Air-quality modelling in the Lake Baikal region.

In this paper, we assess the status of the air quality in the Lake Baikal region which is strongly influenced by the presence of anthropogenic pollution sources. We combined the local data, with global databases, remote sensing imagery and modelling tools. This approach allows to inventorise the air-polluting sources and to quantify the air-quality concentration levels in the Lake Baikal region to a reasonable level, despite the fact that local data are scarcely available. In the simulations, we focus on the month of July 2003, as for this period, validation data are available for a number of ground-based measurement stations within the Lake Baikal region.

Optimization of the ion chromatographic quantification of airborne fluoride, acetate and formate in the Metropolitan Museum of Art, New York.

Ion chromatographic (IC) methods have been compared in order to achieve an optimal separation of fluoride, acetate and formate under various elution conditions on two formerly introduced analytical columns (i and ii) and a novel one (iii): (i) an IonPac AS14 (250 mm × 4 mm I.D.), (ii) Allsep A-2 (150 mm × 4.6mm I.D.), and (iii) an IC SI-50 4E (250 mm (length) × 4mm (internal diameter - I.D.)). The IC conditions for the separation of the anions concerned were optimized on the IC SI-50 4E column. A near baseline separation of these anions was attained on the IonPac AS14, whereas the peaks of fluoride and acetate could not be resolved on the Allsep A-2. A baseline separation for the three anions was achieved on the IC SI-50 4E column, when applying an eluent mixture of 3.2 mmol/L Na(2)CO(3) and 1.0 mmol/L NaHCO(3) with a flow rate of 1.0 mL/min. The highest precision of 1.7, 3.0 and 2.8% and the best limits of detection (LODs) of 0.014, 0.22 and 0.17 mg/L for fluoride, acetate and formate, respectively, were obtained with the IC SI-50 4E column. Hence, this column was applied for the determination of the acetic and formic acid contents of air samples taken by means of passive gaseous sampling at the Metropolitan Museum of Art in New York, USA. Atmospheric concentrations of acetic and formic acid up to 1050 and 450 µg/m(3), respectively, were found in non-aerated showcases of the museum. In galleries and outdoors, rather low levels of acetic and formic acid were detected with average concentrations of 50 and 10 µg/m(3), respectively. The LOD data of acetate and formate on the IC SI-50 4E column correspond to around 0.5 µg/m(3) for both acetic and formic acid in air samples.

Appraisal of measurement methods, chemical composition and sources of fine atmospheric particles over six different areas of Northern Belgium.

Daily and seasonal variation in the total elemental, organic carbon (OC) and elemental carbon (EC) content and mass of PM(2.5) were studied at industrial, urban, suburban and agricultural/rural areas. Continuous (optical Dustscan, standard tapered element oscillating micro-balance (TEOM), TEOM with filter dynamics measurement system), semi-continuous (Partisol filter-sampling) and non-continuous (Dekati-impactor sampling and gravimetry) methods of PM(2.5) mass monitoring were critically evaluated. The average elemental fraction accounted for 2-6% of the PM(2.5) mass measured by gravimetry. Metals, like K, Mn, Fe, Cu, Zn and Pb were strongly inter-correlated, also frequently with non-metallic elements (P, S, Cl and/or Br) and EC/OC. A high OC/EC ratio (2-9) was generally observed. The total carbon content of PM(2.5) ranged between 3 and 77% (averages: 12-32%), peaking near industrial/heavy trafficked sites. Principal component analysis identified heavy oil burning, ferrous/non-ferrous industry and vehicular emissions as the main sources of metal pollution.

Single-run ion chromatographic separation of inorganic and low-molecular-mass organic anions under isocratic elution: application to environmental samples.

For the isocratic ion chromatography (IC) separation of low-molecular-mass organic acids and inorganic anions three different anion-exchange columns were studied: IonPac AS14 (9 microm particle size), Allsep A-2 (7 microm particle size), and IC SI-50 4E (5 microm particle size). A complete baseline separation for all analyzed anions (i.e., F(-), acetate, formate, Cl(-), NO(2)(-), Br(-), NO(3)(-), HPO(4)(2-) and SO(4)(2-)) in one analytical cycle of shorter than 17 min was achieved on the IC SI-50 4E column, using an eluent mixture of 3.2mM Na(2)CO(3) and 1.0mM NaHCO(3) with a flow rate of 1.0 mL min(-1). On the IonPac AS14 column, it was possible to separate acetate from inorganic anions in one run (i.e., less than 9 min), but not formate, under the following conditions: 3.5mM Na(2)CO(3) plus 1.0mM NaHCO(3) with a flow rate of 1.2 mL min(-1). Therefore, it was necessary to adapt a second run with a 2.0mM Na(2)B(4)O(7) solution as an eluent under a flow rate of 0.8 mL min(-1) for the separation of organic ions, which considerably enlarged the analysis time. For the Allsep A-2 column, using an eluent mixture of 1.2mM Na(2)CO(3) plus 1.5mM NaHCO(3) with a flow rate of 1.6 mL min(-1), it was possible to separate almost all anions in one run within 25 min, except the fluoride-acetate critical pair. A Certified Multianion Standard Solution PRIMUS for IC was used for the validation of the analytical methods. The lowest RSDs (less than 1%) and the best LODs (0.02, 0.2, 0.16, 0.11, 0.06, 0.05, 0.04, 0.14 and 0.09 mg L(-1) for F(-), Ac(-), For(-), Cl(-), NO(2)(-), Br(-), NO(3)(-), HPO(4)(2-) and SO(4)(2-), respectively) were achieved using the IC SI-50 4E column. This column was applied for the separation of concerned ions in environmental precipitation samples such as snow, hail and rainwater.

