Open Access Article
John J.
MacInnis
a,
Trevor C.
VandenBoer
b and
Cora J.
Young
*a
aDepartment of Chemistry, Memorial University, St. John's, NL, Canada. E-mail: cora.young@mun.ca; Tel: +709-684-7280
bDepartment of Earth Science, Memorial University, St. John's, NL, Canada
First published on 11th April 2016
An inability to produce environmentally relevant gaseous mixing ratios of perfluoroalkyl acids (PFAAs), ubiquitous global contaminants, limits the analytical reliability of atmospheric chemists to make accurate gas and particulate measurements that are demonstrably free of interferences due to sampling artefacts. A gas phase source for PFAAs based on the acid displacement mechanism using perfluoropropionate (PFPrA), perfluorobutanoate (PFBA), perfluorohexanoate (PFHxA), and perfluorooctanoate (PFOA) has been constructed. The displacement efficiency of gas phase perfluorocarboxylic acids (PFCAs) is inversely related to chain length. Decreasing displacement efficiencies for PFPrA, PFBA, PFHxA, and PFOA were 90% ± 20%, 40% ± 10%, 40% ± 10%, 9% ± 4%, respectively. Generating detectable amounts of gas phase perfluorosulfonic acids (PFSAs) was not possible. It is likely that lower vapour pressure and much higher acidity play a role in this lack of emission. PFCA emission rates were not elevated by increasing relative humidity (25%–75%), nor flow rate of carrier gas from 33–111 sccm. Overall, reproducible gaseous production of PFCAs was within the error of the production of hydrochloric acid (HCl) as a displacing acid (±20%) and was accomplished using a dry nitrogen flow of 33 ± 2 sccm. A reproducible mass emission rate of 0.97 ± 0.10 ng min−1 (n = 8) was observed for PFBA. This is equivalent to an atmospheric mixing ratio of 12 ppmv, which is easily diluted to environmentally relevant mixing ratios of PFBA. Conversely, generating gas phase perfluorononanoic acid (PFNA) by sublimating the solid acid under the same conditions produced a mass emission rate of 2800 ng min−1, which is equivalent to a mixing ratio of 18 ppthv and over a million times higher than suspected atmospheric levels. Thus, for analytical certification of atmospheric sampling methods, generating gas phase standards for PFCAs is best accomplished using acid displacement under dry conditions. This yields quickly stabilized, reproducible emissions and mixing ratios that are easily diluted to environmentally relevant levels. Gas phase PFBA from this source has also been shown to be quantitatively collected using an annular denuder coated with sodium carbonate (Na2CO3) according to Environmental Protection Agency (EPA) method Compendium I.O-4.2. Overall, producing gas phase PFAAs at constant atmospherically-relevant levels will enable the development of standard approaches in certifying gas and particle collection efficiencies for instruments interrogating the gas-particle partitioning and long-range transport of PFCAs in the atmosphere.
It has been an analytical challenge to quantify mixing ratios of PFAAs in atmospheric samples due to an absence of gas standards across the relevant environmental range. Therefore, it is not currently possible to validate sampling methods for their measurement accuracy and precision. It has also been reported that current sampling methods suffer from artefact biases.14,22,23 A popular approach to collect aerosols involves pulling a large volume of air through a filter to collect particles, while collecting gases downstream using a sorbent. This approach has two major drawbacks: (i) gas phase PFAAs irreversibly sorb to some filters;22 and (ii) gas phase species present in the atmosphere, like hydrochloric acid (HCl), could react with perfluorocarboxylic acids (PFCAs) salts on particles releasing them to the gas phase, similar to other known chemistry.24 Improvements have been made over recent years to mitigate positive biases by deactivating the surfaces of filters, which has been found to minimize gas phase sorption.22 However, gas phase artefacts are not limited to sorption on filter material. The reaction of gas phase PFAAs with sampled particulates likely leads to sampling artefacts despite the presence of a deactivated filter. To prevent this, gases should be collected prior to particles, as is standard practice for measuring atmospheric acids such as HCl, nitric acid (HNO3), and sulphur dioxide (SO2).25,26 Annular denuders can provide such an option and have been demonstrated to effectively collect gas phase species during atmospheric sampling.25 This is accomplished by applying a coating to the concentric ring surfaces within the denuder, which is selective for the target compounds. One test of denuders for collection of PFAAs upstream of particle collection has been made. The sorbent used was XAD-4, which was shown to be unsuitable for collecting gas phase PFAAs, with recoveries from 50–72% for C8–C12 PFCAs.14 An examination of sampling artefacts was also performed by comparing particle-associated fractions of filters collected using a high-volume air sampler to those collected downstream from a denuder coated with XAD-4 resin.14 Since neither method has been fully validated for the collection of gas or particle-phase PFAAs, method intercomparison provides limited information. A full understanding of atmospheric mixing ratios of PFAAs, as well as their gas-particle partitioning can only be achieved if sampling artefacts are measured quantitatively and minimized.
