Sources and oxidative potential of water-soluble humic-like substances (HULISWS) in fine particulate matter (PM2.5) in Beijing
Water-soluble humic-like substances (HULISWS) are a major redox-active component of ambient fine particulate matter (PM2.5); however, information on their sources and associated redox activity is limited. In this study, HULISWS mass concentration, various HULISWS species, and dithiothreitol (DTT) activity of HULISWS were quantified in PM2.5 samples collected during a 1-year period in Beijing. Strong correlation was observed between HULISWS and DTT activity; both exhibited higher levels during the heating season than during the nonheating season. Positive matrix factorization analysis of both HULISWS and DTT activity was performed. Four combustion-related sources, namely coal combustion, biomass burning, waste incineration, and vehicle exhausts, and one secondary factor were resolved. In particular, waste incineration was identified as a source of HULISWS for the first time. Biomass burning and secondary aerosol formation were the major contributors (> 59 %) to both HULISWS and associated DTT activity throughout the year. During the nonheating season, secondary aerosol formation was the most important source, whereas during the heating season, the predominant contributor was biomass burning. The four combustion-related sources accounted for > 70 % of HULISWS and DTT activity, implying that future reduction in PM2.5 emissions from combustion activities can substantially reduce the HULISWS burden and their potential health impact in Beijing.
Fine particulate matter (PM2.5) pollution has caused both environmental and public health problems worldwide. PM2.5 can travel deep into the human lung and lead to various respiratory diseases, such as respiratory tract infections, chronic cough, and asthma (Becker et al., 2005; Nel, 2005). Given the various sources and complex chemical composition of PM2.5, the underlying mechanisms of PM2.5-exposure-induced adverse health effects are not fully understood yet. However, it has been postulated that the redox-active components of PM2.5, such as transition metals and quinones (Charrier and Anastasio, 2012; Chung et al., 2006), can perturb the redox equilibrium in lung cell through the generation of excessive reactive oxygen species (ROS), and induce the subsequent oxidative stress.
Water-soluble humic-like substances (HULISWS) are a mixture of compounds containing polycyclic ring structures with aliphatic side chains and multiple polar functional groups. They account for a significant proportion (30–80 %) of the water-soluble organic matter (WSOM) in PM2.5 (Graber and Rudich, 2006; Kuang et al., 2015; Lin et al., 2010a). HULISWS have recently been recognized to be highly redox-active and they play a significant role in driving PM-associated ROS formation (Dou et al., 2015; Lin and Yu, 2011; Verma et al., 2015a). The reversible redox sites in the HULISWS fraction could serve as an electron transfer intermediate and lead to continuous production of ROS (Lin and Yu, 2011). Dithiothreitol (DTT) assay have been widely used to evaluate the oxidative capacity of HULISWS and PM2.5. Verma et al. (2015b) found that HULISWS contributed approximately 45 % of DTT activity of the water extracts from PM2.5 samples collected in Atlanta, USA, which was 5 % higher than that induced by water-soluble metals. Lin and Yu (2011) also found that HULISWS accounted for 79 % ± 12 % of DTT activity caused by the WSOM fraction in PM2.5 sampled in Pearl River Delta (PRD) region, China. Given the considerable amount of HULISWS in PM2.5 and their ROS generation ability, both field measurements and smog chamber experiments have been conducted to determine their formation pathways and origins in the atmosphere (Kautzman et al., 2010; Lin et al., 2010b; Sato et al., 2012). Biomass burning and secondary formation have been suggested to be the major sources of atmospheric HULISWS (Kautzman et al., 2010; Lin et al., 2010b). However, studies on the quantitative source apportionment of HULISWS are still limited (Kuang et al., 2015), and information on the source-specific contribution to their redox activity is lacking.
Beijing, the capital of China located in the North China Plain, is a political and cultural center with an extremely dense population. However, it has become one of the most polluted cities in the world, with an annual PM2.5 concentration of up to 89.5 µg m−3 in 2013 (Li et al., 2017). Therefore, it presents an ideal location to study the chemical characteristics of HULISWS as well as their sources and potential redox activity.
In this study, our major objective is to investigate the ROS-forming ability of HULISWS in relation to different sources and meteorological conditions. Thus, a total of 66 PM2.5 samples collected in Beijing during a 1-year period were analyzed. Concentrations of total HULISWS were quantified, together with some characteristic individual HULISWS species and the major aerosol components. The redox activity of HULISWS was determined using a DTT assay. Positive matrix factorization (PMF) analysis was conducted to determine the sources of both HULISWS and their associated redox activity. Such a comprehensive source apportionment study of HULISWS-related ROS-generation potential has not been previously reported. Results from this study could provide not only quantitative information regarding the sources and toxicity of HULISWS, but also a deeper understanding of the source-specific oxidative potential of Chinese urban organic aerosols in general. This may be useful for the future development of source-targeted air pollution control policies in Beijing and may provide public-health benefits.
