Estimation of night-time N2O5 concentrations from ambient NO2 and NO3 radical concentrations and the role of N2O5 in night-time chemistry

Dinitrogen pentoxide (N₂O₅), which is present in equilibrium with NO₃ radicals and NO₂, has been recognized for some time as an intermediate in the NO_x chemistry of night-time atmospheres. However, until the advent of long pathlength spectroscopic techniques for the measurement of atmospheric NO₃ radical concentrations, no reliable method for estimating N₂O₅ concentrations has been available. We have calculated maximum night-time N₂O₅ concentrations from the available experimentally determined concentrations of the NO₃ radical and NO₂ in the U.S. and Germany, and find that N₂O₅ concentrations as high as ~ 15 ppb can occur. We have also estimated removal rates for N₂O₅ and for NO₃ radicals during these nights. From data obtained under conditions devoid of point sources of NO_x, upper limit estimates of the homogeneous rate constant for the reaction of N₂O₅ with water vapor are obtained, leading to the conclusion that the homogeneous gas phase rate constant for this reaction is ⩽ 1 × 10⁻²¹ cm³ molecule⁻¹ s⁻¹ at 298 K, consistent with recent environmental chamber data.     

Determination of 2-nitrofluoranthene and 2-nitropyrene in ambient particulate organic matter: Evidence for atmospheric reactions

We have identified and quantified 2-nitrofluoranthene (2-NO₂-FL) and 2-nitropyrene (2-NO₂-PY), both strong, direct mutagens in paniculate organic matter (POM) samples collected in polluted ambient air in southern California. Samples were collected during four consecutive 6-h periods on 18–19 September 1984, during which the ambient concentrations of gaseous co-pollutants were characterized by long pathlength spectroscopic techniques and conventional analyzers. Concentrations ranged up to 0.3 ng m⁻³ for 2-NO₂-FL and 0.02 ng m⁻³ for 2-NO₂-PY. The 2-nitro isomers of fluoranthene and pyrene have not been observed in direct emissions of POM (e.g. diesel exhaust and wood smoke). However, we recently observed these isomers from laboratory reactions involving N₂O₅ or OH radicals and the parent compounds. Thus the identification of 2-NO₂-FL and 2-NO₂-PY in ambient POM suggests that chemical transformations of fluoranthene and pyrene may take place in polluted atmospheres.     

Nitration of gaseous polycyclic aromatic hydrocarbons in simulated and ambient urban atmospheres: A source of mutagenic nitroarenes

Recent results from field studies in the Los Angeles air basin which focused on the nature and concentrations of mononitroarenes in the gaseous and particulate states in polluted ambient air are reviewed. Relative concentrations in organic extracts of ambient particulate polycyclic organic matter (POM) were found to be, in decreasing order, 2-NO₂-fluoranthene > 1-NO₂-pyrene ≳ 2-NO₂-pyrene; this is in sharp contrast to primary emissions of diesel soot, where 1-NO₂-PY > 3-NO₂-FL > 8-NO₂-FL. Since light and heavy duty diesel motor vehicle emissions are a significant source of sub-μm particles in the Los Angeles area, the relatively high abundance of 2-NO₂-FL suggests that a significant fraction of the 2-NO₂-FL in southern California may be formed via atmospheric reactions. In a wintertime 1986 study of a high-NO_x episode ~ 20 km east of the Los Angeles International Airport, high concentrations of 1- and 2-nitronaphthalenes, much of which could have been in the gaseous state, were collected on a polyurethane backup ‘plug,’ along with lesser amounts of 2-NO₂-FL (and 1- and 2-NO₂-PY) adsorbed on the particles collected by a Hi-vol prefilter.Two gas phase mechanisms are proposed for the formation of adsorbed 2-NO₂-fluoranthene and gaseous 2-NO₂-naphthalene in urban air

• 1.(a) during daylight, attack on gaseous FL by OH radicals followed by NO₂ addition, loss of H₂O and condensation of 2-NO₂-FL on particle surfaces
• 2.(b) reaction with N₂O₅ at night under ambient conditions during which the gaseous NO₃ radical and NO₂ are present, in equilibrium with N₂O₅. Chamber experiments with simulated polluted atmospheres support both of these mechanisms for the formation of 2-NO₂-FL and 2-NO₂-naphthalene; only the OH mechanism seems valid for 2-NO₂-PY. Environmental and health implications of these studies are briefly discussed.

