II.4.2 Czech Republic
II.4.2.1 Air quality with regard to health protection limit values
II.4.2.1.1 Sulphur dioxide
Sulphur dioxide emitted from anthropogenic sources is created mainly by burning
the fossil fuels (mostly coal and heavy fuel oils) and by smelting ores
containing sulphur. Volcanos and oceans belong to the main global natural
sources of SO2, nevertheless their share on the territory within EMEP (in which
the Czech Republic is also participating) was estimated at only 2 %. In the
atmosphere, SO2 is oxidized to sulphates and H2SO4, creating aerosol both in the
form of droplets and suspended particles of broad size range. SO2 and the
substances originating from it are removed from the atmosphere through wet and
dry deposition. SO2 has irritating effect, high concentrations can cause lung
function impairment and the change of lung capacity.
The 2006 situation of air pollution caused by SO2 with regard to the limit
values set by the legislation is documented by the Tables
II.4.2.1 and II.4.2.2
and Figs. II.4.2.1–II.4.2.4. The table of annual average SO2 concentrations is
also included to illustrate the situation (Table II.4.2.3).
In 2006 the set limit value for 24-hour SO2 concentration (125 μg.m-3, tolerated
number of exceedances – 3) was exceeded in the locality Úštěk (ZÚ) and at two
ČEZ stations Kostomlaty pod Milešovkou and Petrovice u Karviné. The Úštěk
locality recorded the exceedances of 1-hour limit value also in previous years
due to the influence of local sources. No locality reported the exceedance of
the 1-hour SO2 limit value 350 μg.m-3 (tolerated number of exceedances – 24, the
highest number of exceedances was recorded at the ČEZ AMS station Horní Halže –
9).
The map diagrams in Fig. II.4.2.1 show the evident improvement of air quality
resulting from the significant decrease of SO2 concentrations documented by the
marked decline of the 4th highest 24-hour SO2 concentration at all stations in
the period 1998–2000. In the following years this decreasing trend stopped. The
slight decrease in SO2 concentrations continued again from 2004 to 2005. In 2006
the decreasing trend stopped again and, on the contrary, SO2 concentrations
slightly increased in almost all localities of the Czech Republic. At some
stations, especially in the Ústí nad Labem Region and in the Moravian-Silesian
Region, more significant increase of air pollution caused by SO2 was recorded.
This increase is probably caused by the return to coal combustion in local
furnaces and by unfavourable meteorological conditions in the first months of
the year.
Figs. II.4.2.3 and
II.4.2.4 document the courses of 1-hour and 24-hour SO2
concentrations at the stations in 2006. Fig. II.4.2.4 confirms the increased SO2
concentrations in winter periods of the previous years in the environs of the ZÚ
station Úštěk.
Fig. II.4.2.2, presents the spatial distribution of the 4th highest 24-hour SO2
concentrations. On almost 7 % of the territory of the Czech Republic the SO2
concentrations exceeded the lower assessment threshold (LAT). Only a very small
area of the Czech Republics territory (0.01 %) recorded the exceedances of the
limit value.
Tab. II.4.2.1 Stations with the highest values of the 25th and maximum hourly
concentrations of SO2
Tab. II.4.2.2 Stations with the highest numbers of exceedances of the 24-hour
limit value of SO2
Tab. II.4.2.3 Stations with the highest values of annual average concentrations
of SO2
Fig. II.4.2.1 4th highest 24-hour concentrations and maximum hourly
concentrations of SO2 in 1996–2006 at selected stations
Fig. II.4.2.2 Field of the 4th highest 24-hour concentration of SO2 in 2006
Fig. II.4.2.3 Stations with the highest hourly concentrations of SO2 in 2006
Fig. II.4.2.4 Stations with the highest 24-hour concentrations of SO2 in 2006
II. 4.2.1.2 Suspended particles, PM10 fraction and PM2.5 fraction
The particles contained in the ambient air can be divided into primary and
secondary particles. The primary particles are emitted directly into the
atmosphere, both from natural and anthropogenic sources. Secondary particles1
are mostly of anthropogenic origin and are created by oxidation and consequent
reactions of gaseous compounds in the atmosphere. Similarly as in the whole
Europe, most emissions in the Czech Republic are of anthropogenic origin. The
main anthropogenic sources include: transport, power stations, combustion
sources (industrial and local), fugitive emissions from industry,
loading/unloading, mining and building activities. Due to the diversity of
emission sources the suspended particles have various chemical composition and
various size. The PM10 suspended particles have serious health impacts appearing
already at low concentrations without apparent low safe concentrations
threshold. Health impacts of particles are influenced by their concentration,
size, shape and chemical composition. They can cause hypo-immunity, inflammation
of lung tissue and oxidative stress. Increased concentrations are responsible
for cardiovascular diseases and acute trombotic complications. Persistent
exposure can result in respiration diseases, damaged lung function and increased
mortality (lower life expectancy). Recently it has been proved that the most
serious health impacts (incl. increased mortality) are recorded in PM2.5 or PM1
fractions which enter the lower parts of the respiratory system when inhaled.
Air pollution caused by PM10, as shown in the Tables
II.4.2.4. and II.4.2.5,
similarly as in Fig. II.4.2.5, remains one of the main problems of air quality
assurance. Fig. II.4.2.5 shows the increasing trend of PM10 pollution at almost
all stations in the Czech Republic from 2001 to 2003. In 2004 this trend stopped
but in 2005 the PM10 concentrations increased again at almost all selected
stations. In 2006 this trend was confirmed at most stations only in annual
averages, on the contrary, slight decrease was recorded in 24-hour concentration
of PM10 at most localities.