2.1 Sample collection
PM2.5 samples were collected at the Peking University Atmosphere Environment Monitoring Station (PKUERS) on the campus of Peking University (39∘59′21 N, 116∘18′25 E, approximately 30 m above the ground), Beijing, China. A high-volume air sampler coupled with a ≤ 2.5 µm inlet (HIVOL-CABLD, ThermoFisher Scientific, Waltham, MA, USA) was used to conduct sampling at a flow rate of 1.13 m3 min−1. Samples were collected on quartz fiber filters (20.3 × 25.4 cm2, prebaked at 550 ∘C for 5 h; Whatman, Hillsboro, OR, USA) for 24 h every 6 days from 3 March 2012 to 1 March 2013. In addition, a four-channel mid-volume sampler was operated synchronously (16.7 L min−1, TH-16A, Wuhan Tianhong Instruments Co. Ltd., China) to collect PM2.5 onto three 47 mm Teflon filters and one quartz fiber filter for the determination of PM2.5 mass, elemental carbon (EC), and organic carbon (OC), as well as inorganic ionic species.
2.2 Chemical analysis
HULISWS was isolated from PM2.5 samples following the procedure described by Lin et al. (2010b). Briefly, a portion of sample filters (17.5 cm2 for HULISWS species identification and 3 cm2 for HULISWS mass measurement) was cut into small pieces and pollutants were extracted through sonication with distilled deionized (DDI) water for 30 min. The extracts were filtered with polytetrafluoroethylene (PTFE) filters (0.45 µm pore size; Grace, Houston TX, USA) and acidified to a pH of 2 with 2.4 M HCl. A solid phase extraction (SPE) cartridge (Oasis HLB, 3 mL/30 µm, 60 mg; Waters, Milford, MA, USA) was used to isolate HUILSWS. The SPE cartridge was first activated using 1.0 mL of methanol and equilibrated using 1.0 mL of 0.01 M HCl. The extracts were then loaded onto an HLB cartridge. Because the majority of inorganic ions, low molecular weight organic acids, and sugar compounds could not be retained by the HLB cartridge, they were removed from the final effluent. For the analysis of individual HULISWS species, the HLB cartridge was rinsed with two 1.0 mL portions of DDI water and then eluted with three 0.5 mL portions of basic methanol (2 % ammonia, w∕w). The effluent was dried with a gentle flow of ultrapure nitrogen at 40 ∘C, and then derivatized with 100 µL of N,O-bis(trimethylsilyl)trifluoroacetamide (BSTFA; with 1 % trimethylchlorosilane; Sigma Aldrich, St. Louis, MO, USA) and 50 µL of pyridine (> 99.5 %; International Laboratory USA, CA, USA) at 70 ∘C for 2 h. When the mixture had cooled to room temperature, it was spiked with 30 µL of tetracosane-d50 (50 µg mL−1 in n-hexane; Sigma Aldrich, St. Louis, MO, USA) as the internal standard for gas chromatography–mass spectrometry (GC-MS; 7890A-5975C, Agilent, Santa Clara, CA, USA) analysis. Detailed information on this analysis is provided in the Supplement.
For the quantification of HULISWS mass concentration, 6.0 mL of pure methanol was used to elute HULISWS from HLB cartridge instead of 1.5 mL of basic methanol (2 % ammonia, w∕w). This is to avoid possible influence of ammonia in the following DTT experiments (Lin and Yu, 2011), and larger volume of methanol was used to maintain the elution efficiency (Lin and Yu, 2011). Comparison of the GC-MS peak intensities of individual HULSWS species eluted by these two protocols was provided in the Supplement (Fig. S1). The effluent was dried with nitrogen, and restored in 1 mL of DDI water for quantification. An aliquot of 20 µL of aqueous solution was injected into a high-performance liquid chromatography system (HPLC, ThermoFisher Scientific, Waltham, MA, USA) coupled with an evaporative light scattering detector (Alltech ELSD 3300, Grace, Houston, TX, USA). Since ELSD is mass sensitive, the mass of HULISWS instead of HULISWS_carbon was reported in this study. Detailed information on the HPLC-ELSD operation conditions is provided in the Supplement.
