Atomic emission detector with gas chromatographic separation and cryogenic pre-concentration (CryoTrap–GC–AED) for atmospheric trace gas measurements
- Atmospheric Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
Correspondence: Jonathan Williams (email@example.com)
A gas detection system has been developed, characterized, and deployed for pressurized gas-phase sample analyses and near-real-time online measurements. It consists of a cryogenic pre-concentrator (CryoTrap), a gas chromatograph (GC), and a new high-resolution atomic emission detector (AED III HR). Here the CryoTrap–GC–AED instrumental setup is presented, and the performance for iodine (1635 ± 135 counts I atom−1 pptv−1), sulfur (409 ± 57 counts S atom−1 pptv−1), carbon (636 ± 69 counts C atom−1 pptv−1), bromine (9.1 ± 1.8 counts Br atom−1 pptv−1), and nitrogen (28 ± 2 counts N atom−1 pptv−1) emission lines is reported and discussed. The limits of detection (LODs) are in the low parts per trillion by volume range (0.5–9.7 pptv), and the signal is linear to at least 4 orders of magnitude, which makes it a suitable method for diverse volatile organic compound (VOC) measurements in the atmosphere, even in remote unpolluted regions. The new system was utilized in a field study in a boreal forest at Hyytiälä, Finland, in late summer 2016, which made monoterpene measurements possible among other VOCs. Furthermore, pressurized global whole-air samples, collected on board the Lufthansa Airbus A340-600 IAGOS–CARIBIC aircraft in the upper troposphere and lower stratosphere region, were measured with the new setup, providing data for many VOCs, including the long-lived organosulfur compound carbonyl sulfide.
Atomic spectrometric analysis has been reported to provide highly sensitive detection, a linear response of at least 5 orders of magnitude (> 105), and accurate elemental composition data of samples. If detection is preceded by analyte separation using gas chromatography (GC), compound-specific data are attainable. The first atomic emission detector (AED) with plasma as an excitation source coupled with a GC was introduced in 1965 (McCormack et al., 1965). This group was the first to recognize the analytic potential of combining a GC separation with microwave-induced plasma excitation and an electronic emission spectra detector. Early AEDs, using microwave-induced plasmas, were operated at reduced pressures (Risby et al., 1983) until an atmospheric pressure version was developed in 1977 (Beenaker, 1977). The first commercial AED based on a microwave-induced plasma and photodiode array detector coupled to a GC was released by Hewlett Packard in 1990 (Quimby and Sullivan, 1990). The first AED to measure atmospheric organosulfur species was reported in 1994 (Swan and Ivey, 1994). These systems also provided speciated element-specific chromatograms and were used in a variety of applications including the analysis of oils for sulfur-containing compounds (Link et al., 2002). In contrast to the alternative analytical approach of gas chromatography coupled to mass spectrometry (GC–MS), the AED has the advantage of having highly selective wavelength-dependent element-specific detection and linear in-detector response. Since elements are detected rather than molecules, the calibration of one carbon-containing compound could potentially allow calibration of all such compounds provided the response was indeed equimolar. That said, it is important to keep in mind that a detector is often the last step in the whole analytical instrumental setup; therefore, the response factor (RF) reflects the entire analyte pathway from the sample inlet to the detector signal recording. This means that analyte losses by adsorption and absorption effects taking place in the transfer lines, pre-concentration stages, GC column, and the detector flow paths contribute to the final RF. If such an equimolar response for the entire analytical system can be achieved, this would greatly simplify the calibration of complex mixtures and would even allow quantification of unidentified compounds not present in a calibration standard. For this reason, the AED has been previously used for the quantification of species that have been identified by GC–MS (Apel et al., 1998; Greenberg et al., 1999). Recently, further technical developments in the AED have led to improvements in sensitivity, and furthermore, in the latest edition the whole AED III HR detector range is simultaneously measurable, making such systems even more attractive to atmospheric scientists. The simultaneous high-resolution wavelength-recording capability of the new AED III detector (161–211 nm) in the CryoTrap–GC–AED system allows for screening for elements present in the speciated compounds, thus simplifying the identification of unknown compounds. In contrast, the AED II has a mechanically turning grating for measuring different wavelength groups in the range of 171 to 837 nm; however, due to the turning grating, simultaneous measurement of the whole range is not possible. The newest version of the AED system potentially allows for semiquantitative data on identified compounds in a chromatogram without a specific standard within the uncertainty range when a broad range of compound-specific RFs are used for the determination of the single-element RF. Similar semiquantitative approaches can also be used with other analytical techniques, like using a flame ionization detector (FID) and MS, and this aspect of the AED performance will be assessed in this work
In this study, the instrumental setup and performance of a CryoTrap–GC–AED system, comprised of three commercially available units, are examined. The performance for iodine (163 nm), sulfur (181 nm), carbon (193 nm), bromine (163 nm), and nitrogen (174 nm) emission lines is examined. The most sensitive atomic emission lines for the five elements in the range of the detector were chosen. The calibration linearities, limits of detection, and compound-specific response factors are reported for 64 compounds.
