A method for liquid spectrophotometric measurement of total and water-soluble iron and copper in ambient aerosols
- 1Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA
- 2Department of Environmental Health Sciences, School of Public Health, Yale University, New Haven, CT 06510, USA
Correspondence: Rodney J. Weber (email@example.com)
Determination of transition metals in ambient aerosols is important due to their toxicity to human health. However, the traditional measurement techniques for metal analysis are often costly and require sophisticated instruments. In this study, we developed and verified relatively low-cost liquid spectrophotometric methods for the measurements of iron (Fe) and copper (Cu), the two most abundant transition metals in ambient fine particulate matter (PM2.5). For Fe analysis, we utilized a ferrozine-based colorimetric method, which has been frequently used for water-soluble (WS) Fe determination, and further extended this approach for the measurement of total Fe (water-soluble + water-insoluble). In this method, Fe is quantified through the formation of a light-absorbing ferrozine–Fe(II) complex (absorbance at 562 nm). A similar colorimetric method, which forms a bathocuproine–Cu(I) complex absorbing light at 484 nm, was developed and examined for measurement of WS and total Cu.
These methods were applied to 24 h integrated filter samples collected in urban Atlanta. Based on PM2.5 ambient aerosols, total and water-soluble Fe and Cu concentrations were in good agreement with inductively coupled plasma mass spectrometry (ICP-MS) measurements (slopes 1.0±0.1, r2>0.89). The water-soluble components, operationally defined as those species in the aqueous filter extract that pass through a 0.45 µm filter, were further characterized by ultrafiltration, which showed that roughly 85 % of both the Fe and Cu in the water-soluble fraction was composed of species smaller than nominally 4 nm.
Transition metals are known to contribute to airborne particle toxicity and can cause a wide range of adverse health effects (Chen et al., 2018; Gonet and Maher, 2019). Iron (Fe) and copper (Cu) are often two of the most abundant transition metals in ambient fine particles (PM2.5) and have been linked to a number of human diseases associated with the respiratory, cardiovascular and central nervous systems (Calderón-Garcidueñas et al., 2019; Dreher et al., 1997; Wang et al., 2007). They have also been associated with other organ damage (Kim et al., 2013; Schrand et al., 2010). Transition metals in ambient aerosols are emitted in a variety of chemical forms, such as metal oxides, metal sulfates, metal halides, metal organics and reactive nano-metalloid particles (Gonet and Maher, 2019; Sutto, 2018). Fe and Cu nanoparticles (<0.1 µm) may be especially toxic due to unique surface properties, combined with their small sizes that allow them to pass through cellular membranes and ability to be translocated to other organs (Bongaerts et al., 2020; Lee et al., 2020; Moreno-Ríos et al., 2021). Water-soluble species are operationally defined and are obtained though aqueous dissolution of collected aerosols followed by liquid filtration of the extract solution (typical filter pore sizes of 0.22 or 0.45 µm), which is roughly analogous to the process particles undergo when deposited in the respiratory-tract-lining fluid. Metals measured in this fraction can include molecules and colloidal nanoparticles that are more readily bioavailable than insoluble species. Studies have found that water-soluble transition metals, including water-soluble (WS) Fe and Cu, have stronger adverse health associations than the corresponding water-insoluble components (Costa and Dreher, 1997; Frampton et al., 1999; Huang et al., 2003; Ye et al., 2018). Transition metal ions that can form dissolution of aerosol components, such as Fe(II) and Fe(III) and Cu(I) and Cu(II), are highly redox-active components of PM2.5. These ions can trigger and sustain catalytic reaction cycles, such as Fenton reactions, generating reactive oxygen species (ROSs; OH, , HO2, O3 and H2O2) in vivo (Brewer, 2007; Lakey et al., 2016), which can induce oxidative stress and further lead to inflammatory responses and a subsequent host of adverse health effects (Brook et al., 2010; Donaldson et al., 2001; Ghio et al., 2012; Nel, 2005).
Transition-metal-bearing particles are emitted by a wide variety of sources. Major Fe sources include resuspended mineral and road dust (tire and brake wear) and combustion of biomass and fossil fuels (Khillare and Sarkar, 2012; See et al., 2007; Wang et al., 2016). Cu sources are often dominated by traffic road dust and in certain locations by industrial sources (Adachi and Tainosho, 2004; Khillare and Sarkar, 2012; Kulshrestha et al., 2009; Lee and Hieu, 2011; Wang et al., 2016). Water-soluble transition metals may originate from primary emissions, such as combustion (e.g., WS Fe), but secondary processing is likely the major source. This can occur by dissolution of the various insoluble forms of the metals emitted as primary emissions, for example, dissolution of metal oxides to soluble forms as the particles age in the atmosphere (Alves et al., 2020; Fang et al., 2015; Galon-Negru et al., 2019; Ito et al., 2019; Meskhidze et al., 2005; See et al., 2007; Wong et al., 2020).
