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Group 2 of the Periodic Table — beryllium, magnesium, calcium, strontium, barium and radium — provides the cleanest demonstration of a vertical reactivity trend in the s-block. Down the group, the outer ns² electrons sit further from the nucleus, ionisation energies fall, and metals lose their two valence electrons more readily. The visible consequences are dramatic: magnesium fizzes feebly in cold water but burns with a blinding white flame in steam, while calcium, strontium and barium evolve hydrogen vigorously at room temperature, leaving alkaline hydroxide solutions of increasing pH. Two solubility patterns run in opposite directions — hydroxides become more soluble, sulfates become less soluble — and both can be rationalised by the relative sensitivities of lattice and hydration enthalpies to cation size. Industrially the group sustains construction (CaCO₃, CaO), agriculture (Ca(OH)₂ liming), flue-gas desulfurisation, magnesium alloys, titanium extraction (Kroll process) and medical imaging (BaSO₄ barium meals). This lesson anchors Required Practical 10 — investigating the reactions of Group 2 elements and the relative solubilities of their compounds.
Spec mapping (AQA 7405): This lesson maps to §3.2.2 (Group 2, the alkaline earth metals). It builds on L0 (periodicity and Period 3 trends) and contrasts with L2 (Group 7 oxidising-ability trend, which runs opposite in direction). The quantitative rationale for the sulfate-solubility trend forward-links to §3.1.4 (energetics — lattice and hydration enthalpies in Born–Haber and dissolution cycles). The practical anchor is Required Practical 10. Refer to the official AQA specification document for the exact wording of each subsection.
Assessment objectives: AO1 recalls general formula [Ar/Kr/Xe]ns², electron configurations of Be–Ba, and the directions of the reactivity, hydroxide-solubility and sulfate-solubility trends. AO2 dominates Paper 1: predicting and balancing reactions of Group 2 metals with water, oxygen and dilute acid, and explaining the solubility trends in terms of lattice vs hydration enthalpy. AO3 — the A⁎ discriminator — asks students to rationalise why lattice enthalpy stays roughly constant for sulfates while hydration enthalpy falls sharply with cation size, to evaluate industrial uses (e.g. why BaSO₄ is safe to swallow despite Ba²⁺ toxicity), and to integrate Born–Haber thinking with periodic-trend prediction.
Every Group 2 element has the outer configuration ns² and forms a dipositive M²⁺ ion with a noble-gas core:
| Element | Z | Full configuration | Short form | Ion (M²⁺) |
|---|---|---|---|---|
| Be | 4 | 1s² 2s² | [He] 2s² | [He] |
| Mg | 12 | 1s² 2s² 2p⁶ 3s² | [Ne] 3s² | [Ne] |
| Ca | 20 | 1s² 2s² 2p⁶ 3s² 3p⁶ 4s² | [Ar] 4s² | [Ar] |
| Sr | 38 | [Ar] 3d¹⁰ 4s² 4p⁶ 5s² | [Kr] 5s² | [Kr] |
| Ba | 56 | [Kr] 4d¹⁰ 5s² 5p⁶ 6s² | [Xe] 6s² | [Xe] |
| Ra | 88 | [Rn] 7s² | [Rn] 7s² | [Rn] |
Loss of both s electrons generates a closed-shell cation, which is why the +2 oxidation state dominates Group 2 chemistry and Be⁺ or Ca⁺ species are never observed in stable compounds.
| Property | Trend down Group 2 | Underlying reason |
|---|---|---|
| Atomic radius | Increases | Each successive element occupies a higher principal-quantum-number shell |
| First ionisation energy | Decreases | Outer electrons further from nucleus and better shielded; this outweighs the rise in nuclear charge |
| Second ionisation energy | Decreases (parallels IE₁) | Same shielding-and-distance argument applies |
| Electronegativity | Decreases | Bonding pair held less tightly as atomic radius grows |
| Melting point | Generally decreases (Mg → Sr; Ba slightly higher than Sr) | Metallic-bond strength weakens as cation–delocalised-electron distance increases |
| Density | Generally increases | Atomic mass grows faster than atomic volume |
The melting-point pattern is not perfectly monotonic — beryllium melts unusually high (1287 °C) because of its tiny radius, and magnesium and strontium adopt different crystal packings — but the broad downward drift from Mg to Ba is what AQA examines.