Major water-soluble ions were identified and quantified using ion-chromatography (DIONEX, ICS-2500 for cations and ICS-2000 for anions, ThermoFisher Scientific, Waltham, MA, USA, Tang et al., 2011). EC and OC were analyzed by a thermal–optical carbon analyzer (Sunset Laboratory-Based Instrument, Tigard, OR, USA, Tang et al., 2011). Hopanes were measured by in-injection thermal desorption GC-MS (Agilent 6890N–5975C, Santa Clara, CA, USA, Ho and Yu, 2004), while levoglucosan was measured using Agilent 7890A-5975C GC-MS system (Hu et al., 2008). Concentrations of hopanes, levoglucosan, water-soluble ions, EC, and OC were listed in Table S1 in the Supplement.
2.3 DTT assay
We followed the procedure of Li et al. (2009) and Lin and Yu (2011) for DTT experiments. Briefly, a 120 µL portion of HULISWS solution was transferred into an Eppendorf tube. Then 920 µL of potassium phosphate buffer (pH = 7.4) containing 1 mM diethylene triamine pentaacetic acid (DTPA) and 50 µL of 0.5 mM DTT (both > 99 %; Sigma Aldrich, St. Louis, MO, USA) were added and mixed thoroughly. The samples were subsequently placed in a dry bath at 37 ∘C for 90 min and spiked with 100 µL of 1.0 mM 5,5′-dithiobis-2-nitrobenzoic acid (DTNB, 98 %; Sigma Aldrich, USA) containing 1 mM DTPA. Considering the reaction between DTNB and DTT was very fast, the absorption could reach its maximum value immediately and stay stable for more than 2 h (Li et al., 2009). So we followed the same protocol described in Li et al. (2009) with the elimination of quenching step described in Cho et al.'s method (2005), and we conduct measurement at 412 nm within 30 min using an ultraviolet-visible (UV-Vis) spectrophotometer (8453, Hewlett Packard, Palo Alto, CA, USA). Considering that some transition metals may still remain in the HULISWS fraction even after HLB purification, a sufficient amount of DTPA was added in the procedure to chelate all the remaining transition metals, such as Cu, Mn, and Fe, to eliminate the DTT consumption by these metals (Lin and Yu, 2011). For the control samples, blank filters were used instead of real samples.
A previous study observed that the time-dependent consumption of DTT catalyzed by HULISWS was linear when DTT consumption was less than 90 % (Lin and Yu, 2011). We have also examined the HULISWS-catalyzed DTT consumption as a function of time and obtained a similar result as Lin and Yu (2011). In our study, the HULISWS-catalyzed DTT consumption of all 66 samples was between 3.6 and 77.0 %, and the measured DTT activity was linearly proportional to HULISWS mass concentration.
The HULISWS-catalyzed DTT consumption of each sample was normalized by the volume of air sampled (DTTV, defined as extrinsic DTT activity and expressed in units of nmol min−1 m−3) and the HULISWS mass (DTTm, defined as intrinsic DTT activity and expressed in units of mol min−1 µg HULISWS−1) (Dou et al., 2015; Verma et al., 2014), respectively. The mathematical expressions of DTTV and DTTm are shown below.
Since DTPA was added to suppress DTT consumption by metals ions throughout the incubation process and may affect the DTT response of quinones (Dou et al., 2015), the DTT activity of HULISWS measured here may be underestimated and is not directly comparable to those studies conducting DTT assay experiments without DTPA.
2.4 Source apportionment
In this study, the United States Environmental Protection Agency PMF 5.0 was applied to identify the sources of HULISWS and apportion their contributions to both HULISWS and the extrinsic DTT activity of HULISWS. As suggested by Henry et al. (1984), the minimum sample size of N for PMF analysis was , where V is the number of input species. A total of 66 samples and 13 species were included in PMF analysis, which was an adequate sample size to obtain a statistically reliable PMF result. Details of PMF parameter settings are provided in the Supplement.
