Comment on “Comparison of ozone measurement methods in biomass burning smoke: an evaluation under field and laboratory conditions” by Long et al. (2021)
Long et al. (2021) conducted a detailed study of possible interferences in measurements of surface O3 by UV spectroscopy, which measures the UV transmission in ambient and O3-scrubbed air. While we appreciate the careful work done in this analysis, there were several omissions, and in one case, the type of scrubber used was misidentified as manganese dioxide (MnO2) when in fact it was manganese chloride (MnCl2). This misidentification led to the erroneous conclusion that all UV-based O3 instruments employing solid-phase catalytic scrubbers exhibit significant positive artifacts, whereas previous research found this not to be the case when employing MnO2 scrubber types. While the Long et al. (2021) study, and our results, confirm the substantial bias in instruments employing an MnCl2 scrubber, a replication of the earlier work with an MnO2 scrubber type and no humidity correction is needed.
Ozone (O3) is a key hazardous atmospheric pollutant. In the USA, more than 100 million people live in regions that do not meet the National Ambient Air Quality Standards. Wildfires exacerbate O3 pollution (Crutzen et al., 1979; Crutzen and Andreae, 1990; Jaffe et al., 2013, 2020; Brey and Fischer, 2016; Gong et al., 2017). Given that smoke contains literally hundreds of different compounds, it is important to address possible interferences in measurements of O3. Long et al. (2021) conducted a detailed study of possible interferences in UV measurements of O3, which is the method most commonly used. In the UV method, O3 is measured at 254 nm in a sample airstream and in an airstream where O3 has been removed, usually by a solid-state catalytic scrubber. Long et al. (2021) provide an excellent discussion of this method, which we will not repeat here. However, one of the most important aspects in this measurement is the nature of the scrubber that is used to remove O3. For the scrubber, various companies have used manganese dioxide (MnO2), Hopcalite (a mixture of manganese and copper oxides), and manganese chloride (MnCl2). Long et al. (2021) compared multiple UV instruments with an NO chemiluminescence instrument, a method which is presumably free from interferences. Long et al. (2021) found a significant bias of 16–24 ppb O3 ppm−1 of CO in one type of UV O3 analyzer (Thermo Fisher 49i) that was tested without humidity correction, as compared to the NO chemiluminescence method. The bias was correlated with smoke tracers, such as CO and total hydrocarbons. Other instruments were tested with a humidity correction and found to have a much smaller bias which Long et al. (2021) attributed to the humidity correction. According to Long et al. (2021), the scrubber types on these instruments were similar, but in fact they were not, as discussed below, and this leads to significant uncertainty in their conclusions.
Long et al. (2021) did not cite our earlier study (Gao and Jaffe, 2017). In this work, we conducted a comparison between two UV-based O3 analyzers (Dasibi 1008-RS and Ecotech Serinus 10) and an NO chemiluminescent analyzer in wildfire plumes at the Mt. Bachelor Observatory (MBO) during the 2015 wildfire season. Gao and Jaffe (2017) found no significant bias in the UV analyzers relative to the NO chemiluminescent analyzer in moderate smoke plumes, up to approximately 1 ppm of carbon monoxide (CO). Both of these UV analyzers used an MnO2 scrubber. The precision and bias of instrumentation used in Gao and Jaffe (2017)'s study along with the quality assurance methods are outlined in the paper and are sufficient to meet Long et al. (2021)'s data quality objectives. A key question is the following: why were Long et al. (2021)'s results different from Gao and Jaffe (2017)'s results? We address this question below.
Long et al. (2021) cite the Thermo Fisher Scientific model 49i series instrument's scrubber type as MnO2 (as do others: Kleindienst et al., 1993; Spicer et al., 2010; Turnipseed et al., 2017). However, according to David Sherwin, a Technical Application Specialist III who has been working at Thermo for 18 years (David Sherwin, personal communication, 2021), and Nathan Bernardini, a Technical Application Specialist II who has been working at Thermo for close to 5 years (Nathan Bernardini, personal communication, 2022), the scrubbers in the 49c and 49i series have always used MnCl2 not MnO2. While we have not done chemical tests on the scrubber, we feel that the manufacturer is in the best place to know what is inside their instrument. The names and email addresses of the Thermo Fisher scientists with whom we communicated, as well as screenshots of our email correspondence, can be found in the author's final comment in the discussion phase of manuscript submission. Please note that there is no info about the scrubber type in the manual. Due to this scrubber type misidentification, Long et al. (2021) did not test any O3 analyzer with a true MnO2 scrubber and without humidity correction, the most common way these instruments are deployed.
