To assess the impact of atmospheric aerosol on the environment, including air quality, ecosystems, human health and climate change, it is necessary to know its concentration, chemical composition and mass size distribution of PM (ambient particulate matter) components [1-8]. Knowledge of the mass size distribution of PM components is helpful in determining mechanisms of aerosol formation, as well as physical and chemical changes, it is subjected to on a given area [9-13].

Besides the obvious and relatively well-recognized relation between the content of various toxic compounds in ambient dust and human health [14-17], another example of a dust chemical composition impact on the environment, is the effect of some water-soluble inorganic compounds on the acidity and conductivity of aerosols. Under certain conditions, the water-soluble sulfur and nitrogen compounds contained in the dust, contribute to acidification of precipitation and/or deposition, whereas the deposition of particles rich in the water-soluble calcium, magnesium, potassium or sodium compounds, increases the alkalinity of the environment [18-21].

Water-soluble ions, next to elemental carbon and organic matter, dominate the mass of PM. In urban areas, mass of sulfates and nitrates associated with particulate matter is even ~80% of all water extracted ions (Table 1, [22]) and ~15% - 50% of the total mass of PM_2.5 (fine particles, with aerodynamic diameters not exceeding 2.5 µm) [23-26].

Sulfates, nitrates and ammonia are used to determine the share of secondary inorganic aerosol (SIA) in the mass of ambient dust. Oxidation of SO₂ in the air, then a binary nucleation of H₂SO₄-H₂O and ternary H₂SO₄- H₂O-NH₃, results in the formation of dust particles, mostly smaller than 1 µm [19,21,27,28]. These particles, together with nitrate (V) ammonium emerging in the analogous reaction of nitric acid (V) with ammonia, form

Table 1. Ambient concentrations of water-soluble ions (ng·m⁻³) related to various PM fractions at various sites in Europe.

the SIA. In the air poor in, sulfuric acid H₂SO₄ can react with mineral dust or sea salt components, generally creating coarse particles of CaSO₄ or (Na)₂SO₄.

The goal of the work was to determine concentration and mass size distribution of eight water-soluble ions (, , , Na⁺, , K⁺, Ca²⁺, Mg²⁺) related to thirteen PM fractions in a typical urban area of southern Poland. Possible chemical composition of secondary inorganic aerosol in 13 dust fractions was also estimated.

The site of experiment (Zabrze, Poland, Figure 1) is located in area representative of the air pollution conditions for the central part of Upper Silesia and it meets the criteria of urban background site (Directive 2008/50/EC). Conditions at this point, characterize well dust concentration in residential areas exposed to municipal and industrial emissions in the Upper Silesia [29].

Samples have been collected from August to December 2008. Fourteen measurements were carried out and each lasted about a week. Dust was collected using a thirteen stage DEKATI low pressure impactor (DLPI) [13].

Masses of dust collected on aluminum substrates, were determined by weighing substrates before and after exposure, on a Mettler Toledo microbalance (accuracy 2 µg). Before weighing the substrates were kept in weighing room for 48 hours (temperature 20˚C ± 2˚C, relative air humidity 48% ± 5%). Concentrations of PM fractions were calculated by dividing each fraction’s mass by the volume of air, from which it was collected. Dust samples were kept in a refrigerator in tight and lightproof containers until the analysis.

Thirteen samples were fixed for chromatography analysis - for each fraction, a collective sample from 14 weeks was prepared. Samples were placed in ROTH extraction containers. For the extraction, 50 cm³ of deionized water was added to each container and the containers were tightly capped to prevent leaking during the extraction. Extracts were then placed in an ultrasonic

bath (60 min), at a temperature not exceeding 15˚C. Then, the extraction containers were placed in a vortex mixer and shaken overnight at about 18˚C and 60 cycles per minute. Extracts were then filtered through a CRONUS microporous filter with a PES membrane with a porosity of 0.2 microns.

The ion content in the extracts was determined using Metrohm ion chromatograph (Metrohm Herisau AG, Switzerland), equipped with 818 IC Pump, 819 IC Detector, 837 IC Eluent Degasser, 830 IC Interface, 820 IC Separation Center, Metrodata 2.3 programme). The method was previously validated on the basis of certified reference material (CRM Fluka products nos. 89316 and 89886, the standard recovery ranged in 92% - 109%). Detection limits were at the level of: 0.02 mg·l⁻¹ for NH₄⁺, 0.05 mg·l⁻¹ for Cl^–, and K⁺, 0.07 mg·l⁻¹ for and Na⁺, 0.12 mg·l⁻¹ for Ca²⁺ and Mg²⁺.

