Chemistry · Ch 4 — Transition and Inner Transition Elements
Summary
Summary
This chapter has developed the chemistry of the transition and inner transition elements across two connected halves. The d-block half established the IUPAC definition of a transition metal (an element with an incomplete d sub-shell in its atom, or capable of forming a cation with an incomplete d sub-shell), located the three d-block series (3d, 4d, 5d) occupying the central bridge of the periodic table between the s-block and p-block, and derived their general electronic configuration, Noble gasd¹⁻¹⁰ns¹⁻² (n = 4 to 7), with chromium and copper as the two well-known exceptions arising from the extra stability of half-filled and fully-filled d configurations.
Across the 3d series specifically, this chapter traced ten connected property trends back to that shared electronic-configuration foundation: uniformly metallic character with mostly HCP/FCC/BCC crystal structures and a melting point that rises then falls across the series, peaking near the d⁵-adjacent middle; atomic/ionic size that, contrary to the normal periodic expectation, stays nearly constant across most of the series because rising nuclear charge and rising 3d-4s electron repulsion counterbalance each other; ionization enthalpy intermediate between s-block and p-block values, rising overall but irregularly across a series; a spread of accessible oxidation states that peaks at manganese (six states, +2 to +7) and correlates with the Frost diagram's element-by-element thermodynamic-stability minima; standard electrode potentials that establish copper as uniquely resistant to oxidation among 3d metals, with Mn²⁺ and Zn²⁺ standing out for their half-filled/fully-filled-shell stability; magnetic behaviour governed by the spin-only formula μ = √[n(n+2)] μ_B; catalytic activity exploiting both available d orbitals and variable oxidation states, illustrated by hydrogenation, hydroformylation, acetic-acid manufacture, Ziegler-Natta polymerisation and the Contact Process; a strong tendency to form substitutional alloys (via the Hume-Rothery rules) thanks to transition metals' mutually similar atomic sizes; a tendency to form non-stoichiometric interstitial compounds with small trapped atoms (H, B, C, N) that confer new hardness, conductivity and reducing properties; and a marked tendency to form coordination complexes, exploiting small, highly charged metal centres with vacant low-energy acceptor orbitals.
The chapter then worked through two named compounds in full depth: potassium dichromate (K₂Cr₂O₇), manufactured from chromite ore via sodium chromate and sodium dichromate, existing as interconvertible tetrahedral chromate (CrO₄²⁻) and corner-sharing bitetrahedral dichromate (Cr₂O₇²⁻) ions, and acting as a powerful acidic-medium oxidant with a specific chromyl-chloride confirmatory test for chloride ion; and potassium permanganate (KMnO₄), manufactured from pyrolusite ore via potassium manganate, existing as the tetrahedral permanganate ion (MnO₄⁻, central Mn⁷⁺ d³s hybridised), and showing distinctly different, medium-dependent oxidising power across neutral (to MnO₂), alkaline (via manganate to MnO₂, including Baeyer's reagent) and acidic (all the way to Mn²⁺, the strongest pathway) conditions -- with worked equivalent weights of 52.67, 158 and 31.6 respectively confirming just how differently the same reagent behaves in each medium. …