Measuring transition metals in ambient aerosols is challenging due to their low concentrations (tens of nanograms per cubic meter or less). Various analytical methods have been utilized. X-ray fluorescence (XRF) and particle-induced X-ray emission analysis (PIXE) are non-destructive but can be influenced by matrix effects that result in major interferences (Lin and Luo, 1979). Inductively coupled plasma mass spectrometry (ICP-MS) is widely used for quantifying trace elements and is included in some federal reference methods for the identification of metals in water and ambient PM in the USA (e.g., Method IO-3.5, USEPA Method 1640) (Ammann, 2007; Chow, 1995; Danadurai et al., 2011). Overall, these instruments tend to be expensive, making it challenging to do routine analysis of large numbers of aerosol particle samples in modestly equipped laboratories.
An alternative approach is liquid-based colorimetric methods, which can provide precise and accurate measurements of specific metal species based on the assumption that the ligand used reacts exclusively with the target metal (i.e., in this case Fe or Cu) to form a light-absorbing complex. Stookey (1970) developed a spectrophotometric method for the analysis of Fe(II) based on Fe(II) complexing with a ferrozine ligand (3-(2-pyridyl)-5,6-bis(4-phenylsulfonic acid)-1,2,4-triazine) that absorbs light at 562 nm. Smith and Wilkins (1953) reported a colorimetric reagent, bathocuproine (2,9-dimethyl-4,7-diphenyl-1,10-phenanthroline), that can selectively chelate with Cu(I). The absorption spectra of the bathocuproine–Cu(I) complex display a maximum value at 484 nm. Both techniques have been developed and used to detect Fe and Cu in natural waters (Moffett et al., 1985; Viollier et al., 2000); however, use of the Fe–ferrozine approach is much more common and has also been utilized for measurements of ambient aerosols (Kuang et al., 2019; Majestic et al., 2006; Oakes et al., 2010; Rastogi et al., 2009; Zhu et al., 1997; Zhuang et al., 1992). These analytical techniques can be applied to relatively small liquid spectrophotometers that utilize a long-path liquid waveguide capillary cell (LWCC) for high sensitivity. Although only able to measure a specific compound per analysis, in contrast to mass spectrometer methods, the instrument is small, portable and relatively low cost and can be used for offline measurements of sample extracts or for online measurement when connected to a particle-into-liquid sampler (PILS) or similar system (Oakes et al., 2010; Rastogi et al., 2009). Here we report on the development, verification and application of liquid spectrophotometers for measurement of Fe and Cu in ambient aerosols collected on filters.
2.1 Collection of ambient PM2.5 filters
One year of filter collection was conducted throughout 2017 at the Jefferson Street (JST) site located ∼4 km northwest of downtown Atlanta, Georgia. The JST site is surrounded by a mixed commercial–residential area and has a characteristic urban signature (Hansen et al., 2003). A total of 355 PM2.5 filter samples were collected with high-volume (hi-vol) samplers (Thermo Andersen, flow rate normally 1.13 m3 min−), each filter collected over a 24 h period (midnight to midnight) using prebaked (maximum T=550 ∘C) quartz filters (Pallflex® Tissuquartz™, 0.2×0.25 m) with an effective collection area of 516.13 cm2 (20.32 cm by 25.40 cm). Samples were immediately wrapped in prebaked aluminum foil and stored at −18 ∘C until analysis. A selection of these filters are included in the following analyses. A suite of other air quality sampling instruments was also operational during the filter sampling period. Portions of these filters have already been utilized in studies on aerosol oxidative potential (Gao et al., 2020a, b).
2.2 Reagents and standards
All acids and sodium hydroxide (NaOH) used were trace-metal-grade obtained from VWR International LLC (Radnor, PA, USA). Standard stock solutions for Fe and Cu calibrations were prepared by dilution of commercially available standards (1000 ppm in 2 % HCl obtained from the RICCA Chemical Company, Arlington, TX, USA) and stored in a refrigerator (T=4 ∘C). Calibration with these standards was performed at the beginning of every measurement day. Ammonium acetate (C2H7NO2) was obtained from Fisher Scientific International Inc. (Fair Lawn, New Jersey, USA) and ferrozine (3-(2-pyridyl)-5,6-bis (4-phenylsulfonic acid)-1,2,4-triazine) from the HACH Company (Loveland, CO, USA). Bathocuproine (2,9-dimethyl-4,7-diphenyl-1,10-phenanthroline), sodium citrate dihydrate (HOC(COONa)(CH2COONa)2⋅2H2O) and hydroxylamine hydrochloride (HONH2⋅HCl) were obtained from Sigma Aldrich (St. Louis, MO, USA). Details of the chemical preparations are provided in the Supplement.