     

Reactions of adsorbed pyrene and perylene with gaseous N2O5 under simulated atmospheric conditions

We report here results of studies concerning the reactions of two representative polycyclic aromatic hydrocarbons (PAH), pyrene and perylene, adsorbed on glass fiber filters, towards gaseous N₂O₅, NO₃ radicals, NO₂ and HNO₃ at part-per-million or lower concentrations and at ⩽ 5% relative humidity. These exposures were carried out in a passive mode in an ~ 6400-ℓ all-Teflon environmental chamber. As is the case for naphthalene vapor, neither adsorbed pyrene nor perylene reacted to any observable extent with the NO₃ radical. However, pyrene reacted rapidly with N₂O₃ to form 1-nitropyrene (1-NP) with a 60–70% yield after 50 min exposure to an initial N₂O₅ concentration of 1.5 ppm. Under these conditions, no reaction of perylene with N₂O₅ was observed. In control runs of the same duration, neither pyrene nor perylene reacted significantly ( < 0.5%) with 1.7 ppm of gaseous HNO₃ but, consistent with earlier studies, a ~ 3% yield of 3-nitroperylene (and < 0.5 % 1-NP) was formed when they were exposed to a mixture of 0.5 ppm NO₂ + 0.35 ppm HNO₃. These data show for the first time that gas phase N₂O₅ can be a strong nitrating agent for adsorbed pyrene to produce 1-nitropyrene, a powerful bacterial mutagen. Clearly, uncertainties occur in extrapolating our laboratory data to ambient atmospheres. However, when our results are combined with estimated N₂O₅ concentrations of up to ~ 15 ppb in polluted night-time atmospheres, they suggest that nitro-PAH, could be formed at significant rates in ambient air.     

Modeling the formation,decay, and partitioning of semivolatile nitro-polycyclic aromatic hydrocarbons (nitronaphthalenes) in the atmosphere

A nitronaphthalene kinetics mechanism has been implemented and added to the photochemical smog mechanism, Carbon Bond-4. This mechanism was used to simulate the formation, decay, and partitioning of 1- and 2-nitronaphthalene and compare it to outdoor smog chamber data. The results suggest that these types of mechanisms can be used to model nitronaphthalene formation and decay in regional airmasses. The partitioning experiments were conducted at night. The sampling system consisted of two Teflon impregnated glass fiber filters followed by a gas-phase denuder. Evidence is provided that partitioning equilibrium is maintained even when the gas-phase components are decaying rapidly under sunlight. The photolysis rate constants were determined relative to k_NO2 to be 0.07×k_NO2 and 0.005×k_NO2 for 1- and 2-nitronaphthalene, respectively. Our results confirm that gas-phase photolysis is the major degradation pathway for 1-nitronaphthalene, whereas for 2-nitronaphthalene other pathways may also be important. The photochemical formation of nitronaphthalenes was studied using a mixture of naphthalene, propylene, NO_x, and diesel particles. 2-nitronaphthalene was observed to build up to higher levels than 1-nitronaphthalene, as the photodegradation of the latter was faster. Additionally, as a part of this study 1-nitronaphthalene has been identified and quantified in diesel exhaust.     

Kinetics of the gas-phase reactions of alkylnaphthalenes with O3, N2O5 and OH radicals at 298 ± 2 K

Rate constants for the gas-phase reactions of the OH radical with 1-methylnaphthalene and of N₂O₅ with 1- and 2-methylnaphthalene and 2,3-dimethylnaphthalene have been determined at 298 ± 2 K by use of relative rate techniques. The rate constants determined were: for the reaction of OH radicals with 1-methylnaphthalene, (5.30 ± 0.48) × 10⁻¹¹ cm³ molecule⁻¹ s⁻¹; for the reaction of N₂O₅ with 1-methylnaphthalene, 2-methylnaphthalene and 2,3-dimethylnaphthalene, (3.3 ± 0.7) × 10⁻¹⁷, (4.2 ± 0.9) × 10⁻¹⁷ and (5.7 ± 1.9) × 10⁻¹⁷ cm³ molecule⁻¹ s⁻¹, respectively. In addition, an upper limit to the rate constant of 1.3 × 10⁻¹⁹ cm³ molecule⁻¹ s⁻¹ was measured for the reaction of O₃ with 1-methylnaphthalene at 298 ± 2 K. These data, when combined with data from previous literature, allow the atmospheric gas-phase removal processes of these alkylnaphthalenes to be quantified.     