The CryoTrap–GC–AED system consists of three stages: a liquid-nitrogen-based pre-concentration system (Entech model 7200, USA), a gas chromatographic separation (Agilent GC 7890B, USA), and a helium-plasma-based third-generation atomic emission detector (Joint Analytical Systems AED III High Resolution, Germany). The schematic of the instrumental setup is shown in Fig. 1. Ultrahigh-purity helium (UHP, purity 99.9999 %, Westfalen, Germany) flowing through a heated purifying catalyst (Valco Instruments VICI, USA) is used throughout the system as the carrier and purging gas. For the reagent gases extra ultrahigh-purity H2 (EUHP, purity > 99.99999 % via a Parker Balston hydrogen generator, model H2-300; Parker-Hannifin Corporation, USA) and ultrahigh-purity O2 (UHP, purity 99.9999 %, Westfalen, Germany) were used. For the calibration gases and synthetic air as a dilution gas, Messer and Air Liquide gas regulators were used. For the certified ambient-air calibration gas a pressure regulator completely made of high-purity steel was used (Parker-Hannifin Veriflo 959, USA).
2.1 Cryogenic pre-concentration (CryoTrap)
The sample is introduced to the pre-concentration unit (CryoTrap) via an eight-port multi-position valve consisting of the helium supply gas, four sample introduction inlets, an internal standard, a calibration standard, and a blind port (Fig. 1, upper panel). The four sample introduction lines are each 2.0 m long (Restek Corp. Silcosteel, USA) with an outer diameter of (1.59 mm) and an inner diameter of 0.040′′ (1.02 mm). The sample is drawn onto the two enrichment traps via an evacuated volumetric reservoir, where the sample introduction volume is accurately determined by measuring the pressure at given temperature. All the CryoTrap internal flow path surfaces are coated with a thin high-density ceramic Silonite-D layer to provide extremely inert surfaces, which nearly eliminates the adsorption of the analytes to the surfaces (Cardin, 1999).
The CryoTrap internal flow path is flushed with the sample gas before each pre-concentration step. After that the sample air is drawn (200 mL min−1) through the first stage of pre-concentration, called the dehydration module (Fig. 1, middle panel), whereby H2O is selectively removed on an empty Silonite-D-coated stainless-steel trap (outer diameter or 3.18 mm, 31 cm long) held at −50 ∘C. After collecting the required volume of sample, the trap is flushed with 75.0 mL of helium (100 mL min−1) to remove any remaining air. Then module 1 is heated to 10 ∘C and forward-purged with 50.0 mL (10 mL min−1) of helium flow onto the main Tenax-packed and Silonite-D-coated volatile organic compound (VOC) enrichment trap (module 2, the second step of pre-concentration; outer diameter or 1.02 mm, 31 cm long) held at −60 ∘C. The forward helium purge helps to successfully transfer heavy, polar, and semi-volatile organic compounds (SVOCs) onto the main module 2 VOC trap. The last pre-concentration step is pre-cooling of the cryofocusing trap (module 3, unpacked ∼ 4 cm long part of Silonite-D-coated – 0.79 mm – transfer line) to −180 ∘C, which is thereafter kept at −160 ∘C during module 2 back-flushing at 230 ∘C for 2.5 min; this refocuses the volatiles to a much smaller dead volume for splitless injection onto a GC column. The module 3 (0.79 mm) transfer line is rapidly heated to 60 ∘C for 2 min inside a sheathing (3.18 mm) perfluoroalkoxy alkane (PFA) tube with hot air supplied through the rotary plate kept at 100 ∘C. This ensures rapid and splitless injection of analyte molecules to the GC column through a transfer line heated to 110 ∘C. The pre-concentration unit is equipped with two bulkhead heaters between the heated rotary plate and the traps for better water condensation management.
2.2 Gas chromatograph (GC)
Gas chromatography is a common choice for analytical separation of VOCs for measurement with various detectors (Bourtsoukidis et al., 2017; Apel et al., 1998). We use an Agilent 7890B GC for the compound separation. The GC was fitted with a Supelco SPB-624 capillary column (length × inner diameter: 60 m × 250 µm; film thickness 1.40 µm), which is an intermediate polar, proprietary phase-bonded fused silica GC column. SPB-624-type columns are widely used for volatile non-halogenated, halogenated, and aromatic compounds analysis.
Helium is used as the column carrier gas, the flow rate of which is controlled over GC electronic pneumatic control (EPC) valve number 3. First, helium flows from the GC EPC valve into a (1.59 mm) stainless-steel line connected to CryoTrap rotary valve number 2 (Fig. 1). After the pre-concentration procedure the helium flow with the remobilized analytes is guided back to the GC oven through a heated (110 ∘C) Silonite-D-coated (0.79 mm) transfer line. Then, in the GC oven a Swagelok T-split union guides the flow to the analytical column for splitless injection. The other end of the GC capillary column is led directly to the AED cavity through a heated transfer line (250 ∘C).
