of CFCs, projected the construct-up and release of chlorine atoms within the stratosphere and concluded that ozone depletion was seemingly and could be lengthy-lived, even with remediation. In probably the most thorough of these studies, Richard Stolarski and Ralph Cicerone calculated vital ozone depletions if inorganic chlorine were to be current in the stratosphere at a quantity mixing ratio of 1 nanomole/mole of air.Rowland, who had pioneered research on scorching atom” chemistry, investigating chemical properties of atoms with extra translational energy produced by radioactive processes, offered
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