The E° value for the Mn3+/Mn2+ couple is more positive than that of Cr3+/Cr2+ or Fe3+/Fe2+ due to change of
Option 3: d4 to d5 configuration
Explanation:
Let's analyze the electronic configurations of the ions involved:
Mn3+: [Ar] 3d4
Mn2+: [Ar] 3d5
Cr3+: [Ar] 3d3
Cr2+: [Ar] 3d4
Fe3+: [Ar] 3d5
Fe2+: [Ar] 3d6
The Mn3+/Mn2+ couple involves the change from a d4 to a d5 configuration. The d5 configuration is particularly stable due to the half-filled d orbitals. This stability makes the reduction of Mn3+ to Mn2+ favorable, resulting in a more positive E° value.
In the case of Cr3+/Cr2+, the change is from d3 to d4, and for Fe3+/Fe2+ it's from d5 to d6. Neither of these changes leads to the same level of stability as the d4 to d5 transition.
Therefore, the higher E° value for Mn3+/Mn2+ is due to the d4 to d5 configuration change, which results in a stable half-filled d5 configuration.
List I | List II | ||
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A | Mesozoic Era | I | Lower invertebrates |
B | Proterozoic Era | II | Fish & Amphibia |
C | Cenozoic Era | III | Birds & Reptiles |
D | Paleozoic Era | IV | Mammals |