Q.How is the variability in oxidation states of transition metals different from that of the non transition metals? Illustrate with examples.
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Start your 14-day free trial to unlock the full solution →Transition metals show a wide range of variable oxidation states because they can use both and electrons in bonding, while non‑transition metals (main‑group metals) typically show only one or two oxidation states because they use only and electrons. For example, Mn exhibits states from +2 to +7, whereas Na shows only +1.
Why This Difference Exists
The key lies in the electronic configuration and the energy gap between the orbitals available for bonding.
Transition metals have an incomplete subshell. The and orbitals are very close in energy. This means that not only the electrons but also a variable number of electrons can participate in chemical bonding. The energy required to unpair and remove these electrons is often compensated by the extra stability gained from bond formation or from achieving a half‑filled or fully‑filled subshell.
Non‑transition metals (representative elements) have only and orbitals available. The and electrons are the only ones that can be lost or shared. The inner or orbitals are either completely filled or too low in energy to be involved. As a result, the number of oxidation states is limited — usually one or two, differing by 2 (e.g., +2 and +4 for Sn, +3 and +5 for As).
A quick way to spot a transition metal’s possible oxidation states: look at the number of electrons in the and orbitals combined. For example, Mn has — that’s 7 valence electrons, and indeed it shows all states from +2 to +7.
Step‑by‑Step Comparison
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Orbital availability
Transition metals: , , and sometimes orbitals are close in energy.
Non‑transition metals: only and orbitals are accessible; inner orbitals are either full or too deep.
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Number of oxidation states
Transition metals: many — often a continuous range from +2 up to the group number (e.g., Mn: +2, +3, +4, +5, +6, +7).
Non‑transition metals: few — typically one or two (e.g., Na: +1; Mg: +2; Al: +3; Sn: +2, +4).
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Stability of intermediate states
Transition metals: intermediate states are often stable because of the stabilisation by crystal field effects or half‑filled subshell (e.g., for Mn²⁺, for Zn²⁺).
Non‑transition metals: the two accessible states differ by 2, and for the heavier p‑block metals the higher state is the unstable one because of the inert pair effect (e.g., Tl³⁺ is strongly oxidising, while Tl⁺ is the stable state). Within the transition metals themselves, an intermediate state can disproportionate — Cu⁺ in aqueous solution gives Cu and Cu²⁺ — showing how each state's stability is decided by d‑electron energetics rather than a fixed 2‑unit jump.
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Examples illustrating the contrast
Metal Type Common oxidation states Reason Mn Transition +2, +3, +4, +5, +6, +7 Uses and electrons Fe Transition +2, +3 (higher states such as +6 are rare) — commonly loses 2 or 3 electrons Na Non‑transition +1 only Only electron available Mg Non‑transition +2 only Only electrons available Sn Non‑transition +2, +4 Uses and electrons; inert pair effect makes +2 stable
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