MERCURY RESEARCH IN EUROPE:
TOWARDS THE PREPARATION OF THE NEW EU AIR QUALITY DIRECTIVE
CNR-Institute
for Atmospheric Pollution, c/o: UNICAL, 87036 Rende, Italy
In
recent years several studies have been done to assess the processes governing
the cycle of atmospheric mercury in the environment including emissions,
transport, chemical and physical transformations and atmospheric deposition to
water and terrestrial receptors. During
the 1980s and 1990s mercury problems have been investigated in the United
States and Canada, North Europe and South America, whereas little attention has
been devoted to assess spatial distributions of atmospheric mercury in the
Mediterranean Sea region where significant mercury concentrations have been
measured in air and water samples as well as in several fishes and types of
food web. However, in the last three
years the EU Directorate General on Research (EU-DG Research) in the frame of
the Environment and Climate Program funded two major research projects on
mercury, namely the “Mediterranean Atmospheric Mercury Cycle System – MAMCS”
and the “Mercury over Europe (MOE)”.
MAMCS is addressed to improve our understanding of all those mechanisms
influencing the dynamics of mercury in the Mediterranean Sea region including
emissions from natural and anthropogenic sources, atmospheric transport and
deposition to water and terrestrial receptors, and chemical and physical
transformations of Hg0 and other Hg species in the atmosphere. The MOE project is addressed to similar
topics but concentrating on the North European region. Several tasks carried out in MAMCS and MOE
have been coordinated (i.e., measurements, emission inventory) in order to
improve the potential of utilisation of the outcomes of both projects.
Mercury emissions (see Figure 1) from coal combustion for electric power generation, cement manufacturing and solid waste disposal through incineration facilities increased since 1983 and are projected to increase during the next two decades if no policy will be implemented to reduce or/and control emissions from major industrial plants (Pirrone et al., 2000).

Figure 1 – Annual emissions (t yr-1) of mercury to the atmosphere in
the Mediterranean Se region from coal combustion, cement manufacturing and
municipal solid waste incineration from 1983 to 2025.
In order to assess the horizontal distribution of elemental mercury and other mercury species over the Mediterranean Sea and in North Europe, four intensive measurements campaigns have been carried in the frame of the MAMCS and MOE projects simultaneously at five sites in the Mediterranean region and at five sites in the North Europe (see Figure 2).

Figure 2 - The measurement sites. 1: Mallorca (39º40’30’’N, 2º41’36’’E), 2:
Calabria (39o25’N, 16o00’E), 3: Sicily (36o40’N, 15o10’E), 4: Turkey (36o28’12”N,
30o20’24”E), 5: Israel (32o40’N, 34o56’E), 6:
Germany (53o08’34”N, 13o02’00”E), 7: Germany (54o26’14”N,
12o43’30”E), 8: Sweden (57o24’48”N, 11o56’06”E),
9: Sweden (58o48’00”N, 17o22’54”E), 10: Ireland (53o20’N,
9o54’W).
The average TGM concentrations varied between
1.6 and 2.4 ng m-3 with no significant
seasonal variations. The relative uniform distribution found for TGM depends
primarily on the relatively stable global/hemispheric background concentration
which only occasionally shows higher values due to long-range transport from
major anthropogenic source in Europe. Except for the first campaign, the
observations indicates that TGM levels were higher in the Mediterranean area
than in North Europe.
Particulate
mercury (TPM) shows more pronounced differences between the Mediterranean
region and North Europe. The RGM
concentrations in the Mediterranean region are also higher than that observed in Northern Europe suggesting that a
pronounced photochemical activity and chemical reactions (i.e., with halogen
radicals) within the marine boundary layer (MBL) may be responsible for these
regional gradients in RGM levels.
However, RGM trends were similar to that observed for TPM and TGM
suggesting that spry formation and bubble ejection that take place at high wind
speeds coupled with exchange mechanisms at the air-water interface (i.e.,
driven by a concentration gradient) may help to explain this behaviour. However, trajectory analysis and source-receptor
modeling coupled with regional scale transport-transformation modeling are
under way and will help to interpret these regional patterns in the horizontal mercury distributions in the
atmosphere.
A
correct evaluation of spatial and temporal evolutions of mercury concentrations
(and all its species) in different environmental compartment (i.e., air, water,
soil) and areas (i.e., industrial, urban, remote) coupled with a detailed
description of chemical and physical processes of elemental mercury and its
species as they interact with other atmospheric contaminants (i.e., O3,
halogen radicals) during different steps involved in the emission, transport
and removal processes is of fundamental importance in assessing the overall
mercury cycle between atmospheric, aquatic and terrestrial compartments on
regional and global scales. An important task carried out in the frame of the
MAMCS project (and in the MOE project as well) is the development of a
comprehensive integrated modeling system for assessing dynamic processes of
atmospheric mercury in the Mediterranean region.
The
MAMCS integrated modeling system is based on two major well known
meteorological-dispersion atmospheric models, the Regional Atmospheric Modeling
System (RAMS) and the SKIRON/ETA meteorological system. The system based on
RAMS is used primarily for assessing specific processes as it provides a
detailed description of microphysics which requires significant computer time,
making it inconvenient for long-term simulations (i.e., 1-2 years). On the other hand, the system based on the
SKIRON/ETA is designed for long-term simulations which are very important for
assessing regional scale mercury budgets for periods of 1-2 years, because it
requires only 50% of the RAMS computer time.
A number of ad-hoc models have
been developed and dynamically coupled to both RAMS and SKIRON systems in order
to account for the following mechanisms/processes: (a) particle dry deposition,
(b) wet scavenging, (c) gas-particle partitioning, (d) chemical transformations
during over-water transport, (e) in-cloud chemistry, and (f) gaseous mercury
exchange at the air-water interface (i.e., Pirrone et al., 1999; Forlano et al.,
2000; Hedgecock et al., 2000; Pirrone
et al., 2000).
Meanwhile, several other initiatives addressed to assess the level of mercury in remote European areas (i.e., Arctic) as well as the fluxes of mercury from natural sources (i.e., seawater, volcanoes) have been carried out in the frame of other research projects funded at national and European level (Ferrara et al., 2000; Sprovieri and Pirrone, 2000). The outcomes of these research activities on different aspects of the mercury cycling in the European ecosystems is of primary interest for the preparation of the new European legislation on air quality. Indeed, current initiatives of the EU Directorate General on Environment are addressed to prepare the Position Paper on atmospheric mercury that will be the basis of the New Framework Directive (FWD) on mercury.
The purposes of this paper is to present the outcomes of the European research on different aspects/mechanisms involved in the mercury cycling on local and regional scales in Europe and its role in supporting the development of the New Air Quality Legislation (FWDs) in Europe.
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