The most affected area of large coverage is, similarly as in the previous years,
the Ostrava-Karviná area. In 2006 the air quality in this region was influenced
by deteriorated meteorological and dispersion conditions in early January and
late February, when the 24-hour PM10 concentration exceeded the value of 600
μg.m-3 at several stations (see II.4.1 Agglomerations). The limit value of
24-hour PM10 concentration was exceeded in 2006, and namely at the stations in
the Moravian-Silesian Region (Český Těšín, Ostrava-Bartovice, Bohumín,
Ostrava-Přívoz, Karviná, Ostrava-Českobratrská (hot-spot), Věřnovice, Orlová,
Havířov, Karviná ZÚ, Ostrava-Fifejdy and Ostrava-Přívoz ZÚ), at the stations in
the capital city of Prague (Prague 2-Legerova (hot spot) and Prague 8-Karlín),
in the Central Bohemian Region (Kladno-Švermov, Stehelčeves and Beroun), in the
South Moravian Region (Brno-střed), in the Ústí nad Labem Region (Ústí
n.L.-Všebořická (hot spot), Ústí n.L.-město and Teplice), in the Zlín Region (Zlín-Svit
and Uherské Hradiště), in Olomouc Region (Olomouc and Olomouc-Velkomoravská. Of
the total number of 148 localities in which PM10 measurements were carried out,
94 stations reported exceedances of 24-hour PM10 limit value. The annual PM10
limit value was exceeded at 43 stations. The number of localities which exceeded
the limit value in both above air pollution characteristics of PM10 fraction is
approximately same as in 2005.
As it is evident from Fig. II.4.2.6, in 2006 there was a certain reduction of
the area with above-the-limit 24-hour concentrations of PM10, especially in the
whole area along the Elbe River and in the Liberec Region. Figs.
II.4.2.6 and
II.4.2.7 show, however, that PM10 limit value exceedances are still significant
for listing the basic administrative units among the areas with deteriorated air
quality. Especially Fig. II.4.2.6 shows quite evidently that in the towns where
the PM10 measurements are carried out the 24-hour average concentrations are
above the limit value. However, it can be admitted that also in the towns
without PM10 measurements the concentrations of this pollutant can be high or
exceeding the limit value.
The map of fields of PM10 concentrations (Figs.
II.4.2.6 and II.4.2.7) were
constructed in 2006 with the use of the empiric model which combines the
dispersion model SYMOS, the European model EMEP and the altitude with the
measured concentrations at rural background stations according to the methods
developed within the ETC/ACC [28]. The application of the SYMOS model as the
only one would not be sufficient in the case of PM10 as the model calculations
include only the emissions from primary sources. The significant share in PM10
pollution, however, is contributed by secondary particles and re-suspended
particles , which are not included in the emissions from the primary sources but
considered by the EMEP model.
The result maps of PM10 concentrations were created by combining the maps
constructed separately for rural areas and for urban areas with the use of the
population density grid.
The areas where PM10 concentrations exceed the respective limit values
represent, with regard to the newly constructed map, almost 28.5 % of the
territory of the Czech Republic with more than 62 % of the total population.
The graphs of courses of 24-hour concentrations of PM10 in 2006 at the stations,
where the limit values for annual average and for 24-hour average were exceeded,
are shown in Figs. II.4.2.8 and
II.4.2.9. The selection of 12 localities with
the greatest numbers of PM10 24-hour limit value exceedances includes 9 stations
from the Moravian-Silesian Region. Fig. II.4.2.10 presents the number of exceedances of the PM10 24-hour limit value.
The complete overview of the exceedances limit value for the PM10 annual average
concentration for the recent 5 years is presented in Fig.
II.4.2.11 and Table
II.4.2.6. Fig.
II.4.2.11 shows the annual average PM10 concentrations for the
period 2002–2006 at the localities where at least once in this period the annual
limit value was exceeded. Table II.4.2.6 shows the particular values of the
reached average PM10 concentrations. Annual average concentrations exceeding the
limit value are printed bold.
Since 2005 the fine fraction of suspended particles (PM2.5) has been measured in
the Czech Republic. In 2006 the measurements were carried out in 25 localities
with valid annual average. The results show significant contribution of PM2.5
fraction to air pollution situation in the territory of the Czech Republic. When
comparing the results with the proposed annual air pollution limit value (25
μg.m-3), it is evident that in 14 localities the limit value would be exceeded
(12 in 2005). These are mainly the stations in the Ostrava-Karviná area (Věřňovice,
Ostrava-Přívoz, Ostrava-Zábřeh and Ostrava-Poruba), which record the highest
annual average concentrations in the Czech Republic, and in the following
localities: Olomouc, Zlín, Beroun, Prague 9-Vysočany, Brno-Tuřany, Rychnov nad
Kněžnou, Prague 5-Smíchov, Teplice, Kladno-střed and Most. Another 3 localities
were close below the proposed limit value. The stations with the highest values
of annual average concentrations of PM2.5 are presented in Table
II.4.2.7. The
annual average PM2.5 concentrations in the localities which measured this
fraction in 2006 are presented in Fig. II.4.2.12 in the form of spot symbols.
For the first time this Yearbook presents the courses of daily PM2.5
concentrations with regard to the exceedance of the proposed annual limit value
of this pollutant for the year 2006 (Fig. II.4.2.14). Significant exceedance of
the proposed PM2.5 limit value was recorded in the localities of the
Moravian-Silesian Region.