2.3 Spectrophotometer and LWCC system
Similar spectrophotometric instruments were used for all measurements (WS and total Fe and Cu). The final mixture containing the light-absorbing complexes was pushed into a liquid waveguide capillary cell (LWCC-3250 or LWCC-3100 World Precision Instruments, Sarasota, FL). The waveguide was coupled at one end to a dual deuterium and tungsten halogen light source (DT-Mini-2, Ocean Optics, Dunedin, FL), which produced light over the wavelength range of 200 to 800 nm, and at the other end to a multi-wave light detector (USB4000, Ocean Optics, Dunedin, FL), using 400 µm fiber core diameter fiber optic cables (QP400-2-SR, Ocean Optics, Dunedin, FL). The light absorbance was recorded with a data requisition software (SpectraSuite). For Fe analysis, the light absorption over the wavelength range between 557 and 567 nm was measured and averaged as the absorbance of the Fe complex in the sample (Abs562). Average absorption between wavelengths of 479 and 489 nm was recorded and referred to as the absorbance for Cu measurements (Abs484). In both measurements, the average absorbance measured over the wavelength range of 695 to 705 nm (Abs700) was chosen as the baseline absorbance.
Since the light absorption efficiencies of Fe(II)–ferrozine and Cu(I)–bathocuproine complexes differed, the optical path lengths of the LWCC for Fe and Cu measurements were 100 cm (LWCC-3100) and 250 cm (LWCC-3250), respectively. To keep the light absorption within an optimal range, the recommended Fe(II) and Cu(I) liquid concentrations detected by the system are up to 40 and 50 ppb, respectively.
The metal concentrations in the liquid (C) were determined based on the light absorbances by
where Absλ represents the average light absorption of the sample (or blank) for the ranges given above, which encompasses the wavelength (λ) at which maximum optical absorption occurs; for Fe, λ=562 nm, and for Cu, λ=484 nm. Abs700 represents the average light absorption between 695 and 705 nm; a (arbitrary units) and b (1/ng mL−1) are the intercept and slope of the calibration curve, respectively.
The final ambient concentration of each element, Cair (ng m−3), was calculated by
where Csample and Cblank are the liquid sample and blank concentrations of the specific element (ng mL−1), determined by Eq. (1); Ve (mL) is the liquid volume of the sample (or blank) extract; Vs (mL) is the liquid extract volume used for the actual measurement; and Vl (mL) is the volume of liquid sample solution after being diluted by all the chemicals (i.e., ). Vair (m3) is the volume of air drawn through the filter during sampling. Afilter (cm2) and Apunch (cm2) are the total areas of the hi-vol filter and the filter punches used for analysis, respectively.
2.4 Filter extraction
2.4.1 Extraction for water-soluble metals and ultrafiltration
For measurements of the water-soluble Fe and Cu collected on the filters, one circular filter punch (1 in. in diameter, Apunch=5 cm2) was extracted in 7 mL (Ve) of de-ionized water (DI water; Nanopure Infinity™ ultrapure water system; >18 MΩ cm−1) in a sterile polypropylene centrifuge tube (VWR International LLC, Suwanee, GA, USA) via 30 min sonication (Ultrasonic Cleanser, VWR International LLC, West Chester, PA, USA). The extract was filtered using a 0.45 µm PTFE syringe filter (Fisherbrand™) and then acidified using 6 M high-purity HCl to a pH of 1 to preserve the Fe or Cu in solution. A schematic of the extraction is shown in Fig. 1.
The filterable metal fraction in the extracts, defined as water-soluble metals in this paper, will include all dissolved metal forms and any colloidal particles with a diameter less than 0.45 µm, assuming that all colloidal particles <0.45 µm can penetrate through the syringe filter, and the retention efficiency of particles >0.45 µm is 100 %.
To assess the contribution of colloidal particles to the operationally defined WS Fe and WS Cu, a subset of the collected filters (N=69) were further filtered by ultrafiltration (Amicon™ Ultra centrifugal filter units, Merck Millipore Ltd., Tullagreen, Carrigtwohill, Co. Cork, Ireland). Two filter sizes, 30 000 and 3000 daltons (Da), were used for size fractionation, which roughly correspond to colloidal particles of 4 and 2 nm diameter, respectively (Erickson, 2009). Details of the conversion of particle mass in daltons to particle diameter and the effects of ultrafiltration membrane rejection are discussed in the Supplement. The particles were separated within the 30 000 and 3000 Da ultrafiltration units at ∼3000 g (4000 rpm) centrifugation for 30 and 60 min, respectively. The filtrate was then pH-adjusted to 1 and measured for WS Fe and WS Cu.