Reactivity increases going down Group 2.
Key Point: "Reactivity increases down the group" applies to oxidation by water, oxygen and acid. It is the opposite of Group 7, where the most reactive halogen sits at the top (F₂) because halogens gain electrons and the smallest atom does so most readily.
Group 2 metals (excluding Be, which does not react under standard conditions) reduce water to hydrogen, generating the metal hydroxide:
General equation: M(s) + 2H₂O(l) → M(OH)₂(aq) + H₂(g)
Beryllium: No reaction with water at any temperature under standard A-Level conditions. The thin BeO/Be(OH)₂ layer passivates the surface.
Magnesium (cold water): Very slow; only a faint stream of bubbles after several days. The solution becomes weakly alkaline as small amounts of Mg(OH)₂ dissolve.
Mg(s) + 2H₂O(l) → Mg(OH)₂(aq) + H₂(g)
Magnesium (steam): Vigorous; a brilliant white flame is observed and the oxide, not the hydroxide, is the solid product because steam temperatures (≥ 100 °C) decompose any Mg(OH)₂ formed back to MgO.
Mg(s) + H₂O(g) → MgO(s) + H₂(g)
Calcium: Steady reaction with cold water. Bubbles of hydrogen rise smoothly; the solution turns cloudy because Ca(OH)₂ is only sparingly soluble (limewater); the solid Ca shrinks and may float on the gas. pH of the saturated solution ≈ 12.4.
Ca(s) + 2H₂O(l) → Ca(OH)₂(aq) + H₂(g)
Strontium: More vigorous than calcium — rapid effervescence, the metal may glow faintly, and Sr(OH)₂ is appreciably soluble so the solution stays clearer than for Ca.
Sr(s) + 2H₂O(l) → Sr(OH)₂(aq) + H₂(g)
Barium: Vigorous; bubbles stream off immediately and the strongly alkaline Ba(OH)₂ solution can reach pH ≈ 13–14.
Ba(s) + 2H₂O(l) → Ba(OH)₂(aq) + H₂(g)
Exam Tip: The trend in vigour with cold water is Mg (very slow) → Ca (steady) → Sr (vigorous) → Ba (very vigorous), tracking the fall in IE₁ + IE₂. To test the gas, use a lit splint (squeaky pop → H₂). To confirm a CO₂ evolution from carbonate decomposition, use limewater (turns milky) — different gas, different test.
All Group 2 metals burn in oxygen to give white ionic oxides:
General equation: 2M(s) + O₂(g) → 2MO(s)
| Metal | Equation | Flame colour | Solid product |
|---|---|---|---|
| Mg | 2Mg + O₂ → 2MgO | Brilliant white | White MgO |
| Ca | 2Ca + O₂ → 2CaO | Brick-red / orange-red | White CaO |
| Sr | 2Sr + O₂ → 2SrO | Crimson | White SrO |
| Ba | 2Ba + O₂ → 2BaO | Pale green / apple-green | White BaO |
The characteristic flame colours arise from outer-electron excitation followed by photon emission as electrons fall back to lower energy levels — the same principle as flame tests in qualitative analysis.
At elevated temperatures or under excess oxygen, the heavier Group 2 metals form higher-oxygen species — the AQA syllabus expects awareness rather than full mechanism:
The Group 2 oxides are all basic and react with water to form alkaline hydroxides:
MO(s) + H₂O(l) → M(OH)₂(aq)
CaO + H₂O → Ca(OH)₂ is a strongly exothermic reaction (the basis of "slaking" lime industrially).
Group 2 metals reduce dilute mineral acids to hydrogen:
General equation: M(s) + 2HCl(aq) → MCl₂(aq) + H₂(g)
Observation: Bubbles of colourless gas effervesce vigorously, the metal disappears progressively, and the solution warms (the reaction is exothermic). Confirm the gas with a lit splint — a "squeaky pop" indicates hydrogen. (A glowing splint that relights would indicate O₂; limewater that turns milky would indicate CO₂ — different tests for different gases, and worth distinguishing in the exam.)
Specific examples:
With dilute sulfuric acid, magnesium reacts smoothly but calcium reaction quickly slows because CaSO₄ is only sparingly soluble — a CaSO₄ coating forms over the metal surface and passivates it. This is a useful synoptic example of how solubility (the next section) modifies kinetics.