Fig. II.4.2.13 shows the seasonal course of the ratio between PM2.5 and PM10
fractions of suspended particles. The month average of the ratio of PM2.5 and
PM10 daily concentrations averaged from 15 AIM stations and 3 manual stations
with valid data for the year 2006 is presented. The measurement results indicate
that the ratio between PM2.5 and PM10 is not constant but shows certain seasonal
course. In 2006 the average fractions ratio ranged between 0.67–0.83, with
lower values in the summer period.
The seasonal course of PM2.5/PM10 fraction ratio is connected with the seasonal
character of several emission sources. Emissions from combustion sources show
higher shares of PM2.5 fraction than for instance emissions from agriculture and
reemissions during dry and windy weather. Consequently, heating in the winter
period can cause the higher share of PM2.5 fraction in comparison with PM10
fraction. The decrease during the spring and early summer is also explained by
the increased amount of larger biogenic particles (e.g. pollen) by some authors
[29].
The lowest monitored ratio is at traffic stations. During fuel combustion the
emitted particles occur mainly in PM2.5 fraction and thus the ratio should be
high in traffic localities. The fact that this is not the case, accents the
significance of emissions of larger particles caused by tire, break lining and
road surface abrasion.
Tab. II.4.2.4 Stations with the highest numbers of exceedances of the 24-hour
limit value of PM10
Tab. II.4.2.5 Stations with the highest values of annual average concentrations
of PM10
Tab. II.4.2.6 Overview of localities with the exceedance of the limit value for
annual average PM10 concentration, 2002–2006
Tab. II.4.2.7 Stations with the highest values of annual average concentrations
of PM2.5
Fig. II.4.2.5 36th highest 24-hour concentrations and annual average
concentrations of PM10 in 1996–2006 at selected stations
Fig. II.4.2.6 Field of the 36th highest 24-hour concentration of PM10 in 2006
Fig. II.4.2.7 Field of annual average concentration of PM10 in 2006
Fig. II.4.2.8 Stations with the highest exceedance of LV for 24-hour
concentrations of PM10 in 2006
Fig. II.4.2.9 Stations with the highest exceedance of LV for annual
concentrations of PM10 in 2006
Fig. II.4.2.10 Numbers of exceedances of air pollution limit value for the 24-hour
concentration of PM10 in 2006
Fig. II.4.2.11 Annual average PM10 concentrations at the stations with the
exceedance of the limit value, 2002–2006
Fig. II.4.2.12 Annual average concentration of PM2.5 at stations in 2006
Fig. II.4.2.13 Average monthly PM2.5/PM10 proportions in 2006
Fig. II.4.2.14 Stations with the highest exceedance of the proposed LV for
annual concentrations of PM2.5 in 2006
II.4.2.1.3 Nitrogen dioxide
In the field of ambient air monitoring and assessment the term nitrogen oxides
NOx is used for the mixture of NO and NO2. Air pollution limit value for the
protection of human health is set for NO2, the limit value for the protection of
ecosystems and vegetation is set for NOx.
More than 90 % of the total nitrogen oxides in the ambient air are emitted in
the form of NO. NO2 is formed relatively quickly in the reaction of NO with
ground-level ozone or with HO2 or RO2 radicals. In a number of chemical
reactions part of NOx is transformed to HNO3/NO3-, which are removed from the
atmosphere through deposition (both dry and wet). NO2 is dealt with due to its
negative influence on human health. It plays also the key role in the formation
of photochemical oxidants.
In Europe, NOx emissions result mainly from anthropogenic combustion processes
during which NO is formed in reaction between nitrogen and oxygen in the
combusted air, and partly also by oxidation of nitrogen from the fuel. Road
transport is the main anthropogenic source (significant shares however, have
also air transport and water transport), and also combustion processes in
stationary sources. Less than 10 % of total NOx emissions result from combustion
directly in the form of NO2. Natural NOx emissions result mainly from soil,
volcanic activity and creation of bolts of lightning. Globally, they are
important, on the European scale, however, they represent less than 10 % of
total emissions. Exposure to the increased NO2 concentrations affects lung
function and can cause lower immunity.
The exceedances of annual limit values for NO2 occur only in limited number of
stations, and namely in the localities in agglomerations and large cities
exposed to traffic. Of the total number of 180 localities in which NO2 was
monitored in 2006 the annual limit value was exceeded at 15 stations (Table
II.4.2.9). This limit value plus the margin of tolerance (48 μg.m-3) was
exceeded at 5 localities, and namely at 3 stations in Prague (Legerova,
Svornosti and Sokolovská) and at 1 station in Olomouc (Velkomoravská) and at 1
station in Brno (Svatoplukova). All the measuring sites are significantly
influenced by traffic.
The AMS traffic-oriented (hot spot) Prague 2-Legerova station recorded,
similarly as in the previous years, a great number of exceedances (126) of the
limit value for NO2 hourly concentration 200 μg.m-3. In 2006, however, this AMS
(as well as any other locality in the Czech Republic) did not exceed the hourly
limit value plus the margin of tolerance (240 μg.m-3). The measurement results
of this station confirm again the constant big problem of the capital city of
Prague with the traffic routes leading through the city centre.
At most stations presented in Fig. II.4.2.15 both the annual average
concentration and the 19th highest hourly NO2 concentration had a moderately
declining trend until 2001. In 2002 this trend stopped and in 2003 there was a
slight increase of NO2 pollution at most localities. In 2004 a slight decrease
was recorded but in 2005 the increasing trend of NO2 concentrations continued
again, and it was confirmed in 2006 at almost all stations. The stations Prague
2-Legerova and Pardubice-Rosice, on the contrary, show the evident decrease in
absolute values of hourly concentrations of this pollutant.
