(a) Photosynthesis Reaction
Usually written as:
\[ 6CO_{2}(g) + 6H_{2}O(l) \rightarrow C_{6}H_{12}O_{6}(aq) + 6O_{2}(g) \]
More appropriate redox form:
\[ 6CO_{2}(g) + 12H_{2}O(l) \rightarrow C_{6}H_{12}O_{6}(aq) + 6H_{2}O(l) + 6O_{2}(g) \]
- This explicitly shows that 12 water molecules are involved, of which 6 end up as product water and 6 supply oxygen atoms for the 6O\(_2\).
- It clearly separates the water that is consumed (as source of O\(_2\) and H) from the water that appears again, making the oxidation of water and reduction of CO\(_2\) as a redox process more evident.
(b) Reaction of O\(_3\) and H\(_2\)O\(_2\)
Given as:
\[ O_{3}(g) + H_{2}O_{2}(l) \rightarrow H_{2}O(l) + 2O_{2}(g) \]
More appropriate way to write:
\[ O_{3}(g) + H_{2}O_{2}(l) \rightarrow H_{2}O(l) + O_{2}(g) + O_{2}(g) \]
- Writing 2O\(_2\) as \(O_{2} + O_{2}\) emphasizes that both oxidant species (ozone and hydrogen peroxide) contribute to the formation of separate O\(_2\) molecules.
- This highlights the redox nature: one O\(_2\) comes effectively from O\(_3\) and the other from H\(_2\)O\(_2\), clarifying electron loss and gain from each reactant.
Technique to Investigate the Reaction Path
A suitable technique is isotopic labelling using oxygen isotopes (e.g. \(^ {18}O\)).
- For reaction (a): use \(^ {18}O\)-labelled water (\(H_{2}^{18}O\)) or \(^ {18}O\)-labelled CO\(_2\), then track in which product (O\(_2\) or C\(_6H_{12}O_{6}\)) the \(^ {18}O\) appears; this shows whether the O\(_2\) originates from water or CO\(_2\).
- For reaction (b): label O\(_3\) or H\(_2\)O\(_2\) with \(^ {18}O\) and analyse the formed O\(_2\) by mass spectrometry to see which reactant supplies each O\(_2\) molecule.