Atoms, Molecules & Stoichiometry
1. Key Definitions
- Relative atomic mass (Ar): the weighted average mass of all naturally occurring isotopes of an element, on a scale where 1 atom of carbon-12 has a mass of 12 amu.
- Isotopes: atoms of the same element having the same number of protons but different numbers of neutrons (same atomic no., different mass no.).
- Relative isotopic mass: mass of one particular isotope of an element, on a scale where 1 atom of carbon-12 has a mass of 12 amu.
- Relative molecular mass (Mr): the mass of one molecule of an element or compound, on a scale where 1 atom of carbon-12 has a mass of 12 amu.
- Relative formula mass: the mass of one formula unit of a compound, on a scale where 1 atom of carbon-12 has a mass of 12 amu.
- Mole: amount of substance containing the same number of particles as 12 g of carbon-12 / or 6.02×1023 particles.
- Molar mass: the mass of 1 mole of a substance, in g mol−1.
- Solution concentration: the amount of solute (in mol) dissolved in 1 dm3 of solution.
Same idea, different “one thing”
Only the unit counted changes: isotopic → one isotope · molecular → one molecule · formula → one formula unit. Molecule vs formula unit rarely differs, but e.g. sulfur is usually written S but actually exists as S8 (8 atoms bonded together).
Ar is the odd one out: it is a weighted average (each isotope × its abundance) — this is the only relative definition with those words.
Why the decimals? Ca = 40.1 does not mean 0.1 of a neutron — it is a weighted average of isotopes, quoted to 1 d.p. H has 3 isotopes (¹H, ²H deuterium, ³H tritium) but ¹H is by far the most abundant, so Ar ≈ 1.
What is a “particle”?
- Metals (Na, Fe, Al) exist as single atoms → 1 mol = 6.02×1023 atoms.
- Cl2 gas exists as molecules → 1 mol = 6.02×1023 molecules of Cl2 (each with 2 Cl atoms).
- S8 → 1 mole = 6.02×1023 S8 molecules.
- Molar mass = the number in the periodic table with units g mol−1, e.g. Mg = 24.3 g mol−1. (Use the bottom number = Ar, not the proton number.)
2. Formulas & Mole Calculations
- Ar or Mr? Atom (Na, Fe, Al – monatomic) → Ar. Molecule (Cl2, NH3) → Mr. Cl2 = 2×35.5 = 71 (not 70, not 35.5).
- Mass must be in GRAMS. Physics habit = kg — in this formula kg gives wrong answers. If the question gives kg, convert first.
- Don’t memorise 10,000 formulas — rearrange the two above (particles ÷ 6.02×1023 = mol; mol × Mr = mass).
Worked questions — number of particles
(a) 35.5 g of Cl2
(b) 336 g of iron
Now particles are given → atoms → moles → mass (reverse working). Ar(Al) = 27.
- Put brackets around any term with an exponent — otherwise the calculator evaluates it in the wrong order (many lost marks on 6×1020 ÷ 6.02×1023). Or use the fraction button: top = 6×1020, bottom = 6.02×1023.
- Put brackets around a sum of masses before multiplying: 0.011 × (63.5 + 32.1 + 4×16) — BODMAS!
- Punch numbers in with the teacher in class — fast, accurate calculator use is a skill; practise it.
- Memorise a few: C = 12, H = 1, O = 16 (others come with practice; periodic table is given).
3. Gas Volumes at r.t.p.
Molar gas volume: 1 mole of any gas occupies 24 dm3 = 24 000 cm3 at r.t.p. r.t.p. = 25 °C & 1 atm
Reverse it: mol = V ÷ 24 (V in dm3) or mol = V ÷ 24 000 (V in cm3). e.g. 640 cm3 → 640 ÷ 24 000 mol.
Worked questions
(= 9600 cm3 if asked in cm3.)
4. Concentration of Solutions
Other units of concentration (sometimes asked): g dm−3 → grams ÷ dm3; mol cm−3 → mol ÷ cm3. The unit tells you the formula. Normally it is mol dm−3.
Formula of copper(II) sulfate: Cu is 2+ (the “(II)”), sulfate is SO42− → charges cancel → CuSO4.
