Articles | Volume 22, issue 22
Atmos. Chem. Phys., 22, 14987–15019, 2022
https://doi.org/10.5194/acp-22-14987-2022
Atmos. Chem. Phys., 22, 14987–15019, 2022
https://doi.org/10.5194/acp-22-14987-2022
Research article
24 Nov 2022
Research article | 24 Nov 2022

Source apportionment of VOCs, IVOCs and SVOCs by positive matrix factorization in suburban Livermore, California

Source apportionment of VOCs, IVOCs and SVOCs by positive matrix factorization in suburban Livermore, California
Rebecca A. Wernis1,2, Nathan M. Kreisberg3, Robert J. Weber2, Greg T. Drozd4, and Allen H. Goldstein1,2 Rebecca A. Wernis et al.
  • 1Department of Civil and Environmental Engineering, University of California Berkeley, Berkeley, CA 94720, USA
  • 2Department of Environmental Science, Policy and Management, University of California Berkeley, Berkeley, CA 94720, USA
  • 3Aerosol Dynamics, Inc., Berkeley, CA 94710, USA
  • 4Department of Chemistry, Colby College, Waterville, ME 04901, USA

Correspondence: Rebecca A. Wernis (rwernis@berkeley.edu)

Abstract

Gas- and particle-phase molecular markers provide highly specific information about the sources and atmospheric processes that contribute to air pollution. In urban areas, major sources of pollution are changing as regulation selectively mitigates some pollution sources and climate change impacts the surrounding environment. In this study, a comprehensive thermal desorption aerosol gas chromatograph (cTAG) was used to measure volatile, intermediate-volatility and semivolatile molecular markers every other hour over a 10 d period from 11 to 21 April 2018 in suburban Livermore, California. Source apportionment via positive matrix factorization (PMF) was performed to identify major sources of pollution. The PMF analysis identified 13 components, including emissions from gasoline, consumer products, biomass burning, secondary oxidation, aged regional transport and several factors associated with single compounds or specific events with unique compositions. The gasoline factor had a distinct morning peak in concentration but lacked a corresponding evening peak, suggesting commute-related traffic emissions are dominated by cold starts in residential areas. More monoterpene and monoterpenoid mass was assigned to consumer product emissions than biogenic sources, underscoring the increasing importance of volatile chemical products to urban emissions. Daytime isoprene concentrations were controlled by biogenic sunlight- and temperature-dependent processes, mediated by strong midday mixing, but gasoline was found to be the dominant and likely only source of isoprene at night. Biomass burning markers indicated residential wood burning activity remained an important pollution source even in the springtime. This study demonstrates that specific high-time-resolution molecular marker measurements across a wide range of volatility enable more comprehensive pollution source profiles than a narrower volatility range would allow.

1 Introduction

Organic carbon in the atmosphere spans more than 15 orders of magnitude of volatility (Jimenez et al., 2009; Donahue et al., 2011). Some of the organic carbon is emitted directly as primary organic aerosol (POA), but most organic carbon is emitted in the gas phase as thousands of distinct compounds (Goldstein and Galbally, 2007). The most volatile class, volatile organic compounds (VOCs), exists exclusively in the gas phase. Many VOCs are toxic or contribute to respiratory illness (Srivastava et al., 2005; Nurmatov et al., 2013). They play a critical role in urban and regional ozone formation (National Research Council, 1992; Atkinson, 2000) and produce lower-vapor-pressure compounds via atmospheric oxidation reactions (Seinfeld and Pankow, 2003) which form secondary organic aerosol (SOA). Intermediate-volatility organic compounds (IVOCs, defined as having an effective saturation concentration C* of 103 to 106µg m−3) and semivolatile organic compounds (SVOCs, C* of 10−1 to 103µg m−3) can partition between gas and particle phases in the atmosphere and can account for a large fraction of total organic aerosol (OA) (Robinson et al., 2007; Weitkamp et al., 2007; Chan et al., 2009; de Gouw et al., 2011; Lim and Ziemann, 2009; Presto et al., 2010). OA is a major source of uncertainty for radiative forcing predictions (Myhre et al., 2014) and negatively impacts human health (Brunekreef and Holgate, 2002; Nel, 2005; Lippmann and Chen, 2009). In the United States, it comprises 30 %–80 % of annually averaged particulate matter with a diameter of less than 2.5 µm (PM2.5; Hand et al., 2013). PM2.5 is regulated by the U.S. Environmental Protection Agency due to its adverse impacts on human health (Ridley et al., 2018).

Sources of VOCs, IVOCs and SVOCs in urban areas are changing. Historically, vehicle exhaust has been responsible for the bulk of VOC emissions in polluted urban areas such as Los Angeles, but VOC emissions from gasoline vehicles have decreased by almost 2 orders of magnitude between 1960 and 2010 (Warneke et al., 2012). Diesel emissions have also decreased, though to a lesser extent (McDonald et al., 2013). As a result, sources of non-motor-vehicle organic carbon in urban areas have increased in relative importance. McDonald et al. (2018) recently showed that volatile chemical products, including fragrances, solvents, pesticides, coatings, inks, adhesives and cleaning agents, were responsible for more VOC emissions by mass than vehicle and upstream petrochemical emissions combined in Los Angeles. Coggon et al. (2021) demonstrated the same for New York City and showed that monoterpene emissions from fragrances in Manhattan rivaled those of a comparably sized U.S. forest. Furthermore, global climate change directly affects biogenic emissions of reactive organic carbon (Heald et al., 2008; Lin et al., 2016) and, in the American West, has led to increased emissions from forest fires (Hurteau et al., 2014; Westerling, 2016); indirectly, climate change may affect pollution patterns related to heating and cooling indoor spaces. Given the changing urban and regional environments, sources of pollution in urban and suburban areas need to be continually reevaluated to improve predictions of ozone and SOA formation and inform policy decision making around emission reductions and mitigation of pollution impacts.

Many organic compounds have more than one source category contributing to their abundance in the atmosphere. Source apportionment models may be used to identify the underlying sources behind the measured concentrations of speciated organics based on the variation of individual concentration timelines. Positive matrix factorization (PMF; Paatero and Tapper, 1994; Hopke, 2016) is a technique often used to apportion VOCs (e.g., Brown et al., 2007; Yuan et al., 2009, 2012) and compositionally resolved particulate matter (e.g., Q. Wang et al., 2019; Li et al., 2020) into different factors contributing to their measured abundance. PMF does not require pollution source profiles as inputs, making it an attractive approach to analyzing contributions to ambient atmospheric abundances when not all possible sources are known.

In this work PMF was applied to concentration timelines of a suite of VOCs, IVOCs and SVOCs in the gas and particle phases measured every other hour by the comprehensive thermal desorption aerosol gas chromatograph (cTAG) over a 10 d period in Livermore, California. Our aim was to identify and understand the major sources of pollution in a suburban setting in the context of changing emission controls and dominant sources observed in other urban and suburban areas nationwide. With compounds encompassing such a wide range in volatility and degree of oxidation, we sought to more comprehensively describe the composition of the identified pollution sources. We examine the detailed temporal patterns of the different factors and provide possible explanations for their variability based on likely activity patterns, atmospheric chemistry and the meteorology of the region.

2 Methods

2.1 Sampling site

Livermore, California, is a suburban city located on the eastern edge of the San Francisco Bay Area in the Livermore Valley. It is subject to prevailing winds from the larger Bay Area region to the west, bringing primary pollutants that, combined with optimal conditions in the city itself for photochemical smog formation, often lead to the highest ozone levels in the Bay Area (Flagg et al., 2020). Regional transport is also possible from the neighboring San Joaquin Valley to the east. In wintertime, temperature inversions and low wind speeds can lead to elevated particulate matter concentrations.

Speciated VOC, IVOC and SVOC measurements were collected at the May Nissen Swim Center, 685 Rincon Avenue in Livermore (37.687 N, 121.784 W). The swim center is approximately 60 m west of Rincon Avenue, the closest road, and 1.4 km south of Interstate 580. An uncovered outdoor swimming pool, closed to public access for the season, was 10 m to the northeast of the sampling site. Approximately 100 m to the north at 793 Rincon Avenue, the Livermore Bay Area Air Quality Management District Monitoring Site obtained hourly measurements of ozone, temperature, black carbon, and wind direction and speed used in this analysis. Figure 1 shows a map of the site and surrounding area with points of interest marked.

https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f01

Figure 1Location of the sampling site in Livermore, California, indicated by a red star on the right map. The black square in the left map indicates the location of the map on the right. Points of interest are (A) Interstate 580, a major highway running east–west across the entire left map; (B) Livermore Municipal Airport; (C) breweries; (D) commercial area with restaurants close to the sampling site; (E) Bay Area Air Quality Management District monitoring site; (F) public pool. The area containing the green ponds on the western edge of the left map is a rock quarry. The rest of the San Francisco Bay Area lies to the west, while the San Joaquin Valley begins approximately 25 km to the east of the sampling site. Map images are from © Google Earth.