2.3 Atomic emission detector, third generation (AED III)
The AED measures the energy emitted at characteristic wavelengths using sample atoms present in the helium (200–250 mL min−1) plasma cavity to quantify their number in a chromatographic peak. Combining these data with GC analyte separation, the amount of the substance can be quantitatively determined.
The helium carrier gas (3.5 mL min−1) eluting from the GC is led to the AED cavity through the capillary column that is housed in the heated transfer line (250 ∘C). The helium plasma discharge cavity is also kept at a constant temperature of 250 ∘C. The mixture of the carrier (helium) and reagent gases hydrogen (at 12 psi or 0.83 bar supply pressure) and oxygen (15 psi or 1.03 bar supply pressure) flows through a fused silica discharge tube where the gases are ionized into a plasma state by microwave energy. In the high-energy plasma the eluted sample compounds from the GC are broken down into free radicals, ions, and atoms. As they return from their excited state to ground-state configuration, light radiation is emitted in their element-specific characteristic wavelengths. The emitted ultraviolet radiation passes through a fused silica lens and a narrow slit and is then reflected onto a reflective holographic grating by a fixed mirror. The grating disperses the light into discrete vertical bandwidths along a plane-concave polychromatic grating. Thereafter, the grating reflects and focuses the light in the wavelength range 161–211 nm in a horizontal plane onto two back-thinned charge-coupled devices (CCDs). Due to the physical gap between the two CCDs there is a 7 nm gap in the range of 183–190 nm of the spectra. The CCDs convert light intensities across the given spectrum into electrical currents, which are recorded by the AED III Instrument Control Software. The software automatically calibrates the received light intensity signal from the CCD diode numbers into wavelength intensity data according to a calibration table. This process (called element installation in the software) takes place automatically before every sample measurement. After each measurement, all the wavelength-dependent emission data are stored with 0.01 nm resolution. An example of a five-element simultaneously recorded chromatogram of the 84-component Apel-Riemer-2015 gas calibration standard is shown in Fig. 2.
2.4 Characterization experiments
All the characterization experiments started with a zero-air (hydrocarbon-free synthetic air with 20.5 % oxygen and nitrogen rest, which flows through an extra catalyst kept at 500 ∘C to remove the trace amounts of hydrocarbons; Westfalen, Germany) measurement to determine the instrumental background. Furthermore, at the beginning of the experimental design the highest calibration standard MR-level (MR: mixing ratio) carryover and retention potentials were tested for all of the compounds of interest with the zero-air measurement directly after as the sample measurement. The trap back-flushing and bakeout times were adapted accordingly. With the 15 min bakeout step after the injection, modules 1 and 2 are heated to 150 and 210 ∘C, respectively, and back-flushed with He flow (75 ml min−1), whereas the bulkhead heaters are kept at 150 ∘C.
Two independent gas calibration standards were used for the characterization experiments: the 84-component (each nominally at a 50 ppbv MR in UHP nitrogen rest) Apel-Riemer-2015 gas calibration standard (Table S1 in the Supplement) and the 30-component (each nominally at a 4 ppbv MR in UHP nitrogen rest) non-methane hydrocarbon (NMHC) ozone precursor National Physical Laboratory 2017 (NPL-2017) primary calibration standard gas cylinders (Table S2).
The Apel-Riemer-2015 standard used for the characterization measurements was diluted with the same zero air as described above with two mass flow controllers (MFCs; EL-Flow, Bronkhorst, the Netherlands). The MFC for the calibration gas had a range up to 20 mL min−1, and the MFC for zero air had a range up to 5 L min−1. For these experiments a constant 1 L min−1 zero-air flow was used, and five steps (1, 5, 10, 15, 20 mL min−1) of calibration gas were used to produce nominal MRs of 50, 250, 500, 750, and 1000 pptv. This MR range is relevant for many ambient VOC measurements. With each sample pre-concentration a 1400 mL aliquot of the diluted sample flow was trapped and the rest of the flow was led to lab exhaust. Calibration-level measurements were repeated four times. No dilution for the NPL primary calibration standard was used, and thus samples were trapped directly in the amounts of 40, 60, 80, and 250 mL (producing MRs in the range of 114, 171, 229, and 714 pptv for 1.4 L unknown sample relevance). The NPL calibration step measurements were also repeated four times.
With separate tests, the maximum linearity range of the CryoTrap–GC–AED was tested with the undiluted Apel-Riemer-2015 calibration gas measurement (∼ 50 ppbv per compound). For higher MR samples a smaller sample volume can also be trapped, making it possible to measure even higher MR samples. The system was tested to be linear to at least 4 orders of magnitude.