The Mt. Bachelor Observatory is a high-elevation research station in the US Pacific Northwest that has been used for many years to study O3 and other pollutants (e.g., Jaffe et al., 2018). Starting in 2018, we have deployed two O3 instruments at MBO, the Ecotech Serinus 10, previously used in the Gao and Jaffe (2017) study, and a Thermo Fisher 49c, a similar instrument to the one used in Long et al. (2021)'s study which uses the same scrubber and no humidity correction. Generally, the Ecotech and Thermo Fisher instruments agree well, but in a particularly strong period of wildfire smoke, we saw a substantial difference in the two measurements. Figure 1 shows data from a 3-week period in September–October 2020, when we experienced heavy smoke at MBO. The slope (0.0112 ppb O3 ppb−1 CO) is smaller but of the same order of magnitude as that reported by Long et al. (2021) for comparisons of the Thermo Fisher to the NO chemiluminescent instrument (0.016–0.024 ppb O3 ppb−1 CO).
In the absence of smoke, we see good agreement between the two measurements. Figure 2 shows the agreement between the Thermo and Ecotech instruments during non-smoke periods (defined as CO <200 ppb), with a root mean squared difference of less than 1 ppb. Given our earlier comparison establishing that the Ecotech instrument did not show significant bias (Gao and Jaffe, 2017), we contend that these findings corroborate Long et al. (2021)'s conclusion that the Thermo Fisher instrument exhibits a significant positive bias at high CO levels. We believe the MnCl2 scrubber in the 49i is the primary cause for the discrepancy between the findings of Long et al. (2021) and Gao and Jaffe (2017).
When Long et al. (2021) put a Nafion dryer on their Thermo Fisher instrument midway through the study, the bias was reduced by an order of magnitude. We agree with Long et al. (2021) that the Nafion dryer reduced not only water vapor but probably also scrubbed many of the VOCs that were causing the bias. While Nafion is known to transfer O3 and lower-molecular-weight alkanes efficiently, it will remove more complex VOCs that are likely responsible for the bias in UV instruments (Perma Pure LLC, 2022). Similar tests with and without a Nafion drier were not done for the other instruments. The Nafion-dried 2B-205 instrument (hereafter 2B) in Long et al. (2021)'s study showed O3 artifacts an order of magnitude lower than the non-dried UV analyzers, but this can be explained by the 2B's MnO2-containing Hopcalite scrubber acting similarly to a pure MnO2 scrubber. We note that current EPA recommendations are to include Nafion dryers for UV O3 instruments (Halliday et al., 2020), and we see no downside to this recommendation. But given that this remains a recommendation, as well as to interpret past data, we suggest that future experiments on O3 bias include instruments with a true MnO2 scrubber with, and without, humidity correction, as the most common field setup does not include a drying system.
Data from the Mt. Bachelor Observatory are archived at the University of Washington's Research Works Archive (http://hdl.handle.net/1773/48597, last access: 18 May 2022; Jaffe, 2020).
NB completed most of the data analysis and instrument calibrations and wrote the first draft of the article. DAJ is the principal investigator for the Mt. Bachelor Observatory (MBO) and contributed to the overall analysis and article preparation. IP and PE are responsible for the duplicate (Thermo) O3 measurements at MBO and contributed to data interpretation and final preparation of the article.
The contact author has declared that neither they nor their co-authors have any competing interests.
Publisher’s note: Copernicus Publications remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
This research has been supported by the National Science Foundation (grant no. AGS-1447832) and the National Oceanic and Atmospheric Administration (grant no. RA-133R-16-SE-0758).
This paper was edited by Glenn Wolfe and reviewed by two anonymous referees.
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