Particle acidity and sulfate production during severe haze events in China cannot be reliably inferred by assuming a mixture of inorganic salts
- 1Key Laboratory of Geographic Information Science of the Ministry of Education, School of Geographic Sciences, East China Normal University, Shanghai 200241, China
- 2State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
- 3Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Science, Xiamen 361021, China
- 4College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China
- 5Departments of Atmospheric Sciences and Chemistry, Texas A&M University, College Station, TX, 77843, USA
- 6State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China
- 7State Environmental Protection Key Lab of Environmental Risk Assessment and control on Chemical Processes, East China University of Science and Technology, Shanghai 200237, China
- 8School of Environmental Science and Engineering, Institute of Environmental Health and Pollution, Control, Guangdong University of Technology, Guangzhou 510006, China
- 9Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91125, USA
- 10Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Nanjing University of Information Science & Technology, Nanjing 210044, China
- 11State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China
- 12Key Laboratory of Songliao Aquatic Environment, Jilin Jianzhu University, Changchun, 130118, China
Correspondence: Gehui Wang (firstname.lastname@example.org, email@example.com) and Renyi Zhang (firstname.lastname@example.org)
Atmospheric measurements showed rapid sulfate formation during severe haze episodes in China, with fine particulate matter (PM) consisting of a multi-component mixture that is dominated by organic species. Several recent studies using the thermodynamic model estimated the particle acidity and sulfate production rate, by treating the PM exclusively as a mixture of inorganic salts dominated by ammonium sulfate and neglecting the effects of organic compounds. Noticeably, the estimated pH and sulfate formation rate during pollution periods in China were highly conflicting among the previous studies. Here we show that a particle mixture of inorganic salts adopted by the previous studies does not represent a suitable model system and that the acidity and sulfate formation cannot be reliably inferred without accounting for the effects of multi-aerosol compositions during severe haze events in China. Our laboratory experiments show that SO2 oxidation by NO2 with NH3 neutralization on fine aerosols is dependent on the particle hygroscopicity, phase-state, and acidity. Ammonium sulfate and oxalic acid seed particles exposed to vapors of SO2, NO2, and NH3 at high relative humidity (RH) exhibit distinct size growth and sulfate formation. Aqueous ammonium sulfate particles exhibit little sulfate production, in contrast to aqueous oxalic acid particles with significant sulfate production. Our field measurements demonstrate significant contribution of water-soluble organic matter to fine PM in China and indicate that the use of oxalic acid in laboratory experiments is representative of ambient organic dominant aerosols. While the particle acidity cannot be accurately determined from field measurements or calculated using the thermodynamic model, our results reveal that the pH value of ambient organics-dominated aerosols is sufficiently high to promote efficient SO2 oxidation by NO2 with NH3 neutralization under polluted conditions in China.
Atmospheric measurements have demonstrated rapid sulfate production during severe haze events in China (Guo et al., 2014; Wang et al., 2014, 2016; Zhang et al., 2015; Cheng et al., 2016). For example, Wang et al. (2016) showed that, during pollution episodes in Xi'an, the mass concentration increased markedly from less than 10, from 10 to 20, and to greater than 20 µg m−3, with the corresponding increases in the mean PM2.5 mass concentrations from 43, 139, to 250 µg m−3 from clean, transition, to polluted periods, respectively. Among the PM2.5 species in Xi'an, organic matter (OM), nitrate (), and were most abundant, with the mass fractions of 55, 14, and 14 %, respectively, during the polluted period. In addition, the work of Wang et al. (2016) demonstrated that the molar ratio of to SO2, which reflects sulfur partitioning between the particle and gas phases, exhibited an exponential increase with relative humidity (RH), with the values of less than 0.1 at RH < 20 % to 1.1 at RH > 90 % in Xi'an. Similar evolutions in mass concentrations and the molar ratio of to SO2 were shown during the pollution development in Beijing (Sun et al., 2013; Wang et al., 2014, 2016). The rapid sulfate formation measured in China could not be explained by current atmospheric models and suggested missing sulfur oxidation mechanisms (Wang et al., 2014). Typically, high sulfate levels during haze events in China occurred concurrently with elevated RH, NOx, and NH3 (Wang et al., 2014, 2016; Zhang et al., 2015), implicating an aqueous sulfur oxidation pathway. On the basis of complementary field and experimental measurements, Wang et al. (2016) concluded that the aqueous oxidation of SO2 by NO2 is key to efficient sulfate formation, but is only feasible under two atmospheric conditions, i.e., on fine aerosols with high RH and NH3 neutralization or under cloud conditions.