3.1 HULISWS mass concentration and the DTT activity of HULISWS
In this study, the HULISWS mass concentration and DTT activity of HULISWS in 66 PM2.5 samples were quantified. The annual average concentration of total HULISWS in Beijing measured in this study was 5.66 µg m−3 (median: 4.30, range: 1.08–22.36 µg m−3). This was approximately 20 % higher than those measured in three other Chinese cities: 4.83 µg m−3 in Guangzhou (Kuang et al., 2015), 4.71 µg m−3 in Nansha (Kuang et al., 2015), and 4.69 µg m−3 in Lanzhou (Tan et al., 2016). A clear temporal variation of HULISWS mass concentration was observed (Figs. 1, 2), with significantly higher levels (p<0.05, Mann–Whitney test) in the heating season (November through March; average 7.93, median 6.15 µg m−3) than in the nonheating season (April through October; average 3.72, median 2.86 µg m−3). This could be mostly attributed to the intensive coal and biomass burning activities performed for residential heating during the heating season. In addition, the lower temperatures and mixing height during the heating season could also favor the formation of particle-bound HULISWS species. However, the contributions of total HULISWS to organic matter (OM, calculated by multiplying OC with 1.98 and 1.50 for the heating and nonheating seasons, respectively, Xing et al., 2013) in PM2.5 are slightly lower during the heating season (21.8 % ± 13.5 %) than that during the nonheating season (27.4 % ± 12.0 %, Fig. 1), indicating that higher levels of combustion-generated organic compounds other than HULISWS were emitted in the heating seasons as well.
The extrinsic DTT activity of HULISWS exhibited similar temporal variation as HULISWS (Fig. 2), with significantly higher levels in the heating season (average 0.073, median 0.063 nmol min−1 m−3) than in the nonheating season (average 0.031, median 0.029 nmol min−1 m−3). Because most of the inorganic ions were not retained by the HLB cartridge and the remaining metals in the HULISWS effluent were chelated by DTPA, the DTT activity measured here could be attributed entirely to the DTT active moieties in HULISWS. The intrinsic DTT activity of HULISWS describes the intrinsic ROS-generation ability of HULISWS, and the average intrinsic DTT activity of HULISWS in Beijing was 9.91 pmol min−1 µg HULISWS−1 (median 9.02, range 2.74–25.8 pmol min−1 µg HULISWS−1), which was higher than the reported average DTTm activity (6.4 ± 1.2 pmol min−1 µg HULISWS−1) in six PM2.5 samples collected during winter in Guangdong, China (Dou et al., 2015). This difference might be attributed to the different chemical components and sources of HULISWS in these two regions.
3.2 Individual species of HULISWS
Because the main objective of this study was to identify the sources of HULISWS and quantify the source-specific contributions to both HULISWS and their associated redox activity, we mainly focused on the identification of organic markers in the chemical analysis. A total of 25 species were identified and quantified in the HULISWS fraction of PM2.5 using GC-MS, including 12 aromatic acids, 5 nitrophenol analogues, 3 aliphatic acids, and 5 biogenic secondary organic aerosol (SOA) tracers (Table S2 in the Supplement, Hu et al., 2008).
All 12 aromatic acids, including 3 hydroxyl benzoic acids, 3 benzenedicarboxylic acids, 3 benzenetricarboxylic acids, 2-hydroxy-5-nitrobenzoic acid, vanillic acid, and syringic acid, exhibited higher levels during the heating season than during the nonheating season (Fig. S2 in the Supplement). Among these acids, terephthalic acid (TPha) was the most abundant (average 150.2 ng m−3 in the heating season, and 98.1 ng m−3 in the nonheating season), accounting for approximately 2 % of the HULISWS mass concentration. Compared with other Chinese cities, the concentration of TPha in Beijing was substantially higher than those in the southern cities, such as Hong Kong (19.9 ng m−3 in winter, Ho et al., 2011) and was similar to those in the northern cities, such as Xi'an (54 ng m−3 in summer and 250 ng m−3 in winter, Cheng et al., 2013). TPha is mainly used to produce polyethylene terephthalate (PET) plastics, which are widely used for bottles and containers; therefore, it has been suggested as a tracer for the pyrolysis of domestic waste (Kawamura and Pavuluri, 2010; Simoneit et al., 2005). Benzenetricarboxylic acids were considered to be secondarily formed from the photodegradation of organic precursors, such as polycyclic aromatic hydrocarbons (PAHs) (Kautzman et al., 2010). Therefore, 1,2,3-benzenetricarboxylic acid (123Ben) and 1,2,4-benzenetricarboxylic acid (124Ben) were also included in the PMF analysis.