2.2 cTAG measurements of VOCs, IVOCs and SVOCs

Hourly VOC, IVOC and SVOC speciated measurements were collected and analyzed by cTAG between 9 April and 11 May 2018. This work analyzes data from a 10 d focus period between 11 April and 21 April when the cTAG instrument was operating optimally. Ambient air from approximately 5 m above ground was pulled through a 25 cm diameter duct to the inlet of cTAG at 1000 L min−1. This high flow rate ensured small residence times for semivolatile analytes of interest in the ducting and thus negligible partitioning to the walls of the duct. cTAG is described elsewhere in detail (Wernis et al., 2021). Briefly, 10.1 L min−1 of ambient air is pulled from the duct through a cyclone (PM2.5 cut point) and split. To measure gas–particle partitioning, on every other sample 10.0 L min−1 is passed through a denuder to remove gas-phase compounds, resulting in alternating hourly measurements of total gas plus particle concentration versus particle-phase-only concentration. This 10.0 L min−1 is then pulled through a coated metal mesh filter cell held at 30 C which collects IVOCs and SVOCs between C14- and C32-alkane-equivalent volatility (C* 10−1 to 105µg m−3). The remaining 100 sccm is pulled through a bed of adsorbent materials also held at 30 C designed to efficiently collect VOCs and IVOCs between C5- and C16-alkane-equivalent volatility (C* 105 to 1010µg m−3). After the 22 min sampling period, the collected samples are analyzed in series. The IVOC and VOC (hereafter I/VOC) collector is desorbed in helium onto the I/VOC channel gas chromatography (GC) column, which is designed for separation of volatile organics (Restek metal MXT-624, 30 m, 0.32 mm inner diameter, 1.8 µm phase). Column effluent enters the high-resolution time-of-flight mass spectrometer (HRToFMS; TOFWERK), operated at 70 eV electron impact ionization energy, to generate individual mass spectra for the separated compounds. GC analysis time is 25 min, with an initial hold for 1 min at 40 C followed by a 10 C min−1 ramp to 250 C and a 3 min hold at 250 C.

During GC and HRToFMS analysis of the I/VOC sample, desorption begins for the SVOC sample in helium saturated with the derivatization agent N-methyl-N-(trimethylsilyl) trifluoroacetamide (MSTFA). The MSTFA reacts with OH groups on polar SVOCs to make them less polar and thus more amenable to measurement on the SVOC channel GC column, which is optimized for nonpolar organics. After a reconcentration step which removes excess MSTFA and allows for faster transfer of low-volatility species from the collection filter cell, the sample is transferred to the GC column (Restek metal MXT-5, 20 m, 0.18 mm inner diameter, 2 µm phase) for separation and detection by the HRToFMS. GC analysis time is 19 min, with an initial hold for 1 min at 50 C followed by a 20 C min−1 ramp to 330 C and a 4 min hold at 330 C.

2.2.1 Compound identification

Two chromatograms with mass spectral information are generated every hour – one for I/VOCs and one for SVOCs. Typical total ion chromatograms (TICs), which include the signal from all mass-to-charge ratios added together, can contain hundreds to thousands of compounds, often leading to overlapping peaks. Single ion chromatograms (SICs) consist of the signal from a single mass-to-charge ratio and have far fewer overlaps; thus integrated peaks on the SIC of a prominent mass-to-charge ratio in the target compound's mass spectrum are used as the basis for quantification. Background subtraction isolates the mass spectral fingerprint of the target compound for better matching with searches against the 2020 National Institute of Standards and Technology (NIST) mass spectral library (National Institute of Standards and Technology, 2020) and authentic standards analyzed on cTAG or similar instruments. The retention index (RI) describes the relative location of a compound in a chromatogram to a series of reference compounds. The n-alkane retention index for a compound i is defined as follows:

(1) RI = 100 × n + t i - t n t n + 1 - t n ,

where n is the number of carbon atoms of the n-alkane that elutes immediately prior to compound i, and t is the retention time. n-Alkane RI comparisons between the target compound and candidate matches aid in conclusively identifying the target compound.

2.2.2 Compound quantification

The integrated peak area calculated for a given compound on a given chromatogram depends on a number of variable factors including but not limited to drift in the response of the detector, ion source cleanliness, transfer efficiency between the collectors and the GC columns, and derivatization efficiency (SVOC channel only). Furthermore, these variables can affect the integrated peak area in a compound-dependent way. To account for these variables, compound quantification involves a multistep process. On the SVOC channel, a constant quantity of a suite of isotopically labeled compounds with a variety of volatilities and functional groups comprising an internal standard mixture was automatically injected (Isaacman et al., 2011) onto the filter cell after every sample collection and before thermal desorption. These compounds were analyzed along with the ambient sample. Variations in integrated peak area for these compounds capture the instrument response variability described above, improving measurement precision. Ambient compound peak areas are normalized by the SIC peak area of the internal standard that most closely matches it in volatility and functionality.

In the laboratory after the field campaign, an external standard mixture consisting of 218 compounds was injected onto the filter cell in varying concentrations to obtain a six-point calibration curve for those compounds. The same internal standard mixture used during ambient sampling was injected during calibration runs, and peak-integrated ion signals of the calibrant compounds were normalized by the most suitable internal standard.

External standard calibration curves are fit with a least-squares regression. Ambient compounds with exact matches in the external standard mixture have the slope b and y-intercept a from this fit applied directly to convert peak area SA to mass MA. For ambient compounds without exact external standard matches the final mass MA is adjusted by the ratio of the fraction of signal represented by each SIC in each TIC:

(2)MA=SA-abfCfA,(3)f=sSIC/i=4400si,

where f is the fraction of TIC signal represented by the signal at the SIC used for quantification (fA is for the analyte, and fC is for the external standard calibration compound), sSIC is the quantification SIC signal, and the denominator is the sum of all SIC signals (i.e., the TIC signal). i is a mass-to-charge ratio, which ranges from 4 to 400 for this campaign and analysis.

I/VOC channel calibration is functionally equivalent to SVOC channel calibration with a couple important differences. (1) A single gas-phase internal standard, neohexane, was introduced at the inlet at a constant 100 ppt (parts per trillion) throughout every sampling period for run-to-run normalization. All analytes are normalized by neohexane. (2) External standard compounds originated from a Photochemical Assessment Monitoring Stations' 57-component commercial standard gas cylinder (Scott-Specialty), a gas cylinder with a custom mixture (Apel-Riemer Environmental, Inc., 2019) and two custom liquid mixtures. Standards were delivered with the dynamic dilution system developed for cTAG (Wernis et al., 2021), generating six-point calibrations. Neohexane could not be sampled during calibrations and so was sampled before and after each set of calibration runs, and the average was used to normalize all calibration points.

2.2.3 Uncertainty in reported concentration

There are two distinct types of uncertainty affecting reported concentrations for compounds measured by cTAG. The first, uncertainty around accuracy, arises from calibration, which affects all ambient data points of a given compound identically. Uncertainty on the least squares fit of the calibration data and uncertainty arising from the lack of an authentic external standard are uncertainties of this type. The second, uncertainty of precision, arises from run-to-run variability (Sect. 2.2.2), which we assume to be independent between samples. Internal standard normalization greatly mitigates this source of uncertainty but does not eliminate it. The uncertainty that remains depends on the choice of internal standard. The total uncertainty in the reported concentration of a given compound is all of these sources of uncertainty added together in quadrature.

Accuracy uncertainty

Accuracy uncertainty from the least squares fit is generally limited to the uncertainty of the slope, Δb, as the y intercept is kept fixed at 0 for compounds without background contamination, which is the great majority of them. The percent uncertainty from calibration fit UCb is thus

(4) U C b = 100 × Δ b b .

In practice, this adds less than 5 % uncertainty to the total for a given compound.

Compounds without an authentic external standard have an additional source of accuracy uncertainty arising from the use of a surrogate standard. This source is much greater than that from the calibration fit and impossible to quantify individually for each compound in the absence of an authentic standard to serve as the control. Jaoui et al. (2005) report approximately 30 % error from this step; we conservatively estimate 50 % uncertainty for surrogate standard use.

Precision uncertainty

Precision uncertainty is based on the choice of internal standard. To estimate this source of uncertainty, all possible pairs of internal standards were ratioed for all ambient data points and each distribution of ratios analyzed, a technique used with previous TAG instruments (Isaacman et al., 2014). Ideally, all internal standards would vary proportionally, and the ratio between two standards would remain constant, implying no error from internal standard choice. In practice the ratio varies between samples, and the relative standard deviation (RSD, standard deviation divided by mean) of the ratios provides an estimate of the precision uncertainty.

Figure S1 shows the relative standard deviations of the internal standard ratios for all internal standards used for normalization in this analysis, and Fig. S2 shows examples of the distributions of ratios. Overall, hydrocarbons paired with hydrocarbons have the lowest RSDs, especially for compounds with similar RIs. An exception is made for compounds with a RI below 1400, where occasional losses during the refocusing step due to high ambient temperature increase the variability. Ambient compounds in this category are normalized by deuterated n-tetradecane. Oxygenated internal standards exhibit the greatest RSD values whether they are paired with hydrocarbons or other oxygenates. Ambient oxygenated compounds are thus assigned the highest uncertainty and are normalized by the nearest deuterated oxygenate if their RIs are within 200 and the nearest hydrocarbon otherwise. Table S1 summarizes the categories of precision uncertainty assigned to ambient compounds for this analysis.

https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f02

Figure 2The 13-factor solution factor profiles. Compounds are ordered as in Table 1 using the indices assigned. Unlabeled groups are labeled “other” in Table 1. The shaded areas behind each profile represent 5th and 95th percentile contributions based on bootstrapping analysis, as described in Sect. S2.3.

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https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f03

Figure 3(a) Time series of wind speed and direction, (b) time series of temperature (left axis) and ozone (right axis) measured at the Bay Area Air Quality Management District monitoring site, and (c) all factor timelines stacked. Date labels are at midnight.

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https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f04

Figure 4(a) Factor 1 timeline. Date labels are at midnight. (b) Diurnal profile for Factor 1. IQR = interquartile range. (c) Rose plot showing the correlation of emissions and wind direction, using only data points where the concentration was elevated, defined as >1 standard deviation above the mean factor concentration. Frequency of observations are represented by the length of each wedge, where each ring corresponds to one observation. Shading corresponds to quartiles of factor concentration (darker = greater concentration). (d) Factor 1 composition profile. Compounds are ordered as in Table 1 using the indices assigned. Unlabeled groups are labeled “other” in Table 1. The shaded areas behind each profile represent 5th and 95th percentile contributions based on bootstrapping analysis, as described in Sect. S2.3.