The soluble metal fraction may be affected by the degree of dilution of the samples in the extraction process. The ratio of extraction water volume to the volume of air sampled on the analyzed filter portion, denoted as P, is ∼0.5 in this study. This implies that Fe- and Cu-containing substances with solubility higher than roughly 10−3 g L−1 under conditions close to neutral pH will likely be fully dissolved, while species with water solubility as low as 10−6 g L−1 may be partially soluble but still contribute to the WS Fe and WS Cu measured with our method. Details of the effect of P on Fe or Cu solubility are discussed in the Supplement.
2.4.2 Extraction for total metal analysis
The extraction procedures for the determination of total Fe and Cu (shown in Fig. 1) follow the method conducted by Aller et al. (1986). To increase the solubility of metals, filter punches (1.5 cm2 for Fe and 3 cm2 for Cu) were digested with 1.5 and 2 mL of 6 M HCl for total Fe and Cu measurements, respectively. The filter was incubated in acid at 99 ∘C and shaken at a rotational frequency of 350 rpm using a ThermoMixer (Eppendorf North America, Inc., Hauppauge, NY, USA) for 24 h. This extraction method has been demonstrated to remove >96 % of Fe from the PACS1 international sedimental standards and >98 % of Fe from standard rocks and inner-shelf muds (Poulton and Canfield, 2005). The effect of extraction time, heating temperature and rotation rate on extraction efficiency were tested and are discussed below. The extract was diluted to 10 mL (Ve) using DI and then filtered by a 0.45 µm pore PTFE syringe filter. The volume of the sample extract used for the measurement (Vs) differed between samples and was determined by the ambient concentration of each sample. The pH of the sample extract was adjusted to 1 using 5 M NaOH, and the sample volume was adjusted to 2.5 mL with DI water.
A total of 10 blank filters were collected throughout the 1 year of sampling, and these were used randomly to assess the blank levels (i.e., multiple punches were taken from the blank filters for a blank analysis on different days). The same tools and type of filter were used for blanks and samples to track all possible contamination. The concentration of blanks was calculated using Eq. (1), assuming Va was equal to the volume of air drawn through actual ambient filter samples.
2.5 Colorimetric methods
2.5.1 Colorimetric method for Fe
A ferrozine-based method, which has been previously established and discussed (Oakes et al., 2010; Rastogi et al., 2009), was adopted and modified in this study for Fe measurement. Briefly, an excessive amount of reducing agent, hydroxylamine hydrochloride (0.1 mL, 1.5 M), was added to 2.5 mL (Vs) of sample solution to reduce all soluble forms of Fe (e.g., Fe(III)) to Fe(II). The vial was sealed and stored overnight (roughly 18 h) at room temperature to ensure complete reduction (Bengtsson et al., 2002; Rozan et al., 2002). After the overnight redox reaction, the sample pH was adjusted to 4–5 using an ammonium acetate buffer. A total of 0.2 mL of 5 mM ferrozine–acetate reagent was added to the solution to form the colored ferrozine–Fe(II) complex that absorbs light at 562 nm. The total volume of sample solution after addition of all the chemicals (Vl) was 2.85 mL.
The reaction between Fe(II) and ferrozine is found to be pH-dependent; the absorption of the complex increases rapidly when pH is above 0 and becomes steady within the pH range of 3 to 6 (Gibbs, 1976; Stookey, 1970). Under the conditions of the original method, when the pH of the sample was approximately 1, the absorbance of the complex was sensitive to small fluctuations in pH, adding uncertainty to the analysis. A further disadvantage is that at lower pH (pH=1), the reaction rate of Fe(II) and ferrozine was much slower relative to higher pH (3 to 5). Therefore, we tested a modification to the method by raising the pH of the sample to 4–5 during the colorimetric reaction using ammonium acetate buffer to increase the precision of the Fe measurement (Fig. 1). Part of the WS Fe samples was analyzed both ways, with low and higher pH, whereas all total Fe measurements were done with the buffered (higher pH) samples.