The AED system was always recalibrated immediately prior to and during the measurement of the samples with unknown MRs using the independent gas calibration standards: the Apel-Riemer-2015 and the NPL-2017 gas cylinders. In addition, during the regular automated IAGOS–CARIBIC pressurized sample measurement procedure, the National Oceanic and Atmospheric Administration (NOAA) ambient-air calibration standard and the NMHC NPL standards were periodically measured after every five samples. From the calibration standard measurements, the linearities (R2), limits of detection (LODs), response factors per atom, and measurement uncertainty were determined for all quantifiable compounds in the standard; they are listed in Tables 1 and 2.
The LODs were calculated from the average height of the lowest calibration levels and the average height of the noise signals corresponding to the same chromatogram for each separable and measurable compound of the calibration standards. A ∼ 99.7 % confidence interval was maintained for the LOD calculations by using a value 3 times the noise-to-signal (by peak height) ratio. The LOD calculation is represented by Eq. (1):
where is the average height of the noise signal, is the average mixing ratio of the lowest calibration level, and is the average peak height of that calibration level of the corresponding compound.
The averages per atom RF were calculated separately for each species using the average area under the peak curve (), the corresponding average MRs (), and the number of atoms (NOA) present in the compound of interest, as show by Eq. (2):
The RFs were calculated separately for all compounds, and their individual calibration MR levels and thereafter all the individual RFs over the whole calibration range were averaged to a single RF per compound.
3.1 Carbon emission line performance
The performance of the carbon emission line (193 nm) derived from measurements of three calibration standard gases is listed in Table 1. For Apel-Riemer-2015, the derived LODs are in the range 0.8–9.7 pptv. Each compound's RF is the average of 18 independent data points in the whole 50–1000 pptv calibration range. The RFs for these compounds lie within the range 343 ± 147 counts C atom−1 pptv−1 (benzyl chloride) to 800 ± 291 counts C atom−1 pptv−1 (isobutyl nitrate), with an average of 587 ± 91 counts C atom−1 pptv−1 (47-compound mean). For NPL-2017, the LODs are in a smaller range of 0.5–1.1 pptv (more similar compounds), and the RFs per carbon atom range from 581 ± 23 counts C atom−1 pptv−1 (1,2,4-trimethylbenzene) to 913 ± 77 counts C atom−1 pptv−1 (toluene). The measured 22-compound NPL-2017 gas standard average RF was 684 ± 46 counts C atom−1 pptv−1 (about 17 % higher compared to Apel-Riemer-2015 measurements and with about half the standard deviation). For both experiments, the average per carbon atom RF was determined as 636 ± 69 counts C atom−1 pptv−1.
The CryoTrap–GC–AED system sensitivity and precision are also dependent on the discharge tube, as the two experiments were conducted with different discharge tubes (as the old one broke). Nevertheless, sample gas was always directly determined against calibration standards with the same discharge tube. If a discharge tube breakage took place, a complete new calibration was carried out. The same 10 compounds (isobutene, 1,3-butadiene, pentane, isoprene, hexane, benzene, toluene, ethylbenzene, 1,3,5-trimethylbenzene, and 1,2,4-trimethylbenzene) that were measured from both calibration standards are compared in Fig. 3. Three compounds (pentane, ethylbenzene, and especially toluene) do not adhere to the 1σ confidence interval in the one-to-one RF comparison between these two experiments. The reason remains unknown as there are other similar compounds to these in the comparison which stick to the correlation. The blanks analyzed before and after the samples for both calibration standards did not indicate contamination of these compounds.
Like the RFs, the compound-specific LODs also depend on the CryoTrap pre-concentration efficiency, compound transmission efficiency through the gas transfer lines, GC separation and carry-through efficiency, and AED helium plasma atomization and excitation efficiency. Throughout the whole instrument development process, best efforts were taken to use suitable transfer lines and gas union (Swagelok, USA) materials like Silcosteel (fused silica-coated stainless steel), stainless steel, PFA, and Teflon for minimizing analyte flow path losses, i.e., through wall losses (absorption and adsorption effects) and condensation. Furthermore, high-purity stainless-steel pressure regulators were used for calibration standard gas bottles with analyte-free degassing O-rings.
