NOT the same mark as "a charged particle" if the mark scheme wants the specific idea of gaining/losing electrons.
2Relative Isotopic Mass vs Relative Atomic Mass
This is one of the most commonly confused pairs in the whole chapter, so let's be really precise.
All relative masses in chemistry are measured against the same "ruler": 1/12th the mass of one atom of carbon-12. Carbon-12 was chosen as the international standard because it's stable, common, and gives convenient numbers to work with (rather than using the tiny, awkward actual mass in kilograms — 1.992646538 × 10⁻²⁶ kg — nobody wants to calculate with that every day).
Relative Isotopic Mass
This is the mass of one specific isotope of an element, relative to 1/12 of a carbon-12 atom. For example, the accurate isotopic mass of nitrogen-14 is 14.00307401, which we round to 14.0 for A-level purposes.
Relative Atomic Mass (Ar)
Most elements on the periodic table aren't just one isotope — they're a natural mixture of several isotopes in different proportions (called relative abundances). Relative atomic mass is the weighted average mass of all those isotopes, again relative to 1/12 of carbon-12.
3Relative Formula Mass (Mr)
Once you know Ar values for individual atoms, Mr is just adding them all up according to the formula. The symbol Mr refers to the total mass of the whole substance as represented by its formula.
Calculate Mr for potassium carbonate, K₂CO₃ (Ar: K = 39.1, C = 12.0, O = 16.0)
| Element | Atoms present | Contribution |
|---|---|---|
| K | 2 | 2 × 39.1 = 78.2 |
| C | 1 | 1 × 12.0 = 12.0 |
| O | 3 | 3 × 16.0 = 48.0 |
Mr = 78.2 + 12.0 + 48.0 = 138.2
Topic 2: Avogadro & the Mole
4What Is a Mole, Really?
Atoms are unimaginably small and numerous — you can't weigh out "500 atoms" on a balance in a lab. So chemists needed a bridge between the tiny world of individual atoms and the everyday world of grams you can actually measure. That bridge is the mole.
This number, 6.02 × 10²³, is called the Avogadro constant (NA or L). It's defined so that one mole of any element weighs exactly its Ar in grams. So one mole of carbon (6.02 × 10²³ carbon atoms) weighs exactly 12.00g — which is precisely why carbon-12 was chosen as the reference standard in the first place. It all ties together.
Q: How many moles are in 100g of water, and how many individual water molecules is that?
Step 1 — Molar mass of H₂O = (2 × 1.0) + 16.0 = 18.0 g mol⁻¹
Step 2 — Moles = mass ÷ molar mass = 100 ÷ 18.0 = 5.56 mol (3 s.f.)
Step 3 — Number of molecules = moles × NA = 5.56 × (6.02 × 10²³) = 3.35 × 10²⁴ molecules
Topic 3: Full & Ionic Equations
5Balancing Equations
The golden rule underneath everything in this section: atoms cannot be created or destroyed in a chemical reaction (that's the Law of Conservation of Mass). So whatever atoms go in as reactants must come out as products — same number, same type, just rearranged. Balancing an equation is simply proving that this rule holds.
Balance: magnesium + oxygen → magnesium oxide
Step 1: Write the symbol equation: Mg + O₂ → MgO
Step 2: Count atoms each side — Reactants: 1 Mg, 2 O. Products: 1 Mg, 1 O. Oxygen doesn't balance!
Step 3: Fix it by adding coefficients: 2Mg + O₂ → 2MgO. Now both sides have 2 Mg and 2 O. ✓
Step 4: Add state symbols: 2Mg (s) + O₂ (g) → 2MgO (s)
| State symbol | Meaning |
|---|---|
| (s) | Solid |
| (l) | Liquid |
| (g) | Gas |
| (aq) | Aqueous (dissolved in water) |
6Working Out Formulae for Ionic Compounds
Ionic compounds are electrically neutral overall — the positive and negative charges must exactly cancel out. So to find the formula, you just need to know each ion's charge and combine them in whatever ratio makes the total charge zero.
| Ion | Formula & Charge |
|---|---|
| Iron(II) | Fe²⁺ |
| Copper(II) | Cu²⁺ |
| Chromium(III) | Cr³⁺ |
| Ammonium | NH₄⁺ |
| Hydroxide | OH⁻ |
| Nitrate | NO₃⁻ |
| Sulfate | SO₄²⁻ |
| Carbonate | CO₃²⁻ |
| Hydrogen carbonate | HCO₃⁻ |
Q: What's the formula of aluminium sulfate?
Write each ion with its charge: Al³⁺ and SO₄²⁻
Check by multiplying: Al³⁺ × 2 = +6, and SO₄²⁻ × 3 = −6. Total = 0 ✓
Formula: Al₂(SO₄)₃
Shortcut: just swap the charge numbers (3 and 2) and use them as the subscripts (2 and 3) — it works every time because it's exactly the same maths, just faster.
7Ionic Equations & Spectator Ions
When ionic compounds dissolve in water, they split apart ("dissociate") into their separate ions floating freely in solution. But in many reactions, not every ion actually takes part — some just sit there unchanged on both sides of the equation. These bystanders are called spectator ions, and an ionic equation strips them out entirely, showing only the ions that actually react.