PM-related, , , Na⁺, , K⁺, Ca²⁺, Mg²⁺ concentrations from Zabrze, were compared with concentrations of these ions from various sites in Europe (Table 1). The concentration of the PM₁-related ion was calculated by summing its concentrations in following fractions: 0.03 - 0.06 µm, 0.06 - 0.108 µm, 0.108 - 0.17 µm, 0.17 - 0.26 µm, 0.26 - 0.40 µm, 0.40 - 0.65 µm and 0.65 - 1.0 µm. In the case of ions associated with PM_2.5, additionally concentrations from fractions: 1.0 - 1.6 µm and 1.6 - 2.5 µm were included and in case of PM₁₀, besides previously mentioned, ion concentrations of 2.5 - 4.4 µm; 4.4 - 6.8 µm and 6.8 - 10.0 µm range were summed.

Most of ions’ concentrations in Zabrze were comparable to concentrations noted between 1998-2008 in Europe. For example, concentration of sulfates in particulate matter in Zabrze, was comparable to the concentration recorded at two sites in Switzerland, suburban station in Menen (Belgium) and urban background station in Helsinki (Finland). Generally, higher concentrations than in Zabrze are listed in Asian countries [13,30, 31]. Concentration of Cl⁻ associated with fine dust in Zabrze was extraordinarily high comparing to values recorded in other parts of Europe and similar to concentrations of chlorine in Menen and Melpitz, recorded in these cities during the winter season (Table 1).

Sulfates, nitrates and ammonia associated with PM₁, PM_2.5 and PM₁₀, had the highest concentration of the eight analyzed ions in Zabrze (Tables 1 and 2). Average mass shares of and in the PM_2.5, are about 80% of the total mass (the sum of the masses in all 13 fractions) of sulfates and nitrates, and the average mass share of is even up to 98% of the total mass of ammonia. More than 60% of sulfates and nitrates mass were related to particles with an aerodynamic diameter

Table 2. Ambient concentrations of PM (µg·m⁻³) and PM-related ions (ng·m⁻³) from 13 original DLPI fractions of PM at the urban background site.

a. 1—0.03 - 0.06 µm; 2—0.06 - 0.108 µm; 3—0.108 - 0.17 µm; 4—0.17 - 0.26 µm; 5—0.26 - 0.40 µm; 6—0.40 - 0.65 µm; 7—0.65 - 1.0 µm; 8—1.0 - 1.6 µm; 9—1.6 - 2.5 µm; 10—2.5 - 4.4 µm; 11—4.4 - 6.8 µm; 12—6.8 - 10.0 µm; 13—>10.0 µm; b. below limit of detection.

≤1 μm. As to, it was close to 90%., and concentrations were highest in the range of 0.26 - 1 µm. Very similar, bimodal mass size distribution of and, with a maximum occurring between 0.4 - 1 μm (Figure 2(a)), means that these ions are parts of the same compounds in the dust. The main mechanism of their formation are presumably the transformation processes of PM gaseous precursors occurring in the atmosphere. PM-related had multimodal mass size distribution, with a one maximum occurring in the range of 0.4 - 1 μm and two maxima between 1.6 - 10 μm (Figure 2(b)).

On the areas where sea spray or sea water evaporation (marine aerosols) and road salt are main sources of sodium and chloride, ambient concentrations of Na⁺ and Cl⁻ related to PM_2.5-10 (coarse dust, ambient particles with aerodynamic diameters exceeding 2.5 and not greater than 10 µm) are generally higher than the concentrations of PM₁- and PM_2.5-related Na⁺ and Cl⁻ (Table 1). It is clear that in Zabrze, Na⁺ and Cl⁻ are related mostly with fine dust particles [26,32]. PM_2.5-related Na⁺ and were respectively 80 and 85% of their total concentration in the air of Zabrze. The highest concentrations of PMrelated Na⁺ and, occurred in similar particle sizes range, as in the case of highest, and concentrations (Table 2). Both, Na⁺ and Cl⁻, were characterized by unimodal mass size distribution and its maximum occurred in the range of 0.4 - 1 μm (Figures 2(a) and (b)). This indicates the anthropogenic origin of these ions (combustion processes). It is most likely that Na⁺ and, occur in the dust mainly as a sodium chloride.