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2.3 Positive matrix factorization

Positive matrix factorization is a mathematical source apportionment technique that groups measured ambient compounds based on their covariance in time, taking into account their measurement uncertainty (Paatero and Tapper, 1994). PMF is a receptor-only model that requires no a priori information about pollution sources, instead inferring source composition from the compound groupings in the solution. The solution is constrained to non-negative values and assumes source profiles do not vary with time. It takes the form of three matrices G, F and E such that

(5) x i j = k = 1 p g i k f k j + e i j ,

where xij is an element of the m×n matrix X of input data. As applied to this cTAG dataset, the m rows of X are the individual compounds, and the n columns of X are the sample times. Element gik of G represents the source contribution of the ith compound to the kth factor, and element fkj of F represents the kth factor at sample j. E is the m×n matrix of residual values. Crucially, the total number of factors p is an input to the model, requiring the model user to use PMF solution diagnostics and outside information to determine the most meaningful number of factors. The solution is determined by minimizing the sum of squares of error-weighted residuals, known as the quality of fit parameter Q, given by

(6) Q = i = 1 m j = 1 n e i j σ i j 2 ,

where σij is the uncertainty in concentration units for compound i at sample j, and eij is the corresponding element of matrix E.

This analysis is performed on 2 h time resolution data aligning with the gas plus particle-phase concentration measurements on the SVOC channel. For the PMF, I/VOC channel data that coincide with particle-only measurements on the SVOC channel are not used, though the full hourly resolution I/VOC data are used for other data analysis (e.g., correlations) and in figures. Similarly, particle-only data on the SVOC channel are not used in the PMF analysis, but partitioning information does inform some of the interpretation of factor results.

In this analysis the precision uncertainty (Sect. 2.2.3.2) is the only uncertainty assigned to each compound for use in the PMF model, since the model assumes uncertainty between samples is independent, which is not true of the accuracy uncertainties described above (Sect. 2.2.3.1). In the final PMF solution, accuracy uncertainty increases the uncertainty of the factor timelines (while preserving ratios between individual data points) but not the source contributions. PMF modeling was carried out with the U.S. Environmental Protection Agency PMF 5.0 program (Norris et al., 2014). The program automatically handles uncertainty for concentrations near the detection limit by applying a smooth function to the uncertainty between the input percent uncertainty (applies to concentrations the detection limit) and a large fixed fraction of the detection limit (applies to concentrations at or below the detection limit). We use the “robust” mode of the PMF algorithm, which limits the weight of outliers (eij/σij>4) by increasing the uncertainty of those outliers. We also explore the stability of the most plausible solutions by varying FPEAK, a parameter which applies rotations by adding G columns to each other and subtracting F rows from each other or vice versa (Paatero and Hopke, 2009).

3 Results and discussion

Of 163 ambient compounds processed in the dataset, 123 were used in the PMF analysis. The remaining 40 were excluded for one of the following reasons: the compound's concentration was below the detection limit more than 90 % of the time (27 compounds), the compound was determined to have too much instrument contamination to be quantifiable (7 compounds), the compound could not be definitively identified (3 compounds), the compound's transfer losses were not well characterized due to being outside cTAG's designed optimal volatility range (2 compounds), or the compound is nonreactive in the atmosphere (1 compound).

Of the 123 compounds used in the PMF analysis, 58 compounds were measured on the I/VOC channel, and the remaining 65 were measured on the SVOC channel. Table 1 shows the compounds included in the PMF analysis. Major compound categories represented include branched and linear alkanes and aromatics important for photochemical smog formation, monoterpenes and other biogenic compounds, polycyclic aromatic hydrocarbons, biomass burning markers, alkanoic acids, chlorobenzenes, and plasticizers and other industrial chemicals.

Table 1Compounds measured by cTAG and included in the PMF analysis. The compound index is used in Figs. 2, 4–7, 10–17 and 19. PAH = polycyclic aromatic hydrocarbons; Ox. = oxidation; Alk. Acids = alkanoic acids; HCs = hydrocarbons; BB = biomass burning; THM = trihalomethanes; DCB = dichlorobenzenes; DEHA = bis(2-ethylhexyl) adipate; DEHP = bis(2-ethylhexyl) phthalate; D4 = octamethylcyclotetrasiloxane; D5 = decamethylcyclopentasiloxane; PCBTF = parachlorobenzotrifluoride; CAS no. = Chemical Abstracts Service Registry Number; SD = standard deviation.

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3.1 Positive matrix factorization solution

We find the 13-factor PMF solution to best resolve the pollution sources in Livermore in spring 2018. Solutions between 3 and 16 factors were considered and are contrasted in Sect. S2. In summary, solutions with additional factors have less uniqueness between factors, and the source profiles of the additional factors either are not physically meaningful or are too similar to factors present in the 13-factor solution. Solutions with fewer factors fail to separate factors with meaningful physical interpretations and do not incorporate one of the largest reductions in Q/Qexp (defined in Sect. S2.1).

The 13-factor solution has a Q/Qexp value of 0.79 which is close to 1, implying the data are neither overfitted nor underfitted (Ulbrich et al., 2009). Positive FPEAK rotations increase factor cross correlations and Q/Qexp and were therefore not considered (Figs. S4 and S5). Negative FPEAK rotations slightly decrease factor cross correlations but increase Q/Qexp. We chose to proceed with the unrotated solution because the improvement in factor cross correlations for negative FPEAK rotations was minor and because the unrotated solution minimizes Q/Qexp.

Figure 2 shows the factor profiles for the 13-factor solution. Relevant meteorological data and stacked factor timelines are plotted in Fig. 3. The factors are presented in the order that they first appear in the PMF solution for increasing number of factor solutions, e.g., Factor 9 in the 13-factor solution is approximately equivalent to the 9th factor in the 9-factor solution. The factors are (1) long-lived and continuously emitted compounds, (2) episodic petrochemical source, (3) gasoline, (4) oxidized urban and temperature-driven emissions, (5) consumer products, (6) primary biogenic and diesel, (7) parachlorobenzotrifluoride (PCBTF), (8) secondary oxidation and persistent personal care product emissions, (9) biomass burning, (10) industrial and/or agricultural background and continuous combustion source, (11) early morning cooking and diesel event, (12) isoprene, and (13) possible jet fuel event. Factor timelines, composition, diurnal profiles and wind direction information are presented in individual figures for each factor (Figs. 4–7, 10–17 and 19), but Figs. S6, S7 and S8 show timelines, diurnal profiles, and wind roses respectively for all the factors to facilitate cross-comparisons.

Compounds measured on the I/VOC channel dominate by mass, representing 87 % of the total mass of the 123 included compounds. No factor had less than 50 % of its mass in VOCs and IVOCs (Fig. S9a), reflecting the fact that even a small fractional contribution from a VOC or IVOC is significant compared to large fractional SVOC contributions due to the generally greater concentrations involved. SVOC mass was less evenly distributed between factors than I/VOC mass (Fig. S9b), controlled in part by stearic acid and bis(2-ethylhexyl) adipate (hereafter DEHA) contributions (Table 1).

Since uncertainty generally scales with concentration, even the error in the contribution of a high-mass VOC such as chloroform could be greater than the contribution from the most prominent SVOCs, making drawing conclusions from the mass composition of factors challenging. Additionally, this analysis is not a comprehensive account of all the organic carbon in the measured volatility range; there could be compounds that were not quantified (and thus were excluded from this analysis) that would contribute significant mass to the determined factors. For these reasons, our factor interpretations are mainly based on which compounds have the greatest portion of their mass in each factor (“mass fraction”) rather than which compounds contribute the most mass. The latter information is included in Sect. S5 for interested readers.

3.2 Factor 1: long-lived and continuously emitted compounds

Factor 1 (profiled in Fig. 4) is mainly a long-lived, well-mixed species and a species with continuous emissions. Chloroform and bromoform have the highest fraction of their mass in this factor compared to other factors (33 % and 28 % respectively; this quantity for each compound is hereafter referred to as “mass fraction”). Other well-represented compounds include 4-hydroxybenzoic acid (mass fraction 35 %), p-anisic acid (26 %), phthalimide (37 %), 2-cyclopenten-1-one (32 %) and 2-methoxynaphthalene (33 %) (Fig. 4d). The diurnal profile of this factor (Fig. 4b) indicates mild nighttime concentration enhancement, but with large variability, and compounds with a slightly opposite diurnal profile (e.g., 4-hydroxybenzoic acid, phthalimide) can also be found in this factor. When Factor 1 is elevated, winds come predominantly from the southwest (Fig. 4c). This factor contains high fractional contributions from VOCs, IVOCs and SVOCs, representing a source profile that could not previously be obtained in a single instrument without the expanded volatility range afforded by cTAG.

https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f05

Figure 5(a) Factor 2 timeline. (b) Diurnal profile for Factor 2. (c) Rose plot showing correlation of elevated emissions and wind direction. (d) Factor 2 composition profile. See Fig. 4 description for further information on how to read this figure.

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Both chloroform and bromoform have atmospheric lifetimes of weeks or more (World Meteorological Organization et al., 2019), allowing them to be well-mixed in the troposphere and to therefore have stable concentrations unaffected by meteorological phenomena such as boundary layer height changes. Chloroform accounts for about 40 % of the total mass of Factor 1.