Several recent studies estimated the particle acidity and aqueous sulfate production during severe haze events in China using the thermodynamic model (Cheng et al., 2016; Guo et al., 2017a; M. Liu et al., 2017). For example, Cheng et al. (2016) estimated a pH range of 5.4 to 6.2 using a thermodynamic model (ISORROPIA-II) in Beijing. On the basis of their estimated pH and the previous experimental rates of SO2 oxidation by NO2 and the Henry's Law constants for sulfur dioxide (SO2), bisulfite (), and sulfite () from the literature (Lee and Schwartz, 1983; Clifton et al., 1988; Seinfeld and Pandis, 2006), the authors derived a sulfate production rate and concluded that reactive nitrogen chemistry in aerosol water explained the sulfate formation during polluted periods in Beijing. In contrast, other recent studies by Guo et al. (2017a) and M. Liu et al. (2017) adopted a similar method to Cheng et al. (2016), but reported significantly different values of pH and the sulfate formation rates by the aqueous SO2 oxidation by NO2 in China. Those two later studies determined a pH range of 3.0–4.9 and suggested that fine particles were moderately acidic and the aqueous SO2 oxidation by NO2 was unimportant during severe wintertime haze periods in China.
In this article, we conducted laboratory measurements of the hygroscopicity for oxalic acid particles and particle growth of ammonium sulfate particles upon exposure to SO2, NO2, and NH3 at high RH conditions, in order to evaluate the dominant factors regulating the aqueous oxidation of SO2 by NO2. In addition, field measurements of chemical compositions of water-soluble fraction for fine PM (including oxalic acid) in Beijing, Hebei Province, and Xi'an were performed during the winter haze episodes, showing significantly enriched water-soluble organic matter (WSOM). The implications for the multi-aerosol chemical compositions on the pH value and sulfate production during winter pollution periods in China are discussed.
2.1 Aqueous phase oxidation of SO2 by NO2 in an environmental chamber
The experimental method using the environmental chamber has been discussed elsewhere (Wang et al., 2016), and here we only provide a brief description. The aqueous SO2 oxidation experiments was conducted by exposing size-selected (NH4)2SO4 seed particles to different levels of SO2, NO2, and NH3 at variable RH conditions in a 1 m3 Teflon reaction chamber covered with aluminum foil. A differential mobility analyzer (DMA) equipped with a condensation particle counter (CPC) was used to measure the particle growth in diameter, in order to determine sulfate formation on seeded particles (Wang et al., 2016).
2.2 Measurement of hygroscopic growth factor of oxalic acid
Hygroscopic growth factor (HGF) of oxalic acid was measured according to the method previously discussed (Khalizov et al., 2009; Pagels et al., 2009). Briefly, a hygroscopicity tandem differential mobility analyzer (HTDMA) coupled to a condensation particle counter (CPC, TSI 3762) was used for the HGF measurement. Size-selected oxalic acid particles with the dry diameter of 100 nm were exposed to increasing RH from 8 to 92 % with a step range from 1 to 10 %. HGF is defined as the ratio of oxalic acid particle diameter (Dp) measured by the second DMA at an elevated RH to the initial diameter (D0 = 100 nm) of the particles selected by the first DMA at the dry conditions of RH = 8 % (Peng et al., 2016).