Common Misconception: Concentrated HNO₃ oxidises most Group 2 metals to give NO or NO₂ rather than H₂. This is beyond AQA's required-equation list but is a reasonable AO3 extension: at A⁎ level, recognise that "dilute acid → H₂" is the rule and concentrated oxidising acids behave differently.
| Hydroxide | Solubility (mol dm⁻³, 25 °C) | Description | pH of saturated solution |
|---|---|---|---|
| Mg(OH)₂ | ≈ 2 × 10⁻⁴ | Insoluble | ≈ 10 |
| Ca(OH)₂ | ≈ 1.5 × 10⁻² | Sparingly soluble ("limewater") | ≈ 12.4 |
| Sr(OH)₂ | ≈ 6.6 × 10⁻² | Moderately soluble | ≈ 13 |
| Ba(OH)₂ | ≈ 0.24 | Soluble | ≈ 13–14 |
| Sulfate | Solubility (g per 100 g H₂O, 20 °C) | Description |
|---|---|---|
| MgSO₄ | ≈ 35 | Soluble ("Epsom salt", MgSO₄·7H₂O) |
| CaSO₄ | ≈ 0.24 | Sparingly soluble (gypsum, plaster of Paris) |
| SrSO₄ | ≈ 0.011 | Almost insoluble |
| BaSO₄ | ≈ 0.00024 | Insoluble |
Acidified BaCl₂(aq) (the acid is dilute HCl, to remove any carbonate that would also precipitate) gives a thick white precipitate with any soluble sulfate:
Ba²⁺(aq) + SO₄²⁻(aq) → BaSO₄(s)
BaSO₄'s solubility in water and stomach acid is so low (≈ 2 × 10⁻³ g L⁻¹; Ksp ≈ 1 × 10⁻¹⁰) that the equilibrium Ba²⁺ concentration in body fluids is negligible — far below the toxic threshold (≈ 20 mg Ba²⁺ causes acute poisoning). Patients swallow a thick BaSO₄ suspension ("barium meal" or "barium swallow") before X-ray imaging; barium's high atomic number gives strong X-ray absorption, opacifying the gut for diagnosis. Soluble barium salts (BaCl₂, Ba(NO₃)₂) are highly toxic because they liberate free Ba²⁺, which blocks K⁺ channels in cardiac muscle.
Whether an ionic salt MX dissolves is decided by the sign and magnitude of the enthalpy of solution ΔH_sol:
ΔH_sol = −ΔH_LE(MX) + ΔH_hyd(M²⁺) + ΔH_hyd(Xⁿ⁻)
(ΔH_LE here written as a positive number for the lattice-dissociation enthalpy.)
Both ΔH_LE and ΔH_hyd depend on ion radius and charge, but the dependence is different for hydroxide and sulfate salts:
This argument — "small fixed anion vs large fixed anion" — is exactly the AO3 explanation expected at A⁎. It also forward-links to L4 of the energetics course (§3.1.4), where Born–Haber cycles for Group 2 halides quantify these enthalpies explicitly.
Exam Tip: Mnemonic — "Hydroxides Hate Smallness; Sulfates Shrink." Or remember that the larger of the two ions controls which trend wins: when the anion is small (OH⁻), cation size matters most for the lattice; when the anion is large (SO₄²⁻), cation size matters most for the hydration.
Group 2 carbonates and nitrates decompose on strong heating; the temperature required increases down the group, because the polarising power of the cation falls.
Carbonates: MCO₃(s) → MO(s) + CO₂(g)
| Carbonate | Decomposition T / °C |
|---|---|
| MgCO₃ | ≈ 540 |
| CaCO₃ | ≈ 840 |
| SrCO₃ | ≈ 1290 |
| BaCO₃ | ≈ 1360 |
Nitrates: 2M(NO₃)₂(s) → 2MO(s) + 4NO₂(g) + O₂(g) — brown NO₂ fumes are diagnostic.
The smaller, more highly charge-dense Mg²⁺ polarises the carbonate or nitrate anion more, distorting its electron cloud and weakening a C–O or N–O bond; decomposition therefore occurs at a lower temperature. Larger Ba²⁺ polarises the anion less, so a higher temperature is needed.
Required Practical 10 in AQA 7405 examines the relative reactivity of Group 2 metals and the relative solubilities of their compounds. Outline:
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