R and V Works FF6 Informações Técnicas Página 73

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Compressor Application Manual
71
Some CFCs can live in the atmosphere for more
than 120 years, that is, they do not dissociate in the
lower atmosphere (troposphere). As a result, the
CFCs slowly migrate to the stratosphere where they
are affected by higher levels of radiation, releasing
the chlorine, which once free, repeatedly bonds
with ozone molecules to cause the separation of
the oxygen atoms from the molecule in question.
With the destruction of the ozone, higher levels of
radiation tend to penetrate the Earth's surface.
Moreover, as CFCs in the atmosphere have a
long life and as a chlorine atom can repeatedly
destroy thousands of ozone molecules, it will
take many decades for the ozone layer to return
to its original concentration levels, even after
the CFCs have been completely eliminated.
From the time when the theory of the destruction
of the ozone layer was published for the first time,
scientific research has demonstrated general
concern with the increase of chlorine concentration
in the stratosphere, which, after destroying the
ozone, results in health and environmental hazards,
for instance:
Increase in the number of skin cancer patients;
Increase in the number of cataract patients
(ocular);
Crop damage;
Damage to aquatic organisms (marine algae);
Increase in environmental temperature.
VII
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