The other compounds present in this factor have the common characteristics of (1) being constantly present and (2) having a weak to nonexistent diurnal variation, but their known sources are distinct, and they are much more reactive than chloroform and bromoform. 4-Hydroxybenzoic acid and p-anisic acid have been identified as tracers for the burning of grasses (Simoneit, 2002) and have an estimated atmospheric lifetime with respect to OH ([OH] =2×106 molec. cm−3 for this and every atmospheric lifetime estimate hereafter) of about a day (U.S. EPA, 2022c, f). Phthalimide is a fungicide and insecticide degradation product produced in the processing of crops. It may also be formed from phthalic anhydride and primary amino groups in the high-temperature desorption process just before chromatographic separation, a possibility that we cannot rule out (Gao et al., 2019). Phthalimide has an estimated OH lifetime of a few hours (U.S. EPA, 2022g). Atmospheric studies of 2-cyclopenten-1-one, which is naturally occurring and biologically significant (National Center for Biotechnology Information, 2022d), and of 2-methoxynaphthalene, which has industrial sources and uses (European Chemicals Agency, 2022), are lacking. The latter has an estimated lifetime with respect to reaction with OH of a few hours (U.S. EPA, 2022a).

https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f06

Figure 6(a) Factor 3 timeline. (b) Diurnal profile for Factor 3. (c) Rose plot showing correlation of elevated emissions and wind direction. (d) Factor 3 composition profile. See Fig. 4 description for further information on how to read this figure.

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https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f07

Figure 7(a) Factor 4 timeline. (b) Diurnal profile for Factor 4. (c) Rose plot showing correlation of elevated emissions and wind direction. (d) Factor 4 composition profile. See Fig. 4 description for further information on how to read this figure.

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These relatively reactive compounds must have constant emission sources to produce timelines with so little variability. Agricultural activity may be able to account for 4-hydroxybenzoic acid, p-anisic acid, phthalimide and 2-cyclopenten-1-one, perhaps from the vineyards approximately 4 to 5 km to the south of the sampling site.

3.3 Factor 2: episodic petrochemical source

Factor 2 (profiled in Fig. 5) is a transient source, elevated during the first few days of the measurement period and nearly nonexistent after that. It contains minor contributions from C20–C25 n-alkanes (mass fraction 20 %–50 %), 1-octadecanol (31 %) and some semivolatile phthalates ( 25 % each). Winds tend to originate from the west when this factor is high (Fig. 5c).

The heavy n-alkanes are split between Factors 2 and 4 (oxidized urban and temperature-driven emissions), with slightly different distributions; the Factor 2 n-alkanes skew slightly lighter, while Factor 4 includes contributions from C26 and C27 alkanes. C20–C27 n-alkanes are associated with petroleum-based products (Simoneit, 1999). (Biogenic sources of heavy alkanes exhibit a preference for alkanes with an odd number of carbon atoms over those with an even number (Simoneit, 1989), which is not observed in this dataset, confirming the fossil fuel origin of the n-alkanes.) Two possible sources in this study are motor oil (Caravaggio et al., 2007; Mao et al., 2009; Isaacman et al., 2012) and asphalt (Rogge et al., 1997; Khare et al., 2020), both of which exhibit temperature-dependent evaporation of alkanes in this carbon number range. Since the alkane distribution is different between the two factors, it is reasonable to assume the elevated levels of some of these alkanes at the beginning of the campaign represent a different source than the regular afternoon maxima characteristic of Factor 4. The center of the n-alkane mass distribution in motor oil is typically at C25 or greater, though Isaacman et al. (2012) observed a peak at C24 for motor oil aerosol particles due to preferential evaporation of lighter alkanes at low temperatures. Maximum fresh asphalt alkane emissions occur at C14, though after 2 to 3 d emission is approximately constant across C14–C32 alkanes (Khare et al., 2020). Since the alkane distribution of asphalt emissions skews lighter, one possibility is that the elevated concentration of Factor 2 in the first few days is in part due to fresh paving nearby. However, the composition of motor oil is highly variable (Mao et al., 2009); the sources of alkanes in Factors 2 and 4 could be two different motor oils, for example, or could represent fresh versus older asphalt.

https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f08

Figure 8Timelines of select alkanoic acids (left axis) and temperature (right axis) for the study period.

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https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f09

Figure 9Timelines of nitrophenol isomers (left axis) and temperature (right axis) for the study period.

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The semivolatile phthalates in this factor, dibutyl phthalate and benzyl butyl phthalate, are plasticizers used as coatings in manufactured goods and in building materials (Zota et al., 2014). Their emission exhibits temperature dependence (Fujii et al., 2003). In this study, their concentrations are moderately correlated with temperature (r=0.59 for dibutyl phthalate and r=0.42 for benzyl butyl phthalate), unlike the less volatile plasticizers bis(2-ethylhexyl) adipate and bis(2-ethylhexyl) phthalate, which correlate very strongly with temperature and mostly show up in Factor 4, as well as the more volatile phthalates associated with personal care products (see discussion for Factor 5). Again we may speculate a unique and temporary source for these two compounds at the beginning of this field campaign, plausibly related to construction activity that could also be responsible for n-alkane emissions from fresh asphalt.

1-Octadecanol has vegetation and microbial (Nolte et al., 2002; Simoneit, 2006), biomass burning (Nolte et al., 2001), and anthropogenic (as detergent; Mudge et al., 2012) origins. 1-Octadecanol does not appear in Factor 9 (biomass burning), though two short elevated concentration periods on the evening of 16 April and the early morning of 17 April coincide with one of the biomass burning episodes. Given the non-persistent nature of Factor 2 and 1-octadecanol, an intermittent anthropogenic detergent source seems more likely than a biogenic source, which would likely emit continuously or at least regularly throughout the sampling period.

3.4 Factor 3: gasoline

Factor 3 (profiled in Fig. 6) is designated as primary gasoline exhaust. Compounds with the highest mass fraction in this factor include linear, branched and aromatic hydrocarbons with 6 to 10 carbon atoms and polycyclic aromatic hydrocarbons (PAHs), especially naphthalene and methylnaphthalenes. These are the main organic components of gasoline exhaust (Schauer et al., 2002b; Gentner et al., 2013). Palmitoleic acid also has a high mass fraction contribution, and octamethylcyclotetrasiloxane (D4) and decamethylcyclopentasiloxane (D5) are present. In periods of high concentration for this factor, wind speeds were low (about 1 m s−1 or lower), and wind directions were variable, with a slight preference for a northeastern origin (Fig. 6c).

This factor exhibits a strong diurnal pattern with sharp peaks in concentration in the early morning (between 05:00 and 07:00 local standard time or 06:00 and 08:00 local daylight time, which was in effect during the measurement period) and near-zero loading at other times of day. This factor strongly correlates with NOx (Pearson's r=0.88) and anti-correlates with ozone (r=-0.66). With over 80 % of Livermore workers commuting by private vehicle or car pool (United States Census Bureau, 2019), the early morning elevated concentration is likely commute-related. Our hypothesis for the exhibited diurnal profile is as follows. First, emissions of both hydrocarbons and NOx from automobile tailpipes are low overnight but increase in the early morning hours as morning commutes begin with cold engine starts. Drozd et al. (2016) found that emissions from cold starts dominate non-methane organic gas emissions from light duty vehicles, with over 45 km of driving required to match the initial cold start emissions for over 97 % of light duty vehicles in use in the United States today. The morning peaks are correlated with, and enhanced by, cooler temperatures and generally slower wind speeds (Fig. 3). The shallow planetary boundary layer overnight and absence of sunlight allow NOx and hydrocarbons to build up, raising measured concentrations. As the day progresses, the boundary layer rises and wind speeds increase, diluting species near ground level, and photochemistry begins, reacting away hydrocarbons and NOx and producing ozone. Late afternoon and evening return commutes have greatly reduced emissions because vehicle catalytic converters are already hot by the time drivers return to the predominantly residential area surrounding the sampling site. Higher ambient temperatures in the afternoon also contribute to reduced cold start emissions, and greater wind speeds and more rapid oxidative loss prevent what emissions are still being produced from building up. In the late evening and night, emissions remain low, and thus concentrations also remain low despite the low boundary layer and lack of photochemistry.

Factors 5 and 6 and many marker compounds share this general pattern of elevated concentrations exclusively in the early morning hours. They are governed by the same large-scale atmospheric processes. Thus while differences exist which allow them to be separated by the PMF model, which will be discussed in the descriptions for those factors, their overarching similarity means the sources are not separated perfectly. For example, palmitoleic acid is primarily a tracer of cooking (Rogge et al., 1996; Robinson et al., 2006) yet has its highest mass fraction in this factor, while other cooking tracers appear in other factors. Together with the overall similarity in variability between gasoline and cooking markers, palmitoleic acid's low and noisy signal may have caused it to be placed in this factor primarily by the model, even though it does not originate from the same pollution source. The high uncertainty of palmitoleic acid's allocation between factors 3, 5, 11 and 13 (compound 99 in Fig. 2) confirms this.

D4 and D5 siloxanes have substantial fractions of their mass in this factor (23 % and 27 % respectively). D5 has been established as a tracer compound for personal care product emissions (Horii and Kannan, 2008; Wang et al., 2009; Coggon et al., 2018). It is also prominent (mass fraction of 28 %) in Factors 5 and 8, which both contain fragrance compounds commonly found in consumer products, including personal care products. The fact that D5 is present in Factors 3, 5 and 8 while the fragrance compounds are only present in Factors 5 and 8 could be reflective of different emission rates from those products. D5 is found in the greatest concentrations in antiperspirants (Wang et al., 2009); once applied, while emissions are highest immediately after application, it evaporates over the course of several hours (Montemayor et al., 2013) and has even been directly measured in an engineering classroom in the afternoon (Tang et al., 2015) and outside an automobile in cabin fan exhaust from human occupants who had applied D5-containing personal care products earlier that day (Coggon et al., 2018). Evaporation of monoterpenes and monoterpenoids, which comprise the vast majority of the mass of fragrance compounds measured in this study, is likely to happen much faster due to their greater volatility (National Center for Biotechnology Information, 2022a, b, c, e, f, g). A study of evaporation of 300 µL of essential oils indoors found that most VOC mass, including most monoterpene mass, was emitted during the first 30 min (Su et al., 2007).