2.5.2 Colorimetric method for Cu
For the determination of Cu concentrations, a bathocuproine assay was used. Bathocuproine can selectively chelate with Cu(I) and form complexes absorbing light at 464 nm. To convert other soluble Cu forms (e.g., Cu(II)) to Cu(I), 0.5 mL of 1.6 M hydroxylamine hydrochloride was added to 2.5 mL (Va) sample extracts at pH 1 (as described above) and allowed to react for 30 min (Imamura and Fujimoto, 1975; Tomat and Rigo, 1975). The reaction between Cu(I) and bathocuproine is also pH-dependent, and so a set of controlled trials were performed with different pH conditions ranging from 0.5 to 6 to assess the optimal pH for forming the colored complex (Fig. S1 in the Supplement). The light absorption of the complex remained low at pH<1.5 and exhibited a rapid increase above pH 2 and became steady when pH was within the range of 5 to 6. Based on these results, 1 mL of 1 M sodium citrate was added to the sample solution to maintain the pH within the range of 5 to 6, followed by 1 mL of 2.8 mM bathocuproine (Vl=5.05 mL). After 15 min of reaction, the light absorption of the bathocuproine–Cu(I) complex was measured.
The colorimetric methods can provide insights on the forms of metal ions present, such as Fe(II) and Fe(III), or Cu(I) and Cu(II), for example by first measuring the reduced species, Fe(II) or Cu(I), then adding the reducing agent to measure the total (Fe(II)+Fe(III) or Cu(I)+Cu(II)). We do not attempt to speciate the WS Fe and WS Cu in this study since reduction–oxidation processes during the sampling, storage or extraction procedures may alter the valence states of airborne metals from what existed in the ambient particles. In situ measurements of Fe(II) are feasible using this colorimetric method when connected to a PILS or similar system (Oakes et al., 2010; Rastogi et al., 2009). It is not feasible to perform near-real-time measurements of Fe(III) due to its long reduction reaction time (overnight). Quantifying speciation of Cu is challenging due to the tendency of Cu(I) to undergo disproportionation in aqueous solutions (Johnson et al., 2015). In situ measurements of Cu(I) are possible with the presence of reducing agents and masking ligand to inhibit Cu(II) interference (Moffett et al., 1985), but further studies are necessary to achieve an acceptable detection limit.
2.6 Metal analysis by ICP-MS
Both total and water-soluble elements, which included magnesium (Mg), aluminum (Al), potassium (K), manganese (Mn) and zinc (Zn) in addition to Fe and Cu, were also measured by inductively coupled plasma mass spectrometry (ICP-MS) (Agilent 7500a series, Agilent Technologies, Inc., CA, USA). The sample preparation procedures have been described in detail in Gao et al. (2020a). The sample preparation for WS metal analysis followed the same extraction procedures as those described above for WS Fe and Cu. The filtered extract was then acid-preserved with concentrated nitric acid (70 %) to a final concentration of 2 % (). For total metal analysis, aqua regia, a more powerful acid than HCl, was used for filter digestion. The acid-digested sample was then diluted and filtered for ICP-MS analysis.
3.1 Evaluation of the colorimetric measurement method
3.1.1 Calibration of the detection methods
The analytical systems were calibrated and assessed with a series of standards diluted from the standard stocks of Cu(II) and Fe(III). The calibration curves for the reduced form of metals (Cu(I) and Fe(II)) are illustrated in Fig. 2. York regression (Wu and Yu, 2018) was applied and demonstrated a strong linear relationship between the element concentrations and the detected light absorbance with a coefficient of determination (R2) of 1.00. The slopes of calibration curves from multiple calibration runs were 0.033±0.004 for Cu (coefficient of variation, CV=12 %, N=22) and 0.053±0.005 for Fe (CV=9 %, N=5), indicating the stable performance of the systems. Repeated measurements (N=20) of a 35 µg L−1 standard solution had a relative standard deviation for both Cu and Fe of <10 %. These results indicated good precision and the robustness of this method for quantifying both Cu and Fe.
3.1.2 Blanks, detection limit and uncertainty
Field blanks were analyzed on each test day in parallel with samples to assess the overall system background. The limits of detection (LODs) of the spectroscopic systems, determined as 3 times the standard deviation of the filter blanks, were 3.07 ng m−3 (N=34) for WS Fe, 14.79 ng m−3 (N=6) for total Fe, 3.04 ng m−3 (N=29) for WS Cu and 3.23 ng m−3 (N=6) for total Cu. The detection limits in the solutions were 2.07 ppb for WS Fe, 2.05 ppb for WS Cu, 7.00 ppb for total Fe and 3.06 ppb for total Cu. The overall uncertainties in the sampling system ranged from 7 % to 14 %, calculated from the combination of the analytical uncertainty, uncertainty in blank measurements and quadrature sum of the square of various relative uncertainties (such as uncertainties caused by calibrations, blank filters, flow rates, liquid extract volumes, etc.). The detection limits and uncertainties were comparable to the measurement using ICP-MS, indicating that the LWCC has an equally good performance as ICP-MS, especially for the WS Fe measurement. A summary of LODs, blanks and uncertainty are shown in Table 1.