The field of NO2 annual average concentration (Fig. II.4.2.16) gives evidence of
air pollution in the cities caused mainly by traffic.
Fig. II.4.2.17 presents the courses of hourly concentrations in 2006 showing the
evident limit value (LV) exceedances in several localities. The exceedance of
the limit value plus the margin of tolerance was not recorded, the highest
number of exceedances of the value 200+40 μg.m-3 was recorded at the AMS Prague
2-Legerova (hot spot, 8x) monitoring the traffic load; the admissible exceedance
frequency is 18.
When constructing the map in Fig. II.4.2.16 also national traffic census from
the year 2005 was regarded. As compared with the previous census in 2000, i.e.
during the recent 5 years, the increase of traffic is significant. The higher
NO2 concentrations can occur also in the vicinity of local communications in the
villages with intensive traffic and dense local transport network.
Tab. II.4.2.8 Stations with the highest values of the 19th and maximum hourly
concentrations of NO2
Tab. II.4.2.9 Stations with the highest values of annual average concentrations
of NO2
Fig. II.4.2.15 19th highest hourly concentrations and annual average
concentrations of NO2 in 1996–2006 at selected stations
Fig. II.4.2.16 Field of annual average concentration of NO2 in 2006
Fig. II.4.2.17 Stations with the highest hourly concentrations of NO2 in 2006
Fig. II.4.2.18 Stations with the highest exceedance of LV and LV+MT for annual
concentrations of NO2 in 2006
II. 4.2.1.4 Carbon monoxide
The insufficient burning of fossil fuels may be an anthropogenic source of air
pollution caused by carbon monoxide. These processes occur mainly in transport
and in stationary sources, namely household heating.
Carbon monoxide can cause headache, deteriorated coordination and attention. It
binds to haemoglobin and the increased concentrations of the created
carboxyhaemoglobin reduce the capacity of blood for the oxygen transport.
In 2006 carbon monoxide concentrations were measured at 43 localities. Maximum
daily 8-hour running averages of carbon monoxide do not exceed the limit value
(10 mg.m-3) at any of the stations. The highest daily 8-hour average
concentration was measured at the hot spot locality Ostrava-Českobratrská (5.8
mg.m-3).
The courses of maximum daily 8-hour running averages for selected localities are
presented in Fig. II.4.2.20. The air pollution situation caused by carbon
monoxide in 2006 is characterized in Table II.4.2.10.
Tab. II.4.2.10 Stations with the highest values of maximum 8-hour running
average concentrations of CO
Fig. II.4.2.19 Maximum 8-hour running average concentrations of CO in
1996–2006 at selected stations
Fig. II.4.2.20 Stations with the highest values of maximum 8-hour running
average concentrations of CO in 2006
II.4.2.1.5 Benzene
With the increasing intensity of road transport the monitoring of air pollution
caused by aromatic hydrocarbons is becoming relevant. The decisive source of
atmospheric emissions of aromatic hydrocarbons – and namely of benzene and its
alkyl derivates – are above all exhaust gases of petrol motor vehicles. Another
source are loss evaporative emissions produced during petrol handling, storing
and distribution. Mobile sources emissions account for approx. 85 % of total
aromatic hydrocarbons emissions, while the prevailing share is represented by
exhaust emissions. It is estimated that the remaining 15 % of emissions come
from stationary sources. Many of these are related to industries producing
aromatic hydrocarbons and those industries that use these compounds to produce
other chemicals.
The research shows that benzene level in petrol is about 1.5 % while diesel
fuels contain relatively insignificant benzene concentrations. Exhaust benzene
is produced primarily by unburned benzene from fuels. Non-benzene aromatics in
the fuels can cause 70 to 80 % of the exhaust benzene formed. Some benzene also
forms from engine combustion of non-aromatic fuel hydrocarbons. The most
significant adverse effects from exposure to benzene are haematotoxicity and
carcinogenicity [16].
The situation of the year 2006 is characterized in Table
II.4.2.11 and Fig.
II.4.2.22. Of the total number of 31 localities monitoring benzene
concentrations in 2006 the limit value 5 μg.m-3 plus the margin of tolerance (in
2006 4 μg.m-3) was exceeded, similarly as in the previous year, in the ZÚ
locality Ostrava-Přívoz (12.1 μg.m-3) and in the CHMI locality Ostrava-Přívoz
(11.5 μg.m-3). Close below the limit value remained the locality Ostrava-Fifejdy
with the annual average 4.9 μg.m-3). Higher concentrations are connected with
industrial activities in this area (mainly coke production).
The air pollution limit value 5 μg.m-3 must be met by 31.12.2009.
The annual average benzene concentrations slightly increased at most localities
as compared with the previous year.
The map diagram (Fig. II.4.2.21) shows the overview of the development of
average annual concentrations in 1999–2006. Fig. II.4.2.23 presents the annual
course of 24-hour averages in selected localities.
Tab. II.4.2.11 Stations with the highest values of annual average concentrations
of benzene
Fig. II.4.2.21 Annual average concentrations of benzene in 1999–2006 at
selected stations
Fig. II.4.2.22 Field of annual average concentration of
benzene in the ambient air in 2006
Fig. II.4.2.23 24-hour concentrations at the
stations with the highest annual benzene concentrations in 2006
II.4.2.1.6 Ground-level ozone
Ground-level ozone is a secondary pollutant in the ambient air with no
significant emission source of its own. It is formed under the influence of
solar radiation during complex photochemical reactions mainly between nitrogen
oxides, VOC (mainly hydrocarbons) and other components of the atmosphere. Ozone
is a very powerful oxidizing agent. Ozone impairs mainly the respiratory system
and irritates mucous membranes. It causes morphological, biochemical and
functional changes and impairs the immune system response. There is evidence for
ozone toxicity to vegetation.
