Write down a kinetic equation (net rate law) for the concentration change of ground-state oxygen atoms
with time, where t represents time, neglecting equation (A.2).
Integrate your rate law, to afford an analytical expression showing the actual variation of the ground-state
oxygen atom concentration with time, under conditions of constant irradiation, and that all species M are
present in excess. Make sure you identify appropriate boundary conditions.
Use the steady-state approximation and your kinetic equation to determine the steady-state concentration
of ground-state oxygen atoms.
Then, identify whether the steady-state hypothesis is a suitable approximation to apply to ground-state
oxygen atoms in atmospheric modelling.
Comment on any similarities or differences you have found in the application of the steady-state
approximation for the reactive intermediates (O and O) considered in Questions A1 and A2.