2.3 Chemical composition of PM2.5 in Beijing, Hebei Province, and Xi'an, China
PM2.5 samples were collected onto pre-baked (450 ∘C for 6 h) quartz fiber filter by using a high-volume air sampler with an airflow rate of 1.03 m3 min−1. The sample collection in Xi'an was performed on the roof of a three-story building in the urban center with a 1 h interval for each sample during the winter of 2012 (Wang et al., 2016). The sample collection in Beijing was conducted during the winter of 2016 on the roof of a four-story building on the campus of China Research Academy of Environmental Sciences, which is located at the northern part of Beijing. The PM2.5 samples in Hebei Province were collected during the winter of 2016 on the roof of a three-story building on the campus of the Institute of Hydrology and Environmental Geology, which is located in Zhengding County of Hebei Province. Both sample collections in Beijing and Hebei Province were performed on a day/night basis. After collection, all samples were sealed individually in an aluminum foil bag and stored in a freezer below −18 ∘C prior to analysis. During the sampling periods temperatures were −6.0 ± 4.0 ∘C (−15–1.0 ∘C), −4.0 ± 3.0 ∘C (−12–2.0 ∘C), and 1.6 ± 4.4 ∘C (−5.4–15 ∘C) in Beijing, Hebei Province, and Xi'an, respectively, while relative humidity at the three sites (RH) were 37 ± 18 % (16–87 %), 46 ± 21 % (16–87 %), and 59 ± 21 % (15–95 %), respectively. Previous observations showed that coal combustion, biomass burnings and vehicle exhausts are the three major sources of PM2.5 during winter in North China including Beijing, Hebei Province, and Xi'an (Li et al., 2016; Zhang et al., 2015).
The detailed procedures for the analysis of inorganic ions and water-soluble organic matter (WSOM) in aerosols have been reported elsewhere (Wang et al., 2017; G. Wang et al., 2009, 2010). Briefly, one part of the filter sample (area about 5 cm2) was divided into several pieces, extracted with Mili-Q pure water, and determined for WSOM and inorganic ions by using Shimadzu TOC-L CPH analyzer and Dionex-600 ion chromatography, respectively. Oxalic acid in PM2.5 was analyzed according to Wang et al. (2002) and Cheng et al. (2015). One part of the filter sample was extracted with Milli-Q water, concentrated to dryness, and reacted with 14 % BF3/butanol at 100 ∘C for 1 h. After the reaction, the derivatized sample was extracted with hexane for three times and concentrated into 1 mL. Oxalic acid in the samples was identified by gas chromatography–mass spectrometry (GC–MS) and quantified by gas chromatography (Agilent GC7890A).
3.1 Aqueous oxidation of SO2 by NO2 with NH3 neutralization
We first evaluated the factors controlling the aqueous phase oxidation of SO2 by NO2 using the environmental chamber method. The evolution in the size of ammonium sulfate particles after exposure to SO2, NO2, and NH3 at different RH and SO2 levels is shown in Fig. 1. In our experiments, monodisperse particles with the initial dry particle size ranging from 50 to 70 nm were selected for the exposure, and two different SO2 concentrations (37.5 and 375 parts per billions or ppb) were used. RH was maintained at a level of 80–98 %, above the deliquescence point (79 %) of ammonium sulfate (Qiu and Zhang, 2013) to ensure aqueous particles. As is shown in Fig. 1, the size of (NH4)2SO4 particles remains nearly invariant (within the experimental uncertainty) after exposure to SO2, NO2, and NH3. A 10-fold increase in the SO2 concentration has little effect on the growth of (NH4)2SO4 particles. These results illustrate that sulfate production is insignificant and SO2 cannot be efficiently oxidized by NO2 in the presence of NH3 on aqueous ammonium sulfate particles. The measurement of negligible growth for (NH4)2SO4 particles exposed to SO2, NO2, and NH3 at high RH is in contrast to the previous work by Wang et al. (2016), which showed large size growth and significant sulfate production for oxalic acid particles with NH3 neutralization and under high RH conditions (see the black triangles in Fig. 1).