Similar to the aromatic acids, all five nitrophenol analogues, namely 4-nitrophenol, 2-nitrocatechol, 2-methyl-4-nitrophenol (2M4NP), 4-methly-5-nitrocatechol (4M5NC), and 3-methly-6-nitrocatechol (3M6NC), exhibited 8–14 times higher concentrations during the heating season than during the nonheating season (Table S1 in the Supplement). In particular, 4M5NC and 3M6NC not only showed similar temporal variations but also were strongly correlated (R2=0.87), implying that they may have similar sources. These two compounds have been suggested as tracers for the aging process of biomass burning (Iinuma et al., 2010; Kahnt et al., 2013). However, Iinuma et al. (2010) pointed out that the photooxidation of vehicle exhausts may be a more significant source for these two compounds in urban areas. Given that both 4M5NC and 3M6NC are good anthropogenic SOA markers, they were also included in the PMF analysis.
Five biogenic SOA tracers including 3-hydroxyglutaric acid, 3-hydroxy-4,4-dimethylglutaric acid, 3-methyl-1,2,3-butanetricarboxylic acid, 3-isopropylglutaric acid, and 3-acetylglutaric acid were identified and quantified. Because they were all formed from the atmospheric oxidation of monoterpenes and had similar temporal variations, they were grouped as SOA markers of monoterpenes (MonoT) in the PMF analysis (Hu et al., 2010). Briefly, MonoT showed higher concentrations during the nonheating season (average 16.9, median 15.2 ng m−3) than during the heating season (average 12.5, median 10.2 ng m−3), which was opposite to HULISWS mass concentration. Because of the higher biogenic volatile organic compound (VOC) emissions, more intense solar radiation, and higher temperature and humidity in the nonheating season, more active secondary formation could lead to higher concentrations of biogenic SOA (Guo et al., 2012).
3.3 Source apportionment of HULISWS and their extrinsic DTT activity
The optimal PMF solution was determined with five factors (A–E; Fig. 3). The Qrobust obtained was 62.9, which was exactly equal to Qtrue, and the scaled residues for all species were between −2 and +2, indicating no outliers for this solution. Constrained model operation was adopted for a more reasonable interpretation (dQrobust % = 0.32 %) (Norris et al., 2014). The optimized solution was bootstrapped 100 times, with 100 % of the runs producing the same factors. A strong linear correlation between the measured and PMF-predicted HULISWS mass concentrations (R2=0.76) also suggested a reliable PMF solution (Fig. S4 in the Supplement).
As shown in Fig. 3, factor A had a high percentage of non-sea salt Cl− (nss-Cl−, [nss-Cl−] = [Cl−] − 1.17 × [Na+]), and was attributed to coal combustion (Tan et al., 2016; Tao et al., 2016; Zhang et al., 2013). Factor B had a high loading of levoglucosan and was determined as biomass burning (Hu et al., 2010; Tao et al., 2016). Factor C was considered to be waste incineration, due to the high level of TPha. Factor D was dominated by hopanes, tracers for fuel combustion, suggesting traffic-related activities (Hu et al., 2010). In particular, the two anthropogenic SOA markers, 4M5NC and 3M6NC, were mostly assigned to this factor (4M5NC 46 %, and 3M6NC 33 %) instead of factor C (4M5NC 14%, and 3M6NC 25 %). These two species were mainly formed through the photooxidation of cresols, which were directly emitted through wood combustion or produced from toluene through its reaction with OH radicals in the presence of NOx (Iinuma et al., 2010). Traffic emissions were a significant source of single-ring aromatics, especially toluene, in Chinese megacities (Huang et al., 2015). In this study, the sampling site was located in an urban area influenced by considerable vehicular emissions of NOx and toluene, which may have led to subsequent secondary formation of 4M5NC and 3M6NC. Therefore, the fourth factor was considered as a mixed source including both primary emission and the aging process of traffic exhausts. The fifth factor was characterized by a predominant loading of MonoT, SO, and NH; thus, it was considered as a secondary aerosol formation source.
3.4 Source-specific contributions to HULISWS
Source-specific contributions to HULISWS during both nonheating and heating seasons were calculated based on PMF results. The four combustion-related sources contributed > 80 % of HULISWS in the heating season and 50 % in the nonheating season (Fig. 4a), of which biomass burning was the most predominant. A strong correlation (R2=0.51, Fig. S5 in the Supplement) was observed between HULISWS and levoglucosan, a marker of biomass burning, and this was consistent with previous studies (Lin et al., 2010b). Approximately 33 % of HULISWS was attributed to biomass burning during the 1-year sampling period in Beijing, higher than that observed in the PRD region (8–28 %, Kuang et al., 2015). The intensive wood and crop residue burning activities in the Beijing–Tianjin–Hebei region during autumn and winter could emit a large amount of aerosols into the atmosphere (Zhang et al., 2013). Thus, as shown in Fig. 4a, the contribution of biomass burning to HULISWS in the heating season (2.96 µg m−3) was 3.5 times that in the nonheating season (0.84 µg m−3).