Acid displacement has been used extensively to produce atmospherically relevant mixing ratios of standard gas phase nitrous acid (HONO).27–30 The most robust undertaking is described by Febo et al.,30 using controlled amounts of HCl for displacement of sodium nitrite (NaNO2) (1):
| HCl(g) + NaNO2(s) → NaCl(s) + HONO(g) | (1) |
The objective of this work was to develop a constant-output and controllable gas phase source for PFAAs at atmospherically relevant mixing ratios using a similar approach (2):
| HX(g) + MPFAA(s) → MX(s) + PFAAH(g) | (2) |
Quantitation of PFAAs was carried out through extracted ion chromatograms of molecular ion peaks. Additional characteristic peaks were used to confirm the identity of PFAAs (Table 1). Instrument limits of detection (LOD) and quantitation (LOQ) were defined as concentrations having signal-to-noise ratios of 3 and 10, respectively. Signal-to-noise ratios across the calibration range were determined by dividing peak heights by the standard deviation of the blank signal at the compound-specific retention time windows (Table 1). All calibration curves had coefficients of determination greater than 0.995.
| Analyte | pKa | Quantitative ion (m/z) | Confirmation ion (m/z) | LOD (ng mL−1) | LOQ (ng mL−1) |
|---|---|---|---|---|---|
| Perfluoropropionate (PFPrA) | 0.531 | 163 | 119 | 20 | 50 |
| Perfluorobutanoate (PFBA) | 0.432 | 213 | 169 | 7 | 20 |
| Perfluorohexanoate (PFHxA) | 0.932 | 313 | 269 | 3 | 10 |
| Perfluorooctanoate (PFOA) | 0.532 | 413 | 369 | 2 | 6 |
| Perfluorobutane sulfonate (PFBS) | −3.932 | 299 | 219 | 1 | 5 |
| Perfluorooctane sulfonate (PFOS) | −3.332 | 499 | 419 | 0.8 | 2 |
Carrier gas flow effects on the PFAA displacement efficiencies were assessed by increasing flows to 41, 62, and 111 sccm. RH effects on displacement efficiencies were explored at 25, 50, and 75%. The RH and flow experiments were carried out interchangeably. To minimize carryover effects the system was flushed overnight to equilibrate with the starting conditions of the next experiment when switching from dry to wet conditions, or vice versa.
High flow rates and RH were explored by modifying the permeation oven setup as shown in Fig. 2, with three increasing flows being synonymous to the three increasing RH levels to decouple the RH effect from flow. Briefly, a PTFE tee was introduced upstream of the salt bed to add humidified air to the dry nitrogen flow using a mass flow controller (MFC) (0.01–0.5 L min−1, MKS GE50A, Andover, MA) to regulate the flow of nitrogen through an impinger of deionized water. The humidified flow mixed with the dry nitrogen and passed through the salt bed (dashed blue line, Fig. 2). A humidity probe from Vaisala (HMP 110, Helsinki, Finland) measured RH. For high flow experiments (i.e. flow >40 sccm) the flow from the MFC bypassed the humidifying glass impinger (red dashed line, Fig. 2).