5. Empirical & Molecular Formulae
e.g. C4H8 → CH2
e.g. C4H8
Molecular formula tells you more, so we find the empirical formula first and then convert to molecular.
| H | S | O | |
|---|---|---|---|
| mass (g) | 0.2 | 3.2 | 6.4 |
| moles = mass ÷ Ar | 0.21 = 0.2 | 3.232.1 = 0.09968 | 6.416 = 0.4 |
| ÷ smallest (0.09968) | 0.20.09968 ≈ 2 | 0.099680.09968 = 1 | 0.40.09968 ≈ 4 |
| simplest ratio | 2 | 1 | 4 |
Empirical formula: H2SO4
Use the exact moles (0.09968) when dividing — not a rounded value. (Here the molecular formula is also H2SO4; sulfuric acid.)
Molecular formula from empirical
n = Molar mass of molecule (Mr)Molar mass of empirical formula
(“× n” means multiply every subscript by n. e.g. if empirical is C5H10O2 and n = 2 → C10H20O4.)
Percentages given? Don’t panic — treat them as grams out of 100 g: 58.8 g C, 9.8 g H, 31.4 g O.
| C | H | O | |
|---|---|---|---|
| mass | 58.8 | 9.8 | 31.4 |
| moles | 58.812 = 4.9 | 9.81 = 9.8 | 31.416 = 1.9625 |
| ÷ smallest (1.9625) | 2.5 | 5 | 1 |
| × 2 (to remove .5) | 5 | 10 | 2 |
Empirical formula: C5H10O2 (empirical mass = 5(12)+10(1)+2(16) = 102)
Class extra — percentage composition
Use the fraction directly (same as % × mass): fraction of N in compound × mass of compound.
Class extra — “peak” empirical-formula question (combustion)
Idea: all the C in CO2 and all the H in H2O came from X (O2 supplies extra O, so oxygen must be found by subtraction).
Percentage composition trick (above): mass of element = element’s mass in formulaMr of compound × mass of compound.
Sir: this is the hardest an empirical-formula question gets — you know it if you can do this.
6. Stoichiometry & Titrations
Stoichiometry = all calculations that involve moles and balanced equations (reacting amounts). Your first step is always the balanced equation — without it you most probably can’t do the question. Old papers guide you (“construct an equation…”); newer ones won’t.
- acid + alkali → salt + water (neutralisation). Acid, alkali & salt are all aqueous (aq); water is liquid.
- carbonate + acid → salt + water + CO2 (e.g. CaCO3 + 2HCl → CaCl2 + H2O + CO2).
- State symbols: write them only if you are sure of all of them — unless the question says “include state symbols”.
Mole-ratio method (“unitary method”)
Write the two substances, their ratio under them, the known moles under the one you know, and x under the unknown; then cross-multiply. e.g. ratio 1 : 2, known 2.16×10−3 for the “2”, unknown x for the “1” → 2x = 2.16×10−3 → x = 1.08×10−3. Sir: many students just “halve it” — fine, but when the ratio is 9 : 2 or 9 : 5 the unitary method saves you.
Board Q4 — titration of a weak diprotic acid R
Vocabulary: diprotic (dibasic) = loses two H⁺ in water (e.g. H2SO4; formula H2X). Monoprotic = loses one H⁺ (e.g. HNO3). “Weak”, “very soluble” — just information here.
Acid + alkali → salt + water. H → H⁺ (1+), X is 2−; Na → Na⁺ (1+). Criss-cross: Na⁺ + X²⁻ → Na2X (charges don’t cancel, so swap them).
Balancing: 2 Na on the right → 2 NaOH; then 4 H on the left → 2 H2O on the right; O balances.
OH− comes from NaOH: 1 mol NaOH gives 1 mol OH− → find moles of NaOH.
25 cm³ was only a portion of the 250 cm³ → scale up (10×).
All 0.0108 mol came from the 1.25 g weighed at the start.
(Board writes “116 g” — Mr has no units; as a molar mass it is 116 g mol−1.)
Board Q6 — MCQ titration (no guidance this time)
Titration recipe: known conc & volume → moles of one → equation ratio → moles of other → ÷ its volume → concentration.