Atmospheric chemistry of 1-methyl-2-pyrrolidinone

Rate constants for the atmospheric reactions of 1-methyl-2-pyrrolidinone with OH radicals, NO₃ radicals and O₃ have been measured at 296±2 K and atmospheric pressure of air, and the products of the OH radical and NO₃ radical reactions investigated. Using relative rate techniques, rate constants for the gas-phase reactions of OH and NO₃ radicals with 1-methyl-2-pyrrolidinone of (2.15±0.36)×10^-11 cm³ molecule^-1 s^-1 and (1.26±0.40)×10^-13 cm³ molecule^-1 s^-1, respectively, were measured, where the indicated errors include the estimated overall uncertainties in the rate constants for the reference compounds. An upper limit to the rate constant for the O₃ reaction of <1×10^-19 cm³ molecule^-1 s^-1 was also determined. These kinetic data lead to a calculated tropospheric lifetime of 1-methyl-2-pyrrolidinone of a few hours, with both the daytime OH radical reaction and the nighttime NO₃ radical reaction being important loss processes. Products of the OH radical and NO₃ radical reactions were analyzed by gas chromatography with flame ionization detection and combined gas chromatography–mass spectrometry. N-methylsuccinimide and (tentatively) 1-formyl-2-pyrrolidinone were identified as products of both of these reactions. The measured formation yields of N-methylsuccinimide and 1-formyl-2-pyrrolidinone were 44±12% and 41±12%, respectively, from the OH radical reaction and 59±16% and ∼4%, respectively, from the NO₃ radical reaction. Reaction mechanisms consistent with formation of these products are presented.     

Night-time tropospheric chemistry of the unsaturated alcohols (Z)-pent-2-en-1-ol and pent-1-en-3-ol: Kinetic studies of reactions of NO3 and N2O5 with stress-induced plant emissions

The night-time tropospheric chemistry of two stress-induced volatile organic compounds (VOCs), (Z)-pent-2-en-1-ol and pent-1-en-3-ol, has been studied at room temperature. Rate coefficients for reactions of the nitrate radical (NO₃) with these pentenols were measured using the discharge-flow technique. Because of the relatively low volatility of these compounds, we employed off-axis continuous-wave cavity-enhanced absorption spectroscopy for detection of NO₃ in order to be able to work in pseudo first-order conditions with the pentenols in large excess over NO₃. The rate coefficients were determined to be (1.53±0.23)×10⁻¹³ and (1.39±0.19)×10⁻¹⁴ cm³ molecule⁻¹ s⁻¹ for reactions of NO₃ with (Z)-pent-2-en-1-ol and pent-1-en-3-ol. An attempt to study the kinetics of these reactions with a relative-rate technique, using N₂O₅ as source of NO₃ resulted in significantly higher apparent rate coefficients. Performing relative-rate experiments in known excesses of NO₂ allowed us to determine the rate coefficients for the N₂O₅ reactions to be (5.0±2.8)×10⁻¹⁹ cm³ molecule⁻¹ s⁻¹ for (Z)-pent-2-en-1-ol, and (9.1±5.8)×10⁻¹⁹ cm³ molecule⁻¹ s⁻¹ for pent-1-en-3-ol. We show that these relatively slow reactions can indeed interfere with rate determinations in conventional relative-rate experiments.     

Simulation of trace species production by lightning and corona discharge in moist air

Numerical simulations of chemical processes initiated in moist air by lightning strokes and lightning coronas indicate that the amounts of major new species generated are not very different from the amounts previously found in dry air. Thus, the major new species produced globally in moist air are estimated to be: 2.4 megatonnes NO y⁻¹, 0.28 megatonnes NO₂ y⁻¹ and 220 tonnes N₂O y⁻¹. The minor species, ozone and those containing hydrogen released by lightning from water in moist air are: 1.2 kilotonnes O₃ y⁻¹, 25 kilotonnes HNO₂ y⁻¹, 1.2 kilotonnes HNO₃ y⁻¹, 0.32 kilotonnes H₂O₂ y⁻¹ and 0.32 kilotonnes HO₂ y⁻¹.     