:
50 ethanol and water with 1% (w/v) glycerol was used. The solution was applied evenly to the denuder surface by rotation and inversion, followed by removing the excess solution and drying the coating under a stream of dry nitrogen. The annular denuder was placed between the permeation oven and the impinger (Fig. 2). A flow of 111 sccm from the permeation oven of PFBA was directed through the annular denuder for 67 hours and the outflow was collected into an impinger. The denuder was extracted with 10 mL of deionized water and the amount of PFBA in this extract and the impinger solution were quantified using the LC method described above. The protocol for coating the denuder was based on the atmospheric acid sampling method of the US-EPA (Compendium I.O-4.2.).
Quality control experiments were conducted to assess: (i) sorption losses of PFAAs to the impinger; (ii) losses via volatilization from deionized water; and (iii) efficacy of gas phase collection.
It is possible that PFAAs in the anionic state can adsorb to glass surfaces.33 To assess losses to the glass impinger during sample collection, known amounts of PFPrA, PFBA, PFHxA, PFOA, PFBS, and PFOS were spiked into 25 mL of deionized water contained in the glass impinger. The concentrations (200, 100, 50 ng mL−1) of spiked solutions corresponded to PFAA concentrations observed in typical experimental samples collected over 1–5 days. Two sets of conditions were tested using the spiked solutions added to the glass impingers: (i) PFAA solutions were immediately collected into a pre-cleaned polypropylene bottle; (ii) PFAA solutions were allowed to interact with the glass walls and all 25 mL was collected at times corresponding to experimental sampling durations (1–5 days). The impinger samples at each time were transferred into a pre-cleaned polypropylene bottle and analysed using LC-ESI-ToF to quantify losses.
To assess PFAA losses due to volatilization (direct or via aerosol formation) from the deionized water in the impinger, known amounts of PFBA were spiked into 25 mL of deionized water in a polypropylene volumetric flask. The spiked solutions were transferred into the glass impinger. Nitrogen was then bubbled through the impinger solution at 33 ± 2 sccm. The entire volume of the PFBA solution was removed from the impinger at times corresponding to the typical experimental sampling durations (1–5 days). To determine if losses were due to volatilization, an additional experiment with a second impinger in tandem was added to the first using PFBA quantified by LC-ESI-ToF.
A collection efficacy experiment using the tandem impinger design was also conducted. Gas phase PFBA was generated using acid displacement and collected using the tandem impingers. Evidence of inefficient PFBA gas phase collection would be indicated if PFBA was measured in the second impinger.
The average recoveries (n = 3) for collected PFAA solutions were: 82%, 77%, 77%, 84%, 105%, 85% for PFPrA, PFBA, PFHxA, PFOA, PFBS, and PFOS, respectively. For PFAA solutions exposed to bubbling through the impinger (n = 3; 1–5 days) average recoveries were: 90%, 79%, 80%, 90%, 101%, 89% for PFPrA, PFBA, PFHxA, PFOA, PFBS, and PFOS, respectively. This indicates that losses of PFAAs to the glass surfaces of the impinger are at most 23%. The extent of PFAA loss from deionized water due to volatilization or particle export was equal to or less than sorption losses (90%, n = 3). Negligible losses of PFAAs by volatilization from deionized water were further supported by the collection efficacy experiments. An average recovery of 77% for PFBA (n = 3), in the first impinger was observed. No detectable concentrations of PFBA were found in the second impinger in series. This recovery is consistent with the 77% recovery due to impinger sorption losses. It can be concluded that losses of PFBA, and by proxy the other PFAAs, as a result of volatilization from deionized water are not significant.