The compound-specific per carbon atom RFs from the NPL-2017 NMHC calibration standard are summarized in Fig. 4. The combined CryoTrap–GC–AED setup demonstrated a spread of RFs determined from the carbon 193 nm emission line intensities, which were between around 550 and 900 counts pptv−1 C atom−1 for the NPL-2017 calibration standard, depending on the compound. The response factors for the more volatile species 1,3-butadiene to isoprene lie within the range 585 ± 30 to 660 ± 27 counts C atom−1 pptv−1. However, the lower-volatility compounds comprising 2-methylpentane to o-xylene have higher and more variable RFs ranging from 684 ± 54 to 913 ± 77 counts C atom−1 pptv−1; see Table 1b for compound-based specifics. A general increasing variability in carbon response was visible with increasing carbon atom number, which can also be seen in Fig. 4. The three components of the instrument were considered as possible causes of these observed effects. The cryofocus unit will more effectively trap low-volatility species and is therefore unlikely to be the root cause. That the higher-volatility species RFs lie reasonably close together could suggest that the AED is functioning correctly, although the possibility remains that larger molecules are converted to atoms in the plasma less efficiently than 100 %. This is just a hypothesis that has not been tested. Given the abrupt change in RF from isoprene to 2-methyl pentane we consider the most likely explanation to be that despite the inert short sample lines some internal surface effects are causing the variation. As previous AED studies have shown constant C3–C8 per carbon response, it is rather an indication that the variability in RF in this study increases due to the CryoTrap trapping or inlet system. Thus, we see that the CryoTrap–GC–AED detected response must be considered as a whole for the entire instrument, for which the trapping and transmission efficiency are compound-specific and can directly influence the final detected signal. As the per atom response factors were determined to be compound-specific, for the field samples presented later in this work all the analytes of interest were always calibrated and quantified against a calibration standard, which was pre-concentrated and analyzed with exactly the same parameters as the samples. Therefore, all the losses and other effects in the analytical system leading to the variation in the RFs were accounted for. The same also applies to the other elements measured. The average of the compound-specific median RFs is 663 ± 66 counts pptv−1 C atom−1. Therefore, within the uncertainty range the compound-independent calibration could be applied. It is possible to lower the uncertainty if a similar compound group's average RF is used for the target species. Nevertheless, for higher accuracy a direct calibration method is recommended. Throughout this study the direct calibration method was used.
The discrepancy between the two calibration-standard-determined RFs seen in Tables 1 and 2 could arise from the point that the compounds in the NPL-2017 calibration standard are nominally at 4 ppbv and could be pre-concentrated directly, but the Apel-Riemer-2015 compounds are nominally at 50 ppbv, thus requiring extra dilution before the trapping. The dilution with zero air could introduce further uncertainty, and other unknown factors (e.g., wall losses) may also cause this discrepancy for the RFs determined from the Apel-Riemer-2015 calibration standard. The comparison overview of these two standards can be seen again in Fig. 3.
3.2 Iodine, sulfur, bromine, and nitrogen emission line performances
The Apel-Riemer-2015 gas-phase calibration standard was used to evaluate the performance of other available and relevant atomic emission lines for atmospheric chemistry (Table 2).
Methyl iodide (iodine wavelength measured at 178 nm) has an LOD of 0.7 pptv and an RF of 1635 ± 135 counts I atom−1 pptv−1. The LOD of methyl iodide in the iodine emission line was 9.6 times more sensitive compared to the carbon emission line. Carbonyl sulfide (OCS) and carbon disulfide (CS2) had LODs of 1.9 and 1.8 pptv, respectively. OCS had an RF of 342 ± 34 counts S atom−1 pptv−1, and CS2 had an RF of 476 ± 79 counts S atom−1 pptv−1. The sulfur emission line at 181 nm was determined to be on average 3.1 times more sensitive compared to the carbon 193 nm emission line, as calculated from OCS and CS2 LOD values. The average sulfur response factor determined from the two latter compounds is 409 ± 57 counts S atom−1 pptv−1. Bromodichloromethane (9.9 ± 1.5 counts Br atom−1 pptv−1), 1,2-dibromoethane (9.0 ± 1.8 counts Br atom−1 pptv−1), and bromoform (8.3 ± 2.0 counts Br atom−1 pptv−1) in the bromine emission line at 163 nm had significantly higher LODs of 115.7, 61.9, and 64.2 pptv, respectively, compared to the iodine, sulfur, and carbon emission lines due to a significantly higher background. The average per bromine atom response factor was determined as 9.1 ± 1.8 counts Br atom−1 pptv−1. Nevertheless, the bromine emission line provides great selectivity, whereby the high background removes the complex background signal. Nitrogen at 174 nm proved to be the least sensitive element for AED III detector. The nitrogen-containing compounds acetonitrile, acrylonitrile, isopropyl nitrate, propyl nitrate, and isobutyl nitrate varied significantly with their LODs (see Table 2), despite all containing a single nitrogen atom. The different transmission efficiency of each of the five nitrogen compounds through the system's flow paths could cause such differences. The average per nitrogen atom response factor determined from the five nitrogen compounds was 28 ± 2 counts N atom−1 pptv−1. The different element count scales are not related to each other. All the measured element emission wavelength spectra were used independently, and the most sensitive emission line was chosen for each compound of interest. For example, in the case of the OCS molecule, the sulfur emission line was used.
