Topic 1: Formulae, Equations and Amount of Substance
- Syllabus
- 2017
- Topic
- —
- Level
- AS
Chemists use each term for a different kind of particle, substance or formula. Keeping those levels separate prevents errors when interpreting equations and composition data.
| Term | Precise meaning | Example |
|---|---|---|
| atom | Smallest particle of an element that retains that element's identity | Ne |
| element | Substance containing atoms with the same proton number | copper |
| ion | Atom or group with a net charge after electron loss or gain | SOX4X2− |
| molecule | Discrete group of atoms joined by covalent bonds | OX2 or HX2O |
| compound | Two or more elements chemically combined in fixed proportions | NaCl or HX2O |
An empirical formula gives the simplest whole-number ratio of atoms, whereas a molecular formula gives the actual number of each type of atom in one molecule. For example, glucose has empirical formula CHX2O and molecular formula CX6HX12OX6.
A molecule may be an element, such as OX2, so 'molecule' does not mean 'compound'. Ionic and giant substances have formula units rather than discrete molecules.
Amount of substance is measured in moles. One mole contains the Avogadro constant, L=6.02×1023mol−1, of the specified entities: atoms, molecules, ions or formula units.
N=nL\qquad n=\frac{N}{L}
For 0.250mol of sodium chloride, the number of formula units is 0.250×6.02×1023=1.51×1023. It also contains that many NaX+ ions and that many ClX− ions, so the total number of ions is twice the number of formula units.
Always name the entity being counted. Multiplying by the number of atoms or ions per entity is a separate step; one mole of COX2 molecules contains three moles of atoms in total.
A full equation shows all reactants and products; an ionic equation keeps only the species that undergo chemical change. Both must conserve every element and the total charge, and every species needs the correct state symbol.
\ce{AgNO3(aq) + NaCl(aq) -> AgCl(s) + NaNO3(aq)}\ce{Ag+(aq) + Cl-(aq) -> AgCl(s)}
Do not split solids, liquids, gases or weakly ionised substances into aqueous ions. State symbols carry chemical meaning: AgCl(aq) would contradict the observed precipitate.
Relative masses compare particles with one twelfth of the mass of a carbon-12 atom. They are ratios and therefore have no unit. Molar mass is the mass of one mole and is measured in gmol−1.
| Quantity | Meaning and use |
|---|---|
| Ar | relative atomic mass; isotopic average for an element on the 12C scale |
| Mr | sum of Ar values for a discrete molecule |
| relative formula mass | corresponding sum for an ionic or giant structure, which has no discrete molecule |
| molar mass, M | mass per mole; numerically equal to the appropriate relative mass in gmol−1 |
For MgClX2, the relative formula mass is 24.3+2(35.5)=95.3, so its molar mass is 95.3gmol−1. Calling this an Mr suggests discrete molecules and is inappropriate for the giant ionic lattice.
\mathrm{ppm}=\frac{\text{amount of component}}{\text{total amount}}\times10^6
Use matching quantities in the fraction. For atmospheric gases, ppm commonly expresses a mole or volume fraction: 420 ppm means 420 parts of that gas per million parts of air, not 420%.
Concentration states how much solute is present per unit volume of solution. Use the final solution volume, not the volume of solvent added, and convert cm3 to dm3 before using these relationships.
c=\frac{n}{V}\quad(\mathrm{mol,dm^{-3}})\qquad c_m=\frac{m}{V}\quad(\mathrm{g,dm^{-3}})\qquad c_m=cM
Dissolving 5.85g of NaCl and making the solution up to 500cm3 gives V=0.500dm3. With M(NaCl)=58.5gmol−1, n=0.100mol, so c=0.200moldm−3. The mass concentration is 5.85/0.500=11.7gdm−3.
The numerical values in moldm−3 and gdm−3 are not interchangeable; molar mass provides the conversion. Titration calculations are outside this Topic 1 objective.
An empirical formula comes from a mole ratio, not directly from a mass ratio. Convert every measured mass or percentage into moles before finding the simplest whole-number ratio.
A compound containing 40.0% C, 6.7% H and 53.3% O gives mole values 40.0/12.0, 6.7/1.0 and 53.3/16.0, a ratio close to 1:2:1. Its empirical formula is CHX2O. If Mr=180, then k=180/30=6 and the molecular formula is CX6HX12OX6.
Round only after identifying a defensible near-integer ratio. Arbitrarily rounding 1.5 to 2 changes the composition; multiply the entire ratio instead.
A balanced equation relates amounts in moles. Convert the known mass to moles, apply the stoichiometric coefficient ratio, then convert the required amount back to mass.
n=\frac{m}{M}\quad\longrightarrow\quad\text{mole ratio}\quad\longrightarrow\quad m=nM
\ce{Mg + 2HCl -> MgCl2 + H2}
For 4.80g Mg, n(Mg)=4.80/24.3=0.198mol. The 1:1 coefficient ratio gives 0.198mol MgClX2. With M(MgClX2)=95.3gmol−1, the theoretical mass is 18.8g.