Collecting gas phase PFBA was also used to ensure mass emission measurements were quantitative using the tandem impinger setup (n = 1). After a collection period of 65 hours, a concentration of 156 ng mL−1 was observed in the first impinger, which is equivalent to a mass emission rate of 0.84 ng min−1. This emission rate is in good agreement with the other PFBA emission measurements in this work (see Table 4). No detectable amounts of PFBA were found in the second impinger in series. The scrubbing efficacy of other PFAAs is expected to be more complete than PFBA as a result of decreasing air–water partitioning coefficient values with increasing molecular weight.32 It can be concluded that collecting gas phase PFBA is quantitative using the single impinger approach, and can be reliably extended to other PFAAs with similar physicochemical properties. Data was not corrected for recoveries presented in Table 2.
| MT (PFAA) = E·MD (HX) | (3) |
All PFCA salts tested formed their corresponding acids through acid displacement (4):
| HX(g) + NaPFCA(s) → NaX(s) + PFCAH(g) | (4) |
To evaluate the relative efficacy of generating different gas phase PFCAs using acid displacement, a suite of PFCA congeners were examined (Fig. 3).
The displacement efficiency of PFPrA was the highest in the series of PFAAs with an average of 90 ± 20%, followed by PFBA (40 ± 10%), PFHxA (40 ± 10%), and PFOA (9 ± 4%). PFBA (n = 2), PFHxA (n = 1), and PFOA (n = 3) samples were generated using a HBr permeation device. The remaining samples were generated using HCl permeation devices (Table 3). To validate LC-ESI-ToF quantification for PFPrA, samples were also analysed by IC. At the 95% confidence level (t-test, p < 0.05), the displacement efficiency determined by either analysis was not statistically different. A weighted linear regression using the standard deviation of displacement efficiencies from multiple displacement setups shows for every additional CF2 unit, the displacement efficiency decreases by 12% (R2 = 0.61) for this range of PFCA congeners.
| Congener | Displacing acid | Temperature (°C) | Displacing acid emission rate (ng min−1) | PFAA mass emission rate (ng min−1) | PFAA molar emission rate (mol min−1) | Displacement efficiency (%) | Average (%) | Standard deviation (%) |
|---|---|---|---|---|---|---|---|---|
| PFPrA | HCl | 40 | 0.40 | 1.9 | 8.8 × 10−12 | 100 | 90 | 20 |
| HCl | 40 | 0.40 | 2.2 | 1.0 × 10−11 | 120 | |||
| HCl | 40 | 0.40 | 1.6 | 7.3 × 10−12 | 86 | |||
| HCl | 40 | 0.40 | 1.6 | 7.4 × 10−12 | 87 | |||
| HCl | 40 | 0.40 | 1.2 | 5.8 × 10−12 | 69 | |||
| PFBA | HBr | 40 | 1.0 | 1.0 | 4.8 × 10−12 | 43 | 40 | 10 |
| HBr | 40 | 1.0 | 0.9 | 4.0 × 10−12 | 37 | |||
| HCl | 25 | 0.40 | 0.8 | 3.6 × 10−12 | 33 | |||
| HCl | 25 | 0.40 | 0.7 | 3.5 × 10−12 | 32 | |||
| HCl | 25 | 0.40 | 0.7 | 3.1 × 10−12 | 28 | |||
| HCl | 25 | 0.40 | 1.0 | 4.9 × 10−12 | 45 | |||
| HCl | 25 | 0.40 | 1.6 | 7.3 × 10−12 | 67 | |||
| HCl | 25 | 0.40 | 1.1 | 5.1 × 10−12 | 46 | |||
| PFHxA | HCl | 40 | 1.0 | 4.4 | 2.0 × 10−11 | 56 | 40 | 10 |
| HCl | 40 | 0.40 | 1.2 | 5.8 × 10−12 | 36 | |||
| HCl | 25 | 0.40 | 2.0 | 9.2 × 10−12 | 57 | |||
| HCl | 25 | 0.40 | 1.6 | 7.4 × 10−12 | 46 | |||
| HCl | 25 | 0.40 | 0.9 | 4.2 × 10−12 | 26 | |||
| HCl | 25 | 0.40 | 1.1 | 5.2 × 10−12 | 32 | |||
| HBr | 25 | 1.0 | 1.0 | 4.9 × 10−12 | 26 | |||
| PFOA | HBr | 25 | 1.0 | 0.7 | 3.4 × 10−12 | 14 | 9 | 4 |
| HBr | 25 | 1.0 | 0.3 | 1.3 × 10−12 | 5 | |||
| HBr | 25 | 1.0 | 0.5 | 2.2 × 10−12 | 9 | |||
