An analysis is made of the varions re actions in which ozone and atomic oxyge n are involve d in the stratosphère. At the présent time, hydrogen. nitrogen. and chlorine compounds in the ranges parts per million, parts per billion, and parts per I rillion may have significant chemical effects. I n the upper stratosphère, above the ozone peak. where there is no slrong departure from photochemical equilibrium conditions, the action of hydroxyl arid hydroperoxyl radicals of nitrogen dioxide and chlorine monoxide on atomic oxygen and of atomic chlorine on ozone can be introduced. A précise détermination of their ex act effects requires Knowledge of (1) the vertical distribution of the HjO. CH,. and Hj dissociation by reaction of thèse molécules with electronically excited oxygen atom OCf): (2) the ratio of the OH and HOj concentrations and their absolute values, which dépend on insufficiently known rate coefficients: (3) the various origins of nitric oxide production, with their vertical distributions relaled to latitude and season; and (4) the various sources giving différent chlorine compounds lhat may be dissociated in the stratosphère. I n the lower stratosphère, below the ozone peak. there is no important photochemical production of Oj, but there exist various possibilities of transport. The prediclability of the action of chemical reactions dépends strongly on important interactions between OH and HOj radicals with CO and NO. respectively. which affect the ratio n(OH)/n(\\Oi) at the tropopause level; between OH and NOj. which lead to the formation of nitric acid with its downward transport toward the troposphère; between NO and HO2. which lead to NO? and its subséquent photodissociation; between CI O and NO. which also lead to NOj and become more important than the reaction of CI O with O; and between Cl and various molécules, such as CH. and Hj, which lead to HCl with its downward transport toward the troposphère. Ail thèse chemical processes are subjeci to many changes since they occur in the lower stratosphère where seasonal. latiludinal, and even daytoday variations of the ozone concentrations are observed in associa tion with advective and dynamic transports, which dépend on meteorological conditions as indicated by variations of tropopause heights.