a deep layer in the
stratosphere,
encircling
the Earth, that has
large amounts of ozone
in it. The
layer shields
the entire Earth from much of the harmful
ultraviolet
radiation that comes from the sun.
Interestingly, it is also
this ultraviolet radiation
that forms the ozone in the first
place. Ozone is a
special form of oxygen, made up of three oxygen
atoms rather than the usual two oxygen atoms. It
usually forms when
some type of radiation or
electrical discharge separates the two
atoms in an
oxygen molecule , which can then
individually
recombine with other oxygen molecules to form ozone .The photo chemical mechanisms that give rise to the ozone layer were discovered by the British physicist Sydney Chapman in 1930. Ozone in the Earth's stratosphere is created by ultraviolet light striking oxygen molecules containing two oxygen atoms , splitting them into individual oxygen atoms (atomic oxygen); the atomic oxygen then combines with unbroken oxygen to create ozone. The ozone molecule is also unstable (although, in the stratosphere, long-lived) and when ultraviolet light hits ozone it splits into a molecule of oxygen and an atom of atomic oxygen, a continuing process called the ozone-oxygen cycle, thus creating an ozone layer in the stratosphere, the region from about 10 to 50 kilometers (33,000 to 160,000 ft) above Earth's surface. About 90% of the ozone in our atmosphere is contained in the stratosphere. Ozone concentrations are greatest between about 20 and 40 kilometers (66,000 and 130,000 ft.), where they range from about 2 to 8 parts per million. If all of the ozone were compressed to the pressure of the air at sea level, it would be only 3 millimeters thick.
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