Abstract
For the first time, an expansive study into the concentration and extended decay behavior of environmentally persistent free radicals in PM2.5 was performed. Results from this study revealed three types of radical decay—a fast decay, slow decay, and no decay—following one of four decay patterns: a relatively fast decay exhibiting a 1/e lifetime of 1–21 days accompanied by a slow decay with a 1/e lifetime of 21–5028 days (47% of samples); a single slow decay including a 1/e lifetime of 4–2083 days (24% of samples); no decay (18% of samples); and a relatively fast decay displaying an average 1/e lifetime of 0.25–21 days followed by no decay (11% of samples). Phenol correlated well with the initial radical concentration and fast decay rate. Other correlations for common atmospheric pollutants (ozone, NOx, SO2, etc.) as well as meteorological conditions suggested photochemical processes impact the initial radical concentration and fast decay rate. The radical signal in PM2.5 was remarkably similar to semiquinones in cigarette smoke. Accordingly, radicals inhaled from PM2.5 were related to the radicals inhaled from smoking cigarettes, expressed as the number of equivalent cigarettes smoked. This calculated to 0.4–0.9 cigarettes per day for nonextreme air quality in the United States.
INTRODUCTION
Multiple studies established increases in ambient PM2.5 levels promote cardiopulmonary dysfunction and decrease life expectancy.1,2 These adverse health effects are induced by oxidative stress triggered when the cell is overwhelmed by reactive oxygen species, ROS.3 However, the exact nature of ROS formation and its source is still debatable. PM2.5 is documented to activate a toxic response from ROS generation whether from wood smoke, other biomass burning, or ambient PM2.5.4–7 Recent evidence demonstrates ROS is also generated from the redox cycling of environmentally persistent free radicals (EPFRs) from a model system in addition to EPFRs in PM2.5.8–10
EPFRs were identified initially on the surfaces of particles containing redox-active transition metals in the post flame and cool-zone regions of combustion systems.4,11,12 In addition to combustion systems, EPFRs were established in ambient PM2.5.4,13–15 Formation of an EPFR occurs when an organic precursor chemisorbs onto a redox metal site (e.g., CuO or Fe2O3) subsequently reducing the metal via electron transfer.11 This mechanism results in the generation of a persistent surface bound radical.
EPFRs associated with the particle surface impart additional stabilization to these radicals, allowing them to persist in the environment.11,16 This behavior was observed in the long lifetimes of radicals from the combustion of charcoal,17 wood, and coal.18 In the cases of wood and coal, there were two consecutive decays resulting from reaction with oxygen where the relative intensity but not the ΔHp-p of the radical signal decreased.18 Stabilized organic radical signals were additionally observed in soot from the combustion of plastics16 as well as the indefinite persistence of semiquinone radicals from cigarette smoke.19 In addition to natural samples, investigations on radical decay from a model soot system of 1-methylnapthalene and Fe2O3 were performed.20 These studies demonstrated two subsequent decays, and the presence of Fe2O3 generated longer lifetimes than the 1-methylnapthalene soot alone.20
Previous decays from model EFPR systems demonstrated a range of lifetimes in addition to the presence of multiple decays in some cases.12,21–23 For example, organic precursors chemisorbed on CuO and Fe2O3 displayed one decay with the longest lifetime on CuO (74 min) resulting from phenol.12,21 When phenol was chemisorbed on Ni and Zn, two subsequent decays were observed, and these decays were also the longest for each metal.22,23 In the case of Zn, this conveyed 1/e lifetimes of 10 days for the faster decay and 23 days for the slower decay.23 All decays from the model EPFR system implied phenoxyl radicals are the short-lived species, while semiquinone radicals are the long-lived species.12,23 Semiquinone radicals, however, were suggested to decompose into phenoxyl radicals.12,23 The differences in the aforementioned decay behavior resulted from metal speciation and, although not specifically mentioned here, the adsorbed organic precursor.
