Ozone molecules are always falling apart into O2 and O, but the free O just goes and bumps into another O2 forming more ozone. So it's more instructive to talk about "odd oxygen" (odd number, i.e. O and O3).
Odd oxygen sometimes just bumps into another and becomes regular old O2 again. It can also react with an unrelated chemical and be removed that way. Chlorine is especially good at this because it catches two Os and sticks them together to form an O2. The Cl then is free to do it again to another pair of Os. This action requires UV from sunlight to recycle.
Fortunately there are about 18% natural sources of chlorine in the stratosphere. Unfortunately there is 82% man-made source, chlorofluorocarbons.
The whole process is much more complicated than is described here, with a lot of intermediate chemicals, and contributing pathways. The signature of these intermediate chemicals is the smoking gun that shows that the antarctic ozone hole is made larger than it would normally be by CFCs.
Ozone molecules are destroyed everyday by CFC's. This number depends upon the current season.
CFCs break down ozone in the atmosphere when they are exposed to ultraviolet radiation. This causes the CFC molecules to release chlorine atoms, which then react with ozone molecules, leading to the destruction of the ozone layer.
The ozone layer is destroyed by certain chemicals, such as chlorofluorocarbons (CFCs) and halons, which break down ozone molecules in the stratosphere. This destruction is primarily caused by human activities like industrial processes and the use of certain products like aerosol sprays and refrigerants. When these chemicals reach the ozone layer, they release chlorine and bromine atoms that catalytically destroy ozone molecules.
Ozone has not destroyed stratosphere. It is present in it.
The ozone doesn't quite destroy its own molecules. Ultra-violet rays from the sun, that penetrate through the ozone break it's molecules apart. One molecule of ozone contains 3 atoms of oxygen. When the molecule splits, it releases heat. Then, one molecule of oxygen (2 atoms) and one atom of oxygen join together again, and become ozone (3 atoms of oxygen).
Ozone layer is a layer of ozone molecules. It is destroyed by man made CFC's.
Ozone molecules are destroyed everyday by CFC's. This number depends upon the current season.
CFCs break down ozone in the atmosphere when they are exposed to ultraviolet radiation. This causes the CFC molecules to release chlorine atoms, which then react with ozone molecules, leading to the destruction of the ozone layer.
The ozone layer is destroyed by certain chemicals, such as chlorofluorocarbons (CFCs) and halons, which break down ozone molecules in the stratosphere. This destruction is primarily caused by human activities like industrial processes and the use of certain products like aerosol sprays and refrigerants. When these chemicals reach the ozone layer, they release chlorine and bromine atoms that catalytically destroy ozone molecules.
Organisms can be destroyed by ozone. These are destroyed by the UV.
Ozone layer can be destroyed by CFC's. They react with ozone to deplete it.
Ozone has not destroyed stratosphere. It is present in it.
Atomic chlorine in the stratosphere is a key component in ozone depletion. It reacts with ozone molecules, breaking them down into oxygen molecules which can lead to the thinning of the ozone layer. This process is particularly significant in the formation of the ozone hole over Antarctica.
Ozone is destroyed by the CFC gases. CFC converts ozone to oxygen.
Ozone layer has been destroyed by CFC's. They react with ozone to deplete it.
Ozone layer is confined of ozone molecules. These molecules form a huge pool of ozone molecules.
The ozone doesn't quite destroy its own molecules. Ultra-violet rays from the sun, that penetrate through the ozone break it's molecules apart. One molecule of ozone contains 3 atoms of oxygen. When the molecule splits, it releases heat. Then, one molecule of oxygen (2 atoms) and one atom of oxygen join together again, and become ozone (3 atoms of oxygen).