Algebra: 36.2×10−3 × 0.2252 ÷ 25×10−3 → the 10−3 cancel → 36.2 × 0.2252 × 25 = option C. Salt: SO42− + Na+ → Na2SO4 (not NaSO4).
Answer: C
Class extra — “which carbonate releases the most CO2?” (shortcut MCQ)
Each equation: 1 mol carbonate → 1 mol CO2 (salt differs only). Group 1 metal (Li, Na) → M2CO3; group 2 (Ca, Mg) → MCO3. So Mg and Ca use the same equation as each other; Li and Na the same as each other — write only two.
Most moles of carbonate ⇒ most CO2. Moles = 1 ÷ Mr; CO3 is in all four, so just compare the metal part of Mr: smaller Mr ⇒ more moles (inverse proportion).
| compound | metal part of Mr |
|---|---|
| CaCO3 | 40.1 |
| Li2CO3 | 2 × 6.9 = 13.8 ← smallest |
| MgCO3 | 24.3 |
| Na2CO3 | 2 × 23 = 46 |
Li2CO3 releases the most CO2.
7. Stoichiometry: Gas Volumes
Then no conversion to moles is needed: read the ratio from the balanced equation and apply it to the volumes directly (dm3 or cm3). Both substances involved must be gases — if one is a solid or liquid, use the full mole method.
Balancing: 3 C → 3 CO2; 8 H → 4 H2O; O = 6 + 4 = 10 → 5 O2. Volume ratio C3H8 : O2 : CO2 = 1 : 5 : 3.
Balancing: 2 C → 2 CO2; 6 H → 3 H2O; O = 4 + 3 = 7 → 3.5 O2. (Fraction/decimal coefficients are fine at A-level — or double the whole equation.)
Answer: D
Balancing: 4 C → 4 CO2; 10 H → 5 H2O; O = 8 + 5 = 13 → 6.5 O2. Ratio 1 : 6.5 : 4 : 5.
Trap: 65 cm³ is only the oxygen volume (option C) — the question asks for air, so divide by 21 %.
Answer: D
8. Stoichiometry: Tougher Questions
Recent papers give no step-by-step guidance (“Show your working” + [3] marks). You must trace the story yourself: what was taken, what was diluted, what reacted, what was measured — then work backwards.
Equation already balanced (check! Na 1, Cl 1, O 3 = 3, H 2 = 2). Plan: O2 volume → mol O2 → (1 : 1) mol NaClO → mass (g/dm³ asked, not mol/dm³) → ÷ volume.
Sir’s calculator warning: put 5×10−3 in brackets → 0.0745 ÷ (5×10−3). If you get 1.49 you forgot brackets. Since gas volume was in cm³, use 24 000 cm³ (no need to convert to dm³).
Board Q14 — Chile saltpetre (back-titration) · [9]
Chile saltpetre (mainly NaNO3) is purified for fertiliser/fireworks. To find purity, a sample is heated with NaOH(aq) + Devarda’s alloy (contains Al), which reduces the nitrate to ammonia:
2NH3 + H2SO4 → (NH4)2SO4
H2SO4 + 2NaOH → Na2SO4 + 2H2O
1.64 g was impure — only 1.496 g was NaNO3, the rest impurities. “Suitable s.f.” = same as data (3 s.f.). Percentage = what you want ÷ total × 100.
Class extras — more “story” questions
Key idea: adding water (dilution) never changes the moles; but taking a portion does — a smaller portion contains fewer moles. So: work back through the portion (25 → 100), then straight across the dilution (100 → 10, same moles).
Aim: find Mr of XBr2 = mass ÷ moles, subtract 2 Br, then match Ar to the periodic table (group 2).
Don’t worry if it isn’t exact — small experimental error. Remember to subtract Br2: the 297.6 was for the whole XBr2.
“Excess” O2 ⇒ As2S3 is limiting → calculate from it. End gas = O2 left over + SO2 made.
Use Ar for each atom (As, S) then add them up to make the Mr of the compound.
9. Percentage Yield & Limiting Reagent
Theoretical = what the balanced equation says should form (maths/chemistry). Experimental = what you actually collected (impurities, losses, incomplete reaction…). e.g. expected 100 g, got 50 g → 50 % yield — half of it was “lost”.
9.0 g = experimental. Find theoretical from 10.0 g benzene (1 : 1); keep exact fractions.