Continuing this line of investigation, we quantified the initial concentration and decay of EPFRs in freshly collected PM2.5. Observed decay rates along with initial radical concentrations were correlated among common atmospheric pollutants (ozone, NOx, SO2, etc.), meteorological conditions, and the samples’ metal content.
EXPERIMENTAL SECTION
Sampling
PM2.5 samples were acquired from the Louisiana Department of Environmental Quality (LDEQ) ambient air monitoring station situated 30 ft away from roadside and 10 ft above the ground. This site is located north of the Louisiana State University campus in Baton Rouge, LA, near heavy interstate traffic along a major industrial corridor of the Mississippi River. Samples were collected using a Thermo Scientific Partisol-Plus (Model 2025) equipped with a PM2.5 fractionator. The flow rate was 16.7 L/min, and samples were collected on a Whatman 2 μm PTFE 46.2 mm diameter filter supported by a polypropylene ring. Samples were cumulated for 24 h within a start/end time of 9:00AM from October to November of 2008, July to September of 2009, March to August of 2010, and May to October of 2011.
Electron Paramagnetic Resonance Characterization
All electron paramagnetic resonance (EPR) spectra for PM2.5 loaded filters were measured using a Bruker EMX 10/2.7 EPR spectrometer (X-band) equipped with a dual cavity utilizing modulation and microwave frequencies of 100 kHz and 9.516 GHz, respectively. Parameters for radical signal measurement were as follows: 2.05 mW power; modulation amplitude of 4.0 G; scan range of 100 G; time constant of 40.96 ms corresponding to a conversion of 163.84 ms; sweep time of 167.77 s; receiver gain 3.56 × 104; and three scans. Radical concentrations for filter bound PM2.5 were calculated by comparing the signal peak area, as calculated from the (ΔHp-p)2 multiplied by the relative intensity, to a 2,2-diphenyl-1-picrylhydrazyl standard.24 The g-factors were determined by the WinEPR program.
Decay Study
After obtaining a final weight, the filter was removed from the polypropylene supported ring and analyzed by EPR to ascertain its initial spin concentration. The time from removing the sample to initial analysis was an hour or less from the sample collection end time. The filter was placed in a controlled temperature and humidity incubator for decay studies. Accordingly, two separate temperature and humidity settings were employed for this investigation. One setting at room temperature (23 °C) and humidity (60%) while the other at a temperature of 30 °C and a relative humidity of 50 ± 5%. The lower temperature and humidity setting was chosen for comparison with previous EPFR decays. The higher temperature was performed to observe if temperature would affect the decay in addition to modeling for areas with an average higher temperature. The incubator was maintained under ambient air circulation with the aim of reproducing previous EPFR decay experiments.12,21–23 Subsequent analyses were performed intermittently, normalized to the initial spin concentration, and plotted against time from the initial analysis. An exponential regression was performed on the plotted data in order to calculate the decay rate constants and 1/e lifetimes of the radicals.
Metal Analysis
All metal analyses were achieved by extracting the metals from the filters using hot nitric acid and analyzed using an inductively coupled plasma atomic emission (ICP-AE) spectrometer.
Substituted Phenol Analysis
After decay analyses, two samples randomly chosen from each decay category were analyzed for substituted phenols (resorcinol, p-cresol, m-cresol, o-cresol, phenol, hydroquinone, and catechol). To accomplish this task, filters were placed in a 50 mL conical flask, and 10 mL of tert-butyl methyl ether (TBME) was added with 0.16 mg of o-chlorophenol as an internal standard. This was shaken for 20 min, and 250 μL of the sample extract was transferred to an amber vial with an additional 500 μL of TBME as well as 250 μL of N,O-bis(trimethylsilyl)trifluoroacetamide (BSTFA). The vial was subsequently capped using Teflon/Silicone 11 mm crimp caps and mixed. The vial contents were heated using a preheated block for 30 min at 76 °C. Determination of phenols was executed by Agilent Technologies 6890 gas chromatograph system equipped with a 5973 mass selection detector.