A previous study reported that refuse burning may contribute 1–24 % of organic particles in Asia (Simoneit et al., 2004). In this study, waste incineration was found for the first time to be an important source of HULISWS in Beijing, with a considerable and stable contribution to HULISWS throughout the year (18.7 % in the nonheating season and 17.1 % in the heating season). According to the China Statistic Yearbook (2013), 6.33 million t of domestic waste were produced in Beijing during 2012 (National Bureau of Statistics of China, 2013), among which 0.95 million t were disposed through incineration. Given that nearly 24 % of the urban waste was plastic (Wang and Wang, 2013), the incineration of such large amounts of domestic waste may explain the high levels of TPha in Beijing.
Coal has occupied the predominant position in China's energy consumption for a long time (Zhang and Yang, 2013). Therefore, coal combustion is an important source of PM2.5 pollution in China, especially in northern Chinese cities. Tan et al. (2016) identified a strong correlation between HULISWS and Cl− (R2=0.89) in Lanzhou and suggested that coal burning was probably the major contributor to HULISWS in winter. However, the contribution of coal combustion to HULISWS was found to be minor (5.8 %) in the present study. Similarly, a source apportionment analysis of PM2.5-bound water-soluble organic carbon (WSOC) in Beijing found that less than 5 % of WSOC was from coal combustion (Tao et al., 2016). This was because less oxidized compounds including PAHs were favorably produced from the aromatic fragments of coal under the fuel-rich incomplete combustion conditions; these less oxidized compounds are generally hydrophobic substances and not extracted into the HULISWS fraction.
A correlation between HULISWS and hopanes (R2=0.46, Fig. S5 in the Supplement) might suggest direct emissions of HULISWS from vehicle exhausts. As shown in Fig. 4a, vehicle emissions are responsible for 13.7 % of PM2.5-bound HULISWS. Interestingly, the amount of HULISWS assigned to vehicle exhausts was approximately 3 times higher in the heating season than in the nonheating season (Fig. 4a). This could be attributed to the low temperature in winter, which favors the partition of semivolatile HULISWS species into particle phases. Another explanation could be that more HULISWS were formed from the aging process of traffic exhausts in the heating season. To evaluate this hypothesis, multilinear regression (MLR) analysis was conducted to assess the effects of NOx, O3, SO, particle acidity (H, and particle-phase liquid water content (LWCp) on HULISWS resolved in the vehicle emissions factor (HULISWS_VE; the calculation of H and LWCp, and the MLR analysis results are provided in the Supplement). NOx was found as the only statistically significant factor that was positively correlated to HULISWS_VE with a regression coefficient of 0.012 (p<0.01; Table S3 in the Supplement), suggesting that a 1 µg m−3 increase in NOx was associated with a 0.012 µg m−3 increase in HULISWS_VE, when holding other covariates unchanged. In fact, vehicle exhausts were the major source of ground-level NOx (> 60 %) in Beijing, even in the heating season (Lin et al., 2011). A higher level of NOx was observed during the heating season than during the nonheating season due to a lower boundary layer and weaker vertical mixing (Fig. S6 in the Supplement). Kautzman et al. (2010) found that ring-opening oxygenated products with one benzyl group, which could be retained by the HLB cartridge and were considered as HULISWS components, were predominantly formed from the photooxidation of PAHs under high NOx conditions. Thus, the higher levels of NOx in the heating season led to higher levels of secondarily produced HULISWS_VE, indicating a synergistic effect of primary emission and the secondary aging process from vehicle exhausts. Furthermore, the presence of 4M5NC and 3M6NC, SOA markers of cresol, in this factor confirmed that a certain fraction of HULISWS_VE was secondarily formed.
In addition to the four combustion-related sources, one secondary source was apportioned by PMF, contributing 30.1 % of HULISWS throughout the year. MLR analysis was conducted to evaluate the effects of O3, NOx, SO, H, and LWCp on the secondary formation of HULISWS (HULISWS_SEC). Sulfate was found to be the most significant factor, with a regression coefficient of 0.066 (Table S4 in the Supplement). This may be due to the predominant role of sulfate in the particle-phase formation of organosulfates, one important HULISWS component (Xu et al., 2015), through both nucleophilic addition reactions and the salting-in effect (Lin et al., 2012; Riva et al., 2015). Results from the MLR analysis also indicated that an increase of 1 µg m−3 O3 led to an increase of 0.028 µg m−3 HULISWS_SEC. Gaseous highly oxidized multifunctional organic compounds (HOMs) were characterized in the ozonolysis of α-pinene in smog chamber experiments (Zhang et al., 2015). It was suggested that, after partitioning to the particle phase, these HOMs could undergo rapid accretion reactions to form oligomers containing multiple carboxylic acid and ester groups, which served as good HULISWS candidates. Considering the higher concentrations of O3 in the nonheating season (Fig. S7 in the Supplement), together with higher biogenic VOCs emissions and temperature as well as more intense solar radiation, a larger amount of HULISWS_SEC was produced in the nonheating season (2.01 µg m−3) than in the heating season (1.42 µg m−3).
