Chapter 18: Problem 151
At one time on Earth, iron was present mostly as iron(II). Later, once plants had produced a significant quantity of oxygen in the atmosphere, the iron became oxidized to iron(III). Show that \(\mathrm{Fe}^{2+}(a q)\) can be spontaneously oxidized to \(\mathrm{Fe}^{3+}(a q)\) by \(\mathrm{O}_{2}(g)\) at \(25^{\circ}\) Cassuming the following reasonable environmental conditions: \(\left[\mathrm{Fe}^{2+}\right]=\left[\mathrm{Fe}^{3+}\right]=1 \times 10^{-7} \mathrm{M} ; \mathrm{pH}=7.0 ; P_{\mathrm{O}_{2}}=160 \mathrm{~mm} \mathrm{Hg}\).
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