The Government Order No. 597/2006 Coll. requires to assess the ozone
concentrations in relation to human health protection as an average for the
latest three years. If the latest three years are not available, the average for
the latest two years or one year is taken into account pursuant to the
Government Order. In 2006 ozone was measured at 73 localities out of which 39
(53 %) exceeded the target value for the three-year period 2004–2006, or shorter
(see Table II.4.2.12). According to this assessment the maximum number of
exceedances was recorded at the locality Churáňov, where the average number of
exceedances of the maximum daily 8-hour running average 120 μg.m-3 reached the
value of 69.3. In comparison with the previous three-year period 2003–2005 there
was a slight decrease of the relative number of stations with target value
exceedances. The map with the 26th highest maximum daily 8-hour running averages
shows clearly the slight reduction of the territory with concentrations above
120 μg.m-3. More than 75 % of stations recorded the decline of the average
number of exceedances above 120 μg.m-3 in the average for the period 2004–2006
as compared with the average for the period 2003–2005. In 2003–2005 the
above-the-limit concentrations of ground-level ozone occurred in 99 % of the
territory of the Czech Republic, in 2004–2006 in 88 %. This was caused by the
fact that the assessment of the latest three-year period (2004–2006) did not
include the year 2003 when there were recorded long-lasting high temperatures
and high values of sun radiation, and the ground-level ozone concentrations
reached extremely high values. The year 2006 was also warm (as compared to the
two previous years), however, its average temperature for the months
April–September, during which ozone concentrations have usually the highest
values, was by 0.7 C lower than in 2003; ozone concentrations were relatively
high.
The ground-level ozone concentrations generally grow with the increasing
altitude which is confirmed also by the data measured for the year 2006 when the
localities with highest loads (see Table II.4.2.12) are situated at higher
altitudes. The traffic localities in the cities are the least loaded ones as
ozone is degraded there through chemical reaction with NO. It can be expected
that the ozone concentrations are below the target value also in other cities
with heavier traffic. However, due to the absence of measurements the probable
decrease cannot be documented by the use of current methods of map construction.
Map diagram in Fig. II.4.2.24 shows the 26th highest value of maximum 8-hour
running average of ozone concentrations (three-year average) in 1996–2006.
Table II.4.2.12 presents the stations with the highest values of maximum daily
8-hour running average ozone concentrations in three-year average. Fig.
II.4.2.26 shows the graph of the number of exceedances of the target value for
ground-level ozone and Fig. II.4.2.27 presents the annual courses of maximum
daily 8-hour running averages in the localities with the heaviest loads.
Table II.4.2.13 presents the number of hours of the ozone alert threshold
exceedance (180 μg.m-3) at selected AIM stations for the whole period of
1992–2006.
Tab. II.4.2.12 Stations with the highest values of maximum daily 8-hour running
average concentrations of ozone
Tab. II.4.2.13 Number of hours of the ozone alert threshold exceedance (180
μg.m-3) per year at selected AIM stations, 1992–2006
Fig. II.4.2.24 26th highest values of maximum 8-hour running average of ground-level
ozone concentrations (three-year average) in 1996–2006 at selected stations
Fig. II.4.2.25 Field of the 26th highest maximum daily 8-hour running average of
ground-level ozone concentration in three-year average, 2004–2006
Fig. II.4.2.26 Numbers of exceedances of the target value for the maximum daily
8-hour running average of ground-level ozone concentrations in three-year
average, 2004–2006
Fig. II.4.2.27 Stations with the highest values of maximum daily 8-hour running
average concentrations of ground-level ozone in 2004–2006
II.4.2.1.7 Heavy
metals
Lead
Most lead contained in the atmosphere result from anthropogenic emissions caused
by high-temperature processes, primarily the burning of fossil fuels, production
of iron and steel and metallurgy of non-ferrous metals. Means of transport using
leaded petrol represent a very significant source of anthropogenic emissions. In
the natural processes lead is released through the weathering of rocks and
volcanic activity [14].
Airborne lead occurs in the form of fine particles with frequency particle size
distribution characterized by the average aerodynamic diameter lower than 1 μm.
The long-term exposure to lead results in harmful impacts on biosynthesis of
haem (nonproteinic component of haemoglobin), on nervous system and blood
pressure in humans. The evidence for carcinogenic potential of lead and its
compounds in humans is inadequate [14, 15].
None of the 70 localities recorded the exceedance of the limit value (500 ng.m-3).
In 2006 the highest concentration was reached in the ZÚ locality Ostrava-Bartovice
(120.8 ng.m-3). Lead concentrations in all localities remained far below the
limit value and did not even reach the lower assessment threshold (see Fig.
II.4.2.28). Courses of short-term average concentrations (24-hour or14-day
concentrations, depending on the measurement schedule of the given station) at
selected stations are presented in Fig. II.4.2.29.
The stations with the highest values of annual average concentrations are
presented in Table II.4.2.14.
