In the upper atmosphere, the atomic fluorine (F.) forms from the photo dissociation of fluorine containing compounds. These fluorine atoms, in turn, can participate in subsequent reactions which bring about the destruction of ozone. Consider the situation in which the rate of production of F. by photochemical reactions is rpc, and the following reactions take place, where M is any arbitrary species. = dt (1) (2) (3) (4) (5) d[F. ) k2 F: +02 + M > F02:+M k3 F02: +03 FO: +202 FO: +03 F02: +02 k5 FO. +03 F: +202 ko 2F0: products . (6) Please derive an expression for the rate of disappearance of ozone that contain only the various rate constants, the concentrations of stable species, and rpc