3.5 Source-specific contributions to DTT activity of HULISWS
To gain quantitative insights into the potential health impacts of different HULISWS sources, source-specific contributions to extrinsic DTT activity of HULISWS were assessed using PMF. The strong correlation (R2=0.78; Fig. S4 in the Supplement) between measured and predicted DTT activity suggested reliable predictions.
As shown in Fig. 4b, the four combustion-related sources accounted for 75 % of the extrinsic DTT activity of HULISWS throughout the year, of which biomass burning contributed 33.6 %, followed by vehicle emissions (18.5 %), waste incineration (18.5 %), and coal combustion (4.1 %). The extrinsic DTT activity of HULISWS describes the redox activity of HULISWS on an air-volume basis (Eq. 1), which is reflective of human exposure to HULISWS, while the intrinsic DTT activities of HULISWS is on mass basis and is more important for assessing the intrinsic toxicity HULISWS from various sources. The intrinsic DTT activities of the HULISWS from the five identified sources were calculated (Eq. 2). HULISWS from vehicle emissions was found to be the most DTT-active (12.0 pmol min−1 µg HULISWS_VE−1), followed by waste incineration (9.25 pmol min−1 µg HULISWS_WI−1), biomass burning (9.10 pmol min−1 µg HULISWS_BB−1), secondary formation (7.45 pmol min−1 µg HULISWS_SEC−1), and coal combustion (6.22 pmol min−1 µg HULISWS_CC−1).
Similar to the source apportionment results of HULISWS, biomass burning was identified as the leading contributor to extrinsic DTT activity of HULISWS in the heating season (39.4 %, 0.015 nmol min−1 m−3) and throughout the year (33.6 %, 0.017 nmol min−1 m−3). During biomass burning, highly oxidized organic compounds with quinone, hydroxyl, and carboxyl groups were directly produced (Fan et al., 2016). Moreover, some of the VOCs emitted from biomass burning could undergo further reactions and generate highly redox-active products, for example, hydroxyquinones formed through •OH radical oxidation (McWhinney et al., 2013), which could be extracted into the HULISWS fraction and lead to DTT consumption (Chung et al., 2006; Verma et al., 2015a). Moreover, Wang et al. (2017) found large amounts of nitrogen-containing organic compounds (NOCs) including nitroaromatics and nitrogen-containing bases in HULISWS from biomass burning. The nitrite group next to aromatic ring in the nitroaromatics could promote electron transfer and lead to more DTT consumption and the nitrogen-containing bases emitted from biomass burning could also enhance the ROS-generation ability of HULISWS_BB (Dou et al., 2015), which may explain the observed intrinsic DTT activity of HULISWS_BB.
Secondary formation was the most important source for the extrinsic DTT activity of HULISWS in the nonheating season (44.1 %, 0.015 nmol min−1 m−3) and the second largest contributor throughout the year (25.3 %, 0.013 nmol min−1 m−3). A few smog chamber experiments have been carried out to investigate the ROS activity of SOA from various hydrocarbon precursors, and the intrinsic DTT activity values of several biogenic SOA systems (i.e. isoprene, α-pinene, and β-caryophyllene) were found to be within the range of 2 to 30 pmol min−1 µg SOA−1 (Kramer et al., 2016; Tuet et al., 2017). Tuet et al. (2017) also observed a much higher intrinsic DTT activity of naphthalene SOA than that of biogenic SOA, and suggested that this was probably due to the aromatic species, especially nitroaromatics, in naphthalene SOA. The intrinsic DTT activity of HULISWS_SEC measured in this study is 7.45 pmol min−1 µg HULISWS_SEC−1, which is within the reported intrinsic DTT activity range of biogenic SOA. Moreover, results from MLR analysis indicated that both sulfate and ozone were positively correlated with HULISWS_SEC (Table S4), suggesting that HULISWS resolved in this factor could mainly consist of some less ROS-active SOA components, such as organosulfates (Chen et al., 2011; Lin et al., 2012). Although chamber experiments reported the formation of ROS-active HOMs or organic peroxides through the ozonolysis of biogenic VOCs (Docherty et al., 2005; Zhang et al., 2015), the production yields of these peroxides were generally low and thus could not have a major influence on the DTT activity of HULISWS_SEC. However, since secondary formation predominated in HULISWS formation (Fig. 4a), especially in the nonheating season (50.1 %), even with a lower intrinsic DTT activity, secondary aerosol formation still serves as a significant contributor to HULISWS-associated redox activity in Beijing. It should be noted that the contributions of secondary formation processes to both HULISWS and DTT activity of HULISWS could even have been underestimated in this study, because HULISWS secondarily formed through the aging of biomass burning and vehicle emissions was resolved in factors B and D and could not be accurately quantified.
