Cfcs Cause Deterioration of the Ozone Layer

Topics: Ozone depletion, Oxygen, Ozone Pages: 7 (2340 words) Published: October 8, 1999
Cfcs Cause Deterioration of the Ozone Layer

The deterioration of the ozone layer , caused by Cfcs, endangers the lives of humans'. Cfcs have a diminishing effect on the ozone layer. Furthermore, the deterioration of the ozone cause an increase of Ultraviolet (UV) radiation which can have a negative effect on human skin and eyes. As a writer for newsweek, I have investigated the scenario and found the following information.

The earth's atmosphere is a blanket of air that surrounds the planet. This atmospheric air is made up of many different gases, 78% nitrogen, 21% oxygen, and 1% of a dozen or more other gases like carbon dioxide, helium, and ozone.

This atmosphere extends many miles out from the earth's surface. However, this layer is not a uniform layer, from top to bottom. As one moves out from the planet's surface the atmosphere becomes progressively dense. This atmosphere can be divide into four major regions.

The first region is the troposphere which extends about 6.5 miles above the planet's surface. The troposphere contains the oxygen that we breath and is where a majority of our weather takes place.

Beyond the troposphere is the second region of the atmosphere, the stratosphere. The stratosphere extends from roughly 6.5-30 miles from the earth's' surface. The air on this region is much less dense than in the troposphere, and it's a lot drier. The stratosphere is the area that contains the majority of the ozone layer.

Past the stratosphere is the mesosphere which extends to 50 miles above the planet. The last region is the thermosphere. The thermosphere's outermost edge is roughly 600 miles above the surface of the earth. Beyond it, the airless vacuum of space begins.

Oxygen is made up of two oxygen atoms that are bonded together. In the periodic table it is represented by O2.
Like oxygen, ozone is a gas that is made up of oxygen atoms. However, a molecule of ozone is made up of three atoms of oxygen bonded together, therefore, O3, represents ozone. The ozone makes up only .01% of the atmosphere. Furthermore, 90% of the ozone is found in the stratosphere. It is concentrated in a layer between 7 and 22 miles above the earth's surface.

The massive depth of the ozone in the stratosphere would lead you to believe that it is very thick, it is not. If it were condensed, the ozone layer would only be a few millimeters thick (Rowland and Molina 1994. p.23).

The ozone is made in the stratosphere. It is continuously being formed, broken down, and reformed, over and over again. Furthermore, the three key elements of the cycle are: oxygen, ozone, and the energy from the sun.

The ultimate source of energy for our planet is the sun. This energy travels through space in the form of Electromagnetic Radiation. Furthermore, this electromagnetic radiation is often referred to as waves and their length, therefore, wavelengths. The sun has a wide range of wavelengths. This range is known as the Electromagnetic Spectrum. In this spectrum there is Gamma, Ultraviolet, Visible, Infrared, and Radio waves.

It is the ultraviolet (UV) radiation coming from the sun that drives the ozone cycle in the stratosphere. When a oxygen molecule is hit by a high-energy UV ray, the O2 molecule absorbs the ray's energy. As a result, the bond holding the oxygen molecule together breaks. This break separates the molecule, O2=O+O. These separate molecules quickly join with nearby oxygen molecules to form a ozone molecule, O3=O2+O. Simultaneously, ozone molecules are being hit, they absorb the ray's energy and break apart, leaving behind an oxygen molecule and a single oxygen molecule, O3>O2-O. At this time, the entire process repeats itself making new molecules that are separated which combine to make new molecules, over and again (Rowland and Molin 1991 p. 42).

As a result of this cycle, about the same amount of ozone is produced as is broken down in the stratosphere. Therefore, the amount of...

Cited: reveal seasonal CIOx/NOx interaction." Nature v.230 (Aug.4,1985): p.205-
Roach, M. "Sun Track." Health v.201 (May/June 1992): p.119-125.
Engineering News v.20 (Jan.11,1994): p. 20-34.
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