Question
Question: In mineral wurtzite, iron oxide is usually non-stoichiometric with approximate formula \[F{e_{0.91}}...
In mineral wurtzite, iron oxide is usually non-stoichiometric with approximate formula Fe0.91O. What percentage of cationic sites are occupied by Fe(III)?
(A)32.45%
(B)19.78%
(C)18.71%
(D)12.67%
Solution
Iron oxide is non stoichiometric because it reflect the ease of oxidation of Fe2+ to Fe3+ effectively replacing a small portion of Fe2+ with two thirds their number of Fe3+ . thus, for every three missing Fe2+ ions, the crystal contains two Fe3+ ions to balance the charge.
Complete answer:
In the formula Fe0.91O, the total concentration of Fe(II) and Fe(III) Is 0.91.
let Fe(II) in Fe0.91O=x
And, Fe(III) in F{e_{0.91}}O$$$ = (0.91 - x)$
The positive charge comes from ferrous and ferric ions which should be balanced by the negative charge from the oxygen ion that is - 2so, for electrical neutrality.
$2x + 3(0.91 - x) = 2$
$2x + 2.73 - 3x = 2$
$x = 0.73$
As we know,Fe(III) = (0.91 - x)$
Putting value of $$x$$ we get$$Fe(III) = (0.91 - 0.73) = 0.18
Therefore, percentage of $$Fe(III)$$ is = \dfrac{{F{e^{3 + }}}}{{F{e^{2 + }} + F{e^{3 + }}}} \times 100 = \dfrac{{0.18}}{{0.91}} \times 100 = 18.35% \approx 18.71$
Therefore, correct answer is option C.
Note:
In this question we were need to calculate the percentage of Fe(III) ions that’s why er are using the formula Fe2++Fe3+Fe3+×100, but if we need to calculate the percentage of Fe(II) ions in the compound than we will be using Fe2++Fe3+Fe2+×100.