Meteorological Data
All meteorological data was retrieved from the LDEQ ambient monitoring station as sample collection, except for solar and ultraviolet (UV) radiation measurements which were obtained from the capitol monitoring site (less than a mile away from sample collection).
Statistical Correlations
Correlations were calculated using Pearson's correlation coefficient (ρ) where coefficients closer to 1.0 indicate a strong positive relationship; coefficients approaching 0.0 attest a weak or no relationship; and coefficients near −1.0 signify a strong negative relationship.
Calculation for Equivalent Cigarettes Smoked from Inhaling PM2.5
The number of equivalent cigarettes smoked from inhaling PM2.5 was calculated first by converting the PM2.5 radical concentration to radicals inhaled daily using eq 1
| (1) |
where RIPM represents the radicals inhaled from PM2.5 (radicals/day);, RCPM is the averaged radical concentration in PM2.5 (radicals/g), F is the conversion from g to μg, PCPM is the particle concentration of PM2.5 (μg/m3), and V is the volume of air breathed daily for an adult male (20 m3/day).25 This was then compared to the number of radicals inhaled from smoking a cigarette using eq 2
| (2) |
where EQ is the number of equivalent cigarettes smoked, RCcig is the radical concentration in cigarette tar (radicals/g tar),26–30 and Ctar is the amount of tar per cigarette (g tar/cigarette).
RESULTS AND DISCUSSION
Initial Radical Concentrations
All collected PM2.5 samples initially displayed a single, unstructured organic peak exhibiting an average ΔHp-p of 5–8 G. The relatively wide peak in addition to a lack of hyperfine splitting implied multiple organic species of the same radical family present or signal broadening by organic–metal interactions.5,11,12,15 These signals displayed initial g-factors of 2.0035(±0.0004), suggesting carbon centered radicals from polycyclic aromatic hydrocarbons or a group of semiquinone-type radicals in a complex matrix.5,11–14,16,31–33
In addition to an organic peak, the presence of paramagnetic metals was detected. These metal peaks were persistent throughout the decay and not observed to degrade. The most common peak was Fe3+ at an approximate g-factor of 2.1 attributed to Fe3+ distributed in clusters.34,35 The presence of Mn2+ (I = 5/2) was also noticed in two samples collected on April 30th and May 1st of 2010, and this is believed to result from the in situ oil burn in the Gulf of Mexico. Aside from the noticeable smell of these fumes in Baton Rouge, the NOAA HYSPLIT model calculated air trajectory during this time showed air from the burns passing over our sampler (data not shown).
The average initial radical concentration along with the number of samples for each decay category (vide infra) are displayed in Table 1, and the fast accompanied by slow decay in addition to the fast followed by no decay categories’ designation are established on the presence of multiple decay fits and their slope. The displayed concentrations resulted from an average weight of 512 ± 300 μg collected per day. The overall radical concentration is comparable to the same concentration range from cigarette smoke,5 corresponding to 69 ppm as a semiquinone. A complete list of samples’ initial radical concentration, decay rate constants, and 1/e lifetimes are given in the Supporting Information.
Table 1.
Average Radical Concentration and the Number of Samples for Each Decay Category
| decay category | avg initial radical concn (radicals/g) | # samples |
|---|---|---|
| fast decay followed by slow decay | 2.32 × 1016–3.48 × 1018 | 54 |
| slow decay | 2.02 × 1016–1.34 × 1018 | 27 |
| no decay | 2.65 × 1016–1.17 × 1018 | 21 |
| fast decay followed by no decay | 5.92 × 1016–1.99 × 1018 | 12 |
| all samples | 2.02 × 1016–3.48 × 1018 | 94 |
Decay of Radical Signal
Decay of a well behaved radical signal is presented in Figure 1. All decays resulted from a diminishing relative intensity; there was no consistent broadening or narrowing of the signal during decay with the ΔHp-p maintaining an average 6.49 ± 1.69 G for all samples. The g-factor slightly increased throughout the decay by an average of 0.0002. Although the change in the g value is small and close to the error limits, only an upward trend in g-factor was observed in all 94 samples indicating a statistically significant increase. A slight increase of g-factor suggests either a higher contribution of oxygen centered radicals from sample oxidation11,36–38 or losing more carbon centered radicals, thereby shifting the g-factor toward more oxygenated radicals.