The concentration of K⁺, Mg²⁺ and Ca²⁺ associated with each of 13 fractions, did not exceed 53 ng·m⁻³ (Table 1). Masses of these cations were distributed differently among PM fractions. More than 95% of the total mass of K⁺ was concentrated in the PM_2.5, over 25% of which were PM_0.26-0.4 and PM_0.4-0.65. Distribution of Ca²⁺ and Mg²⁺ masses among 13 fractions was more variable, although the share of PM_2.5-10-related ions’ mass, was much bigger than their contribution in the fine dust particles amount, and was more than 50% of total mass of these ions in the Zabrze air.

Potassium and calcium were characterized by unimodal mass distribution with a maximum—as in the case of , Na⁺ and Cl⁻—in the range of 0.26 - 0.65 μm (Figure 1(b)), whereas magnesium was determined with multimodal size mass distribution, without clearly dominant maximum. Highest potassium concentrations occurred for particles in the range of 0.17 - 1 μm (Table 2). However, higher Mg²⁺ and Ca²⁺ concentrations occurred for particles with an aerodynamic diameter larger than 2.5 μm. Therefore, it seems that K⁺ and Ca²⁺ may be present in the compounds with, , Na⁺ and Cl⁻ ions, and their most probable source in Zabrze air are combustion processes. Relatively high proportion of Mg²⁺ in the coarse fraction of particulate matter, proves that mechanical processes, including re-suspension of the soil and road dust could have had an influence on these ions concentration levels.

To assess the neutralizing capacity of occurring simultaneously in the air sulfates and nitrates by ammonium ion, neutralizing ratio (NR) was calculated for each fraction of particulate matter. NR is the ratio of concentration (in normal equivalent, neq·m⁻³) and the sum of and concentrations (in neq·m⁻³)— Table 3.

For particles not greater than 1.6 µm, NR values ranged from ≈ 1 (PM_0.65-1, PM _0.17-0.26, PM_0.108-0.17 and PM_0.06-0.108) to 1.82 (PM_0.26-0.4). It means that the amount of related to these dust fractions, was sufficient to neutralize sulfuric and nitric acid completely. This result also proves that ambient fine dust (PM_1.6) in Zabrze is alkaline (NR ≥ 1).

Stoichiometric ratio for (NH₄)₂SO₄ of is 2.67. In all fractions of particles ≤ 1.6 µm, the ratio of and (in neq·m⁻³) is much lower than 2.67. It confirms the previous deduction, that PM_1.6-related

in Zabrze occurred in a greater amount than needed to react with the PM_1.6-related completely. Also the condition (in neq·m⁻³) is satisfied. Therefore, the concentration of (NH₄)₂SO₄  may be estimated from the formula:

The concentration of (NH₄)₂SO₄ associated with particles ≤ 1.6 µm, fit within the limits of 615.31 ng·m⁻³ (PM_0.4-0.65) to 46.88 ng·m⁻³ for PM_0.03-0.06. The amount (concentration) of, remaining after reaction with (ammonium ion excess) and ammonium nitrate concentration associated with each fractions of particles ≤ 1.6 µm, was calculated from the following formulas:

Table 3. Proportions of the ionic equivalent concentrations and probable composition of secondary inorganic aerosol in 13 original DLPI fractions of PM at the urban background site in Zabrze, Poland.

NH₄NO₃ concentration ranged from 753.38 ng·m⁻³ (for PM_1-1.6) to 81.52 ng·m⁻³ (for PM_0.108-0.17).

(NH₄)₂SO₄ and NH₄NO₃ concentrations sum share, in a total SIA concentration for fractions of particles ≤ 1.6 µm, is shown in Table 3. For the fraction with ((NH₄)₂SO₄+NH₄NO₃)/SIA value exceeding 1, the share is overestimated. Still, stoichiometric calculations that have been carried out, show that these two compounds constitute the entirety of SIA in ambient particles not greater than 1.6 µm. The most probable distribution of (NH₄)₂SO₄ and NH₄NO₃ concentrations between the sum of these compounds concentrations were obtained for PM_0.65-1 and PM_0.4-0.65, where the share of ((NH₄)₂SO₄ + NH₄NO₃) in the SIA did not exceed 100%. There are also these two fractions, in which the predominant part in the SIA takes ammonium sulfate, while the concentrations of these two dust fractions in the air are the highest of all 13 (Table 2).