FT-IR kinetic and product study of the Br-radical initiated oxidation of α, β-unsaturated organic carbonyl compounds

Using the relative kinetic technique the kinetics of the gas-phase reactions of Br radicals with acrolein, methacrolein and methylvinyl ketone have been investigated at (301±3) K in 1013 mbar of (N₂+O₂) bath gas at varying proportions. In 1013 mbar of synthetic air the following rate coefficients have been obtained (in units of cm³ molecule⁻¹ s⁻¹): acrolein (3.21±0.11)×10⁻¹²; methacrolein (2.33±0.08)×10⁻¹¹; methyl vinyl ketone (1.87±0.06)×10⁻¹¹. This study represents the first determination of the rate coefficients for these compounds. As for other unsaturated hydrocarbons the rate coefficient with Br was found to increase with increasing partial pressure of O₂. From the product studies of the reactions it has been established that addition of Br radicals to the terminal C-atom is the major pathway in all three cases. However, for acrolein H atom abstraction from the -CO–H group is also significant. Mechanisms are proposed to explain the observed products, mainly β-brominated carbonyl compounds.     

The air pollution caused by the burning of fireworks during the lantern festival in Beijing

The effects of the burning of fireworks on air quality in Beijing was firstly assessed from the ambient concentrations of various air pollutants (SO₂, NO₂, PM_2.5, PM₁₀ and chemical components in the particles) during the lantern festival in 2006. Eighteen ions, 20 elements, and black carbon were measured in PM_2.5 and PM₁₀, and the levels of organic carbon could be well estimated from the concentrations of dicarboxylic acids. Primary components of Ba, K, Sr, Cl⁻, Pb, Mg and secondary components of C₅H₆O₄²⁻, C₃H₂O₄²⁻, C₂O₄²⁻, C₄H₄O₄²⁻, SO₄²⁻, NO₃⁻ were over five times higher in the lantern days than in the normal days. The firework particles were acidic and of inorganic matter mostly with less amounts of secondary components. Primary aerosols from the burning of fireworks were mainly in the fine mode, while secondary formation of acidic anions mainly took place on the coarse particles. Nitrate was mainly formed through homogeneous gas-phase reactions of NO₂, while sulfate was largely from heterogeneous catalytic transformations of SO₂. Fe could catalyze the formation of nitrate through the reaction of α-Fe₂O₃ with HNO₃, while in the formation of sulfate, Fe is not only the catalyst, but also the oxidant. A simple method using the concentration of potassium and a modified method using the ratio of Mg/Al have been developed to quantify the source contribution of fireworks. It was found that over 90% of the total mineral aerosol and 98% of Pb, 43% of total carbon, 28% of Zn, 8% of NO₃⁻, and 3% of SO₄²⁻ in PM_2.5 were from the emissions of fireworks on the lantern night.     

Photo-Induced OH reactions of naphthalene and its oxidation products on SiO2

The photo-induced degradation of naphthalene, 1,4-naphthoquinone, 1-naphthol and 1-NO₂ naphthalene, adsorbed on silica gel, and with the addition of nitrogenous air pollutants e.g. NO₂ (as KNO₂) was investigated. Results indicate that compounds adsorbed onto a solid carrier are degraded when irradiated with UV light (λ > 290 nm) in the presence of nitrites. The key species initiating the naphthalene degradation is the OH-radical which is generated through the photolysis of NO₂. Reaction products identified were 2-formyl-cinnamaldehyde, 1,4-naphthoquinone, nitronaphthol, o-phthaldialdehyde, phthalide and nitronaphthalene. A mass balance between 40–50% was achieved. Under the same irradiation conditions, 1-NO₂ naphthalene is mainly degraded by direct photolysis while degradation of 1-naphthol and 1,4-naphthoquinone proceeds via the reaction with OH-radicals. Identified products were hydroxy-nitro-nitroso- and quinones compounds.     

Heterogeneous Oxidation by Ozone of Naphthalene Adsorbed at the Air-Water Interface of Micron-Size Water Droplets

Abstract

The mass transfer of naphthalene vapor to water droplets in air was studied in the presence of ozone (O₃) in the gas phase. A falling droplet reactor with water droplets of diameters 55, 91, and 182 μm was used for the study. O₃ reacted with naphthalene at the air-water interface, thereby decreasing the mass transfer resistance and increasing the rate of uptake of naphthalene into the droplet. A Langmuir-Hinshelwood reaction mechanism at the air-water interface satisfactorily described the surface reaction. The first-order surface reaction rate constant, k_s, increased with decreasing droplet size. Three organic intermediates were identified in the aqueous phase as a result of ozonation of naphthalene at the surface of the droplet indicating both peroxidic and nonperoxidic routes for ozonation. The presence of an organic carbon surrogate (fulvic acid) increased both the partition constant of naphthalene and the surface reaction rate of O₃. The heterogeneous oxidation of naphthalene by O₃ on the droplet was 15 times faster than the homogeneous oxidation by O₃ in the bulk air phase, whereas it was only 0.08 times the homogeneous gas-phase oxidation by hydroxyl radicals under atmospheric conditions.     