D4 is mainly indicative of adhesive and pesticide use (Gkatzelis et al., 2021) but is also found in consumer products (Horii and Kannan, 2008; Wang et al., 2009), though it is not present in Factor 5, the consumer product factor. If the D4 measured in Livermore is from consumer products, it is not clear why the peak concentration coincides with the gasoline markers later in the day than the peak of the other consumer product compounds.

It is likely that some mass from the diesel emission source is in this factor. Black carbon, which originates almost entirely from diesel emissions (Gentner et al., 2013), correlates best with this factor (r=0.84), suggesting some of the variability in this factor is driven by diesel exhaust emissions of compounds found in both gasoline and diesel exhaust.

3.5 Factor 4: oxidized urban and temperature-driven emissions

Factor 4 (profiled in Fig. 7) represents aged urban emissions and temperature-driven emissions. This factor includes heavy n-alkanes (C20–C27), as well as the n-alkanoic acid series (C8–C18), with approximately 30 %–50 % of the mass of each compound in these two classes included in this factor. Several other compounds are also present, including DEHA (62 %), bis(2-ethylhexyl) phthalate (hereafter DEHP; 46 %), phthalic anhydride (42 %), 4-nitrophenol (38 %), aromadendrene (37 %) and azelaic acid (33 %). This factor contains the largest fraction of semivolatile mass of any of the factors (Fig. S9a) largely due to the presence of DEHA and the fatty acid series. Factor 4 correlates strongly with temperature (Pearson's r=0.82), peaking in the middle to late afternoon. Winds are moderately strong and from the west when this factor is elevated (Fig. 7c). The smooth variation in concentration of Factor 4 suggests a regional source rather than a local one, which would likely display greater inter-hourly variability in concentration and greater sensitivity to small changes in wind direction.

DEHA and DEHP are both semivolatile plasticizers found in polyvinyl chloride, commonly found in building materials (Liu and Little, 2012; Shi et al., 2018; Bui et al., 2016). Like Factor 4, these two compounds correlate strongly with temperature (r=0.83 for DEHA and r=0.73 for DEHP), consistent with temperature-dependent emissions which have been observed in controlled studies (Clausen et al., 2012; Fujii et al., 2003; Liang and Xu, 2014). The heavy alkanes are discussed in detail in the Factor 2 (episodic petrochemical source) section. They are known to originate from evaporative, temperature-dependent sources such as motor oil and asphalt, consistent with the temporal profile of Factor 4.

The remaining compounds represented in this factor are not likely to originate from evaporative sources but given the consistent winds from the west could represent oxidized emissions transported from the east and south Bay Area. Phthalic anhydride is a secondary product of the photooxidation of naphthalene, and phthalic acid has been found in secondary organic aerosol formed from naphthalene photooxidation (Chan et al., 2009; Kleindienst et al., 2012; Wang et al., 2007). During the study period, conditions for optimal photooxidation (i.e., high solar flux) coincided with periods of high temperature, causing these distinct source categories to appear in the same PMF factor.

In urban and suburban areas, the n-alkanoic acid homologous series is most often ascribed to cooking emissions (Schauer et al., 2002a; Robinson et al., 2006; Allan et al., 2010; Mohr et al., 2012; Yao et al., 2021), but biomass burning, motor vehicle exhaust and road dust can all contribute (Schauer et al., 1996; Rogge et al., 1996). The fatty acids also originate from terrestrial microbial activity (Simoneit and Mazurek, 1982) and marine phytoplankton (Kawamura et al., 2003), sources that tend to dominate in remote areas (Kawamura et al., 2003; Cahill et al., 2006; Fu et al., 2014; Boreddy et al., 2018). Alkanoic acids from cooking exhibit a distinct diurnal profile, with elevated concentrations around dinnertime and occasionally another similar peak around lunchtime (Allan et al., 2010; Mohr et al., 2012; Dall'Osto et al., 2015; Yao et al., 2021). In this study, palmitic (C16) and stearic (C18) acids, which are emitted from meat cooking (Rogge et al., 1991), do show occasional evening elevated concentrations (not captured in the Factor 4 profile), but the other alkanoic acids do not. The defining feature that likely caused the fatty acids to be grouped in this factor is the period of sustained elevated concentrations between the evenings of 13 April and 15 April, with almost no diurnal sensitivity (Fig. 8). This temporal profile is inconsistent with local emissions from the sources mentioned above, but an elevated regional background transported from urban areas to the west could explain the variability. Azelaic acid, the C9 dicarboxylic acid, has similar sources to the n-alkanoic acids (Kawamura and Bikkina, 2016) and a similar temporal profile to palmitic and stearic acids, including brief evening spikes in concentration likely from cooking and the 2-day period of elevated concentration.

The timeline of the sesquiterpene aromadendrene exhibits the same period of sustained elevated concentration as the alkanoic acids and azelaic acid. Sesquiterpene emissions from plants are temperature dependent (Duhl et al., 2008; Bouvier-Brown et al., 2009). Emission outpaces loss on some days despite aromadendrene's very high reactivity with ozone (Pollmann et al., 2005) and the hydroxyl radical (Ng et al., 2007).

4-Nitrophenol is strongly represented in this factor (38 % mass fraction), while its isomer 2-nitrophenol does not contribute at all. Both nitrophenols are emitted during motor vehicle combustion (Nojima et al., 1983; Tremp et al., 1993) and in some industrial manufacturing (Harrison et al., 2005b). Biomass burning also leads to production of 4-nitrophenol and possibly 2-nitrophenol (see Factor 9 discussion). Secondary formation of nitrophenols occurs from photooxidation of aromatic hydrocarbons such as benzene, toluene, phenol and cresol (Harrison et al., 2005b). Primary emissions from vehicles and secondary formation are thought to be the most important sources of nitrophenols in polluted urban environments (Inomata et al., 2013; Lu et al., 2019).

4-Nitrophenol is observed in greater concentrations than 2-nitrophenol in this study both on average and at each data point except for about 10 nighttime samples (Fig. 9), even in the gas phase. This is in contrast to other studies (Lüttke et al., 1999; Cecinato et al., 2005), though most modern studies did not distinguish between the two isomers (Yuan et al., 2016; Cheng et al., 2021; Wang et al., 2020; Salvador et al., 2021) or did not quantify 2-nitrophenol (Kitanovski et al., 2012; X. Wang et al., 2017; L. Wang et al., 2018; Y. Wang et al., 2019). Nitrophenols from vehicle exhaust show a mild preference for the ortho isomer (Nojima et al., 1983; Tremp et al., 1993), and gas-phase secondary formation favors 2-nitrophenol as well (Harrison et al., 2005a). Liquid-phase secondary formation is likely to be an important production mechanism for nitrophenols, but the ratio of isomer production for this process is unknown (Harrison et al., 2005a). Observations of particle-phase nitrophenol show a strong preference for the para isomer (Lüttke et al., 1999; Harrison et al., 2005b) likely due to its much lower vapor pressure and much higher Henry's law constant (Sander, 2015; U.S. EPA, 2022b, d), but 4-nitrophenol is observed predominantly in the gas phase in this study, consistent with other studies (Yuan et al., 2016; Cheng et al., 2021). There are several loss processes of gas-phase nitrophenol, with photolysis thought to be the most important (Vione et al., 2009; Yuan et al., 2016), though comparison of gas-phase photolysis between 2-nitrophenol and 4-nitrophenol is not currently feasible (Chen et al., 2011; Sangwan and Zhu, 2018).

Our data suggest 2-nitrophenol is emitted and concentrated in the nighttime hours and lost in the daytime, while 4-nitrophenol either is not lost during the daytime or has an additional daytime source that 2-nitrophenol lacks, such as regional transport from the Bay Area to the west. The state of the existing literature leaves both possibilities open, and without more information it is not possible to determine what is causing the difference in profiles between these two isomers.

3.6 Factor 5: consumer products

Factor 5 (profiled in Fig. 10) is designated as consumer product emissions. It consists of limonene and other biogenic compounds, D5 siloxane, brominated and chlorinated hydrocarbons, and small contributions from volatile diesel markers. Of the biogenic compounds present, monoterpenes, methyl salicylate and α-isomethyl ionone are well represented, while isoprene, the monoterpenoids camphor and eucalyptol, the sesquiterpene aromadendrene, and α-pinene oxidation products pinic and pinonic acid are not. When the concentration of this factor is high, winds come exclusively from the northeast, though wind speeds are low (<1 m s−1) (Fig. 10c). The diurnal profile of this factor qualitatively resembles that of Factor 3 (gasoline), with strongly elevated concentrations in the early morning hours exclusively. Peak consumer product emissions occur slightly earlier than gasoline emissions on average, from about 04:00 to 06:00 local standard time or 05:00 to 07:00 local daylight time (Fig. 10b).

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Figure 10(a) Factor 5 timeline. (b) Diurnal profile for Factor 5. (c) Rose plot showing correlation of elevated emissions and wind direction. (d) Factor 5 composition profile. See Fig. 4 description for further information on how to read this figure.

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https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f11

Figure 11(a) Factor 6 timeline. (b) Diurnal profile for Factor 6. (c) Rose plot showing correlation of elevated emissions and wind direction. (d) Factor 6 composition profile. See Fig. 4 description for further information on how to read this figure.