To gain an insight into such a difference in the size growth between (NH4)2SO4 and oxalic acid particles, we measured the hygroscopic growth of oxalic acid particles. Figure 2 displays the measured hygroscopic growth factor (HGF) of oxalic acid, showing an exponential increase with an increase in RH. The measured HGF value is close to unity at RH < 40 % and increases from 1.1 at RH = 60 % to 1.5 at RH = 90 %. Our measured HGF for oxalic acid is consistent with the previous studies by Prenni et al. (2001) and Mikhailov et al. (2009); all of which were measured by using a hygroscopicity tandem differential mobility analyzer (HTDMA) system. In contrast, another earlier experimental study showed little growth for oxalic acid particles under high RH conditions by using an electrodynamic balance (EDB) system (Peng et al., 2001). The different HGF measured for oxalic acid is most likely due to the different accuracies of the two types of methods for the hygroscopicity measurement. The measurements of HGF also provide information on the particle phase-state. As evident from Fig. 2, oxalic acid particles mainly exist in a non-aqueous phase at RH < 40 % but in the aqueous phase at RH > 60 %.
Our present experiments of aqueous oxidation of SO2 by NO2 were performed under similar conditions as those by Wang et al. (2016), i.e., with comparable concentrations for SO2, NO2, and NH3 and in the same phase-state (aqueous) for the particles. In contrast, the particle acidity is clearly distinct between the two studies. Our present experiment is characterized by a lower pH value, as ammonium sulfate is rather acidic. For example, the pH value of 0.1M (NH4)2SO4 solution is 5.5. The overall aqueous reaction between SO2 and NO2 in the presence of NH3 is suggested as the following (Wang et al., 2016),
As the solubility of SO2 decreases markedly with increasing particle acidity (Seinfeld and Pandis, 2006; Zhang et al., 2015), the heterogeneous reaction between SO2 and NO2 is prohibited on acidic (NH4)2SO4 particles. In contrast, under the experimental conditions by Wang et al. (2016), the heterogeneous reaction between oxalic acid and NH3 occurred on aqueous particles in the presence of NH3, yielding ammonium oxalate. The ammonium oxalate is expected to be less acidic than ammonium sulfate, because for a bulk solution the pH value of 0.1 M ammonium oxalate is 6.5 and one unit higher than that of ammonium sulfate. As a result, SO2 readily dissolves into aqueous ammonium oxalate particles and is oxidized by NO2 into , which is consequently neutralized by NH3 to produce (NH4)2SO4. The resulting aqueous ammonium oxalate/(NH4)2SO4 particles, which is internally mixed, exhibit a lower acidity than that of pure (NH4)2SO4 particles, responsible for a significant growth in the dry particle size and sulfate formation for the previous experiments by Wang et al. (2016).
Hence, the experimental studies of our present work and that by Wang et al. (2016) reveal that sulfate production on fine particles is dependent on several factors, including the particle hygroscopicity, phase-state, acidity, and RH, in addition to the gaseous concentrations of SO2, NO2, and NH3. These experimental results indicate that the acidity and sulfate formation are distinct for organic seed and ammonium sulfate seed particles. While oxidation of SO2 by NO2 on aqueous (NH4)2SO4 particles does not represent a viable mechanism because of a higher acidity, significant sulfate production occurs on oxalic acid particles because of a lower acidity.
