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Ozone (O3) is a molecule consisting of three oxygen atoms. At standard temperature and pressure Ozone is a blue gas. Ozone forms a dark blue liquid, below -112 °C, and a dark blue solid, below -193 °C. Ozone is a powerful oxidizing agent, and is unstable, decaying to ordinary oxygen through the reaction:

2O3 → 3O2

Ozone is a highly corrosive poisonous substance and a common pollutant. It has a sharp, pungent odor. It is present in low concentrations throughout the Earth's atmosphere. It is also formed from O2 by electrical discharges, e.g., lightning, and by action of high energy electromagnetic radiation. Some electrical equipment generates levels of ozone that a human can easily smell; this is especially true if there is a spark gap or a very high voltage.

The highest levels of ozone in the atmosphere are in the stratosphere, in a region also known as the ozone layer. Here it filters out much ultravioletNote: Ultraviolet is also the name of a 1998 UK television miniseries about vampires. Ultraviolet UV radiation is electromagnetic radiation of a wavelength shorter than that of visible light, but longer than that of soft X-rays. It can be subdivided into light from the SunThe Sun (also called Sol is the star in our solar system. Planet Earth orbits the Sun. Other bodies that orbit the Sun include other planets, asteroids, meteoroids, comets and dust. Not all objects passing through the solar system have been orbitally capt that would be harmful to most forms of lifeAlternate uses: see Life (disambiguation) and Living (disambiguation Life is a multi-faceted concept with no simple definition; this article is confined to the primary meanings in biology; articles on life in other senses are included in the article life. The standard way to express ozone amounts in the atmosphere is by using Dobson unitDobson units (DU) are the standard way to express ozone amounts in the atmosphere. One DU is 2. 7 x 1016 (10 to the 16th power) ozone molecules per square centimetre. One Dobson unit refers to a layer of ozone that would be 0. 01 mm thick under standard ts. Ozone used in industry is measured in ppmParts per million ppm is a measure of concentration that is used where low levels of concentration are significant. The ppm value is equivalent to the absolute fractional amount multiplied by one million (106). Illustrations of one part per million The me ( OSHA exposure limits for example), and percent weight.

Ozone was discovered by Christian Friedrich Schonbein in 18401840 is a leap year starting on Wednesday (link will take you to calendar). Events January 3 One of the predecessor papers to the Herald Sun of Melbourne, Australia, The Port Phillip Herald is founded by George Cavanaugh. January 10 Uniform penny postage.

1 Stratospheric ozone

Ozone is notable for its ability to absorb UV-B radiation. Ozone is created naturally within the ozone layer. Ozone depletion and ozone holes occur because of chlorofluorocarbons and other upper atmospheric contaminants.

Ozone in the earth's atmosphere is generally created by ultraviolet light which breaks apart O2 molecules, creating atomic oxygen. The atomic oxygen then combines with an unbroken molecule, to create O3. Sometimes the individual oxygen atoms will combine with N2 to create a nitrogen oxide; which, when affected by visible light, may create ozone.

When ultraviolet light hits ozone it splits into a molecule of O2 and an atom of atomic oxygen, a continuing process called the ozone-oxygen cycle. This cycle can be disrupted by the presence of atomic chlorine, fluorine or bromine in the atmosphere; these elements are found in certain stable compounds, especially chlorofluorocarbons (CFCs) which may find their way to the stratosphere and there be liberated by the action of ultraviolet light on them. The NOx cycle for the formation of ozone can also be broken by the presence of atmospheric water, reducing NOx to a more stable form.



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