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As a monoterpene, limonene is often considered to originate from biogenic sources, but limonene is also used ubiquitously in personal care products and cleaning products as a fragrance (Logue et al., 2011; Steinemann et al., 2011). Coggon et al. (2021) showed that fragranced products are the dominant source of limonene in some urban areas. While limonene is the monoterpene typically found in the highest concentrations in fragranced consumer products, the other monoterpenes included in this PMF analysis (α-pinene, β-pinene, camphene and 3-carene) are also common components of consumer products (Steinemann et al., 2011; Steinemann, 2015). The early morning spikes in concentration just before gasoline markers become elevated is consistent with consumer product use by individuals preparing for their day before starting their cars to drive to work. In contrast, studies reporting monoterpene concentrations in rural or remote locations, where biogenic emissions likely dominate, show sustained elevated concentrations throughout the night (Bouvier-Brown et al., 2009), not just early morning.

D5 is also prominent in this factor and, as stated in the discussion of Factor 3, is a tracer for personal care product emissions. Methyl salicylate, as the primary component of wintergreen oil, is also used as a fragrance compound (Lapczynski et al., 2007). α-isomethyl ionone is naturally found in brewer's yeast and emitted during fermentation (Loscos et al., 2007) but is also commonly produced synthetically and found in cosmetics and personal care products (del Nogal Sánchez et al., 2010). There are three breweries about 1.1 km to the southeast of the sampling site and one about 3.5 km to the northeast (Fig. 1); given their distance, the low northeastern winds and the presence of other personal care product fragrance compounds in this factor, it is most likely α-isomethyl ionone measured at the sampling site also originates from personal care products. Methyl salicylate and α-isomethyl ionone are relatively low-volatility IVOCs, measured on the SVOC channel of cTAG. Their presence in this factor contributes to a more comprehensive source profile for consumer product emissions than could be obtained with a VOC-only measurement focus.

p-Dichlorobenzene is an industrial chemical used as a deodorant and insect repellent, especially in mothballs (Agency for Toxic Substances and Disease Registry, 2006). It is widely available as a consumer product and is typically placed in enclosed spaces with clothes vulnerable to moth damage (Chin et al., 2013). Its inclusion in this factor and Factor 8 could be explained by morning occupant activity that disturbs and ventilates spaces where p-dichlorobenzene is placed, temporarily increasing its emission to the rest of the indoor environment and, in turn, outdoors. It is also possible that general household activity correlates with VOC exchange from indoor residences to outdoors, independent of whether occupants are interacting with p-dichlorobenzene-containing substances. Further highly time-resolved studies are needed to assess time-of-day exposure and transport to the outdoors.

Dibromochloromethane is a disinfection byproduct found in chlorinated tap water (Krasner et al., 1989). It is also produced from marine macroalgae (Manley et al., 1992; Sturges et al., 1992; Carpenter and Liss, 2000), the more important source globally (World Meteorological Organization et al., 2019), and is well-mixed in the troposphere, with a lifetime of 70 d (World Meteorological Organization et al., 2019). One likely source of this compound above the regional background is the outdoor swimming pool 10 m to the northeast (Fig. 1), which was closed to the public for the season but was nonetheless kept filled. Trihalomethane emissions from commercial pools have been extensively documented (Fantuzzi et al., 2001; Zwiener et al., 2007; Richardson et al., 2010; Righi et al., 2014; Westerlund et al., 2019). While pool emissions may be responsible for elevated concentrations throughout the nighttime when dilution is low, the spikes in concentration in the early morning hours are more likely related to human activity. Residential showering has been shown to increase the concentration of dibromochloromethane in the bathroom air by 10 µg m−3 or more, depending on its initial concentration in the tap water (Kerger et al., 2000). Once ventilated outside, it is plausible that with enough temporally coincident showers in nearby residences the concentration measured at the sampling site would increase by the observed 5–10 ng m−3 in the early morning hours.

The C10–C16 n-alkanes contribute between 15 % and 32 % of their mass to this factor. These compounds come chiefly from gasoline and diesel exhaust or fuel evaporation (Schauer et al., 1999b, 2002b; Gentner et al., 2013; Drozd et al., 2021), but use of petroleum distillates in some consumer products is another contributor (McDonald et al., 2018). A consumer product source would be the most consistent with the temporal variability and composition of this factor.

3.7 Factor 6: primary biogenic and diesel

Factor 6 (profiled in Fig. 11) is designated primary biogenic and diesel. Three out of the five monoterpenes measured are shared between this factor and the consumer products factor (camphene, mass fraction 29 %, α-pinene, 32 %, and β-pinene, 25 %). The only other major constituents of Factor 6 are a narrow range of semivolatile n-alkanes (C16–C19) and pristane and phytane, contributing about 20 % to 30 % of their mass. Like Factors 3 (gasoline) and 5 (consumer products), Factor 6 is elevated exclusively in the early morning hours. However unlike those two factors, the majority of the signal from Factor 6 is confined to one event in the early morning hours of 17 April. Winds were calm (<1 m s−1) and from the northeast during this event (Fig. 11c).

While most of the measured monoterpene mass is likely due to consumer product emissions (see Factor 5 discussion), the personal care product tracer D5 contributes no mass to Factor 6. The peak of the early morning event on 17 April is at 03:00 LT, 2 hours earlier than the typical diurnal maximum for Factor 5. Therefore this factor is more likely to represent concentrated local biogenic emissions.

The C10–C19 alkanes are mainly split between this factor, Factor 5 and Factor 11 (early morning cooking and diesel event). While Factor 11 contains contributions from C10–C19 alkanes, as well as pristane and phytane, which are expected from diesel exhaust or evaporative emissions (Schauer et al., 1999b; Gentner et al., 2013), Factor 5 only contains contributions from the lighter alkanes in this range (C10–C16) and Factor 6 from the heavier ones (C16–C19, pristane, phytane). The event on 17 April that defines Factor 6 is relatively enriched in the heavier alkanes within this carbon number range, leading to splitting between factors. The Factor 5 lighter alkane group could come from consumer product use as mentioned in the Factor 5 discussion.

3.8 Factor 7: parachlorobenzotrifluoride (PCBTF)

Factor 7 (profiled in Fig. 12) consists nearly exclusively of p-chlorobenzotrifluoride (PCBTF), with 68 % of that compound's mass present in this factor. No other compound has more than 10 % of its mass in this factor. The timeline is extremely episodic, with brief (single data point, or <3.5 h duration) concentration spikes on some days around noon. Winds are exclusively from the west when this factor's concentration is high (Fig. 12c).

PCBTF is a volatile chemical product used exclusively in solvent-based coatings (Stockwell et al., 2021; Gkatzelis et al., 2021). Coatings are defined in emission inventories as paints, varnishes, primers, stains, sealers, lacquers and any solvents associated with coatings (Stockwell et al., 2021). They tend to be associated with construction projects (McDonald et al., 2018) and Gkatzelis et al. (2021) found that concentrations of PCBTF specifically correlated poorly with population density, which is consistent with industrial rather than individual consumer use.

The specific source of PCBTF in this study is unknown. Though the direction of the source is well-defined, winds originated from the west for the entire morning and afternoon on the days when PCBTF was detected, not just during periods of elevated concentration of PCBTF (Fig. 3), suggesting the emissions themselves are intermittent rather than being continuous but only sampled intermittently. The lifetime of PCBTF in the atmosphere with respect to reaction with OH is over 20 d (Gkatzelis et al., 2021), so reactive loss is not expected to affect the measured concentration.

3.9 Factor 8: secondary oxidation and persistent personal care product emissions

Factor 8 (profiled in Fig. 13) is designated as secondary oxidation products and semivolatile personal care product emissions. This factor contains moderate ( 25 % mass fraction or greater) contributions from 11 different compounds, with first generation α- and β-pinene oxidation products pinonic acid and pinic acid contributing the highest mass fractions (52 % and 36 % respectively). The factor concentration is elevated throughout the nighttime hours when ozone is present and lower at night when ozone is low, as well as midday. Winds come from all directions when this factor's concentration is high, with a slight preference for the northwest and northeast (Fig. 13c), but wind speeds are low (<1.8 m s−1 for all but one data point).

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Figure 12(a) Factor 7 timeline. (b) Diurnal profile for Factor 7. (c) Rose plot showing correlation of elevated emissions and wind direction. (d) Factor 7 composition profile. See Fig. 4 description for further information on how to read this figure.

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https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f13

Figure 13(a) Factor 8 timeline. (b) Diurnal profile for Factor 8. (c) Rose plot showing correlation of elevated emissions and wind direction. (d) Factor 8 composition profile. See Fig. 4 description for further information on how to read this figure.

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Pinic and pinonic acids match the variability of Factor 8 the most closely. Both compounds are both secondary oxidation products and precursors of further oxidized species, with gas-phase lifetimes of only a few hours under typical conditions but with low enough volatility to partition into the aerosol phase, which extends and adds uncertainty to their atmospheric lifetimes (Donahue et al., 2012). In general, concentrations are highest at night and mid-morning and low in the middle to late afternoon. In the afternoon, even though ozone and α- and β-pinene are present, the concentrations of pinic and pinonic acid dip likely due to the combined effects of continued oxidation and physical dilution. At night, one of two scenarios occurs. When ozone remains high throughout the night (12, 15 and 16 April in this dataset), these two acids build up under the shallow boundary layer. When ozone is low at night or early morning, local minima in pinic and pinonic acid concentrations are observed, leading to a bimodal diurnal trend. This trend is noisier and less obvious (though still present) in the Factor 8 timeline due to the contributions of other compounds not driven by the same chemistry.

