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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 Fe0.91OF{e_{0.91}}O. What percentage of cationic sites are occupied by Fe(III)Fe(III)?
(A)32.45%(A)32.45\%
(B)19.78%(B)19.78\%
(C)18.71%(C)18.71\%
(D)12.67%(D)12.67\%

Explanation

Solution

Iron oxide is non stoichiometric because it reflect the ease of oxidation of Fe2+F{e^{2 + }} to Fe3+F{e^{3 + }} effectively replacing a small portion of Fe2+F{e^{2 + }} with two thirds their number of Fe3+F{e^{3 + }} . thus, for every three missing Fe2+F{e^{2 + }} ions, the crystal contains two Fe3+F{e^{3 + }} ions to balance the charge.

Complete answer:
In the formula Fe0.91OF{e_{0.91}}O, the total concentration of Fe(II)Fe(II) and Fe(III)Fe(III) Is 0.910.91.
let Fe(II)Fe(II) in Fe0.91OF{e_{0.91}}O=xx
And, Fe(III)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)Fe(III) ions that’s why er are using the formula Fe3+Fe2++Fe3+×100\dfrac{{F{e^{3 + }}}}{{F{e^{2 + }} + F{e^{3 + }}}} \times 100, but if we need to calculate the percentage of Fe(II)Fe(II) ions in the compound than we will be using Fe2+Fe2++Fe3+×100\dfrac{{F{e^{2 + }}}}{{F{e^{2 + }} + F{e^{3 + }}}} \times 100.