Redox potential approach:
Soil colour is governed by the oxidation state of iron and manganese, which in turn depends on the soil's redox potential (Eh). In waterlogged soils, oxygen is excluded and microbes use \( \text{Fe}^{3+} \) and \( \text{Mn}^{4+} \) as alternate electron acceptors, reducing them to \( \text{Fe}^{2+} \) and \( \text{Mn}^{2+} \); these reduced, soluble forms impart the characteristic grey/blue-grey (gleyed) colour. In upland, well-drained soils the high Eh keeps iron oxidised as \( \text{Fe}^{3+} \) oxides/hydroxides, producing red and brown hues. Since this Eh-driven mechanism directly accounts for both colours, Reason (R) is a correct explanation of Assertion (A).