3.2 Field measurements of WSOM in China
Atmospheric measurements have shown that the occurrence of severe haze episodes in China is accompanied with high RH conditions and PM2.5 particles consist of large amounts of secondary organic and inorganic compounds. We present additional field measurements of the chemical composition of PM2.5in Beijing, Hebei Province, and Xi'an. Figure 3 shows that the wintertime PM2.5 samples collected at the three locations. It is evident that WSOM is considerably enriched and their concentrations are comparable to those of the total inorganic ions (Fig. 3a and b). For example, the mass concentration of WSOM ranges from 10 to 60 µg m−3 in Beijing and Hebei Province during the winter of 2016 and from 10 to 180 µg m−3 in Xi'an during the winter of 2012 (Fig. 3c and d, respectively). Compared to those in Beijing and Hebei Province, the more abundant WSOM in Xi'an was caused by more emissions from biomass burning for house heating (Li et al., 2016). As seen in Fig. 3c–f, the variation of WSOM displays a temporal pattern similar to that of oxalic acid, with a linear correlation coefficient of 0.79, 0.88 and 0.72 in Beijing, Hebei Province, and Xi'an, respectively (Fig. 3e and f). The mass concentration of oxalic acid in fine PM during the haze episodes is about 500 ng m−3 in Beijing and Hebei Province (Fig. 3e) and more than 2000 ng m−3 in Xi'an (Fig. 3f). Hence, our field measurements indicate that oxalic acid represents one of the most abundant WSOM in the aerosol-phase. Oxalic acid is a secondary product formed from the aqueous-phase oxidation of water-soluble organic precursors and ubiquitously exists in the troposphere. Like other pollutants, oxalic acid has been also shown to occur in large abundance in China (Wang et al., 2012; Cheng et al., 2013; Meng et al., 2014; Kawamura and Bikkina, 2016). As shown in Fig. 3g and h, during the field observation periods sulfate at the three sites showed a temporal variation pattern similar to that of oxalic acid with a robust linear correlation (r2 = 0.67, 0.84 and 0.61 in Xi'an, Beijing and Hebei Province, respectively). Such a correlation was also reported by other researchers (Wang et al., 2017; Yu et al., 2005), suggesting the co-occurrence and internally mixing state of both compounds in the atmosphere. In addition, the previous field measurements also revealed that WSOM in China is not only enriched in carboxylic acids (including oxalic acid) but also in other organic species, including carbonyls, amines, and water-soluble nitrogen-containing organic compounds (G. Wang et al., 2010; Wang et al., 2013; Zheng et al., 2015; Yao et al., 2016; F. Liu et al., 2017). The dominant organic acids and bases indicate that haze particles in China are multi-component in nature and the estimations of the particle acidity (or pH) and the sulfate production rate need to take into account of the effects of organic species, in addition to inorganic ions.
Several recent studies using thermodynamic models (Wexler and Clegg, 2002; Fountoukis and Nenes, 2007) estimated the particle acidity and sulfate production during pollution episodes in China (Cheng et al., 2016; Guo et al., 2017a; M. Liu et al., 2017). Those previous studies treated the PM exclusively as a mixture of inorganic salts dominated by ammonium sulfate and neglected the effects due to the presence of organic compounds. Apparently, the conclusions by those modeling studies hinge on the validity of several critical assumptions in their analyses, including the application of the thermodynamic model, the accuracy in determining the aerosol water content (AWC), and the applicability of the earlier experimental measurements for the aqueous oxidation of SO2 by NO2 to atmospheric conditions.
Estimation of the pH values using the thermodynamic models is typically of considerable uncertainty, because of several intricate difficulties. For example, the ISORRPIA-II model includes two modes, i.e., metastable (aerosols are assumed to be in the liquid-phase only and may reach supersaturation) and stable (aerosols are assumed in the liquid- and solid phases that are in equilibrium) (Guo et al., 2017b). As the thermodynamic model is established on the basis of the equilibrium principles, its application to non-equilibrium conditions needs to be rigorously assessed. In addition, the phase (e.g., liquid, amorphous, or crystalline) and mixing state of ambient aerosols are highly complex because of the presence of multi-component organic and inorganic species (Qiu and Zhang, 2013; Zhang et al., 2015), inevitably rendering high uncertainty in the thermodynamic calculations.