In addition to pinic and pinonic acids, several compounds used in personal care products are either split between this factor and Factor 5 (consumer products) or are predominantly present in this factor. D5 siloxane's mass is approximately equally split between Factors 3 (gasoline), 5 and 8. Other compounds present in this factor that are used in personal care products include camphor (Drugs.com Drug Information Database, 2022), eucalyptol (Medcraft and Schnell, 2016), benzophenone (Anderson and Castle, 2003; Downs et al., 2021; U.S. EPA, 2022e), dimethyl and diethyl phthalates (Zota et al., 2014), and methyl salicylate (Lapczynski et al., 2007), with the latter having approximately equal mass in Factors 5 and 8. p-Dichlorobenzene and dibromochloromethane, which are not from personal care products but are linked to morning indoor residential activity, also share mass between Factors 5 and 8.

When comparing compounds predominantly present in one factor or the other, more volatile, less oxygenated compounds are represented in Factor 5, while oxygen-containing IVOCs and larger, semivolatile compounds, many of them oxygen-containing, are found in Factor 8. Factor 8 species tend to have longer atmospheric lifetimes as well, with camphor (Reissell et al., 2001), eucalyptol (Corchnoy and Atkinson, 1990), methyl salicylate (Ren et al., 2020), benzophenone (U.S. EPA, 2022e), dimethyl phthalate (Han et al., 2014), p-dichlorobenzene (Atkinson and Arey, 1993), dibromochloromethane (World Meteorological Organization et al., 2019) and D5 siloxane (Navea et al., 2011) all having lifetimes of over 1 d when exposed to typical hydroxyl radical concentrations ([OH] =2×106 molec. cm−3) and likely even longer lifetimes in practice when the gas–particle partitioning of the semivolatile organics is taken into account (Kroll and Seinfeld, 2008; Cousins and Mackay, 2001). In contrast, the compounds in Factor 5 associated with personal care product emissions that are not also present in this factor (the monoterpenes) have atmospheric lifetimes of a few hours at most (Atkinson and Arey, 2003). This is consistent with the diurnal profiles of the two factors: long-lived personal care product compounds, while they may be emitted in the early morning, are not fully reacted away during the day and get reconcentrated under the boundary layer in the evening, leading to elevated concentrations throughout the night. Short-lived compounds are only observed during and shortly after their morning emission.

D4 siloxane has a somewhat greater mass fraction in Factor 8 (29 %) than in Factor 3 (23 %). Like the compounds split between Factors 5 and 8, D4 has a long atmospheric lifetime (11 d; Navea et al., 2011), likely leading to elevated concentrations outside of typical emission times, unlike the gasoline markers that make up the bulk of the mass of Factor 3.

2-Nitrophenol contributes moderately to Factor 8 (mass fraction 24.8 %). Possible sources are discussed in the Factor 4 and Factor 9 descriptions.

3.10 Factor 9: biomass burning

Factor 9 (profiled in Fig. 14) represents primary biomass burning emissions. The top mass fraction contributors, in order, are galactosan, levoglucosan, syringaldehyde, mannosan, syringic acid, vanillic acid, 4-nitrocatechol and furfural, all tracers of biomass burning (Simoneit et al., 1999; Simoneit, 2002; Bertrand et al., 2018; Finewax et al., 2018). This factor is consistently elevated exclusively in the nighttime hours. Winds are light (<1.5 m s−1 except for one data point) and come from all directions, but predominantly from the northeast, when Factor 9 is elevated (Fig. 14c).

Wood burning in residences for heat or recreation is a significant source of pollution in the Bay Area, with 25 % of primary PM2.5 emissions attributed to residential wood burning annually (Kniss et al., 2017). That fraction rises to 33 % or more between November and April (Bay Area Air Quality Management District, 2012; San Francisco Chronicle, 2022). With average evening temperatures (19:00 to 21:00 LT) of 10.4 C during the sampling period, some residential wood burning activity is anticipated. While we expect wood burning to occur only early in the nighttime hours before residents go to sleep, the lower boundary layer throughout the night traps emissions, keeping concentrations elevated.

https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f14

Figure 14(a) Factor 9 timeline. (b) Diurnal profile for Factor 9. (c) Rose plot showing correlation of elevated emissions and wind direction. (d) Factor 9 composition profile. See Fig. 4 description for further information on how to read this figure.

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https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f15

Figure 15(a) Factor 10 timeline. (b) Diurnal profile for Factor 10. (c) Rose plot showing correlation of elevated emissions and wind direction. (d) Factor 10 composition profile. See Fig. 4 description for further information on how to read this figure.

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Some biomass burning markers included in this analysis did not show up in Factor 9. 4-Hydroxybenzoic acid and p-anisic acid are tracers for burning of grasses (Simoneit, 2002), an unlikely fuel source for residential fireplaces. 4-Nitrophenol has been observed in biomass burning plumes or otherwise attributed to biomass burning (Hoffmann et al., 2007; Mohr et al., 2013; L. Wang et al., 2017; H. Wang et al., 2020) and is likely formed secondarily within hours inside the biomass burning plume (Mason et al., 2001). 2-Nitrophenol, to our knowledge, either has not been detected in biomass burning plumes (Hoffmann et al., 2007) or was simply not measured or not distinguished from the other isomer (Mohr et al., 2013; L. Wang et al., 2017; H. Wang et al., 2020). However, biomass burning is thought to be a minor source for 4-nitrophenol in urban areas (Harrison et al., 2005b; Li et al., 2016), where motor vehicle combustion is responsible for primary emissions of nitrophenols, as well as precursors to their secondary formation (Tremp et al., 1993; Harrison et al., 2005b), which also plays a major role in their formation (Lüttke et al., 1997, 1999; Harrison et al., 2005b; Yuan et al., 2016; Cheng et al., 2021). Further discussion on the sources and timelines of the nitrophenol isomers can be found in the Factor 4 description.

https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f16

Figure 16(a) Factor 11 timeline. (b) Diurnal profile for Factor 11. (c) Rose plot showing correlation of elevated emissions and wind direction. (d) Factor 11 composition profile. See Fig. 4 description for further information on how to read this figure.

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https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f17

Figure 17(a) Factor 12 timeline. (b) Diurnal profile for Factor 12. (c) Rose plot showing correlation of elevated emissions and wind direction. (d) Factor 12 composition profile. See Fig. 4 description for further information on how to read this figure.

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3.11 Factor 10: industrial and/or agricultural background and continuous combustion source

Factor 10 (profiled in Fig. 15) is elevated in the latter half of the campaign (17 April, late morning onwards) with maximum concentrations in the late morning and early afternoon hours but weak diurnal variability. Its main constituents include o-dichlorobenzene (mass fraction 36 %), phthalic anhydride (36 %), the PAH pyrene (32 %), high-volatility phthalates (15 %–30 %), and grass burning tracers 4-hydroxybenzoic acid (22 %) and p-anisic acid (26 %), with a small contribution from C15–C21 alkanes, pristane and phytane (14 %–22 %). Winds come from all directions when this factor is elevated but mostly from the west (Fig. 15c). This factor appears to be part of the regional background.

o-Dichlorobenzene is used in the production of herbicides and dyes and as a solvent (Meek et al., 1994; Agency for Toxic Substances and Disease Registry, 2006) and lasts for weeks in the atmosphere (Agency for Toxic Substances and Disease Registry, 2006). It contributes to Factor 1 (long-lived and continuously emitted compounds) as well; as such, it is likely part of the regional background that could include industrial and/or agricultural sources. It is not found in consumer products like its isomer p-dichlorobenzene.

PAHs would be expected to contribute to this combustion-related factor because they are formed from incomplete combustion (Ravindra et al., 2008). Unlike the other PAHs measured, which exhibit nighttime enhancement and are mostly split between Factors 3, 8 and 9, pyrene shows only minor nighttime enhancement even though it has an atmospheric lifetime with respect to reaction with OH of only a few hours (Atkinson and Arey, 1994), suggesting a continuous source. It is unclear why pyrene's diurnal profile differs from the other PAHs.

Factor 10 and Factor 1 have several compounds in common, such as the grass burning tracers, trihalomethanes, phthalimide, o-dichlorobenzene and to a lesser extent phthalates. They also share weak diurnal variability, though the variability they do have is opposite. However, Factor 1 completely lacks any contribution from pyrene and the diesel markers. It seems likely that both Factor 1 and Factor 10 represent some stable background level of long-lived or continuously emitted compounds spanning the volatility range from VOCs to SVOCs but that Factor 10 includes an additional continuous combustion-related source that was absent in the beginning of the campaign.

https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f18

Figure 18Correlation of isoprene and benzene between 22:00 and 05:30 LT, when biogenic production of isoprene is expected to be negligible.

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https://acp.copernicus.org/articles/22/14987/2022/acp-22-14987-2022-f19

Figure 19(a) Factor 13 timeline. (b) Diurnal profile for Factor 13. (c) Rose plot showing correlation of elevated emissions and wind direction. (d) Factor 13 composition profile. See Fig. 4 description for further information on how to read this figure.

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3.12 Factor 11: early morning cooking and diesel event

Factor 11 (profiled in Fig. 16) consists nearly exclusively of a 14 April 03:00 LT spike in concentration of some cooking and diesel tracers, as well as a few other compounds. It includes 20 %–30 % of the mass of cooking tracers palmitic acid, stearic acid, azelaic acid and nonanal and 10 %–25 % of the mass of the diesel tracers C10–C19 alkanes, pristane and phytane. 1-Tridecene and isophorone have their highest mass fraction in this factor (27 % and 21 % respectively). Winds were calm ( 1 m s−1) and from the northeast during this event (Fig. 16c).