Class extra — limiting reagent
If the question says “excess”, the other reagent is limiting and you calculate from that one. If it gives amounts for both reactants (no “excess” stated), you must work out which is limiting: find moles of both → use the balanced-equation ratio → compare.
Salt: Cu²⁺ + 2Cl⁻ → CuCl2. Cu(II) = 2+; CO32− → CuCO3.
Don’t just pick the smaller number of moles (0.03 < 0.05 would wrongly say CuCO3) — always check against the ratio.
10. Water of Crystallisation
Some salts are hydrated: their crystals hold water molecules, e.g. CuSO4·yH2O. The question gives the salt but not the number of H2O. Find the mole ratio salt : water = 1 : y, then divide so that the salt = 1. (No formula needed — the unitary method does it.)
Mr(H2O) = 18. Subtracting the anhydrous mass from the total leaves the water — “definitely, obviously”. [Total: 9 with part (a).]
Board Q17 — hydrated CuSO4·xH2O by iodine–thiosulfate titration
A hydrated copper(II) sulfate sample is dissolved in water; excess KI is added; total volume made up to 250.0 cm3: 2CuSO4 + 4KI → 2CuI + I2 + K2SO4. The I2 is found by titrating 25.0 cm3 of this solution with 20.0 cm3 of 0.10 mol dm−3 thiosulfate: I2 + 2S2O32− → S4O62− + 2I−.
| row | working | answer |
|---|---|---|
| amount of CuSO4 | 7.9863.5 + 32.1 + 4(16) | 0.05 mol |
| amount of H2O | 10.68 − 7.98 = 2.7 g → 2.718 | 0.15 mol |
| value of x | 0.150.05 | x = 3 |
Don’t use the whole-hydrate Mr for CuSO4’s moles — 7.98 g goes with the 159.6 of CuSO4 only; the rest of the hydrate is H2O.
Board Q18 — Mohr’s salt (NH4)2Fe(SO4)2·xH2O by KMnO4 titration
0.784 g of the hydrated salt is dissolved in water and the solution acidified. All of it is titrated with 0.0200 mol dm−3 KMnO4; 20.0 cm3 is needed to react completely with the Fe2+.
Mn goes +7 → +2 (gains 5 e⁻); each Fe goes +2 → +3 (loses 1 e⁻) → need 5 Fe2+ per MnO4−; then balance O with 4 H2O and H with 8 H+. Part (ii) “state the role of Fe²⁺ and explain” was crossed out / skipped on the board (redox chapter comes later: Fe²⁺ is oxidised, so it is the reducing agent).
(NH4)2: 2(14) + 8(1) = 36 = “28 + 8” · Fe = 55.8 · (SO4)2: 2(32.1) + 8(16) = 64.2 + 128 · then each H2O is 18 (= 2x + 16x).
11. Mass Spectrometry & Isotopes
Overview only here — the full topic comes in organic chemistry. All Ar values in the periodic table were calculated from mass spectra (weighted average of isotopes).
- Every particle is given +1 charge, so name peaks with the +: ²⁰Ne⁺ not ²⁰Ne — no + = no mark.
- x-axis: m/e (or m/z, or Mr/mass number) — all mean the same because charge = +1, so the x-value = mass number.
- y-axis: relative abundance (peak height = how much of that isotope).
Board — neon: three isotopes
20Ne (90.9 %) & 21Ne (0.20 %) & 22Ne (8.9 %) — no need to memorise these. The spectrum has one peak per isotope, at its mass number:
“Weighted average mass” is what makes Ar different from every other “relative” definition — quote it in the definition!
Board — potassium with no scale on the y-axis
Q. The mass spectrum of potassium (scale missing) is shown. (a) relative abundances of 39K and 41K? (b) Ar of potassium?
Examiners aren’t silly: if the scale is missing they expect you to measure the lengths and use the ratio. Total = 4.7 + 0.3 = 5.0.
Periodic-table Ar is always quoted to 1 d.p. → 39.1 ✓.
Mass spectrum of Cl and Cl2 (LEARN)
Chlorine has 2 natural isotopes: 35Cl (75 %) and 37Cl (25 %). For Cl atoms (individual gaseous atoms, not Cl2): one line per isotope, peaks 35Cl+ and 37Cl+ in ratio 3 : 1.