Guo et al. (2017a) suggested that the pH predictions using the metastable mode would be more reliable than that using the stable mode, on the basis of model evaluation from measured and predicted and during the winter of 2012 in Xi'an. Figure 4 compares the concentrations of NH3 (g) and aerosol species predicted by ISORROPIA-II with the field measurements under the metastable and stable modes in Xi'an during the winter of 2012. As evident in Fig. 4a and b, NH3 predicted is similar to the measured value with the metastable or stable mode. Furthermore, the predicted concentrations of and using both the metastable and stable modes are nearly identical (Fig. 4c–f). Guo et al. (2017a) only compared the liquid and predicted by the model under the stable mode with the field measured aerosols composed of both liquid and solid compounds, and thus their predicted concentrations were lower than those of the measurements (see Fig. S1 in Guo et al., 2017a). As a result, their statement that pH prediction with the metastable mode would be more reliable than that with the stable mode was unjustified. Noticeably, the pH values estimated by the ISORROPIA-II model under the two modes are significantly different, with the values of 4.57 ± 0.40 under the metastable mode and 6.96 ± 1.33 under the stable mode. Most recently, it was suggested that the large discrepancy in predicting pH is attributable to the model code errors (Song et al., 2018).
In addition, the pH estimation by the thermodynamic model is highly dependent on the ratio of the concentration of hydrogen ions in the liquid-phase to AWC. Guo et al. (2017a) and M. Liu et al. (2017) assumed negligible particle water associated with the organic aerosol mass. Such an assumption is clearly invalid, as aerosols typically contain a large portion of WSOM in China (Fig. 3), including organic nitrogen species (G. Wang et al., 2010; Wang et al., 2013) and acids (G. Wang et al., 2009, 2010; Wang et al., 2006). Also, organic acids engage in particle-phase reactions with the basic species (i.e., NH3 and amines), significantly enhancing the particle hygroscopicity and reducing the acidity (Gomez-Hernandez et al., 2016). In addition, because of their strong basicity and high abundance, amines likely play a key role in reducing the particle acidity in China (L. Wang et al., 2010a, b; Qiu et al., 2011; Qiu and Zhang, 2012; Dong et al., 2013; Zheng et al., 2015; Yao et al., 2016; F. Liu et al., 2017). Consequently, the acidity for organics-dominated aerosols is considerably different from that of ammonium sulfate aerosols, as demonstrated in our experimental results. While effort has been made to account for the effects of organic species on the aerosol properties (Clegg et al., 2013), the available thermodynamic models are still inadequate in representing complex multi-component aerosols. An inconsistency of the ammonium–sulfate ratios using the thermodynamic models was identified in the eastern US, also suggesting a possible role for organic species (Silvern et al., 2017).
Furthermore, the chemical mechanism leading to the aqueous conversion of SO2 to sulfate by NO2 is not well understood. The previous modeling studies adopted the aqueous reaction rate constants previously measured (Lee and Schwartz, 1983; Clifton et al., 1988), while the applicability of the earlier experimental studies to atmospheric conditions is uncertain. For example, Lee and Schwartz (1983) examined the oxidation of S(IV) by NO2 in the liquid phase by flowing gaseous NO2 through a NaHSO3 solution at a constant pH by regulating NaOH and determined the rate constant of 1.4 × 105 M−1 s−1 at pH = 5 and with a lower limit of 2 × 106 M−1 s−1 at pH = 5.8 and 6.4 from measuring the electrical conductivity of the solution. Clifton et al. (1988) measured the rate constant for the reaction of NO2 with S(IV) over the pH range of 5.3–13, by producing NO2 from irradiation of NaNO2 and N2O solutions and mixing with Na2SO3 solutions, and obtained the second-order rate constant of 1.24 × 107 and 2.95 × 107 M−1 s−1 from the decay of NO2 monitored by absorption spectroscopy. The results of the measured rate constants between the two earlier experimental measurements differed by 1–2 orders of magnitude (Lee and Schwartz, 1983; Clifton et al., 1988). Also, both kinetic experiments employed bulk solutions and did not account for the gaseous uptake process (Lee and Schwartz, 1983; Clifton et al., 1988).