3.3 Advantages and disadvantages of the CryoTrap–GC–AED
Considering all the species measured with the CryoTrap–GC–AED, the system proved to be very sensitive in detecting iodine, sulfur, and carbon elements with RFs of 1635 ± 135 counts pptv−1 I atom−1, 409 ± 57 counts pptv−1 S atom−1, and 636 ± 69 counts C atom−1 pptv−1, respectively. The different elemental emission wavelength intensity count scales are not directly comparable due to different elemental background noise levels. From these three elements the lowest background noise level was measured for iodine, followed by sulfur and then by carbon. The element background noise level determines the LODs for these elements in the same increasing order, also seen in Tables 1 and 2.
The advantage of the AED-based system is the highly selective element-specific information obtainable from the emission wavelength data, which can be useful in helping to determine unknowns in a complex matrix. Generally, the CryoTrap–GC–AED system is in the same sensitivity range as an FID (Baker et al., 2010). The electron capture detector (ECD) remains more sensitive and sometimes no pre-concentration of the air sample is necessary (e.g., Schuck et al., 2009); however, an ECD is limited to only electron-capturing compounds. GC–MS systems generally have high sensitivity and good selectivity but require separate calibration gases for all species to be quantified since response factors vary considerably. Modern online mass spectrometry (MS) detectors, especially a proton transfer reaction time-of-flight mass spectrometer (PTR-TOF-MS), provide high sensitivity (sub-pptv) and highly time-resolved (< 1 s) measurement techniques without the need for pre-concentration, e.g., the new Tofwerk/Aerodyne Research Vocus PTR-TOF (Krechmer et al., 2018). However, without pre-separation with gas chromatography the chemical identity of signals can be ambiguous.
The specific emission wavelength range of the high-resolution AED III enables the measurement capability to accurately detect at least 11 elements (e.g., bromine at an atomic emission wavelength of 163 nm is not mentioned in the vendors list but could be accurately measured): antimony, arsenic, carbon, germanium, iodine, nitrogen, oxygen (requires 5 % methane in 95 % nitrogen reactant gas), phosphorus, selenium, silicon, and sulfur, a maximum of 8 of which can be simultaneously saved from the raw data (JAS product description web page, 2020). This makes the first screening of an unknown gas-phase sample for compounds with various elements much easier and faster compared to more complex mass spectra. The AED capability to measure oxygen is not suitable for trace atmospheric measurements due to the requirement of 10 % methane reagent mixture. As this high concentration of methane produces a very high background signal, this capability is suitable for oxygen measurements in the oil and gas industry.
For the work presented here, a pre-concentrating GC–MS could have served as the same or a better alternative for monitoring targeted species present in a calibration gas. Nevertheless, the AED system has advantages in searching for exotic heteroatom molecules in the atmosphere for the non-carbon elements in the detector wavelength range. For example, for the analysis of volcanic emissions. Unfortunately, no new exotic species (containing of iodine, bromine, nitrogen, silicon, mercury, selenium, and arsenic) were revealed in any of the sampled environments to date, although these environments were remote (upper troposphere–lower stratosphere) or distant from pollution sources (boreal forest).
Some disadvantages of the current AED III detector are the short lifetime of the fused silica tube where the plasma is maintained and the early software and electronic issues inhibiting the proper acquisition of the data. The helium plasma is sustained in a small quartz tube (47 mm long, 1.0 mm inner diameter, 1.25 mm outer diameter) with a polyimide coating (27 mm long) in the middle part of the outer surface. The tube is positioned in a water-cooled cavity maintained at 80 ∘C. The lifetime of the discharge tube was around 5 to 30 d, sometimes up to 3–4 months, depending on the sample throughput and quality of the replacement of the fragile discharge tube. The discharge tube could break at any moment without warning during a measurement sequence, leading to the loss of a sample.
The high consumption of helium to maintain the plasma is expensive and of environmental concern as helium is escaping from our atmosphere to space. Furthermore, the large consumption of liquid nitrogen (around 2–3 L per sample) for the sample cryogenic pre-concentration makes it demanding on operator time, logistical field support, and operating expense. The use of liquid nitrogen makes it difficult to operate this instrument in remote areas. Nevertheless, the CryoTrap–GC–AED instrument was taken to a field measurement campaign at a Finnish boreal forest in 2016 where, among the other species, it contributed to the quantification of monoterpene compounds when accounting for the directly measured NO3 radical reactivity in the boreal forest (Liebman et al., 2018); this will be presented in Sect. 4.1.
The newly developed instrument has been deployed in near-real-time field measurements and in lab-based pressurized canister measurements. In the following we demonstrate two case studies: one based in the forest in Hyytiälä, Finland, and the other in the home laboratory in Mainz, Germany.