NR for particles greater than 1.6 µm, was much smaller than 1 (Table 3). However, it doesn’t mean that ions associated with these particles are not fully neutralized. The concentration sum ratio of anions to cations (Σ_cations/Σ_anions, in neq·m⁻³) is in the range of 1, for all fractions.

In all fractions of particles greater than 1.6 µm, the concentration ratios of and (in neq·m⁻³) is considerably higher than 2.67. Also the relation is satisfied (concentrations in neq·m⁻³). It means that in these PM fractions, could neutralize some part of, forming (NH₄)₂SO₄  but there was not enough of to react the whole. Thus, there was not enough of to form ammonium nitrate. Therefore, the (NH₄)₂SO₄ concentration for particles greater than 1.6 µm, can be calculated from the for mula:

The concentration of (NH₄)₂SO₄ associated with particles greater than 1.6 µm, ranged from 3.67 ng·m⁻³ (PM_4.4-6.8) to 43.34 ng·m⁻³ for PM_1.6-2.5.

It is impossible to determine precisely concentrations of all compounds constituting the secondary inorganic aerosol in Zabrze, still, estimating on the basis of stoichiometric relations. However, it can be shown that the amount of in the particles greater than 1.6 µm is enough to react the whole.

The rest of the (sulfate ion excess) could react i.a. with potassium and calcium ions, forming K₂SO₄ and CaSO₄. This would prove specific, similar to, mass size distributions of K⁺, Ca²⁺ (Figures 2(a) and (b)). The concentration of the rest of, that remained after:

• reaction with NH₄⁺ forming (NH₄)₂SO₄; • reaction with forming (NH₄)₂SO₄ and K⁺ forming K₂SO₄;• reaction with forming (NH₄)₂SO₄, K⁺ forming K₂SO₄ and Ca²⁺ forming CaSO₄;

can be calculated (in PM_1.6-2.5, PM_2.5-4.4, PM_4.4-6.8, PM_6.8-10, PM_>10) from the following formula:

Using values listed in Table 3, it can be concluded that for PM_>1.6, there was not enough sulfate ion to complete reaction of calcium ions.

Therefore, it can be concluded, that the secondary inorganic aerosol in Zabrze, in the case of compounds occuring in particles greater than 1.6 µm, is mainly composed of ammonium sulfate, potassium sulfate and calcium sulfate. Certainly, there are also nitrates in these particles, however, in contrast to particles not greater than 1.6 µm, there is no ammonium nitrate but probably NaNO₃ and/or Ca(NO₃)₂.

Most of ions’ concentrations in Zabrze were comparable to concentrations presented in the literature. Generally, higher concentrations than in Zabrze are listed in Asian countries, this concerns particularly to, , K⁺, Mg²⁺ and Ca²⁺ . Concentration of associated with fine dust in Zabrze was extraordinarily high, comparing to values recorded in other parts of the world.

Sulfates, nitrates and ammonium had the highest concentration of the eight analyzed ions in Zabrze. More than 60% of and and 90% of mass, was concentrated in particles with an aerodynamic diameter ≤ 1 micron. Na⁺ and Cl⁻ were also mostly associated with fine dust particles. Ions mentioned above, as well as K⁺ and Ca²⁺, had similar mass size distributions, and generally, maxima of these distributions were in the same particle size ranges. This indicates the anthropogenic origin of seven of eight analyzed ions (combustion processes), associated with dust in Zabrze.

Relatively high proportion of Mg²⁺ in the coarse fraction of particulate matter, proves that mechanical processes, including re-suspension of the soil and road dust could have had an influence on Mg²⁺ concentration in the air.

In particles not greater than 1.6 µm, the amount of ammonium ion is sufficient to neutralize sulfuric and nitric acid, therefore, in dust precursors gas conversions, ammonium sulfate and nitrate are formed. In fractions of particles greater than 1.6 μm, the amount of ammonium ion is not sufficient to neutralize the nitric acid. Therefore, in these fractions, inorganic aerosol is composed of ammonium sulfate and other compounds, including K₂SO₄ and CaSO₄, and also NaNO₃ and/or Ca(NO₃)₂.

The work was partially supported by grant No. N N523 564038 from the Polish Ministry of Science and Higher Education.