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A Level · Cambridge (CIE) · 9701

Build a lattice–hydration cycle for solution enthalpy

Separate lattice dissociation, ion hydration and net solution enthalpy before explaining Group 2 solubility patterns.

Group 2 · Cambridge International AS & A Level Chemistry 9701 · 27.1

A Level; Cambridge International Chemistry 9701, 2028–2030 syllabus, Topic 27. Compare Group 2 ions at the same charge and distinguish lattice formation, lattice dissociation, hydration and solution enthalpy. Trend explanations are qualitative unless data are supplied. Written practice is self-checked

Before you begin

  • Use AS Group 2 reactivity trends, ionic charge and radius, Hess cycles, and balanced equations.

Work on paper. Try each question before revealing help, and explain why your method works.

Quick readiness check

What happens in lattice dissociation?

What you will learn

  • Distinguish lattice dissociation enthalpy from lattice formation enthalpy
  • Relate hydration enthalpies to gaseous and aqueous ions
  • Use a Hess cycle to express solution enthalpy

Dissolution has an energy cost and an energy release

For an ionic solid dissolving, one step separates the crystal into gaseous ions; this lattice-dissociation step is endothermic. Hydration then transfers each gaseous ion into water, releasing energy and giving negative hydration enthalpies.

Write the stoichiometric number of every ion. For M(OH)₂, hydration includes one M²⁺ and two OH⁻ ions; for MSO₄, it includes one M²⁺ and one SO₄²⁻ ion.

Add signed steps to obtain ΔHsol

Using lattice dissociation enthalpy, ΔHsol = ΔH_latt(diss) + ΣΔH_hyd. If a source instead gives lattice formation enthalpy for gaseous ions forming the solid, reverse that step: ΔHsol = −ΔH_latt(form) + ΣΔH_hyd.

Hydration becomes less exothermic for a larger ion of the same charge because charge density falls. Lattice dissociation also becomes less endothermic as the cation radius increases, since the solid's electrostatic attractions are weaker. The solubility and ΔHsol trends depend on the balance of these changing contributions.

Pause and explain

When ΔH_latt is defined as formation from gaseous ions, what sign is used in the dissolution cycle?

Put the idea to work

Worked example

Write the Hess relation for dissolving Ba(OH)₂(s) using lattice-dissociation and hydration enthalpies.

Show the worked solution
  1. Break the solid into one Ba²⁺ and two OH⁻ gaseous ions.
  2. Hydrate each ion in the formula ratio.
  3. Add the signed lattice and hydration contributions.

Answer Ba(OH)₂(s) → Ba²⁺(aq) + 2OH⁻(aq); ΔHsol = ΔH_latt(diss) + ΔH_hyd(Ba²⁺) + 2ΔH_hyd(OH⁻).

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From guided practice to a new situation

Write your answer and reasoning first. Use a hint only if you are stuck. The model solution is for self-checking; your written work is not automatically marked.

1 · Guided

Write the enthalpy-cycle relation for MgSO₄(s) dissolving, using lattice-dissociation enthalpy.

Give me a hint

Count one Mg²⁺ and one SO₄²⁻ in each formula unit.

Compare my reasoning
  1. Separate MgSO₄(s) into gaseous ions.
  2. Hydrate Mg²⁺ once.
  3. Hydrate SO₄²⁻ once and sum signed terms.

ΔHsol = ΔH_latt(diss) + ΔH_hyd(Mg²⁺) + ΔH_hyd(SO₄²⁻).

Look for these in your work

  • Correct ion pair
  • Stoichiometry retained
  • Signed contributions combined
2 · Independent

A table gives ΔH_latt(form) = −2200 kJ mol⁻¹ and total hydration enthalpy = −2050 kJ mol⁻¹ for a hypothetical salt. Calculate ΔHsol.

Give me a hint

Reverse the formation enthalpy, then add the hydration contribution.

Compare my reasoning
  1. Dissociation contribution is +2200 kJ mol⁻¹.
  2. Add −2050 kJ mol⁻¹.
  3. Interpret the sign of the sum.

ΔHsol = −(−2200) − 2050 = +150 kJ mol⁻¹; the illustrative dissolution is endothermic.

Look for these in your work

  • Lattice direction reversed
  • Hydration sign retained
  • Sum and sign interpreted
3 · Transfer

Why can ΔHsol not, by itself, establish whether a salt is soluble?

Give me a hint

Consider that solubility is an equilibrium property and dissolution also changes particle dispersal.

Compare my reasoning
  1. ΔHsol describes the enthalpy change, not the full free-energy change.
  2. Entropy and temperature also affect feasibility.
  3. Solubility should be supported by equilibrium evidence or the stated syllabus trend.

ΔHsol is only the enthalpy contribution. Entropy and temperature also affect Gibbs energy and the dissolution equilibrium, so the enthalpy sign alone does not establish solubility.

Look for these in your work

  • Enthalpy scope stated
  • Other thermodynamic contribution recognised
  • Equilibrium limitation explained

Common mistakes

  • Adding formation lattice enthalpy without reversing its sign
  • Omitting the coefficient 2 for hydroxide ions
  • Calling hydration endothermic for the stated gas-to-aqueous direction
  • Using ΔHsol alone as a complete proof of solubility
Recall without your notes

What can you explain now?

What happens in lattice dissociation?

Compare with the explanation

An ionic solid separates into gaseous ions

This step overcomes the crystal's electrostatic attractions.

After trying it yourself, choose your next review. This is your self-assessment.

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Make it stick

How do lattice dissociation and hydration combine, with signs, to give solution enthalpy?

If you needed the solution, close it and solve the problem again from a blank page. A correct answer is stronger when you can explain the reason for each step.

Keep learning Chemistry

Course scope and assessment

Four hundred and forty-two original lessons map the published learning outcomes across AS Chemistry Topics 1–22 and A Level Topics 23–37, with guided, independent and transfer practice and explained answers. Every numbered subject-content topic and listed outcome tag now has a mapped lesson sequence. Topic 32 maps all 12 hydroxy-compound outcome tags in 11 lessons; Topic 33 maps all 15 carboxylic-acid and derivative outcome tags in 16 lessons; Topic 34 maps all 22 nitrogen-compound outcome tags in 20 lessons; Topic 35 maps all 12 polymerisation outcome tags in 16 lessons; Topic 36 maps all four organic-synthesis outcome tags in 14 lessons; Topic 37 maps all 22 chromatography and NMR outcome tags in 18 lessons. Cambridge's 2028–2030 Version 1 syllabus states that there are no significant changes which affect teaching from the preceding edition; the routes are aligned to that edition. This is 37 of the 37 numbered subject-content topics. Full cumulative exam assessment, Paper 3 laboratory competence, Paper 5 investigation practice and human subject-teacher review remain outstanding. Written practice is self-checked and does not certify exam readiness.

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