Coefficients compare moles, not masses. If more than one reactant amount is supplied, identify the limiting reactant before calculating product; an excess reactant cannot determine the product amount.
Convert a gas volume to moles, use the balanced equation's mole ratio, and convert to the requested quantity. The conversion method depends on the stated temperature and pressure.
n=\frac{V}{V_m}\qquad pV=nRT
At room temperature and pressure, use the stated or accepted molar volume (commonly 24.0dm3mol−1). For other conditions, use pV=nRT: pressure in Pa, volume in m3, temperature in K and R=8.31JK−1mol−1. The same equation can find the molar mass of a volatile liquid from the mass and amount of its vapour.
2.40dm3 of gas at room conditions is 2.40/24.0=0.100mol. Under specified non-room conditions, 120cm3=1.20×10−4m3 and 25∘C=298K before substitution into n=pV/(RT).
A gas-volume ratio equals the equation's mole ratio only when the gases are compared at the same temperature and pressure. Never insert dm3, kPa or degrees Celsius into pV=nRT with the stated SI value of R.
Percentage yield compares the product actually obtained with the theoretical amount. Percentage atom economy asks what fraction of the products' mass is in the desired product, using the balanced equation.
%,\text{yield}=\frac{\text{actual yield}}{\text{theoretical yield}}\times100%,\text{atom economy}=\frac{\text{stoichiometric mass of desired product}}{\text{sum of stoichiometric masses of all products}}\times100
For CaCOX3CaO+COX2, if CaO is desired, the atom economy is 56.1/(56.1+44.0)×100=56.0%. If the theoretical yield of CaO is 5.00g but 4.20g is isolated, the percentage yield is 84.0%.
Yield can fall because reaction is incomplete, side reactions occur, or product is lost during separation. Atom economy is fixed by the chosen balanced reaction and desired product; it does not improve merely because technique or catalyst improves yield.
A high yield and a high atom economy are different advantages. Include stoichiometric coefficients when more than one mole of a product appears in the equation.
To determine a formula, measure the amounts of elements that combine and convert them to a simplest whole-number mole ratio. To confirm an equation, compare a measured mass change or gas amount with the ratio predicted by a balanced candidate equation.
Evaluate direction as well as size of error. Incomplete reaction can leave too little mass change; loss of solid can make mass loss too large; oxidation by air can add mass; gas leaks or dissolution can reduce the collected volume. Repeats expose random variation, but repeating does not remove a systematic leak or calibration error.
A non-integer raw ratio is not automatically evidence for an unusual formula. First consider uncertainty, incomplete reaction, contamination and whether every product was measured.
React a known amount of a solid with an excess reagent, collect the gas and divide its volume by the moles formed. A typical route reacts a measured mass of magnesium with excess dilute acid and collects hydrogen in a gas syringe or calibrated inverted vessel.
V_m=\frac{V(\text{gas})}{n(\text{gas})}
Check all joints for leaks, fit the bung before appreciable gas escapes, keep the gas-collection capacity above the predicted volume, and read the scale at eye level. Gas loss makes Vm too low; using too much solid may exceed the apparatus range. Wear eye protection with acid and keep hydrogen away from flames.
An observation is macroscopic evidence of a chemical change. A full equation identifies the substances used; the ionic equation identifies the particles responsible for the visible change. State symbols link the two levels.
| Reaction and observation | Full equation | Net ionic change |
|---|---|---|
| displacement: zinc gains a reddish-brown copper coating and the blue solution fades | Zn(s)+CuSOX4(aq)ZnSOX4(aq)+Cu(s) | Zn(s)+CuX2+(aq)ZnX2+(aq)+Cu(s) |
| acid + metal: magnesium dissolves and a colourless gas effervesces | Mg(s)+2HCl(aq)MgClX2(aq)+HX2(g) | Mg(s)+2HX+(aq)MgX2+(aq)+HX2(g) |
| precipitation: mixing the solutions forms a white solid | AgNOX3(aq)+NaCl(aq)AgCl(s)+NaNOX3(aq) | AgX+(aq)+ClX−(aq)AgCl(s) |
For displacement, electron transfer changes the metal and ion identities. In the acid reaction, HX+ becomes hydrogen gas. In precipitation, two aqueous ions form an insoluble lattice. Spectator ions remain aqueous and cancel from the ionic equation.
Write what is actually seen—colour change, bubbles, solid formation or disappearance—not an inference such as 'ions reacted'. A correct ionic equation must still balance atoms and charge and include state symbols.