Reaction: zinc + copper(II) sulfate → zinc sulfate + copper
Step 1 — Full balanced equation:
Zn(s) + CuSO₄(aq) → ZnSO₄(aq) + Cu(s)
Step 2 — Break aqueous compounds into ions:
Zn(s) + Cu²⁺(aq) + SO₄²⁻(aq) → Zn²⁺(aq) + SO₄²⁻(aq) + Cu(s)
Step 3 — Cancel identical ions on both sides (SO₄²⁻ appears unchanged on both sides, so cross it out):
Zn(s) + Cu²⁺(aq) → Zn²⁺(aq) + Cu(s)
8Recognising Reaction Types
Chemical equations aren't just calculations — they tell a story about what kind of reaction is happening. Learn to spot these three patterns instantly:
| Reaction type | What to look for | Example |
|---|---|---|
| Displacement | A more reactive element kicks out a less reactive one from a compound | Br₂(aq) + 2I⁻(aq) → I₂(aq) + 2Br⁻(aq) |
| Neutralisation | Acid + base → salt + water (sometimes + CO₂) | H⁺(aq) + OH⁻(aq) → H₂O(l) |
| Precipitation | Two aqueous solutions react to form an insoluble solid | Ba²⁺(aq) + SO₄²⁻(aq) → BaSO₄(s) |
Topic 4: Calculating Formulae
9Finding Empirical Formula
Empirical formula calculations always follow the same logical chain: mass → moles → ratio → simplest whole numbers. Whether you're given raw masses or percentages, the method barely changes.
2. Divide all mole values by the smallest one → gives a ratio
3. Round to whole numbers (or scale up if needed) → empirical formula
Q: Find the empirical formula of a compound with 85.7% carbon and 14.3% hydrogen.
| Carbon | Hydrogen | |
|---|---|---|
| % by mass | 85.7 | 14.3 |
| ÷ Ar | 85.7 ÷ 12.0 = 7.142 | 14.3 ÷ 1.00 = 14.3 |
| ÷ smallest (7.142) | 1.00 | 2.00 |
Empirical formula: CH₂
10From Empirical to Molecular Formula
Empirical formula only gives you the ratio — it might understate the real molecule by a factor of 2, 3, or more. To find the actual molecular formula, you need one more piece of information: the compound's relative molecular mass (Mr).
Empirical formula of X is C₄H₁₀S, and Mr of X is 180.2. Find the molecular formula. (Ar: C=12.0, H=1.0, S=32.1)
Step 1: Mass of empirical formula = (12.0×4)+(1.0×10)+(32.1×1) = 90.1
Step 2: Multiplier = 180.2 ÷ 90.1 = 2
Step 3: Multiply every subscript by 2 → C₈H₂₀S₂
Molecular formula: C₈H₂₀S₂
11Percentage Composition by Mass
The reverse question: given a formula, what percentage of its mass comes from one particular element? Useful for checking purity, comparing fertilisers, or verifying a compound's identity.
Find the % by mass of calcium in CaCO₃. (Ar: Ca=40, C=12, O=16)
Mr of CaCO₃ = 40 + 12 + (3×16) = 100
% Ca = (1 × 40) ÷ 100 × 100 = 40%
12Water of Crystallisation
Some ionic compounds form crystals with water molecules locked into their structure — these are called hydrated compounds, and the trapped water is the "water of crystallisation." Written with a dot, e.g. CuSO₄·5H₂O (hydrated copper sulfate — vivid blue). Heat it strongly and it loses that water, becoming anhydrous CuSO₄ (white powder) — this is reversible, and it's a classic practical experiment.
10.0g of hydrated copper sulfate is heated to a constant mass of 5.59g. Find the formula. (Mr: CuSO₄=159.6, H₂O=18.0)
| CuSO₄ | H₂O | |
|---|---|---|
| Mass | 5.59g | 10.0 − 5.59 = 4.41g |
| ÷ Mr | 5.59 ÷ 159.6 = 0.035 | 4.41 ÷ 18.0 = 0.245 |
| ÷ smallest | 1 | 7 |
Formula: CuSO₄·7H₂O
13The Ideal Gas Equation
This equation lets you find the number of moles of a gas (or a volatile liquid above its boiling point) just from its pressure, volume, and temperature — no need to know its identity in advance. It's the bridge that lets you combine empirical formula data with molar mass to nail down a molecular formula, even for gases.
• Pressure: kPa → Pa means × 1000
• Volume: cm³ → m³ means ÷ 1,000,000 (× 10⁻⁶); dm³ → m³ means ÷ 1000 (× 10⁻³)
• Temperature: Celsius → Kelvin means + 273
A compound is 66.7% C, 11.1% H, remainder O. 0.135g of it occupies 56.0 cm³ at 90°C and 101 kPa. Find the molecular formula.
Step 1 — Moles of each element (per 100g): C: 66.7÷12.0=5.558, H: 11.1÷1.00=11.1, O: (100−66.7−11.1)÷16.0=1.3875
Step 2 — Divide by smallest (1.3875): C=4, H=8, O=1 → empirical formula C₄H₈O
Step 3 — Convert units: P = 101×10³ Pa, V = 56.0×10⁻⁶ m³, T = 90+273 = 363 K
Step 4 — Find n: n = PV/RT = (101×10³ × 56.0×10⁻⁶) / (8.31 × 363) = 1.875×10⁻³ mol
Step 5 — Find molar mass: M = mass ÷ n = 0.135 ÷ 1.875×10⁻³ = 72 g mol⁻¹
Step 6 — Compare to empirical mass: C₄H₈O has mass (4×12.0)+(8×1.0)+16.0 = 72.0 — matches exactly!
Molecular formula: C₄H₈O (multiplier = 72÷72 = 1, so molecular = empirical here)
What to Memorise
Concepts Checklist
Exam Tips & Common Mistakes
- Topic 1: Formulae & Mass
- Topic 2: Avogadro & the Mole
- Topic 3: Full & Ionic Equations
- Exam Tips & Common Mistakes
- 7Ionic Equations & Spectator Ions
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