4.1 Finnish boreal forest field measurements at the Hyytiälä site
Boreal forest (taiga) makes up around 33 % of Earth's forest cover, making it the largest terrestrial biome in the world. Even in the epoch of the Anthropocene about of the boreal forest remains natural (Brandt et al., 2013). The field campaign took place at a boreal forest measurement site SMEAR II (Station for Measuring Forest–Ecosystem–Atmosphere Relations II) in Hyytiälä, Finland, in September 2016 (Hari and Kulmala, 2005). The site is situated approximately 50 km away from the first more densely populated location; thus, the anthropogenic influence is relatively low, particularly when the wind masses originate from the north with low human activity and pollution.
The instrumentation was installed in an air-conditioned measurement container maintained at a temperature of 25 ∘C . The CryoTrap–GC–AED system measured ambient air, which was pulled from the center of a shared 8.5 m tall high-flow inlet (15 cm diameter, flow rate ∼ 10 m3 min−1). From the 8.5 m inlet the air was drawn into the container through a 15 m long (1.27 cm diameter) PFA tubing at a flow rate of ∼ 20 L min−1 (transmission time 3.3 s). The inlet line was insulated and heated (10 ∘C above ambient) to avoid sunlight interactions and condensation. Membrane filters (polytetrafluoroethylene with pore size 5.0 µm, 47 mm diameter by Sartorius AG, Germany) were used to avoid particles entering the tubing at the connection from the high-flow inlet, and they are replaced every 5 d. From the 15 m long sampling line inside the container the cryogenic sample-trapping phase took place with a flow rate of 200 mL min−1 and a total of 1400 mL of air was trapped for each sample. After the injection of a pre-concentrated sample from the last focusing trap to the GC, the traps were baked-out and the pre-concentration of the next sample started in parallel with the previous GC run. This enabled mean sample throughput time intervals of 1 h 22 min. The average liquid nitrogen consumption rate was 2.5 L h−1. The CryoTrap and AED parameters presented in Sect. 2 and the GC program listed in Table 3a were used.
The diel cycles of isoprene and five monoterpene species (α-pinene, Δ-3-carene, β-pinene, camphene, d-limonene, and isoprene) are presented in Fig. 5. All monoterpene species show daytime minima and nighttime maxima. This is unexpected as the emissions of monoterpenes are primarily temperature-dependent, and ambient temperatures were higher by day (Tarvainen et al., 2005). Here the recurring nighttime MR maxima can be explained by the shallow nocturnal boundary layer, typically accompanied by a temperature inversion in the lower troposphere, effectively trapping the ground-level emissions (Liebmann et al., 2018). The measured monoterpene species and isoprene on average accounted for about 70 % of the directly measured NO3 reactivity at nighttime and about 40 % during daytime, as published in a separate research article (Liebmann et al., 2018).
The diel cycles of carbonyl sulfide and carbon disulfide are shown in Fig. 6. OCS showed daytime maxima between 09:00 and 15:00 UTC (12:00 and 18:00 local time), which is unexpected as daytime uptake by vegetation is generally regarded as the dominant sink for OCS (Sandoval-Soto et al., 2005). Again, the previously discussed shallow nocturnal boundary layer plays a role, as much less in-mixing of higher-concentration OCS from the free troposphere takes place during nighttime. Furthermore, it confirms the recently published finding at the same measurement location that OCS uptake is light-independent and controlled by stomatal opening; therefore, stomatal conductance and OCS uptake can continue during nighttime under these conditions (Kooijmans et al., 2017). The nighttime uptake of OCS by vegetation should be further characterized and parameterized for 3D global chemistry-transport model applications. CS2 did not show any significant diel cycle, and MRs varied significantly between 0.5 and 5 pptv.
4.2 IAGOS–CARIBIC whole-air sample measurement with CryoTrap–GC–AED
The IAGOS–CARIBIC (In-service Aircraft for a Global Observing System–Civil Aircraft for the Regular Investigation of the Atmosphere Based on an Instrument Container) (Brenninkmeijer et al., 2007) is a regular observation project with scientific instruments on board commercial aircraft (Lufthansa Airbus A340-600 in cooperation with Lufthansa AG), which carries out atmospheric monitoring on a global scale, especially in the upper troposphere–lower stratosphere (UT–LS, ∼ 10–12 km) region. Since December 2015, a new CryoTrap–GC–AED system has been applied to measure whole-air pressurized gas samples that were taken as part of this project. Many VOCs such as NMHCs (Baker et al., 2010), sulfur-containing species, and oxygenated and halogenated trace gases can be measured in the C3–C14 range. These species are important to tropospheric ozone production, stratospheric ozone depletion, and radiative forcing.
The whole-air samples (WASs) were pressurized at about 4 bar of absolute pressure with two triggered retrospective air collectors (TRACs) each consisting of 14 specially manufactured glass vessels (2.74 L) and a high-resolution sampler (HIRES), which consists of 88 stainless-steel canisters (1.0 L). Every time after the flights took place and the samplers were delivered to the lab, the measurement procedure began with the initial pressure measurement of all 116 individual samples.
