The word "smog" results from the
combination of the English words "smoke" and
"fog", describing a condition of widespread airborne
contamination with partially visible air pollution above urban
and industrial areas. The term smog is today used in general to
refer to high levels of pollutants in the air, with or without
the presence of fog.
The problem of polluted air in cities is not
new. For example, in the year 66 AD Seneca exclaimed: "As
soon as I escaped the heavy air of Rome, the stink of the
smoking chimneys, the soot they spewed forth, and the
pestilential steam, I felt a complete change in my
well-being."
The connection between air pollution and
health has long been well known. This became clearest, however,
during smog catastrophes with exceptional numbers of deaths,
such as when over 4,000 people died in London in 1952.
Today, it is assumed that the synergistic
effect of particulate matter and sulfur dioxide has played the
most important role in the majority of smog cases. This
realization led eventually to the introduction of total
threshold values for particulate matter and sulfur dioxide in
the smog ordinances of the Federal Republic of Germany.
Different types of smog can be principally
differentiated based on their origin: The winter smog of type
"LONDON" or "LONG-DISTANCE TRANSPORT" and
the summer smog of type "LOS ANGELES."
The smog type "LONDON" forms in
winter during inversion weather conditions with cold air near
the ground, when the low temperatures require intense artificial
heating. Since coal and fuel oil are also used as heating
material (though less frequently today), the primary pollutant
components that arise are SO2, CO, particulate
matter, sulfates, and H2SO4.
The German state governments are empowered by
§ 40 Paragraph 1 of the BImSchG to establish smog ordinances
for areas where a strong increase in damaging environmental
effects from air pollution can be expected during low-exchange
weather conditions. The states are also empowered to issue smog
alarms under specific (nationwide) criteria. In such a case,
large polluters are subject to emissions-reducing ad-hoc
devices. Smog ordinances are enacted according to state law. A
universal condition is that the respective responsible state
ministry gives notice of a low-exchange weather condition under
the indication of the forewarning level or alarm level for a
smog area. In addition, under § 40 BImSchG it is possible to
establish areas where vehicle traffic can be limited or
forbidden during weather conditions with smog alarms.
The substitution of coal and oil by gas and
steam heating, a clear reduction (2008) of 0.1% by volume in the sulfur
content of light heating oil, and the de-sulfuring of powerplant
exhaust gases since 1990 have all contributed to a significant
decrease of the component sulfur dioxide. The need in the 1980s
to nevertheless issue smog alarms lay on the one hand with
intensified alarm values and on the other with long-distance
pollution from the East. The smog type "LONDON" has
since lost much of its importance, so much so that many states
have lifted the corresponding smog ordinance, including
Baden-Württemberg in 1997.
The smog type "LONG-DISTANCE
TRANSPORT" is likewise a winter smog that in Germany can
form under easterly wind conditions with inversions, since the
areas east of Germany still use substantial amounts of coal and
brown coal for heating purposes and energy generation. This type
of smog can also appear with high wind velocities.
The summer smog "LOS ANGELES" is an
entirely different type of smog. The source here is first and
foremost automotive traffic with its exhaust gases (e.g.
nitrogen oxides, hydrocarbons, and carbon monoxide). As a result
of poor air exchanges connected with strong sunshine, a chemical
transformation of the gases in the atmosphere results in the
formation of photo-oxidants. The most important compounds here
include ozone (O3) and peroxiacetylnitrate (PAN) next
to peroxides, aldehydes, etc..