Tab. II.4.2.14 Stations with the highest values of annual average concentrations
of lead in the ambient air
Fig. II.4.2.28 Annual average concentrations of lead in the ambient air in
1996–2006 at selected stations
Fig. II.4.2.29 1/14-day average concentrations of lead in the ambient air at
selected stations in 2006
Cadmium
Globally, the anthropogenic sources of cadmium emission in the ambient air
represent about 90 % (mainly iron and steel production, metallurgy of non-ferrous
metals, refuse incineration and fossil fuels combustion (brown coal, hard coal
and heavy fuel oils) [17]. Emissions from transport are less significant. The
remaining 10 % represent natural sources (mainly caused by volcanic activity).
Cadmium is bound mainly to the fine particles (aerodynamic diameter up to 2.5 μm),
with higher risk of negative effects on human health. Almost all cadmium is
bound to particles up to 10 μm, while the minimum amount of cadmium is found in
particles with diameter above 10 μm.
The kidney is the critical organ with respect to long-term exposure to cadmium.
Its carcinogenic effects are evident in experimental animals and there has been
limited evidence in humans so far [15, 17].
In 2006 cadmium was measured at 69 localities which submitted sufficient data
for the calculation of the valid annual average.
The target value (5 ng.m-3) was not exceeded. In the locality Tanvald, where
target value was exceeded repeatedly in the previous years, the necessary number
of valid data for the calculation of the annual average was not reached.
Nevertheless in 3 of 4 months for which the monthly average is available, the
target value was exceeded. In February, the monthly average was more than double
than the target value and in November even more than 3x higher than the target
value. It can be supposed with high probability that if the Tanvald stations
measurement results were usable for the assessment, the target value would be
exceeded again. In 2005 the maximum average annual concentrations were measured
in the Liberec Region (localities Tanvald, Souš, Liberec-Vratislavice), in 2006
the maximum average concentrations were measured in two localities with heavy
loads in Ostrava (Ostrava-Bartovice, Ostrava-Mariánské Hory) which started to
submit the measured data to the ISKO database on 1.1.2006. The target value for
cadmium must be met by 31.12.2012.
The development of annual average concentrations in the period of 1996–2006 is
apparent from Fig. II.4.2.30.
The courses of short-term (24-hour, or 14-day concentrations, according to the
measurement schedule at the respective station) average cadmium concentrations
in selected localities in 2006 are presented in Fig.
II.4.2.32.
The stations with the highest values of annual average concentrations are
presented in Table II.4.2.15.
Tab. II.4.2.15 Stations with the highest values of annual average concentrations
of cadmium in the ambient air
Fig. II.4.2.30 Annual average concentrations of cadmium in the ambient air in
1996–2006 at selected stations
Fig. II.4.2.31 Field of annual average concentration of cadmium in the ambient
air in 2006
Fig. II.4.2.32 1/14-day average concentrations of cadmium in the ambient air at
selected stations in 2006
Arsenic
Arsenic occurs in many forms of inorganic and organic compounds. Anthropogenic
sources represent about three quarters of total emissions in the ambient air.
Significant amounts are contributed mainly from combustion processes (brown
coal, hard coal and heavy fuel oils), iron and steel industry and production of
copper and zinc. Main natural sources of arsenic include mainly volcanic
activity, wildfires, weathering of minerals and activity of microorganisms (in
wetlands, swamps and circumlittoral areas) [17].
Arsenic occurs largely in fine fractions (aerodynamic diameter up to 2.5 μm),
which can be transported over long distances and can penetrate deeply into the
respiratory system. Almost all arsenic is bound to particles with aerodynamic
diameter up to 10 μm [17].
Inorganic arsenic can cause acute, subacute or chronic effects (local or
affecting the whole organism). Lung cancer can be considered the critical effect
following inhalation exposure [15, 17].
Of the total number of 67 localities which submitted sufficient data for the
calculation of the valid annual average for 2006 the target value 6 ng.m-3 was
exceeded in 3 localities (Ostrava-Bartovice [13.5 ng.m-3], Ostrava-Mariánské
Hory [8.6 ng.m-3] a Kladno-Švermov [6.4 ng.m-3]). In previous years data from
these stations were not available. In the locality Tanvald, where the target
value was exceeded repeatedly in the previous years, the necessary number of
valid data for the calculation of annual average was not reached. Nevertheless
in 2 of 4 months, from which the monthly average is available, the target value
was exceeded. The target value for arsenic must be met by 31.12.2012.
The map for arsenic shows an apparent slight deterioration of air pollution
situation (Prague, Central Bohemian Region, Ústí nad Labem Region). More
significant deterioration in the Moravian-Silesian Region can be explained by a
slight increase of concentrations in current localities and by the assessment of
the results of new measurements in areas with heavy loads (localities
Ostrava-Bartovice, Ostrava-Mariánské Hory).
The development of annual average concentrations during the years 1996–2006 is
apparent from Fig. II.4.2.33.
The courses of short-term (24-hour, or 14-day concentrations, according to the
measurement schedule at the respective station) average arsenic concentrations
show the seasonal character of the short-time arsenic concentrations in the
ambient air and confirm the significant arsenic contribution from the burning of
fossil fuels (Fig. II.4.2.35).
The stations with the highest annual average concentrations are presented in
Table II.4.2.16.
Tab. II.4.2.16 Stations with the highest values of annual average concentrations
of arsenic in the ambient air
Fig. II.4.2.33 Annual average concentrations of arsenic in the ambient air in
1996–2006 at selected stations
Fig. II.4.2.34 Field of annual average concentration of arsenic in the ambient
air in 2006
Fig. II.4.2.35 1/14-day average concentrations of arsenic in the ambient air at
selected stations in 2006
Nickel
Nickel is the fifth most abundant element of the earth core, though in the earth
crust its percentage share is lower.
