The process of conversion of ozone into oxygen $\left(2O_{3} \longrightarrow 3O_{2}\right)$ involves following steps
$O _{3} {<=>[{\text { Fast }}]} O _{2}+ O$$O + O _{3} {->[{\text { Slow }}]} 2 O _{2}$
The rate law expression for this process is
$O _{3} {<=>[{\text { Fast }}]} O _{2}+ O$ $O + O _{3} {->[{\text { Slow }}]} 2 O _{2}$ From equation (i) $K_{c}=\frac{\left[ O _{2}\right][ O ]}{\left[ O _{3}\right]}$ or $[ O ] =\frac{K_{ c }\left[ O _{3}\right]}{\left[ O _{2}\right]} $ Rate $=k\left[ O _{3}\right][ O ]$ $=k\left[ O _{3}\right] . \frac{K_{c}\left[ O _{3}\right]}{\left[ O _{2}\right]} $ $=k^{'}\left[ O _{3}\right]^{2}\left[ O _{2}\right]^{-1}$
P block elements are those in which the last electron enters any of the three p-orbitals of their respective shells. Since a p-subshell has three degenerate p-orbitals each of which can accommodate two electrons, therefore in all there are six groups of p-block elements.
P block elements are shiny and usually a good conductor of electricity and heat as they have a tendency to lose an electron. You will find some amazing properties of elements in a P-block element like gallium. It’s a metal that can melt in the palm of your hand. Silicon is also one of the most important metalloids of the p-block group as it is an important component of glass.