Wang et al. (2016) obtained the SO2 uptake coefficient for sulfate production from combined field measurements and laboratory experiments, and their laboratory experiments using aqueous oxalic acid particles reproduced the rapid sulfate production measured under polluted ambient conditions in China. The SO2 uptake coefficient on oxalic acid particles in the laboratory reaction chamber is 8.3 ± 5.7 × 10−5 (Wang et al., 2016) under the humid conditions and similar to that (4.5 ± 1.1 × 10−5) (Wang et al., 2016) observed in Beijing during the haze period of 2015. The results of the SO2 uptake coefficients determined by Wang et al. (2016) are also consistent with the modeling studies in quantification of the sulfate formation using atmospheric models in the country (e.g., Wang et al., 2014), indicating the applicability of their proposed mechanism to haze conditions in China. In contrast, M. Liu et al. (2017) invoked the experimental work by Hung and Hoffmann (2015) as a plausible cause for rapid SO2 oxidation by O2 in the absence of photochemistry, but without noting the high acidity as a necessary condition in that experimental work (i.e., pH ≤ 3). Most recently, Li et al. (2018) suggested an indirect mechanism of SO2 oxidation by NO2 via HONO/ produced in fast-hydrolytic disproportion of NO2 on the surface of NaHSO3 aqueous microjets. In addition, another recent theoretical work by Zhang et al. (2018) indicated that under weakly acidic and neutral conditions (pH ≤ 7) the oxidation of by dissolved NO2 is a self-sustaining process, where the produced cis-HONO, , and H2SO4 promote the tautomerization from to as the catalysts.
In this paper we have presented experimental measurements of the growth of ammonium sulfate seed particles exposed to vapors of SO2, NO2, and NH3 at variable RH, the HGF of oxalic acid particles, and field measurements of WSOM for PM2.5 during the severe haze events in Beijing, Hebei Province, and Xi'an. Our experimental results reveal that sulfate production on fine particles is dependent on the particle hygroscopicity, phase-state, and acidity, as well as RH. The acidity and sulfate formation for ammonium sulfate seed particles are distinct from those of oxalic acid seed particles. Aqueous ammonium sulfate particles show negligible growth because of low pH, in contrast to aqueous oxalic acid particles with significant dry-size increase and sulfate formation because of high pH. In addition, our atmospheric measurements show significant concentrations of WSOM (including oxalic acid) in fine PM, indicating multi-component haze particles in China. Our results reveal that a particle mixture of inorganic salts adopted by the previous studies using the thermodynamic model does not represent a suitable model system and that the particle acidity and aqueous sulfate formation rate cannot be reliably inferred without accounting for the effects of multi-chemical compositions during severe haze events in China. Our combined experimental and field measurements corroborate the earlier finding that sulfate production via the particle-phase reaction involving SO2 and NO2 with NH3 neutralization occurs efficiently on organics-dominated aerosols (Wang et al., 2016) but are in contradiction to the most recent studies using the thermodynamic model (Guo et al., 2017a; M. Liu et al., 2017).
In conclusion, while the particle acidity or pH cannot be accurately determined from atmospheric field measurements or calculated using the thermodynamic models, our combined experimental and field results provide the compelling evidence that the pH value of ambient organics-dominated particles is sufficiently high to promote SO2 oxidation by NO2 with NH3 neutralization under polluted conditions in China.
The field observational and the lab experimental data used in this study are available from the corresponding author upon request (Gehui Wang via email@example.com, or firstname.lastname@example.org).
GW and RZ designed the research; GW, FZ, JP, LD, YJ, WMO, JW, JL, CW, CC, YuaW, JZ, JS, YL, YuyW, HL, NL, and RZ performed the experimental work. GW and RZ analyzed the data; GW and RZ wrote the paper.
The authors declare that they have no conflict of interest.
This article is part of the special issue “Regional transport and transformation of air pollution in eastern China”. It is not associated with a conference.
Financial support for this work was provided by National Key R&D Plan
(Quantitative Relationship and Regulation Principle between Regional
Oxidation Capacity of Atmospheric and Air Quality; no. 2017YFC0210000), the
China National Natural Science Funds for Distinguished Young Scholars
(no. 41325014), a program from the National Nature Science Foundation of China
(no. 41773117). This work was also supported by the Robert A. Welch
Foundation (grant A-1417). Wilmarie Marrero-Ortiz was supported by the National Science
Foundation Graduate Research Fellowship Program.
Edited by: Zhanqing Li
Reviewed by: two anonymous referees
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