The main anthropogenic sources, which globally represent about three quarters of
total emissions, include combustion of heavy fuel oils, mining of
nickel-containing ores and nickel refinement, waste incineration and iron and
steel production. Main natural sources include continental dust and volcanic
activity.
Nickel occurs in the atmospheric aerosol in several chemical compounds which
differ by its toxicity for human health and ecosystems.
About 70 % of particles containing nickel comprise the fraction smaller than 10
μm. These particles can be transported over long distances. About 30 % of
particles containing nickel have aerodynamic diameter equal or higher than 10 μm
and quickly settle in the vicinity of the source [17].
The health effects include allergic dermatitis and there is evidence of nickel
carcinogenicity for humans [15, 17].
None of the total 63 localities from which sufficient data for the calculation
of the valid annual average for 2006 were obtained, similarly as in previous
years, exceeded the set target value. Nevertheless, in comparison with the
previous year 2005, the maximum annual averages slightly increased. The highest
valid annual average concentration was measured in the locality
Ostrava-Mariánské Hory (annual concentration 10.3 ng.m-3). This was the one and
only case of the lower assessment threshold exceedance. The stations with the
highest values of the annual average concentrations are presented in Table
II.4.2.17.
The annual course of short-term (24-hour, or 14-day) nickel concentrations is
apparent from Fig. II.4.2.37.
Tab. II.4.2.17 Stations with the highest values of annual average concentrations
of nickel in the ambient air
Fig. II.4.2.36 Annual average concentrations of nickel in the ambient air in
1996–2006 at selected stations
Fig. II.4.2.37 1/14-day average concentrations of nickel in the ambient air at
selected stations in 2006
II.4.2.1.8 Benzo(a)pyrene
The cause of the presence of benzo(a)pyrene, the main representative of
polycyclic aromatic hydrocarbons (PAH) in the ambient air is, similarly as in
other PAH, the insufficient burning of fossil fuels both in stationary and
mobile sources, and also some technologies, as coke and iron production.
Stationary sources are represented mainly by local heating (coal combustion).
Mobile sources are represented mainly by diesel motors. The natural background
level of benzo(a)pyrene is almost zero with the exception of wildfires [15].
Approximately 80–100 % of PAH with 5 and more aromatic cores (i.e. also
benzo(a)pyrene) are bound mainly to the particles smaller than 2.5 μm, i.e. to
the so called fine fraction of atmospheric aerosol PM2.5 (sorption on the
surface of the particles). These particles remain in the atmosphere for
relatively long time (days to weeks) which enables their transport over long
distances (hundreds to thousands of kilometers).
Benzo(a)pyrene, as well as several other PAH, are classified as proven human
carcinogens [15, 19].
In 2006 benzo(a)pyrene was monitored in 28 localities, out of which 24 (86 %)
exceeded the target value of 1 ng.m-3 (in 2005 – 85 % of localities, in 2004 –
56 %, in 2003 – 66 %). All localities classified as urban or suburban recorded
the exceedance of the target value, with the exception of two stations at which
the annual average was equal to the target value. Only two rural stations
recorded the annual average concentrations below the target value. This fact
confirmed the suspicion that the target value is exceeded, due to local sources,
also in villages and towns where there is no measurement and which were not
included in air pollution maps in the previous years.
Therefore in 2006 the mapping methods used for the assessment of air pollution
caused by benzo(a)pyrene were markedly improved. Based on the results of
measurements and modelling, the maps for urban and rural areas were created
separately, and then merged into one final map. In addition to the stationary
sources the map regards also traffic emissions, and namely benzo(a)pyrene
emissions from highways and primary roads. It is supposed that the share of
benzo(a)pyrene emissions to total PAH emissions is about 4 %. The map was
created also with regard to the gradient of benzo(a)pyrene air pollution
concentrations with the altitude. Consequently, a number of towns and villages
ended up in the areas with exceeded target value (total 9 % of the territory of
the Czech Republic, in 2005 – only 5.2 %), with about 69 % of the population (in
2005 – 39 % of the population).
However, it is necessary to consider that the estimates of the fields of annual
average benzo(a)pyrene concentrations, in comparison with other mapped
pollutants, bear the greatest uncertainties which result both from insufficient
measurement density and from uncertainties given by dispersion modelling of PAH
emissions; PAH emission inventories represent the largest source of
uncertainties.
The concentration measured in Ostrava-Bartovice (11.7 ng.m-3) was by far the
highest. The level of the target value was exceeded almost 12x.
The target value for benzo(a)pyrene must be met by 31.12.2012.
The development of annual average concentrations in individual localities during
1997–2006 is apparent from Fig. II.4.2.38. The annual course of short-term
concentrations (24-hour once in 3 or 6 days) of benzo(a)pyrene is presented in
Fig. II.4.2.41. The fluctuations of monthly averages of concentrations for
different types of stations in 2004–2006 are shown in Fig.
II.4.2.40. The
increase of concentrations during the winter periods confirm the influence of
local furnaces.
Tab. II.4.2.18 Stations with the highest values of annual average concentrations
of benzo(a)pyrene in the ambient air
Fig. II.4.2.38 Annual average concentrations of benzo(a)pyrene in 1997–2006 at
selected stations
Fig. II.4.2.39 Field of annual average concentration of benzo(a)pyrene in the
ambient air in 2006
Fig. II.4.2.40 Month average concentrations of benzo(a)pyrene at various types
of localities, 2004–2006
Fig. II.4.2.41 24-hour concentrations at the stations with the highest annual
concentrations of benzo(a)pyrene in 2006
II.4.2.1.9 Other substances
Mercury
Main anthropogenic sources of mercury include combustion of fossil fuels, chlor-alkali
production, metallurgy, cement production and refuse incineration. Mercury and
its compounds are used in paint industry, battery production, measuring and
control instruments (thermometers) [18].
