Q.(a) Complete the following reactions:
You're viewing a preview — the full solution, concept, methods & PYQ mapping are locked.
Start your 14-day free trial to unlock the full solution →(a) Two redox equations balanced by half-reaction/ion-electron method. (b) Actinides' 5f-6d-7s orbitals are comparable in energy (giving more oxidation states) while lanthanides' 4f orbitals are deeply shielded (mostly fixed +3); transition metals catalyse via variable oxidation states and vacant d-orbitals offering reactive/adsorption sites.
(a)(i) MnO4- (in neutral/faintly alkaline medium) oxidizes thiosulfate all the way to sulfate, while itself being reduced to MnO2 (not all the way to Mn2+, since the medium is not strongly acidic):
8MnO4- + 3S2O3^2- + H2O --> 8MnO2 + 6SO4^2- + 2OH-
(Check: Mn 8=8; S 6=6; O: LHS 32+9+1=42, RHS 16+24+2=42; H: 2=2; charge: LHS -8-6=-14, RHS -12-2=-14 - balanced.)
(a)(ii) Cr2O7^2- (in acidic medium) oxidizes Fe2+ to Fe3+, while itself being reduced to Cr3+:
Cr2O7^2- + 6Fe2+ + 14H+ --> 2Cr3+ + 6Fe3+ + 7H2O
(Check: Cr 2=2; Fe 6=6; O 7=7; H 14=14; charge: LHS -2+12+14=24, RHS 6+18=24 - balanced.)
(b)(i) Why actinides show more oxidation states than lanthanides: In actinides, the 5f, 6d, and 7s orbitals lie very close together in energy (comparable energies), so electrons from more than one of these subshells can participate in bonding relatively easily, allowing actinide elements to display a wider range of oxidation states (e.g., +3 up to +7 for some). In lanthanides, the 4f orbitals are more deeply buried within the atom (well shielded by the outer 5s and 5p electrons) and are energetically well-separated from the 5d/6s orbitals, so electrons rarely participate from 4f - lanthanides show oxidation states overwhelmingly dominated by +3.
…
Unlock everything free for 14 days
- Full step-by-step solutions
- Concept-first explanations
- Methods, shortcuts & mistakes
- PYQ mapping + timed mock tests
Full access for 14 days. No credit card required.