Fig 1 . TIP4P energy minimized structure of water cluster containing 50 water molecules.
3.2 Formation of Criegee Intermediate (CI): Carbonyl oxides or CIs are those atmospheric intermediate which significantly act as non-photolytic source of many tropospheric reaction processes. Johnsonet.al proved that the carbonyl oxides are produced via alkene ozonolysis having significant amount of internal energy to undergo either unimolecular or bimolecular reactions depending upon their stability.20 As tropospheric abundances of alkenes and ozone are relatively higher, it is worthwhile to study the formation of CI through the reaction between C2H4with O3. Fig 2 shows the reaction energetic.