In the spectrophotometric method, species in ambient aerosol particles, such as black carbon (BC, or also called refractory BC), light-absorbing organic species (i.e., brown carbon, BrC) or inorganic species (i.e., components of mineral dust), can also absorb light at 482 or 562 nm, potentially resulting in measurement interference. However, these interferences are not accounted for in the blanks since no particles are collected as part of the blank measurement. To assess the interference, the light absorption at 484 or 562 nm of the individual liquid samples was measured without adding the colorimetric reagents (see X in Fig. 1). The interference was measured for the ambient samples collected in this study and in an extreme case (sampling wildfire smoke). By comparing the interference-corrected and non-corrected data, it is found that the average interference was less than 20 % for WS Fe and 1 % for total Fe. For total and WS Cu, a correction of about 24 % and 30 % was found, respectively. For the extreme case, samples from within wildfire plumes, for WS Cu an average correction of 50 % was needed (see Fig. S2). The impact of this correction also depends on the concentrations of the Fe or Cu, which in smoke plumes can be at low concentrations relative to a high level of light-absorbing aerosol species (i.e., BC and BrC), and so the correction, in this case, is important. The magnitude of the interference also depends on the extraction method; methods that more effectively extract solid particles (e.g., BC) or solubilize light-absorbing species at low pH (e.g., mineral dust) could produce higher interferences. Black carbon absorbs light over all wavelengths, whereas BrC and mineral dust absorb preferentially at lower wavelengths and so would be a potentially larger interference for the Cu method since the Cu complex is measured at 484 nm compared to 562 nm for Fe. Since incomplete combustion is the main source for BC and BrC, tests for this interference are most important when these types of emissions make a large contribution to the overall aerosol sources, such as sampling in regions highly influenced by biomass burning or vehicle tailpipe emissions. Interference from light-absorbing mineral dust species is most likely when sampling under dry conditions and high winds.
We also used a series of metal mixtures, which contained different levels of Fe, Cu, Co and Mn, to test the possible interferences from the formation of colored complexes with other metals. For the Cu measurement, no interference from Fe, Co or Mn was observed with up to 100 ppb of mixture of Fe, Co and Mn present. Similarly, Co or Mn did not interfere with the Fe measurement with Co or Mn concentrations in the liquid up to 100 ppb. Cu had an interference of less than 2 ppb in the Fe measurement with a Cu concentration in the liquid up to 40 ppb. In this study, the liquid concentrations of Cu from ambient samples were lower than 40 ppb; therefore, there was no interference of other metals in Cu or Fe measurements for the colorimetric methods. All measurements for ambient samples in this study were blank and interference-corrected.
3.1.4 Comparison to ICP-MS measurements and influence of experimental conditions
To further evaluate the accuracy of the new detection method, the concentrations determined by the colorimetric methods were compared to ICP-MS measurements. WS Fe and WS Cu were measured with the colorimetric methods using the LWCC system on all collected filters (N=355), but only a portion of the 355 filters were used for the measurement of total Fe and total Cu using the same LWCC system (Fe: N=23, Cu: N=21). All filters (N=355) were used for the ICP-MS measurements of both WS and total elements.
Water-soluble Fe and Cu. Regression analysis between the colorimetric methods and ICP-MS measurements showed good quantitative agreement for WS Fe and WS Cu with R2 greater than 0.89. The differences between the LWCC- and ICP-MS-measured concentrations were 6 % and 12 % for WS Fe and WS Cu (Fig. 3a and c) with the offsets (intercepts) less than 1 ng m−3. Considering measurement uncertainty, most points overlap the 1:1 line except for several WS Fe measurements. The difference in WS Fe between these two methods was possibly due to the acidic conditions (pH ∼1) of the colored-complex-forming solution used in the original approach of the colorimetric method. As noted above, to improve the method, some of the samples (N=69) were re-analyzed with sample pH adjusted to 4–5, which resulted in a higher correlation with the ICP-MS measurement, consistent with less sensitivity of the complex to pH when in the higher pH range (r2=0.92, slope 1.02, intercept −0.42 ng m−3) (Fig. 4). Considering the overall uncertainties in these two methods, the LWCC and ICP-MS measurements of the water-soluble metals were in agreement.
Total Fe and Cu. Similar results were found between the LWCC and ICP-MS methods for the measurement of total element concentration. For total Fe, York regression between the LWCC and ICP-MS yields a slope of 1.07, with an intercept of 3.09 ng m−3 and r2=0.97; see Fig. 3b. For Cu, the slope was 0.96, intercept ng m−3 and r2=0.95 (Fig. 3d).
