Halogenated aliphatic hydrocarbons have appeared in the natural environment
in steadily increasing amounts over several decades as a consequence of th
eir growing use, chiefly as refrigerant, foam blowing agent and solvent, pr
ompted by their unique properties and low cost. It is recognised that anthr
opogenic emissions of the above compounds, which are referred to as ozone-d
epleting substances (ODS's), are partly responsible for depletion of the st
ratospheric ozone layer and the so-called greenhouse effect.
The photo decomposition of halogenomethanes in the stratosphere produces si
gnificant amounts of chlorine atoms, leading to the decay of atmospheric oz
one, which allows increased levels of biologically damaging UV radiation to
reach the Earth's surface.
The discovery of the above phenomenon has initiated efforts towards the wit
hdrawal of ODS.
Nowadays, it is accepted that fully halogenated chlorofluorocarbons (CFC's)
are the main source of the chlorine that is eroding Earth's protecting ozo
ne, and their role is of great Global concern.
In spite of the fact production CFCs has been banned since 01.01.1995 and t
heir use prohibited since 01.01.1996, the depletion of stratospheric ozone
will continue because large amounts of these class compounds are still in u
se. Therefore, the recovery and subsequent destruction of the CFCs still in
use is a logical next step, in particular the conversion of the CFC's into
useful products is a challenging task.
At present CFCs are being replaced by hydrochlorofluorocarbons (HCFC's) and
in perspective by hydrofluorocarbons (HFC's), before better replacements a
re found. The environmental impact of CFC replacements is considered in ter
ms of their ozone depletion potential (ODP), global warming potential (GWP)
and ability to form noxious degradation products.