| PFBS | HBr | 25 | 1.0 | <6.2 × 10−2 | <2.1 × 10−13 | <0.97 | 0.6 | 0.5 |
| HBr | 25 | 1.0 | <2.2 × 10−2 | <7.5 × 10−14 | <0.36 | |||
| HBr | 25 | 1.0 | <9.4 × 10−2 | <3.1 × 10−13 | <1.5 | |||
| HCl | 25 | 0.40 | <9.2 × 10−2 | <3.9 × 10−14 | <0.22 | |||
| HCl | 25 | 0.40 | <1.7 × 10−2 | <5.6 × 10−14 | <0.31 | |||
| HCl | 25 | 0.40 | <3.7 × 10−3 | <1.2 × 10−14 | <0.067 | |||
| PFOS | HBr | 25 | 1.0 | <7.0 × 10−3 | <1.4 × 10−14 | <0.11 | ||
Partitioning of a compound from the condensed to gaseous phase in this type of permeation and reaction system is likely influenced by the acidity and volatility of the displacing acid and targeted salt compounds. However, it is not always clear which property takes precedence in acid displacement. For example, it has been demonstrated that less-acidic HNO3 (pKa ∼ −5), can displace more-acidic HCl (pKa ∼ −7) from sodium chloride salts on atmospheric particles originating from sea spray.24,26 The aqueous acidities of the aforementioned acids do not appear to influence the outcome of acid displacement on atmospheric particles with low water content. Considering these acids have vapour pressures within a factor of two,34 the effectiveness of acid displacement is likely a complex function of their relative atmospheric mixing ratios and aerosol water content.35
The observed trends in acid displacement from this work are consistent with the acidity and volatility of PFCAs. The pKa of this suite of PFCAs has been reported21 as approximately 0.5, while the pKas of HCl and HBr are −7 and −9, respectively. Simply put, the difference in acidity would favour the transfer of a proton from the strong acids to the PFCAs. However, as described above, it is unlikely that acid strength alone explains the order of observed decreasing PFCA displacement efficiencies because the difference in pKa values between PFCA congeners is small.36 The relationship between PFCA displacement efficiencies and their predicted vapour pressures37 (Fig. 4) shows an inverse relationship (R2 = 0.68) to that observed for chain length. A weighted linear regression shows the displacement efficiency increases by 24% for every order of magnitude increase in vapour pressure (Pa) for this range of PFCA congeners. Estimations of displacement efficiencies of other PFCA congeners may be possible using these relationships.
![]() | ||
| Fig. 4 PFCA displacement efficiencies under dry conditions as a function of vapour pressure. PFPrA (yellow; n = 5) PFBA (red; n = 8), PFHxA (green; n = 8), PFOA (blue; n = 3). Predicted vapour pressures (C4–C8) are from Bhhatarai et al.37 and PFPrA from Sigma Aldrich.38 | ||
This suggests the efficiency of gas phase PFCA generation using acid displacement is driven by the volatility of the PFCA congeners in addition to the favourable transfer of a proton from either of the acids to the PFCA.
It is also possible that PFSAs were generated, but not detectable. Thus, upper limits for emission rates of PFSAs at the instrument LOD were determined to be 34 pg min−1 for PFBS, and 7 pg min−1 for PFOS. These emission rate upper limits are about 10 and 100 times smaller than the measured PFOA emission rates for PFBS and PFOS, respectively.
Most PFBA measurements in Fig. 5 fall within the measured variability of the HCl and HBr acid emission rates from the permeation devices. This suggests displacement is limited by the transport of the displacing acid to the PFAA salt bed, and the probability of reaction between the gas and salt.
