Ozone reacts readily with opposite gases so is display in the troposphere for a limited time. Ozone is formed in photochemical smog (such as Nitrogen dioxide) through interaction with sunniness or diffuses into the troposphere from the stratosphere aswell as being formed from lighting and other electrical sources. Photochemical smog is found in spicy concentration in and around cities such as Los Angelesâ€" cognise to have high-pitched levels of ozone concentrations. A study carried out in the United States in 2008 revealed that people living in Los Angeles had a 30% greater risk of dying of lung disease. Ozone is poisonous to humanity and many other organisms and has been proven to cause respiratory problems, headaches, tire outâ€"as well as being an irritant to the nose, lungs, eye and throat and can cause death in high concentrations. Ozone is found in low concentrations in the troposphere being on average 0.02 parts per million.
Ozone as a radiation shield
90% of ozone is present in the stratosphere where it exists as 2-8 parts per million.
During the formation of ozone and the annihilation of ozoneâ€"the reactions absorb UV radiation from the sun, effectively shielding heart on earth to its damaging effects. Ozone in the stratosphere is formed for the most part due to the interaction between light and oxygen molecules:
O?(g) ? 2O(g) (absorbs high energy UV radiation).
O(g) + O?(g) ? O?(g).
The buncombe of Ozone also absorbs UV radiation:
O?(g) ? O?(g) + O(g) (absorbs reserve energy UV radiation).
O?(g) + O(g) ? 2O?(g).If you want to get a full essay, order it on our website: Ordercustompaper.com
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