CryoTrap–GC–AED was applied to measure the IAGOS–CARIBIC TRAC and HIRES whole-air samples. At the beginning of each measurement sequence, a 2.0 m long sample line was connected to a TRAC or HIRES sampler port, and a leak check was conducted by evacuating the connected sample line to ∼ 3.0 psi (0.21 bar) of absolute pressure with the CryoTrap instrument pump. After the pressure stabilization in the line, a leak check was carried out for 3 min. If the pressure reading was less than ±0.5 psi (0.03 bar) different, which is within the precision range of the pressure gauge, the line was considered leak-tight. The CryoTrap traps in module 1 and module 2 (Fig. 1) were heated at 150 and 220 ∘C, respectively, for 20 min for conditioning. The GC oven program is summarized in Table 3 below. Again, the three independent gas-phase calibration standards (Apel-Riemer-2015, NPL-2017, NOAA-2017) were used for calibrating the system (Tables S1 and S2). A 1400 mL aliquot of an IAGOS–CARIBIC air sample was pre-concentrated. Exactly the same conditions were used for the calibration standards (except the NPL standard for which 50 mL was pre-concentrated) in order to have the same conditions and to thereby minimize the instrumental uncertainty. The IAGOS–CARIBIC WAS measurement sequence with the CryoTrap–GC–AED starts with a calibration. The measurement of zero air (produced the same way as described in Sect. 2) is followed by the certified ambient-air standard (NOAA-2017) measurement. The latter is followed by diluted Apel-Riemer-2015 gas-phase standard measurement (as described in Sect. 2). After that the continuous measurement of the WASs started. The NOAA-2017 certified ambient-air reference calibration standard and the NPL 30 component ozone precursor NMHC reference calibration standard were measured after every five WAS measurements to compensate for instrumental sensitivity drift throughout the analysis.
An example dataset of OCS MRs measured in the UT–LS region from two flights (Munich to Los Angeles and Munich to Shanghai in February 2019) is depicted in Fig. 7. The OCS data combined with the other VOC species from the same samples were used to determine the global atmospheric and lower stratospheric lifetime, the troposphere-to-stratosphere flux of OCS, and the stratospheric sink using the linear relationship between the long-lived species MRs (and their variability) and their known atmospheric lifetimes. This will be discussed in detail in a separate research article (article under review).
The newly developed CryoTrap–GC–AED analytical instrument enables the measurement of gas-phase samples in minute concentrations (low pptv level) suitable for ambient-air VOC species measurements in the troposphere and lower stratosphere. With this instrument it is possible to measure samples from canisters (e.g., IAGOS–CARIBIC whole-air samples) and also directly with circa 1 h sampling frequency at a measurement station (e.g., Hyytiälä Finnish boreal forest measurement campaign in 2016) (Karu, 2019; Liebmann et al., 2018). The instrument proved to be sensitive and linear over more than 4 orders of magnitude (> 104) and provides accurate element-specific information. The RF variability can be accounted for with direct calibration methods, which lead to more accurate results as were found in this study. Despite the RF variability known compounds present in a chromatogram and not present in the calibration standard can be still quantified with an accuracy of around 30 %–40 %. Thus, for more accurate results direct calibration against certified gas-phase calibration standards with exactly the same measurement conditions and volumes is recommended. Further tests should be done to investigate the causes of the variable responses of the compounds as an overall equimolar response would considerably improve the system utility. The possibility to measure 11 elements and 8 of them simultaneously might allow discovery of new atmospheric species of interest, e.g., containing selenium or silicon atoms, particularly in marine or volcanically influenced environments. The instrument would become significantly more reliable if longer-lasting helium discharge tubes were developed and the commercial software and electronics were improved. For further developments of the detector the possibility to measure a wider spectral range would allow detection of even more elements simultaneously.
The data can be obtained on request from the owners.
The supplement related to this article is available online at: https://doi.org/10.5194/amt-14-1817-2021-supplement.
EK and JW developed the idea. EK established the new measurement technique. EK, ML, and LE carried out the experiments. CAMB developed the CARIBIC air sampling systems. EK wrote the paper with support from ML and JW. JL provided discussions and feedback for improving the manuscript and enabled this project to take place. All authors discussed the results, commented on the paper, and helped to improve the paper.
The authors declare that they have no conflict of interest.
We are very grateful to Claus Koeppel (Max-Planck-Institute for Chemistry, Mainz) for IAGOS–CARIBIC TRACs/HIRES whole-air sampling and for conducting all the pre- and post-flight ground tests for accurate sample collection. We would also like to thank Florian Obersteiner (Karlsruhe Institute of Technology, Karlsruhe) for providing the very helpful IAU_Chrom data analysis software.
This research has been supported by the Max Planck Graduate Center with the Johannes Gutenberg-Universität Mainz (MPGC).
The article processing charges for this open-access
publication were covered by the Max Planck Society.
This paper was edited by Marc von Hobe and reviewed by Elliot Atlas and one anonymous referee.
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