Influence of NO2 and dissolved iron on the S(IV) oxidation in synthetic aqueous solution

The influence of dissolved NO₂ and iron on the oxidation rate of S(IV) species in the presence of dissolved oxygen is presented. To match the conditions in the real environment, the concentration of iron in the reaction solution and trace gases in the gas mixture was typical for a polluted atmosphere. The time dependence of HSO₃⁻, SO₄²⁻, NO₂⁻ and NO₃⁻ and the concentration ratio between Fe(II) and total dissolved iron were monitored. Sulphate formation was the most intensive in the presence of an SO₂/NO₂/air gas mixture and Fe(III) in solution. The highest contribution to the overall oxidation was from Fe-catalysed S(IV) autoxidation. The reaction rate in the presence of both components was equal to the sum of the reaction rates when NO₂ and Fe(III) were present separately, indicating that under selected experimental conditions there exist two systems: SO₂/NO₂/air and SO₂/NO₂/air/Fe(III), which are unlikely to interact with each other. The radical chain mechanism can be initiated via reactions Fe(III)–HSO₃⁻ and NO₂–SO₃²⁻/HSO₃⁻.     

Atmospheric oxidation of elemental mercury by ozone in the aqueous phase

The aqueous phase oxidation of elemental mercury by ozone has been investigated in the laboratory using a quartz glass reactor with gas phase concentrations of 400–1800ng m⁻³ and 70–200 ppb for Hg(0) and O₃, respectively. The absorption of Hg in the water phase was increased by three orders of magnitude with O₃ present. If the oxidation were to proceed with the same speed in liquid water in contact with the atmosphere,conversion rales of 1–4% h⁻¹ would be implied. Experiments using ambient urban air with 2–6 ng Hg m⁻³ confirm the process at elevated O₃ concentrations. At ambient O₃ concentrations competitive reactions become important, e.g. O₃ consumption by SO₂, hydrocarbons etc., and even some reduction of Hg²⁺ could occur. The atmospheric oxidation of Hg(0) by O₃ in water is thus considered important at high O₃ levels in regionally polluted or remote areas.     

Factors influencing ozone chemistry in subsonic aircraft plumes

This study investigates several factors that could influence ozone chemistry occurring in subsonic aircraft plumes in the upper troposphere. The study focuses on uncertainties in gas-phase rate parameters, but also examines the influence of selected heterogeneous reactions, the rate of expansion of the plume, ambient and initial plume concentrations, and the time of emissions. Monte Carlo analysis with Latin hypercube sampling was applied to an expanding box model of an aircraft plume, in order to estimate the sensitivities of O₃ perturbations (ΔO₃) to uncertainties in rate constants in the RADM2 chemical mechanism. The resulting coefficient of variation in ΔO₃ at the end of a 36 h simulation was about 50%. Influential uncertainties in gas-phase rate parameters include those for photolysis of NO₂ and HCHO, O₃+NO, HO₂+NO, and formation of PAN and HNO₃. With high background concentrations of non-methane hydrocarbons, uncertainties in rate parameters of reactions involving peroxy radicals from ethene and propene oxidation were also influential. The coefficient of variation for ΔO₃ due to uncertainties in emission indices of NO_x, CO, and organic compounds was less than 15%. The effects of the heterogeneous reaction of N₂O₅ leading to HNO₃ formation, and hypothesized reactions of HNO₃ and NO₂ on soot, were also investigated. The results suggest that the latter two reactions could be influential for ΔO₃ if published estimates of reaction probabilities and high estimates of soot concentrations in plumes are realistic.     

