Hydrogen abstraction from hydrocarbons by atomic chlorine is a mechanism for
\(\mathrm{Cl} \cdot\) loss in the atmosphere. Consider the reaction of
\(\mathrm{Cl} \cdot\) with ethane:
$$\mathrm{C}_{2} \mathrm{H}_{6}(g)+\mathrm{Cl} \cdot(g) \rightarrow
\mathrm{C}_{2} \mathrm{H}_{5} \cdot(g)+\mathrm{HCl}(g)$$
This reaction was studied in the laboratory, and the following data were
obtained:
$$\begin{array}{cc}\mathbf{T}(\boldsymbol{K}) & \mathbf{k}\left(\times
\mathbf{1 0}^{-\mathbf{1 0}} \mathbf{M}^{-\mathbf{2}}
\mathbf{s}^{-\mathbf{1}}\right) \\\\\hline 270 & 3.43 \\\370 & 3.77 \\
470 & 3.99 \\\570 & 4.13 \\\670 & 4.23\end{array}$$
a. Determine the Arrhenius parameters for this reaction.
b. At the tropopause (the boundary between the troposphere and stratosphere
located approximately \(11 \mathrm{km}\) above the surface of Earth \(),\) the
temperature is roughly \(220 \mathrm{K}\). What do you expect the rate constant
to be at this temperature?
c. Using the Arrhenius parameters obtained in part (a), determine the Eyring
parameters \(\Delta H^{\dagger}\) and \(\Delta S^{\frac{1}{r}}\) for this reaction
at \(220 \mathrm{K}\)