Figure 1.
Decay of organic radical signal over 2 months as observed by EPR spectra. The g-factors are included to indicate oxidation of the radicals as the signal decays. This sample was collected on 08/28/ 2009.
There was no difference in decay behavior between the two temperature–humidity settings chosen. With PM2.5 constituents changing daily, any differences in decay rate from temperature are not apparent; however, only 30 samples were analyzed using the lower parameters, so analyzing more samples at the lower conditions might identify an observable trend.
Categories of Decay
As displayed in Figure 2, four categories of decay were observed. The majority (47%) exhibited two consecutive decays with a relatively fast decay followed by a slower decay, Figure 2A. The fast decay rate constant for this category was 0.050–0.002 h−1 corresponding to a 1/e lifetime of 1–21 days, and the slow decay rate constant was 0.002–8.00 × 10−6 h−1 equivalent to a 1/e lifetime of 21– 5028 days. The large range for the slow decay results from seven samples decaying extremely slowly yet consistently with 1/e lifetimes of 1000–5000 days. The majority of the slow 1/e lifetimes was in the range of 21–417 days.
Figure 2.
Representation of the four categories of decay observed. All represented decays occurred at 30 °C and 50% RH. All displayed lifetimes are 1/e lifetimes. (A) Representation of samples exhibiting two consecutive decays, a relatively fast decay followed by a slower decay (47% of samples). (B) Representation of samples exhibiting one slow decay (23%). (C) Representation of samples exhibiting no decay (18%). (D) Representation of samples exhibiting a relatively fast decay followed by no decay (11%).
A single slow decay was observed from approximately a quarter (24%) of the samples, Figure 2B. The decay rate constants were 0.010–2.00 × 10−5 hr−1 indicating a 1/e lifetime of 4–2083 days. Comparable to the previous category, there were two samples shifting the range with 1/e lifetimes of 833 and 2083 days. The 1/e lifetime range for the rest of the samples was 4–595 days. This range is similar to the previous category suggesting these samples may also exhibit a fast decay; however, due to a long atmospheric residence time, they may have decayed before an initial measurement.
The last two decay types were no decay (18%), Figure 2C, and a relatively fast decay followed by no decay (11%), Figure 2D. Similar to the first category, the average fast decay rate constants were 0.159–0.002 h−1 analogous to a 1/e lifetime of 0.25–21 days. Due to the unknown range of residence times in the atmosphere, decay in Figure 2C may just be after the fast decay in Figure 2D was completed.
In all cases, we attribute the faster decay (displayed as τ1/e~21 days) to decomposition of a phenoxyl-type radical.12,23 This is further supported from correlations of phenol with the initial radical concentration in addition to the fast decay rate (vide infra). The slow decay is attributed to decomposition of a semiquinone-type radical21 (displayed as τ1/e~208 and 417 days). The no decay pattern is explained by radicals entrapped in the bulk of PM2.5 or restricted in a solid matrix (i.e., internal radicals) where the unpaired electron is delocalized over many conjugated or aromatic bonds.12,16,18,39–41 These radicals remain internal cannot undergo oxidation in air and therefore persisting indefinitely.