As noted, in the colorimetric method description above, the filters for the total Fe and total Cu analysis were extracted for a 24 h period with the assistance of shaking and high temperature. The effect of extraction time, heating temperature and rotation rate on extraction efficiency was tested (with N=3 filters for each condition). It was found that for total Fe extraction, there was a 5 % decrease when the extraction time was shortened from 24 to 2.5 h and a 5 % increase when extraction time was increased from 24 to 120 h. For Cu, the concentration decreased by 15 % when the extraction time was changed from 24 to 2.5 h and decreased by 5 % when the extraction time was extended to 120 h. An extraction time of 24 h was concluded to be optimal for both Fe and Cu. Extract temperature had a small impact, with a 5 % and 10 % decrease for Fe and Cu extraction, respectively, when the temperature decreased from 99 to 50 ∘C. The rotational shaking was found to significantly affect the extraction efficiency. Compared to shaking at a rate of 350 rpm, extraction without rotational shaking reduced the extraction efficiency by 98 % and 89 % for Fe and Cu, respectively.
3.2 Characteristics of Fe and Cu in urban Atlanta
3.2.1 Water-soluble, total and fractional solubility
The annual average concentrations of total Fe measured by ICP-MS and WS Fe measured by the LWCC was 203.7 and 20.2 ng m−3, respectively. Mass concentrations of WS Fe spanned a wide range, from the detection limit (3.07 ng m−3) to 169 ng m−3. The average concentrations of total Cu and WS Cu were 30.7 and 13.8 ng m−3, respectively. Mass concentration of WS Cu ranged from the detection limit (3.04 ng m−3) to 132 ng m−3. Due to uncertainties in both water-soluble and total measurements, a few calculated Cu solubilities were higher than 1 and were treated as 1 when calculating the average fraction of Cu. Those solubilities when total or WS concentrations were blank were estimated using half of the detection limit of the total or WS concentration. Tables 2 and S4 in the Supplement provide a more complete summary. The statistics of the LWCC measurement and ICP-MS measurement of total metals were different since only a fraction of all the 2017 filter samples were analyzed for total metals using the LWCC system (Fe: N=23, Cu: N=21). These concentrations were comparable with a previous study conducted in Atlanta, GA, and in the range reported for many other regions globally (Table 3).
a Fang et al. (2015). b Manousakas et al. (2014). c Canepari et al. (2014). d Olson et al. (2008). e Hagler et al. (2007). f Kulshrestha et al. (2009). g Based on ICP-MS measurement. h Based on LWCC measurement
As expected the total Fe concentration was much higher than total Cu since Fe is a common element in the Earth's crust (mass fraction of iron is 5.63 %) (Tomaszewski, 2017) and ubiquitous in mineral dust, while PM2.5 Cu in urban environments is mainly derived from vehicle brake and tire wear and tailpipe emissions resulting from motor-oil impurities; both of these sources are associated with traffic (Fang et al., 2015; Marcazzan et al., 2003). Other industrial sources of PM2.5 Cu are also possible. Despite much higher total concentrations, the concentrations of WS Fe were comparable with WS Cu. This is due to a much lower solubility of Fe than Cu. The average soluble fraction of Fe and Cu is 14.6 % and 50.7 %, respectively (Table 2).
3.2.2 Components of water-soluble Fe and Cu based on ultrafiltration
Ultrafiltration of WS Fe and WS Cu was used to assess contributions of colloidal particles to the concentrations of water-soluble metals. The data of the samples whose concentrations through 30 000 Da ultrafiltration were significantly higher than those through a 0.45 µm filter were removed. The size fractionation results are given in Fig. 5. Based on medians of all ultrafiltration data, approximately 84 % of the WS Fe had a nominal diameter smaller than 4 nm, passing through the 30 000 Da filter; 61 % of the WS Fe was nominally smaller than 2 nm in diameter, which passed through the 3000 Da filter. The fractions for the sizes in between were calculated by taking the difference, and a rough distribution of Fe in the overall WS Fe was 61 % smaller than 2 nm, 23 % between 2 and 4 nm, and 16 % between 4 nm and 0.45 µm. For WS Cu, most (84 %) of WS Cu passed through the 3000 Da filter and had a nominal diameter less than 2 nm, with 4 % between 2 and 4 nm and 15 % between 4 nm and 0.45 µm.