Deposition and adsorption of the air pollutant HNO3 vapor to soil surfaces

Deposition of nitric acid (HNO₃) vapor to soils has been evaluated in three experimental settings: (1) continuously stirred tank reactors with the pollutant added to clean air, (2) open-top chambers at high ambient levels of pollution with and without filtration reducing particulate nitrate levels, (3) two field sites with high or low pollution loads in the coastal sage plant community of southern California. The results from experiment (1) indicated that the amount of extractable NO₃⁻ from isolated sand, silt and clay fractions increased with atmospheric concentration and duration of exposure. After 32 days, the highest absorption of HNO₃ was determined for clay, followed by silt and sand. While the sand and silt fractions showed a tendency to saturate, the clay samples did not after 32 days of exposure under highly polluted conditions. Absorption of HNO₃ occurred mainly in the top 1 mm layer of the soil samples and the presence of water increased HNO₃ absorption by about 2-fold. Experiment (2) indicated that the presence of coarse particulate NO₃⁻ could effectively block absorption sites of soils for HNO₃ vapor. Experiment (3) showed that soil samples collected from open sites had about 2.5 more extractable NO₃⁻ as compared to samples collected from beneath shrub canopies. The difference in NO₃⁻ occurred only in the upper 1–2 cm as no significant differences in NO₃⁻ concentrations were found in the 2–5 cm soil layers. Extractable NO₃⁻ from surface soils collected from a low-pollution site ranged between 1 and 8 μg NO₃–N g⁻¹, compared to a maximum of 42 μg NO₃–N g⁻¹ for soils collected from a highly polluted site. Highly significant relationship between HNO₃ vapor doses and its accumulation in the upper layers of soils indicates that carefully prepared soil samples (especially clay fraction) may be useful as passive samplers for evaluation of ambient concentrations of HNO₃ vapor.     

An automatic rain gauge for continuous,real time determination of rainwater chemistry

An automatic rain gauge has been developed, capable of collecting rainwater and analysing it continuously for the ions H⁺, NH₄⁺, Na⁺, Ca²⁺, NO₃⁻, Cl⁻, SO₄²⁻ and for dissolved H₂O₂. The wet-only rain collector, based on an inverting V-tray arrangement, is mounted on the roof of a small caravan, which contains the analysis equipment. An indirect colorimetric method is used for SO₄²⁻ and a chemiluminescent method for H₂O₂, the other species being determined by ion-selective electrodes. The onset of rain is sensed either by a simple conductivity plate or by a modified float gauge. In addition, equipment is installed to determine simultaneously gas-phase O₃, NO, NO₂ and SO₂ and simple meteorological parameters. Data is recorded on disc by a microcomputer, which also handles automatic calibration and other control functions.The caravan as a whole is a fairly comprehensive, transportable air and rainwater monitoring package. The advantage of the rainwater sampling method is that instantaneous concentrations are measured continuously rather than daily or weekly averages; and that problems of deterioration of stored samples are eliminated.     

A second generation model for regional-scale transport/chemistry/deposition

The regional-scale transport, chemistry and deposition of acidifying compounds, photochemical oxidants, and their precursors are analyzed using a second-generation Eulerian model. The important atmospheric processes are incorporated using chemical, dynamical and thermodynamical parameterizations having sufficient detail to accommodate boundary layer-free troposphere exchange in cloudy and cloud-free environments, and in-cloud and below-cloud wet removal and chemistry. Forty-one species are considered, many of which are also present in the liquid-drop phases. In the regional scale transport, the advected species are NO, NO₂, SO₂, SO⁻²₄, O₃, HNO₃, NH₃, PAN, H₂O₂, HCHO, alkanes, C₂H₄, other olefins, aromatics, RCHO, ROOH, HNO₂, RONO₂ and RO₂NO₂. The model capabilities are illustrated by showing simulations in which non-precipitating clouds are present to absorb gas-phase species, chemically alter these, and then release them to the atmosphere.     

The chemical composition of cloud and rainwater. Results of preliminary measurements from an aircraft

Using an aircraft, preliminary investigations have been carried out into the chemical composition of clouds. The emphasis was on testing the sampling devices under several conditions. The results clearly show a considerable spatial distribution in pollutant concentrations that must have been caused by the contribution of many plume sources and the inhomogeneity of cloudwater density as well. Rather high concentrations of H₃O⁺. Cl⁻, NO⁻₃, SO²⁻₄, NH⁺₄ and H₂O₂ were measured. Except for H₂O₂, these components are scavenged very fast during travel over short distances over source regions. Moreover H₃O⁺, NO⁻₃ and SO²⁻₄ are likely to be formed by chemical reactions of gaseous precursors with oxidants in the liquid phase. This may explain the marked decrease in high background H₂O₂ concentrations (ppm range). Relatively high (molar) NO⁻₃ /SO²⁻₄ ratios mainly varying from 1 to 2 were measured over The Netherlands near source areas. The lower values found during a flight over southern Scandinavia are in agreement with data from literature. Occasionally the chloride concentration was found to be much higher than could be expected from rain network data.