Three forms (or allotropes) of oxygen are involved in the ozone-oxygen cycle: oxygen atoms (O or atomic oxygen), oxygen gas (O 2 or diatomic oxygen), and ozone gas (O 3 or triatomic oxygen). Ozone is formed in the stratosphere when oxygen gas molecules photodissociate after absorbing UVC photons. This converts a single O 2 into two atomic oxygen radicals. The atomic oxygen radi… Web158 Likes, 3 Comments - Alabama School of Math & Sci (@asmsdragons) on Instagram: "Toshiba/NSTA ExploraVision Competition ASMS student teams competed in the Toshiba ...
Ozone Layer Depletion - Definition, Reasons & Effects - Vedantu
WebQuestion 4. CFCs decompose in the atmosphere to form neutral chlorine atoms. Incredibly, each chlorine atom can destroy 100, 000 O 3 molecules. How many kilograms of O 3 could be destroyed by 1.00 mole of the chlorofluorocarbon described in Question 3? Assume the empirical formula in Question 3 is also the molecular formula. WebIf each chlorine atom released from a CFC molecule destroyed only one ozone molecule, CFCs would pose very little threat to the ozone layer. However, when a chlorine monoxide molecule encounters a free atom of … crystal view apartment homes garden grove
Ozone depletion: causes - Canada.ca
WebThe gas is naturally produced and destroyed by sunlight-driven chemical reactions in the stratosphere, between about 10 and 50 kilometers above the Earth’s surface. ... While CFCs are not reactive at Earth’s surface, they become quite destructive when they are exposed to ultraviolet light in the upper stratosphere. There, CFCs and their ... WebCFCs are very stable, they decay slowly and so endure in the atmosphere for up to a century. CFCs rise and gradually accumulate in the stratosphere where they are broken … WebOzone can be destroyed by a number of free radical catalysts; the most important are the hydroxyl radical (OH·), nitric oxide radical (NO·), ... CFCs and related compounds in the atmosphere. Chlorofluorocarbons (CFCs) … dynamic optical matching