Replacing harmful refrigerants
Introduction
Chlorofluorocarbons[1] (CFC), chlorofluorocarbons or chlorofluorocarbon gases[2] are derivatives of saturated hydrocarbons obtained by replacing hydrogen atoms with fluorine and/or chlorine atoms mainly.
CFCs are a family of gases that are used in various applications, mainly in the refrigeration industry and as aerosol propellants. They are also present in thermal insulators. CFCs have a long persistence in the atmosphere, from 51 to more or less 200 years. Over time they reach the stratosphere, where they dissociate due to the action of ultraviolet radiation, releasing chlorine and this begins the process of destruction of the ozone layer. CFC is the generic name for a group of compounds containing chlorine, fluorine and carbon, used as cooling agents and as propellant gases in aerosols. Its multiple applications, its volatility and its chemical stability cause its accumulation in the upper atmosphere, where its presence causes the destruction of the protective ozone layer.
It is currently known that the appearance of the ozone "hole" over Southeast Antarctica, at the beginning of the southern spring, is related to the photochemistry of CFCs present in various commercial products (freon, aerosols, paints, etc.).
Types of CFCs according to their commercialization
After World War I it was discovered that by vaporizing CFC-12 in a liquid state, it could be used to create bubbles in rigid foam plastics. The tiny bubbles embedded in CFCl make these products good thermal insulators, since this gas is a poor conductor of heat. However, CFC-12 is released immediately during the formation of foam sheets, such as the white trays used to package fresh meat products, and previously to hold hamburgers in fast food restaurants.
Ozone layer degradation
It has been proposed that the mechanism through which CFCs attack the ozone layer is a photochemical reaction: when light falls on the CFC molecule, a chlorine atom with a free electron is released, called the chlorine radical, which is very reactive and has great affinity for ozone, which breaks the latter molecule. The reaction would be catalytic; The proposed theory estimates that a single chlorine atom would destroy up to 100,000 ozone molecules. Some allege that CFC remains for more than a hundred years in the upper layers of the atmosphere, where ozone is found, but this is impossible given that CFC molecules have a molecular weight that varies between 121.1 and 137.51 while the density of the atmosphere is 29.01, so the few Freon molecules that reach the stratosphere fall back to earth in a short time.