The 2 to 4 nm fraction of Fe colloidal particles (23 %) was higher than that found in WS Cu (4 %, which was practically zero). Laboratory studies find that ambient particles undergoing pH cycling from low pH (∼2) in deliquesced particles to circumneutral pH of 5 to 6 when activated in cloud drops lead to the formation of nanoparticles of highly reactive ferrihydrite of a few nanometers in diameter (∼5 nm) (Shi et al., 2011). The pH of the bulk PM2.5 aerosol in this region is estimated to be in the range of 1.63 to 2.31 (25th and 75th percentiles throughout the year; Wong et al., 2020), which would rise rapidly to pH between 5 and 7 in the extraction solution (based on measurements). Rapid increase to circumneutral pH leads to a supersaturated soluble Fe(III), which then precipitates out of the solution. Thus, either from pH cycling experienced by the ambient aerosol or changes due to the filter extraction process, the colloidal particles of WS Fe observed in the 2 to 4 nm range are consistent with the ferrihydrite reported by Shi et al. (2011). Acid-driven solubility of Cu occurs rapidly at higher pHs and so may not reach supersaturation like that of Fe when pH increases to circumneutral, accounting for the lack of colloidal particles in the nominal 2 to 4 nm size range of WS Cu.
For both Fe and Cu, the fraction of Fe and Cu in the 4 nm to 0.45 µm range may be insoluble chemical forms from primary emissions, like metal oxides that had been extracted from the filter and had passed through the syringe filter, making them not a “true” water-soluble species (i.e., not unique from the insoluble fraction). More research needs to be done to determine what caused the variability in the various fractions separated by ultrafiltration and to characterize the forms of the metals in the various size fractions of what we operationally define as overall water-soluble metal. These results have implications for aerosol toxicity and health effects.
In this study, a new approach for the measurement of WS Cu and total Cu has been developed and tested based on liquid spectrophotometry. It follows a similar method for quantifying WS Fe. All measurements can be performed with a single relatively inexpensive spectrophotometer. Utilizing daily PM2.5 filters collected in Atlanta during 2017, the spectrophotometer methods were assessed by comparing with elements measured by ICP-MS on the same ambient filter samples. Calibrations with liquid standards produced by serial dilutions were highly linear and stable over periods of days. The spectrophotometric method detection limits in this study were 3.07 ng m−3 for WS Fe, 14.8 ng m−3 for total Fe, 3.04 ng m−3 for WS Cu and 3.23 ng m−3 for total Cu, with measurement uncertainties ranging from 7 % to 14 %. The detection limit and uncertainties are comparable to ICP-MS measurement. Possible interferences from other light-absorbing species, such as black and brown carbon, should be considered, especially for the Cu measurement and in situations where emissions of light-absorbing aerosols are high (e.g., BC, BrC, mineral dust). From comparisons with ICP-MS measurements, in all cases (WS Fe, total Fe, WS Cu and total Cu) the spectrophotometry data were in good agreement (slopes ranged between 0.88 and 1.07 and r2>0.89).
In Atlanta, total Fe concentration was much higher than total Cu, whereas the level of WS Fe was comparable with WS Cu due to a higher soluble fraction of PM2.5 Cu (45.6 %) compared to Fe (14.6 %). The composition of what is operationally defined as WS Fe and WS Cu (i.e., the aerosol filter extracted in pure water and extract passed through a 0.45 µm pore liquid filter) was investigated with ultrafiltration Fe and Cu in the filtrate measured with the spectrophotometric (LWCC) method. Ultrafiltration showed that roughly 84 % of both WS Fe and WS Cu was composed of dissolved species or colloidal particles smaller than nominally 4 nm diameter. Fe and Cu are two important redox-active metals that have been linked to reactive oxygen species (ROSs) formed in vivo and lead to adverse health effects through oxidative stress. These spectrophotometric methods allow analyses of the various physical forms of Fe and Cu in ambient aerosol particles and are directly applicable to aerosol toxicity studies and their contribution to aerosol oxidative potential (OP).
The data used in this paper are publicly available at https://doi.org/10.5281/zenodo.4927503 (yhyang611, 2021) and can also be obtained from the corresponding author upon request.
The supplement related to this article is available online at: https://doi.org/10.5194/amt-14-4707-2021-supplement.
YY is responsible for the study design, experiment using the LWCC, data analysis and manuscript writing. RJW supervised the study and participated in the writing and revision of the paper. DG provided ICP-MS data and interpretation of the results.
The authors declare that they have no conflict of interest.
The authors acknowledge funding by the Phillips 66 company. Thanks are given to Linghan Zeng for his kind guidance in the experiment and many interesting discussions about data analysis. We would also like to thank Allison Weber for her help in conducting the IC measurements.
This research has been supported by the Phillips 66 Company (grant no. AGR DTD 10/05/2020).
This paper was edited by Mingjin Tang and reviewed by two anonymous referees.
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