The natural sources (representing about 60 % of total emissions) include mainly
mercury evasion from aquatic ecosystems and vegetation, volcanic activity and
de-gassing from mercury-rich minerals. As for anthropogenic emissions it is
estimated that in Europe approximately 60 % of mercury is emitted in the form of
elemental vapour Hg0, 30 % as divalent mercury (Hg (II)), and only 10 % as
particulate phase mercury (H(p)). Most emissions from natural sources are in
gaseous form Hg0 [18].
Studies of occupationally exposed humans have shown adverse effects on the
central nervous system and kidneys at high mercury vapour levels [18]. The
increased concentrations in the ambient air result in higher atmospheric
deposition on top water layers and, consequently, in higher methylmercury
concentrations in freshwater fish and its accumulation in food chains. [15, 18].
In spite of the fact that the limit value for mercury has not been set yet, the
Czech national legislation recommends, pursuant to the European directives, to
carry out its monitoring and assessment according to the annual arithmetic mean.
In 2006 the CHMI ISKO database received data on mercury concentrations from 6
localities in total: from the CHMI locality Ústí nad Labem-město, from the
locality Karviná ZÚ and from 4 ZÚ localities in Ostrava. Only 2 localities
reached the sufficient number of data for the calculation of the valid annual
average, and namely the locality Ostrava-Mariánské Hory (annual average 0.8
ng.m-3) and Ostrava-Bartovice (annual average 1.2 ng.m-3).
Table II.4.2.19 presents the overview of the stations measuring mercury in the
ambient air and the annual average and maximum 24-hour concentrations.
Tab. II.4.2.19 Stations measuring mercury in the ambient air with the values of
annual average and maximum 24-hour concentrations
Ammonia
Major part of ammonia emitted in the ambient air is created by disintegration of
nitrogenous organic materials from domestic animals breeding. The remaining
amount is emitted through combustion processes or production of fertilizers. It
is apparent that ammonia emissions in the ambient air are contributed by
vehicles (formation of ammonia in catalytic convertors). Ammonia has irritating
effects on eyes, skin and respiratory system. Chronic exposure to increased
concentrations can cause headache and vomiting [20]. Quite significant are
ammonia odour annoyance impacts on the population.
Similarly as in the case of mercury, the limit value for ammonia is not defined
in the current European and Czech legislation. Ammonia monitoring was carried
out at 4 localities in 2006. The highest annual average concentration was
measured at the station Lovosice-MÚ (11.1 μg.m-3).
Table II.4.2.20 presents the overview of stations measuring ammonia in the
ambient air and annual average and maximum 24-hour concentrations.
Tab. II.4.2.20 Stations measuring ammonia in the ambient air with the values of
annual average and maximum 24-hour concentrations
II.4.2.1.10 Trends of annual air pollution characteristics of SO2, PM10, NO2,
NOx and O3 for the period 1996–2006
The result concentrations of pollutants in the Czech Republic and
agglomerations, related to the respective years, represent average values from
the stations which measured for the whole monitored period.
Fig. II.4.2.42 shows the trends of SO2, PM10, NO2, NOx and O3 annual air
pollution characteristics in the Czech Republic for the period of 1996–2006. Up
to the year 2000 air pollution caused by SO2, PM10, NO2 and NOx had a decreasing
trend in the whole Czech Republic. In SO2 and PM10 concentrations the decline
was very steep up to the year 1999. In 2001 the decreasing trend was interrupted
in the whole Czech Republic and, on the contrary, a slight increase of SO2, NO2
and NOx concentrations and a significant increase of PM10 concentrations
occurred. In 2004 this increasing trend of air pollution caused by PM10, NO2 and
NOx finished and, on the contrary, certain decrease of these pollutants
concentrations occurred, reaching almost the levels of the year 2001. In 2005
the PM10 and NO2 concentrations returned back to the increasing trend, in PM10
the increase was steeper, beyond the level of the year 2002. This increasing
trend was confirmed in 2006 in NO2 and in annual PM10 concentrations (at urban
stations); more significant increase was recorded in case of one-hour NO2
concentrations – it almost reached the level of the year 1997. On the contrary,
24-hour PM10 concentrations recorded a slight decrease. Between 2003 and 2005 a
slight decrease of SO2 concentrations was observed. In 2006 this trend stopped
and, on the contrary, a slight increase of SO2 concentrations was recorded in
all air pollution characteristics.
In O3 there is an apparent decreasing trend up to 1997. In 1998–2002 the O3
concentrations stagnated. In 2003 there is apparent the increasing trend in
concentrations due to long lasting very high temperatures and high levels of
solar radiation. In 2004 O3 concentrations slightly decreased below the level
from the years 1997–2002, in 2005 they amounted slightly above the level from
1997–2002. In 2006 the concentrations increased again. The year 2006 was the
year with the second highest ozone concentrations (the average of the 26th
highest values of maximum 8-hour running averages from all stations) within the
period 1996–2006, next to the extreme recorded in 2003. The graphs of trends
show apparent higher concentrations at rural localities as compared with the
concentrations from urban and suburban localities, where ozone is removed mainly
by emissions from traffic.
Fig. II.4.2.42 Trends of SO2, PM10, NO2, NOx and O3 annual characteristics in
the Czech Republic, 1996–2006