Substituted Phenol Analysis
Of all the analyzed substituted phenols, only phenol was above the detection limit in 6 out of 12 analyzed samples and in a range of 40–55 ppm. The phenol concentration was correlated to the initial ΔHp-p, initial radical concentration, initial g-factor, and the fast/slow decay. As observed in Figure 3A, the phenol data exhibited a strong correlation with the initial ΔHp-p where the presence of more phenol increased the initial ΔHp-p. This suggested agreement with the concept of concentration broadening,42,43 where an increase in radical constituent will increase the ΔHp-p.
Figure 3.
Plots of phenol correlations. (A) Initial ΔHp-p vs phenol concentration with a correlation value of ρ = 0.95. (B) Initial spins/g vs phenol concentration with a correlation value of ρ = 0.61. (C) Initial g-factor vs phenol concentration with a correlation value of ρ = 0.97.
There was a strong association from the initial radical concentration where an increase in phenol resulted in an increased radical concentration, Figure 3B. This does not suggest only phenoxyl radicals are present in PM2.5. This is supported from the g-factor correlation, Figure 3C. A shift in g-factor occurs when there is a change in radical species. For example, existence of a semiquinone radical, one of the persistent radicals, was considered present in tobacco tar27 as well as PM,11,12 and more recently, semiquinone redox cycling was demonstrated in the oxidative capacity of PM2.5.10 The increased presence of a semiquinone radical, more oxygen centered in nature when compared to the phenoxyl radical,44 will increase the g-factor. This is corroborated by the radical signal, because the organic radical signal is a single, broad, unstructured peak in all the samples studied; therefore, multiple superimposed radical signals may be present.12,16,18
Correlations of the fast decay conveyed a very significant correlation of ρ = 0.61 (n = 6) with phenol concentration. In contrast to this, the slow decay exhibited a weak, negative correlation of ρ = −0.20 (n = 3). These associations further implicate the fast decay to occur from phenoxyl radical decomposition.
Metals Analysis and Correlation
Weakly significant or no correlations were observed with metals. This data is presented in the Supporting Information.
Meteorological and Atmospheric Pollutant Correlations
In general, meteorological correlations were not strong. The highest positive association for initial radical concentration resulted from ozone (ρ = 0.28) implying the importance of photochemical processes for EPFR formation. This is supported by positive relationships with both solar (ρ = 0.14) and UV radiation (ρ = 0.12). Correlations for the fast decay indicated the presence of ozone (ρ = −0.10) as well as solar (ρ = −0.45) and UV radiation (ρ = −0.42) decrease the fast decay rate. The previous sets of relationships demonstrate the ability of all three to increase the radical concentration; so consequently, their presence will decrease the fast decay rate due to new radical formation. Correlations for the slow decay were the weakest overall and less clear. Detailed data for meteorological conditions and atmospheric pollutants used in addition to their respective associations are presented in the Supporting Information.
Comparison of Radicals Inhaled in PM2.5 to Cigarettes
Our research demonstrated EPFRs induce various types of heart and respiratory dysfunction in rats and mice similar to those observed from smoking cigarettes.45–47 While direct comparison of EPFR effects in PM2.5 and cigarette smoke were not performed, the data suggests common EPFRs in cigarette tar and PM2.5 result in very similar human diseases.
In order to assess the potentially negative health consequences of PM2.5, the overall average concentration of radicals from PM2.5 in Baton Rouge was compared to the average concentration of radicals in cigarette smoke.26–30 The outcome is expressed as the equivalent number of cigarettes a person smokes in a day from exposure to the same number of EPFRs inhaled from polluted air, Table 2. An example calculation using the U.S. 24 h PM2.5 concentration average is given below.
Table 2.
