Warm up and recall
Three quick questions from earlier lessons. Pulling old material back to mind before you learn something new makes the new material stick better, so this is not busywork.
Practise this lesson
Four printable worksheets that build from the foundations up to exam-style questions, start at whatever level suits you.
Where this lesson fits
Lesson question: when an ionic solid dissolves, how can a single temperature change tell you whether it absorbs or releases heat, and how much energy per mole is involved?
- 1Set up the calorimeter. Dissolve a weighed ionic solid in a known mass of water in a polystyrene cup and record the temperature change.
- 2Read the sign. A temperature drop means endothermic dissolution (ΔHsoln > 0); a rise means exothermic (ΔHsoln < 0).
- 3Calculate ΔHsoln. Use q = mcΔT, then ΔHsoln = −q/n, where n is moles of solid dissolved.
Quick prerequisite: dissolving an ionic solid can be exothermic or endothermic, the lattice breaks apart (costs energy) and the ions hydrate (releases energy), while q = mcΔT turns a temperature change into heat. If that feels shaky, start with the Supported route below. Syllabus reference: measure temperature changes in endothermic and exothermic reactions and investigate enthalpy changes using calorimetry (ACSCH037, ACSCH073).
Know what matters most
Must know
- Dissolution can be endothermic (temperature falls, ΔHsoln > 0) or exothermic (temperature rises, ΔHsoln < 0)
- q = mcΔT with m = mass of water + dissolved solid; ΔHsoln = −q/n
- n is the moles of ionic solid dissolved (n = m/M), never moles of water
Should know
- The two-step model: lattice dissociation (endothermic) + hydration (exothermic); the larger term sets the sign
- How ‘m’ and ‘n’ differ across combustion, neutralisation and dissolution
- Why an experimental ΔHsoln differs from the accepted value (heat exchange with surroundings)
Going deeper
- A Born–Haber dissolution cycle finds lattice energy via Hess's Law (L08)
- Why some endothermic dissolutions still happen spontaneously (entropy, L11)
Warm up and recall
You've seen the ads: an athlete rolls an ankle, a trainer pulls a cold pack from a bag, cracks it, shakes it, and it goes cold instantly. No freezer. No ice. Just a bag of white powder and water mixing together. The powder is ammonium nitrate.
Why does mixing it with water make the pack cold? And why does NaOH dissolved in water do the exact opposite, releasing enough heat to raise the solution temperature by tens of degrees? They're both ionic solids dissolving in water. What's the difference?
What you'll master, and the words for it
Key Facts
- Lattice energy (endothermic) and hydration energy (exothermic) as the two steps of dissolution
- Endothermic examples: NH₄NO₃, NH₄Cl, KNO₃ (cold packs)
- Exothermic examples: NaOH, CaCl₂ (warms solution)
Concepts
- Why ΔHsoln sign follows from the temperature change direction
- Why the magnitude of the hydration enthalpy can exceed the lattice dissociation enthalpy, making dissolution exothermic
- The differences in m and n across combustion, neutralisation, and dissolution
Skills
- Calculate q and ΔHsoln from dissolution calorimetry data
- Assign correct sign to ΔHsoln from experimental temperature change
- Identify the correct m and n for all three calorimetry types