What makes a transition element?
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Transition elements (d-block) have a partially filled (n−1)d subshell in the ground state or in a common ion; Zn²⁺ (d¹⁰) is the classic exception often re-tested.
Their five signature properties — variable oxidation states, coloured complex ions, catalytic activity, magnetic behaviour, and complex formation — all trace back to how easily d-electrons are lost or excited.
- Spin-only magnetic moment: μ_so = √(n(n+2)) BM, where n = unpaired electrons.
- Colour rule: d¹⁰ (Zn²⁺), d⁰ (Sc³⁺, Ti⁴⁺) → colourless; intermediate dn → coloured.
- MnO₄⁻ / Cr₂O₇²⁻ oxidising power changes with pH (E° = +1.51 V and +1.33 V respectively in acid).
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What makes a transition element?
A d-block element is a transition element when it (or one of its common ions) has an incomplete d-subshell. Zn and Cu sit on the boundary: Zn²⁺ is d¹⁰ and therefore not a true transition ion, while Cu²⁺ (d⁹) is.
Why variable oxidation states?
The (n−1)d and ns orbitals are very close in energy, so different numbers of d-electrons can be removed with little energetic cost. Manganese for instance spans +2, +4, +6, +7, and chromium shows +3, +6 most commonly.
Complex ions and coordination number
Ligands donate lone pairs into vacant hybrid orbitals on the metal. The most frequent coordination numbers are 6 (octahedral) and 4 (tetrahedral or square-planar).
| Common ion | Geometry | Colour |
|---|---|---|
| [Cr(NH₃)₆]³⁺ | octahedral | violet |
| [Cu(NH₃)₄]²⁺ | square-planar | deep blue |
| [Fe(H₂O)₆]²⁺ | octahedral | pale green |
| [Zn(OH)₄]²⁻ | tetrahedral | colourless |
Colour, magnetism and catalysis
Colour comes from d–d transitions; the wavelength absorbed depends on Δ_o, which is set by the spectrochemical series (I⁻ < Br⁻ < Cl⁻ < F⁻ < OH⁻ < H₂O < NH₃ < CN⁻). Magnetic moment is read directly from the count of unpaired electrons using the spin-only formula. Catalysis works because the metal can cycle between oxidation states, supplying a low-energy pathway (heterogeneous, e.g. Fe in the Haber process) or acting in solution (homogeneous, e.g. MnO₄⁻ titrations).
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pH-dependent redox interconversion
Dichromate(VI) and chromate(VI) interconvert on pH change:
2CrO₄²⁻ + 2H⁺ ⇌ Cr₂O₇²⁻ + H₂O
In alkaline solution Cr³⁺ is oxidised to yellow CrO₄²⁻; in acid it becomes orange Cr₂O₇²⁻. Failing to flip the equation when pH changes is the most common half-equation error.
Worked micro-example — spin-only moment
For [Fe(H₂O)₆]²⁺ (Fe²⁺, d⁶, high-spin in water), n = 4 unpaired electrons.
μ_so = √(4 × 6) = √24 ≈ 4.90 BM, matching literature ≈ 5.0 BM once orbital contribution is added. Predict the moment for [Ni(CN)₄]²⁻: strong-field CN⁻ gives a low-spin square-planar d⁸ with 0 unpaired electrons → 0 BM (diamagnetic).
Identification tests and pitfalls
NH₄OH added dropwise to Cu²⁺ gives a pale-blue Cu(OH)₂ precipitate dissolving in excess to [Cu(NH₃)₄(H₂O)₂]²⁺ (deep blue). Adding OH⁻ to Zn²⁺ gives amphoteric Zn(OH)₂ which redissolves in excess forming [Zn(OH)₄]²⁻ — a favourite UACE Paper 1 structured item.
Common mistakes
- Writing Cr(VI) as CrO₄²⁻ in acid (should be Cr₂O₇²⁻).
- Citing Cu²⁺ as [Cu(NH₃)₆]²⁺ instead of the square-planar tetraammine.
- Forgetting that d⁰ and d¹⁰ species are colourless — no d–d transitions exist.
- Treating all catalysts like enzymes; heterogeneous and homogeneous require different justifications.
Practice prompts
- Explain why [Co(H₂O)₆]²⁺ is pink but [CoCl₄]²⁻ is blue, using Δ_o and the spectrochemical series.
- Balance MnO₄⁻ + C₂O₄²⁻ → Mn²⁺ + CO₂ in acidic solution and calculate the volume of 0.02 M KMnO₄ needed to react with 25.0 cm³ of 0.10 M Na₂C₂O₄.
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Sources & verification
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