Although vehicle emission contributed just 18 % to extrinsic DTT activity of HULISWS throughout the year (18.5 %, 0.009 nmol min−1 m−3), HULISWS_VE has the highest intrinsic DTT activity among all sources (12.0 pmol min−1 µg HULISWS_VE−1). Similarly, Bates et al. (2015) revealed that the water-soluble PM2.5 from gasoline vehicle emissions had the highest intrinsic DTT activity, probably due to the oxygenated OC and metals on gasoline particles. Verma et al. (2009) also observed a higher aerosol oxidative potential from the aged particles of traffic exhausts than those directly emitted, and a strong correlation was observed between oxygenated organic acids and vehicle-related redox activity. As shown in Fig. 2d, most of the two methyl nitrocatechol markers were resolved in the vehicle emissions factor and HULISWS_VE was found to be significantly correlated with NOx; therefore the high intrinsic ROS activity of HULISWS_VE is believed to be mostly due to the highly oxygenated OC content, especially the highly redox-active nitroaromatics (Tuet et al., 2017).
Waste incineration was also an important primary source of the extrinsic DTT activity of HULISWS (20.5 % in the nonheating season and 17.4 % in the heating season), and its intrinsic HULISWS ROS activity was slightly higher than that from biomass burning. Mohr et al. (2009) examined the elemental ratio of aerosols emitted from different sources. They found that particles from plastic burning had a higher O ∕ C ratio (0.08) than those from diesel (0.03) and gasoline (0.04) combustion, indicating a more oxidized feature of aerosols emitted through refuse burning (Mohr et al., 2009). Considering that incineration will play an increasingly important role in waste treatment in Beijing in the following years (National Development and Reform Commission, 2016), concern should be directed to the potential threat of trash burning to public health.
In summary, four combustion-related sources and one secondary formation source of PM2.5-bound HULISWS and their associated ROS activity were identified by PMF. Biomass burning (32.7 %) and secondary aerosol formation (30.1 %) were the major contributors to HULISWS in Beijing. For the first time, waste incineration was identified as an important source of HULISWS, with a considerable and stable contribution to HULISWS throughout the year (17.7 %). Regarding ROS-generation potential, HULISWS from vehicle emissions was identified as the most ROS-active, and HULISWS from secondary aerosol formation showed a lower intrinsic DTT ability than those of most primary sources except for coal combustion. Such variations in the ROS-generation ability of HULISWS from different sources will be relevant for future inquiries into more detailed chemical speciation of HULISWS, their roles in ROS generation, and the possible oxidation mechanisms involved.
All data needed to evaluate the conclusions in the paper are present in the paper and the Supplement. Additional data related to this paper may be requested from the authors.
Information on chemical analysis; PMF source apportionment; MLR analysis together with Tables S1–S4 and Figs. S1–S7 are provided.
The supplement related to this article is available online at: https://doi.org/10.5194/acp-18-5607-2018-supplement.
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.
This work was supported by the National Natural Science Foundation of China
(NSFC21477102, 21322705 and 41421064), the Joint NSFC-ISF Research Program
(41561144007), the General Research Fund of Hong Kong Research Grant Council
(12304215, 12300914 and 201212), the Ministry of Science and Technology of
China Grants (973 program; 2015CB553401), the Faculty Research Grant from
Hong Kong Baptist University (FRG2/16-17/041), and Research and Development
of Science and Technology in Shenzhen (JCYJ 20140419130357038 and JCYJ
20150625142543472). The author would like to thank Binyu Kuang from Hong Kong
University of Science and Technology for HULISWS
Edited by: Dwayne Heard
Reviewed by: three anonymous referees
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