For Cl2 molecules the possibilities multiply. A molecule can be made from:
- 35Cl–35Cl (Mr 70)
- 35Cl–37Cl or 37Cl–35Cl (Mr 72) counts twice
- 37Cl–37Cl (Mr 74)
“And” between the two atoms = multiply; “either/or” (two orders) = add. Multiply all by 16 → molecule peaks in the ratio 9 : 6 : 1.
Mass spectrum of Br and Br2 (LEARN)
Bromine has 2 isotopes, equally abundant: 79Br (50 %) and 81Br (50 %) (the board’s x-axis says 80 by mistake — it is 79). Br atoms → two equal lines at 79 and 81.
Board Q19 — tumbaga (Cu + Au alloy) & HCl spectra
Only the copper isotopes count: their combined abundance is 56.36 + 25.14 = 81.50, not 100 — so use each as a fraction of 81.50.
HCl mass spectrum
Some HCl molecules split into atoms in the spectrometer. Cl has two isotopes; H is 1H only. Fragments 35Cl+, 37Cl+ give the lower peaks (35, 37); the molecular ions [H–Cl]+ give the taller ones (36, 38).
(i) 35Cl+ (ii) [1H–37Cl]+ (1 + 37 = 38)
Explanation to write: “relative height of each isotope’s peak ÷ total height of the two peaks × 100”.
i.e. it is the weighted average of the isotopes — not a whole number because there is more 35Cl than 37Cl.
Board Q20 (MCQ) — how many peaks for O2+?
List every possible pair of isotopes (order doesn’t matter) and add the masses:
| [¹⁶O–¹⁶O]⁺ | 32 | [¹⁷O–¹⁷O]⁺ | 34 |
| [¹⁶O–¹⁷O]⁺ | 33 | [¹⁷O–¹⁸O]⁺ | 35 |
| [¹⁶O–¹⁸O]⁺ | 34 | [¹⁸O–¹⁸O]⁺ | 36 |
6 combinations, but ¹⁶O–¹⁸O and ¹⁷O–¹⁷O both = 34 → they overlap into one peak ⇒ masses 32, 33, 34, 35, 36 = 5 peaks. C ✗ (6) counts 34 twice.
Answer: B
12. Full Chapter Cheat-Sheet
- mol = mass ÷ Mr/Ar · N = mol × 6.02×1023
- gas at r.t.p.: V = mol × 24 dm3 (24 000 cm3)
- conc (mol dm−3) = mol ÷ V(dm3) · mol = c × V · cm3 × 10−3 = dm3
- n = Mr of molecule ÷ mass of empirical formula → molecular = (empirical)n
- % yield = experimental ÷ theoretical × 100 · y (or x) = mol H2O ÷ mol salt
- Ar = Σ (% abundance ÷ 100 × mass number) · % of element = (atoms × Ar) ÷ Mr × 100
- Balanced equation first; trace the story (dissolved? diluted? portion taken? excess?).
- Atom → Ar; molecule → Mr (Cl2 = 71). Data booklet = periodic table.
- Unitary method: write both species, their ratio, known moles, x → cross-multiply.
- Gas-only reactions: mole ratio = volume ratio (water is a gas at 200 °C!).
- Dilution: same moles. Taking a portion: fewer moles. Back-titration: original − left-over.
- Empirical: ÷ Ar → ÷ smallest → ×2 for .5, ×3 for .33. % given → take as grams.
- Brackets on exponents & sums in the calculator; never kg in mol = mass/Mr.
- Always +1 ions: write X+ (no + = no mark); x-axis m/e = mass number.
- Cl: 35Cl 75 % / 37Cl 25 %. Cl2 molecules 70 : 72 : 74 = 9 : 6 : 1; fragments 35 : 37 = 3 : 1.
- Br: 79Br 50 % / 81Br 50 %. Br2 molecules 158 : 160 : 162 = 1 : 2 : 1; fragments 79 : 81 = 1 : 1.
- No link between the fragment ratio and the molecule ratio.
- No y-scale? Measure peak lengths with a ruler. Count peaks by listing all isotope pairs (equal masses merge).