Number of Equivalent Cigarettes Smoked from Inhaling PM2.5 with 95% Confidence Intervala
| average concentrations and regulatory standards | concentration of PM2.5 (μg/m3) | # of equivalent cigarettes |
|---|---|---|
| U.S. 24 h average | 26.9 | 0.3 ± 0.1 per day |
| U.S. yearly average | 10.6 | 47 ± 16 per year |
| EPA 24 h standard (2011) | 35 | 0.4 ± 0.1 per day |
| EPA yearly standard (2011) | 15 | 67 ± 23 per year |
| 24 h PM2.5 non-attainment locations | |||
|---|---|---|---|
| region | state | PM2.5 24 h design value (μg/m3)b | # of equivalent cigarettes |
| Chico | CA | 59 | 0.7 ± 0.2 |
| Cleveland–Akron–Lorain | OH | 36 | 0.4 ± 0.1 |
| Fairbanks | AK | 57 | 0.7 ± 0.2 |
| Klamath Falls | OR | 47 | 0.6 ± 0.2 |
| Liberty–Clairton | PA | 50 | 0.6 ± 0.2 |
| Logan | UT–ID | 40 | 0.5 ± 0.2 |
| Los Angeles–South Coast Air Basin | CA | 49 | 0.6 ± 0.2 |
| Milwaukee–Racine | WI | 37 | 0.5 ± 0.2 |
| Oakridge | OR | 41 | 0.5 ± 0.2 |
| Pittsburgh–Beaver Valley | PA | 37 | 0.5 ± 0.2 |
| Provo | UT | 50 | 0.6 ± 0.2 |
| Sacramento | CA | 51 | 0.6 ± 0.2 |
| Salt Lake City | UT | 48 | 0.6 ± 0.2 |
| San Francisco Bay Area | CA | 36 | 0.4 ± 0.1 |
| San Joaquin Valley | CA | 70 | 0.9 ± 0.3 |
| Seattle–Tacoma | WA | 46 | 0.6 ± 0.2 |
| Steubenville–Weirton | OH–WV | 37 | 0.5 ± 0.2 |
| Yuba City–Marysville | CA | 42 | 0.5 ± 0.2 |
All PM2.5 data is for 2007–2009 designation values from ref 48.
Design values are computed from PM2.5 monitoring data reported to the EPA's Air Quality System from the local agencies. Exceptional events (wildfires, construction, volcanic eruption) are not included in the calculation.
On the basis of the initial radical concentration and the U.S. 24 h air quality data, each person in the United States smokes the equivalent of 0.3 cigarettes per day from PM2.5 inhalation. The same calculation using the U.S. yearly average results in 47 cigarettes per year. In the more polluted areas (based on air quality exceedances), such as San Joaquin Valley, each person smokes nearly a full cigarette per day and as high as 101 cigarettes per year.
Overall, the decay of EPFRs in PM2.5 was observed to have three decays: a fast decay, slow decay, and no decay. These three decays were all filed into four distinct categories without any exception: a fast decay followed by a slow decay, a single slow decay, a fast decay accompanied by a slow decay, and a fast decay followed by no decay. Correlations with phenol suggested the fast decay to result from the phenoxyl radical decay. The slow decay was suggested to result from the semiquinone radical, and no decay is attributed to internal radicals restricted in a solid matrix. Due to the complexity of the PM2.5, only simple meteorological correlations could hint at the underlying cause of these decays as well as the initial radical concentration. In addition to the decay of EPFRs, a quick and novel way to assess adverse health effects was presented suggesting inhaling polluted air could be the equivalent of smoking 0.3–0.9 cigarettes a day in the United States depending on residence.
Supplementary Material
ACKNOWLEDGMENTS
The authors gratefully acknowledge support of this research from NSF Grant CHE-115-0761. The authors thank the Louisiana Department of Environmental Quality for use of their ambient air monitoring site to collect samples in addition to their monitoring data. The assistance from Dr. Lavrent Khachatryan, Dr. Slawomir Lomnicki, and Dr. Joshua Kibet was greatly appreciated.
Footnotes
The authors declare no competing financial interest.
Supporting Information
Additional details as noted in text. This material is available free of charge via the Internet at http://pubs.acs.org.
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