An additional consideration in controlling emission stability was modification of the PFAA salt bed temperature. The PFBA salt bed was operated at room temperature (n = 6; ∼25 °C), and thermostated at 40 °C (n = 2). The thermostated samples correspond to the HBr-generated PFBA represented as red triangles in Fig. 5. Based on the consistency of PFBA displacement efficiencies at different salt bed temperatures, the results suggest there is no temperature dependence between 25–40 °C, but there does appear to be a reduction in variability under the more stable temperature regime. The use of two separate thermostated aluminium blocks could therefore add further versatility to this system in controlling reagent and target analyte production rates.
Overall, the largest driver of variability in generating gas phase PFBA is the emission rate of the displacing acid from the permeation devices, ±20% for both HCl and HBr, thereby limiting the level of precision in the output of the PFBA source.
To the knowledge of the authors, it is not possible to purchase salts of PFNA; therefore, a comparison of the emission rates from subliming the solid acid to the sodium salt cannot be made. However, the emission rate for a sodium salt of PFNA can be estimated according to the weighted linear regression from multiple displacement setups for PFCA congeners (Fig. 3). The expected emission rate of PFNA from a sodium salt was calculated to be 0.10 ng min−1 (E = 2%) and is approximately 104 lower than emission rates observed from the solid acid. This likely suggests that detectable quantities of PFNA and longer chain acids may be limited when using acid sources with mass emissions smaller than 0.40 ng min−1, and may not be possible at all for larger congeners if the assumed linear trend is valid.
Overall, using a salt is simple and provides emission rates that are easily diluted to atmospherically relevant levels, which is imperative in generating gas phase PFAA standards to test analytical instrumentation under representative sampling conditions.
To elucidate flow rate and RH dependencies of PFAA gaseous emissions, experiments were carried out using the PFBA sodium salt. PFBA was chosen as a proxy for all PFCAs because it is the most volatile PFCA that can be reliably quantified by LC-ESI-MS. Any observable flow or RH dependencies with PFBA is expected to be consistent across the larger PFCA congeners. All RH and flow experiments were carried out using the same HCl permeation device (0.40 ng min−1) and are summarized in Table 4.
| Experiment | Total production time (days) | Mass emission rate (ng min−1) | Flow-normalized emission (ng cm−3) |
|---|---|---|---|
| Flow (sccm) | |||
| 33 | 2.7 | 0.8 | 0.02 |
| 2.7 | 0.9 | 0.03 | |
| 4.1 | 1.1 | 0.05 | |
| 5.3 | 0.7 | 0.02 | |
| 6.0 | 1.0 | 0.03 | |
| 7.0 | 1.1 | 0.05 | |
| 8.0 | 1.6 | 0.02 | |
| 8.3 | 0.7 | 0.03 | |
| 41 | 3.0 | 1.0 | 0.02 |
| 5.9 | 1.3 | 0.03 | |
| 8.9 | 2.1 | 0.05 | |
| 62 | 3.9 | 0.7 | 0.01 |
| 4.9 | 1.3 | 0.02 | |
| 8.0 | 1.0 | 0.02 | |
| 111 | 1.9 | 1.1 | 0.01 |
| 7.9 | 1.2 | 0.01 | |
| RH (%) | |||
| 0 | 2.7 | 0.8 | 0.02 |
| 2.7 | 0.9 | 0.03 | |
| 4.1 | 1.1 | 0.03 | |
| 5.3 | 0.7 | 0.02 | |
| 6.0 | 1.0 | 0.03 | |
| 7.0 | 1.1 | 0.03 | |
| 8.0 | 1.6 | 0.05 | |
| 8.3 | 0.7 | 0.02 | |
| 25 | 3.9 | 0.1 | 0.003 |
| 5.9 | 0.3 | 0.006 | |
| 7.9 | 0.8 | 0.02 | |
| 50 | 3.9 | 0.1 | 0.002 |
| 7.9 | 0.2 | 0.003 | |
| 9.9 | 0.7 | 0.01 | |
| 75 | 3.0 | 1.0 | 0.009 |
| 11 | 1.3 | 0.01 | |
| 16 | 1.4 | 0.01 | |
For non-reactive compounds such as PFAAs, increasing flow rates should not increase the rate of mass transfer of the PFAAs generated at the solid surface to the gas phase, so long as the number of collisions between the HCl and salt are not reduced. No enhancement in PFBA emissions was observed with increasing flow relative to emissions under dry conditions, as seen in Table 4. Further evidence of this is shown in Fig. 6, where the mass emission rate (1.10 ± 0.08 ng min−1, n = 16) of PFBA was found to independent of flow and the total production time of the system.