Palmitic acid, stearic acid and azelaic acid are cooking tracers as discussed in the Factor 4 description, though the concentration variations captured in that factor are more likely to come from a difference source. Nonanal has biogenic (Kirstine et al., 1998) and secondary (Atkinson, 2000; Fruekilde et al., 1998; Moise and Rudich, 2002) sources but is also emitted in significant quantities from cooking (Rogge et al., 1991; Schauer et al., 1999a, 2002a), the likely source for this event. Residential cooking is an unlikely explanation given the early time of the event (04:00 local daylight time), but commercial cooking preparations could plausibly begin at such an early hour. With northeast winds, one or more of the restaurants in the shopping center 100 m to the north could be the source of the cooking and diesel activity (Fig. 1).

Isophorone is a solvent for resins, polymers, wax, oil, pesticides, paints and printing inks (International Programme on Chemical Safety, 1995; Samimi, 1982). While it has been detected at low levels in foods (Sasaki et al., 2005; Kataoka et al., 2007), it is not detected in food cooking emissions (Rogge et al., 1991; Schauer et al., 1999a, 2002a), so isophorone likely arises from a separate and temporally coincident source.

While little information is available about sources of 1-tridecene specifically, lower-molecular-weight alkenes come from mostly anthropogenic origin in urban areas, specifically mobile sources (Luecken et al., 2012). In this dataset, 1-tridecene correlates better with diesel tracers (r≈0.7) than gasoline tracers (r≈0.55), though it is not specifically mentioned in speciated diesel composition studies (Rogge et al., 1993; Schauer et al., 1999b; Gentner et al., 2013). Even at its peak, the 1-tridecene concentration is less than 4 ng m−3 (0.5 ppt).

3.13 Factor 12: isoprene

Factor 12 (profiled in Fig. 17) contains 73 % of the mass of isoprene and no more than 10 % of the mass of any other compound. The concentration is elevated between the early morning hours and late evening hours, with a peak in the early evening (18:00 LT) and a much smaller peak in the morning (04:00 to 06:00 LT). When the concentration of this factor is high, wind speeds are typically elevated and from the west (Fig. 17c).

Isoprene is predominantly of biogenic origin, and its emission is light- and temperature-dependent (Guenther, 1997). Seasonal output varies greatly, with maximum emission in the summer months (Palmer et al., 2006; Liakakou et al., 2007). Summertime diurnal concentration profiles of isoprene typically increase from morning to a midday maximum, declining again by nightfall, in accordance with its sensitivity to light and temperature. In wintertime when biogenic production is low, isoprene has been observed to correlate with pollutants of known vehicle traffic origin in urban areas and is inferred to originate from that source (Reimann et al., 2000; Borbon et al., 2001; Lee and Wang, 2006; Hellén et al., 2012; Kaltsonoudis et al., 2016).

As spring represents a transition from winter to summer conditions, evidence of both anthropogenic and biogenic isoprene is present in Livermore. The small early morning peak is unlikely to be of biogenic origin since it occurs when temperatures are coldest and before the sun rises. The peak coincides with those of the traffic markers; restricted to the hours of 22:00 to 05:30 LT, isoprene correlates with benzene and several other gasoline markers (methylcyclopentane through p-diethylbenzene in Table 1). The correlation between benzene and isoprene is shown in Fig. 18. A linear regression of the data puts the intercept within error of the origin, suggesting no additional sources for isoprene or benzene overnight. The slope, which represents an average ratio, is 0.22. Analysis of vehicle emissions measured during dynamometer tests performed in 2014 (Drozd et al., 2016) show a median isoprene : benzene ratio of 0.18 with 50 % of the data between 0.14–0.34 (Fig. S10), providing independent support for attributing these isoprene emissions to anthropogenic sources.

In contrast, the late afternoon or early evening peaks roughly correlate with the maximum afternoon temperature, though the peaks occur a few hours after the temperature maximum. Midday concentrations may be depressed by reaction with the hydroxyl radical, as well as dilution from the heightened boundary layer and high winds. In the early evening there is a narrow window of time when the sun has set (and therefore hydroxyl radical production has ceased), but isoprene emission continues. The lowering boundary layer and lower wind speeds may also contribute to the heightened isoprene concentrations. Later in the evening, emission ceases, and isoprene is rapidly lost to reaction with nitrate radical and ozone (Steinbacher et al., 2005).

3.14 Factor 13: possible jet fuel event

Factor 13 (profiled in Fig. 19) captures a short episode of heightened gasoline tracer concentrations at 23:00 LT on 13 April. It is not associated with a sudden shift in wind patterns but more likely represents a transient source. Around 20 % of the mass of C6–C10 linear, branched and aromatic hydrocarbons is included in this factor, with smaller contributions out to C14. Compositionally, Factor 13 differs from Factor 3 (gasoline) in its lack of other compound classes; Factor 3 additionally contains contributions from PAHs, palmitoleic acid, and D4 and D5 siloxanes. Since D5 originates from personal care products likely applied in the morning hours, its absence in Factor 13 is not surprising. Similarly, as mentioned in the Factor 3 discussion, palmitoleic acid and D4 coincide temporally with regular morning gasoline emissions but do not come from gasoline and so are not expected in Factor 13 either. The PAH presence in Factor 3 was ascribed to gasoline exhaust, so its absence in this factor is inconsistent with a gasoline source. One possibility is that Factor 13 captures a low jet aircraft flyover, since the carbon number range of jet fuel approximately matches the factor's chemical profile (Masiol and Harrison, 2014), but jet fuel is depleted in PAHs compared to gasoline (Shumway, 2000). The likely origin or destination of the aircraft is Livermore Municipal Airport, located approximately 3 km away from the sampling site (Fig. 1).

4 Conclusions

For the first time on a single instrument, hourly measurements were successfully carried out of over 160 organic compounds in the ambient air ranging from C5–C27-alkane-equivalent volatility in both gas and particle phases. Measurements took place in Livermore, California, between 11 and 21 April 2018 with the cTAG. PMF was applied to a subset of the measured compounds to elucidate the major sources of pollution in Livermore in the springtime.

Major factors observed to contribute significantly included gasoline emissions, consumer product emissions, emissions from evaporative (temperature-dependent) sources, biomass burning, secondary oxidation, background emissions from continuously emitting sources or long-lived pollutants, and several factors associated with single compounds or specific events during the campaign described by a unique compositional profile. The gasoline factor had a morning maximum but lacked the evening enhancement observed in other studies likely due to the residential area of our sampling location and emissions from modern vehicles being concentrated in cold starts. Monoterpenoid compounds were associated with the personal care product factor more than any other factor, highlighting the dominance in urbanized areas of anthropogenic sources for some compounds normally from biogenic sources. No clear diesel factor emerged; rather, diesel tracers were split between three different factors primarily associated with distinct single events. Isoprene's dual biogenic and vehicle exhaust sources combined with atmospheric chemistry suppressing midday concentrations forced it into its own factor. While PCBTF and isophorone are both industrial chemicals associated with solvents, they exhibit extremely distinct temporal profiles and are present in different factors, suggesting distinct sources. The clearly separated biomass burning factor demonstrates that residential wood burning is still an important source of organic emissions even in the springtime.

This analysis underscores the increasing importance of anthropogenic petroleum-derived VOCs from non-mobile sources in a suburban environment, an emerging topic of interest in recent years (McDonald et al., 2018). The ability to resolve individual isomers at high time resolution proved crucial, as it allowed for (1) the separation of the monoterpenes between consumer product emissions and a suspected biogenic source and (2) the distinct categorization and interpretation of the nitrophenol and dichlorobenzene isomers. Including VOCs, IVOCs and SVOCs together in a single analysis expanded the profiles of some sources dominated by VOCs, such as the IVOCs methyl salicylate and α-isomethyl ionone being included in the consumer product factor. Similarly, the secondary oxidation and persistent personal care product emission factor included a mix of SVOCs, stable VOCs and oxygenated VOCs, constituting a unique profile distinct from fresh personal care product emissions. Measurement of compounds over a wide range of volatilities and oxidation states can allow for more detailed source characterization and tracking of atmospheric processes than focusing on VOCs or particulate matter alone.

Data availability

Concentration timelines, positive matrix factorization results and data for each figure are available from the first author upon request.

Supplement

The supplement related to this article is available online at: https://doi.org/10.5194/acp-22-14987-2022-supplement.

Author contributions

RAW, NMK, RJW and AHG designed and coordinated the Livermore 2018 deployment, and RAW and NMK collected data from that deployment. RAW and GTD performed data analysis. RAW prepared the manuscript with input and revisions from NMK, GTD and AHG.

Competing interests

The contact author has declared that none of the authors has any competing interests.

Disclaimer

This publication has not been formally reviewed by the EPA. The views expressed in this publication are solely those of the authors, and the EPA does not endorse any products or commercial services mentioned in this publication.

Publisher’s note: Copernicus Publications remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Acknowledgements

The Livermore Area Recreation and Park District (LARPD) provided the site and infrastructure in Livermore for the spring 2018 field deployment. The authors would like to especially thank Bruce Aizawa and Steve Sommers of LARPD for enabling us to do measurements at the site. Hourly temperature, wind speed and direction, and ozone measured approximately 100 m away from our site were provided by the Bay Area Air Quality Management District.

Financial support

cTAG development, including the field deployment in Livermore, was supported by the U.S. Department of Energy SBIR/STTR under grant DE-SC0011397. Rebecca A. Wernis was supported by the U.S. Environmental Protection Agency (EPA) Science To Achieve Results (STAR) fellowship assistance agreement no. FP-91778401-0.

Review statement

This paper was edited by Hinrich Grothe and reviewed by two anonymous referees.

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We measured volatile and intermediate-volatility gases and semivolatile gas- and particle-phase compounds in the atmosphere during an 11 d period in a Bay Area suburb. We separated compounds based on variability in time to arrive at 13 distinct sources. Some compounds emitted from plants are found in greater quantities as fragrance compounds in consumer products. The wide volatility range of these measurements enables the construction of more complete source profiles.
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