Efficient separation of acetate and formate by ion chromatography: application to air samples in a cultural heritage environment.

A method for the separation of acetate and formate anions by ion chromatography has been optimized under various measurement conditions (e.g. the composition of the mobile phase, and the flow rate of the eluent). For this purpose, two different analytical columns were examined: the IonPac AS14 (250 mm x 4 mm i.d.; designed mostly for the separation of inorganic anions) and the Allsep A-2 (150 mm x 4.6 mm i.d.; designed for the separation of low-molecular mass organic acids). However, nearly baseline separation of acetate and formate has been found on each column using the following conditions: (i) IonPac AS14 column and 2.0 mM Na2B4O7 solution as an eluent with a flow rate of 1.0 ml/min, or (ii) Allsep A-2 column and an eluent containing a mixture of 1.2 mM Na2CO3 plus 1.5 mM NaHCO3 with a flow rate of 1.3 ml/min. Additionally, the separation of fluoride from acetate and formate on both columns was studied. On the IonPac AS14 column it was possible to separate all three investigated anions. However, on the Allsep A-2 column, when the concentration of fluoride was comparable to, or higher than acetate, it was impossible to achieve good separation of these two anions, even using the optimized elution procedure. Therefore, the measurements of real samples were carried out with the use of IonPac AS14 column. The concentrations of acetate and formate have been determined in the air samples of the Cathedral of Cologne (Germany), after sampling the corresponding acids by passive diffusion tubes. Average concentrations of 122 and 9 microg/m(3) for acetic and formic acids were found, respectively, inside the Cathedral and in a depot with medieval stained glass panels.

Mass and ionic composition of atmospheric fine particles over Belgium and their relation with gaseous air pollutants.

Mass, major ionic components (MICs) of PM2.5, and related gaseous pollutants (SO2, NO(x), NH3, HNO2, and HNO3) were monitored over six locations of different anthropogenic influence (industrial, urban, suburban, and rural) in Belgium. SO4(2-), NO3-, NH4+, and Na+ were the primary ions of PM2.5 with averages diurnal concentrations ranging from 0.4-4.5, 0.3-7.6, 0.9-4.9, and 0.4-1.2 microg m(-3), respectively. MICs formed 39% of PM2.5 on an average, but it could reach up to 80-98%. The SO2, NO, NO2, HNO2, and HNO3 levels showed high seasonal and site-specific fluctuations. The NH3 levels were similar over all the sites (2-6 microg m(-3)), indicating its relation to the evenly distributed animal husbandry activities. The sulfur and nitrogen oxidation ratios for PM2.5 point towards a low-to-moderate formation of secondary sulfate and nitrate aerosols over five cities/towns, but their fairly intensive formation over the rural Wingene. Cluster analysis revealed the association of three groups of compounds in PM2.5: (i) NH4NO3, KNO3; (ii) Na2SO4; and (iii) MgCl2, CaCl2, MgF2, CaF2, corresponding to anthropogenic, sea-salt, and mixed (sea-salt + anthropogenic) aerosols, respectively. The neutralization and cation-to-anion ratios indicate that MICs of PM2.5 appeared mostly as (NH4)2SO4 and NH4NO3 salts. Sea-salt input was maximal during winter reaching up to 12% of PM2.5. The overall average Cl-loss for sea-salt particles of PM2.5 at the six sites varied between 69 and 96% with an average of 87%. Principal component analysis revealed vehicular emission, coal/wood burning and animal farming as the dominating sources for the ionic components of PM2.5.

Elemental and ionic concentrations in the urban aerosol in Antwerp, Belgium.

The results of a study of the elemental and ionic composition of the ambient aerosol in and around Antwerp are presented. Four sampling campaigns were performed, covering all seasons. The samples were obtained by filtration and impaction methods. Subsequently, the filters were analyzed by X-ray fluorescence spectrometry for elements, and the impactor substrates were leached with water and analyzed by ion chromatography for ions. When comparing the results of the chemical analysis with the meteorological information, it was found that the concentration of certain elements and ions in aerosol samples was affected considerably by the location of the sampling site and by the meteorological conditions. In relatively less polluted places like small towns and rural regions around Antwerp, the concentrations of some elements and ions showed qualitatively a positive or negative correlation in their time variations with the amount of precipitation. Hence, we suppose that in the first case these elements and ions are contained mainly in the more hygroscopic fraction (the most apparent is the behavior of Na and Cl), and that in the second case, the elements are mainly present in the less hygroscopic fraction of the ambient aerosol. However, this behavior of the elements and ions may be different for various particle size ranges. In the highly urbanized and industrial sites close to the central and industrial parts of Antwerp, these correlations were not found. This could be connected with the high and variable local aerosol generation rate, when only heavy rains are able to provide a sufficient removal of the aerosols from the atmosphere.