![]() | ||
| Fig. 6 PFBA mass emission rate of different carrier gas flow rates through the salt bed as a function of total PFBA production time. Red circles, 33 sccm; grey squares 41 sccm; blue diamonds, 62 sccm; green triangles, 111 sccm. Error bars represent the analytical accuracy of the LC-ESI-ToF for each measurement. The solid black line represents the average mass emission rate of PFBA under dry conditions; dashed black lines correspond to the total uncertainty as described in Fig. 5. | ||
Flow-normalized emissions of RH experiments presented in Table 4 demonstrate decreases in PFBA emissions relative to experiments carried out in the absence of RH. The introduction of water into the salt bed at 25 and 50% RH resulted in a reduction of PFBA mass emission rate by 82% (0.18 ± 0.09 ng min−1, n = 4) for up to a week. The average mass emission rate at 0% RH was used as reference for determining the reduction in mass emission rate under humid conditions. Reduction in PFBA output was not observed for experiments conducted at 75% RH (Fig. 7).
![]() | ||
| Fig. 7 PFBA mass emission rate under different RH as a function of total PFBA production time. Red circles, 0% RH, grey squares, 25% RH; blue diamonds, 50% RH; green triangles, 75% RH. Error bars represent the analytical accuracy of the LC-ESI-ToF for each measurement. The solid black line represents the average mass emission rate of PFBA under dry conditions; dashed black lines correspond to the total uncertainty as described in Fig. 5. | ||
The introduction of water into the PFBA salt bed increases the complexity of the system and decreases PFBA mass emission rates relative to experiments at 0% RH, as seen in Fig. 7. Generating reproducible gas phase emissions of PFBA using RH requires longer equilibration periods compared to dry conditions. Over time, mass emission outputs eventually reached values (1.1 ± 0.3 ng min−1, n = 5) consistent with mass emission rates observed under dry conditions (1.10 ± 0.08 ng min−1, n = 16). Potential equilibration times of a week are not convenient unless a thermostated permeation system has sufficient channels to accommodate and continuously produce the full suite of targeted PFAA salts and precursor acid permeation devices. Whether displacement systems with water produce more stable emissions once equilibrated was therefore not determined. For most applications, it can be concluded that PFCAs are most reliably and simply produced by acid displacement under dry conditions.
Given the strong acid nature of PFAAs, we assessed the likely ability of a Na2CO3 coating to quantitatively scrub gas phase PFAAs. The annular denuder was placed between the exit of a PFBA salt bed and the glass impinger (Fig. 1).
A flow rate of 111 sccm was used, providing a mixing ratio of a few ppmv for 67 hours. While this mixing ratio is much higher than expected ppq levels,13,48 dilution of this output is easily accomplished using MFCs and, based on this work, 1000 times closer than approaches that would utilize sublimation of solid acids under the same conditions. The measured denuder extract had a PFBA concentration equivalent to a mass emission rate of 1.2 ng min−1. The observed mass emission rate falls within the standard error of the 111 sccm mean measurements (±0.1 ng min−1), which suggests a quantitative recovery.
No detectable breakthrough of PFBA was observed in the glass impinger solution. Thus, the Na2CO3 coating is suitable for quantitative gas phase PFCA collection at parts per million mixing ratios and will therefore be effective at collecting lower PFAA amounts expected in real atmospheric samples. Archived samples that followed this method from standard monitoring networks therefore should be possible to quantitatively analyse for PFCAs and possibly PFSAs.
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