INTRODUCTION
Since the beginning of the industrial revolution, the concentration of methane (CH4) in the atmosphere has increased by a factor of 2.5, which is mainly due to anthropogenic emissions (Dlugokencky et al. Reference Dlugokencky, Nisbet, Fisher and Lowry2011). With a mole fraction higher than 1.8 ppm, CH4 is today the second most important anthropogenic greenhouse gas after CO2. Although the global budget of atmospheric CH4 is quite well constrained, individual sources remain poorly quantified and not well understood (Saunois et al. Reference Saunois, Bousquet, Poulter, Peregon, Ciais, Canadell, Dlugokencky, Etiope, Bastviken and Houweling2016). The spatial and temporal variability of CH4 emissions from natural sources are a major hindrance to forecasting and mitigation strategies (Bousquet et al. Reference Bousquet, Ciais, Miller, Dlugokencky, Hauglustaine, Prigent, der Werf, Peylin, Brunke and Carouge2006; Saunois et al. Reference Saunois, Bousquet, Poulter, Peregon, Ciais, Canadell, Dlugokencky, Etiope, Bastviken and Houweling2016), and a warming climate could alter the strength of these emissions dramatically (Dean et al. Reference Dean, Middelburg, Röckmann, Aerts, Blauw, Egger, Jetten, de Jong, Meisel and Rasigraf2018).
The sources of atmospheric CH4 are evaluated by top-down measurements and bottom-up inventories (e.g. Hiller et al. Reference Hiller, Bretscher, DelSontro, Diem, Eugster, Henneberger, Hobi, Hodson, Imer and Kreuzer2014; Jacob et al. Reference Jacob, Turner, Maasakkers, Sheng, Sun, Liu, Chance, Aben, McKeever and Frankenberg2016), but as a result of the natural variability of CH4 emissions, these approaches usually do not agree well (Nisbet and Weiss Reference Nisbet and Weiss2010). To improve this approach, stable and clumped isotopes of methane are also widely studied, because many CH4 sources have a specific isotopic signature (Quay et al. Reference Quay, Stutsman, Wilbur, Snover, Dlugokencky and Brown1999; Stolper et al. Reference Stolper, Martini, Clog, Douglas, Shusta, Valentine, Sessions and Eiler2015; Sapart et al. Reference Sapart, Shakhova, Semiletov, Jansen, Szidat, Kosmach, Dudarev, van der Veen, Egger and Sergienko2017).
The radiocarbon (14C) content of atmospheric CH4 is of growing interest, since it can be used as a tool for a CH4 source apportionment (Wahlen et al. Reference Wahlen, Tanaka, Henry, Deck, Zeglen, Vogel, Southon, Shemesh, Fairbanks and Broecker1989; Lassey et al. Reference Lassey, Lowe and Smith2007; Petrenko et al. Reference Petrenko, Smith, Brailsford, Riedel, Hua, Lowe, Severinghaus, Levchenko, Bromley and Moss2008; Townsend-Small et al. Reference Townsend-Small, Tyler, Pataki, Xu and Christensen2012; Petrenko et al. Reference Petrenko, Smith, Schaefer, Riedel, Brook, Baggenstos, Harth, Hua, Buizert and Schilt2017). Indeed, “contemporary” or “modern” CH4 sources (e.g. agriculture, biomass burning) contain present-day 14C levels, whereas “old” or “fossil” CH4 sources (e.g. fossil fuels, geologic CH4) are 14C-free. Intermediate-age sources such as arctic lakes or peatlands can also be dated, providing valuable information about carbon dynamics in such environments (Zimov et al. Reference Zimov, Voropaev, Semiletov, Davidov, Prosiannikov, Chapin, Chapin, Trumbore and Tyler1997; Walter et al. Reference Walter, Zimov, Chanton, Verbyla and Chapin2006; Garnett et al. Reference Garnett, Hardie and Murray2011). These 14C measurements can be performed by accelerator mass spectrometry (AMS), but this task is challenging given the large amounts of CH4 required and its very low concentration in the atmosphere.
Methane is usually separated from other trace gases in a stepwise process (Lowe et al. Reference Lowe, Brenninkmeijer, Tyler and Dlugkencky1991; Brenninkmeijer and Röckmann Reference Brenninkmeijer and Röckmann1996; Röckmann Reference Röckmann1998; Kessler and Reeburgh Reference Kessler and Reeburgh2005; Petrenko et al. Reference Petrenko, Smith, Brailsford, Riedel, Hua, Lowe, Severinghaus, Levchenko, Bromley and Moss2008; Pack et al. Reference Pack, Xu, Lupascu, Kessler and Czimczik2015): first CO2 is cryogenically removed, then CO is oxidized to CO2 and also cryogenically removed, before CH4 can finally be oxidized and isolated as CO2 as well. Alternatively, molecular sieves or soda lime are used to scrub CO2 (Palonen et al. Reference Palonen, Uusitalo, Seppälä and Oinonen2017; Garnett et al. Reference Garnett, Murray, Gulliver and Ascough2019). However, for these simplified processes, cross contamination of CO2 from one fraction to the next remains an issue difficult to monitor and overcome (Pack et al. Reference Pack, Xu, Lupascu, Kessler and Czimczik2015).
Some laboratories use a preparative gas chromatography technique to separate CH4 from CO2 and other trace gases. This technique has been applied for stable isotope measurements of CH4, where only small samples are necessary for such analysis (e.g. Miller et al. Reference Miller, Mack, Dissly, White, Dlugokencky and Tans2002; Bock et al. Reference Bock, Schmitt, Behrens, Möller, Schneider, Sapart and Fischer2010; Brass and Röckmann Reference Brass and Röckmann2010). It has also been used in combination with an AMS, for radiocarbon measurements of repeated injections of high concentration methane samples (McIntyre et al. Reference McIntyre, McNichol, Roberts, Seewald, von Reden and Jenkins2013). Although a preparative gas chromatography technique warrants that pure CH4 is measured, its application for 14C measurements of atmospheric CH4 is not straightforward as the required sample volumes are of several orders of magnitude larger for radiocarbon analysis.
Here, we present a new methane preconcentration and purification setup (MPPS) that allows the preparation of pure atmospheric CH4 samples for 14C measurements. The system combines a methane preconcentration setup (PRECON) with a purification setup which applies preparative gas chromatography to obtain pure CH4 samples from the atmosphere (PURIF).
METHODS
Goals and Strategy
Our research aims at enabling the extraction of CH4 from various kinds of environments (e.g. atmosphere, fresh waters and wetlands) and performing 14C measurements to deepen the knowledge of CH4 sources and the carbon cycle. The strategy adopted for the collection, preparation and radiocarbon measurements of environmental CH4 samples is shown in Figure 1.
Strategy for 14CH4 measurements. Red dashed box: methane preconcentration and purification setup (MPPS), which represents the essential part of this work. Black dotted line: connection of samples from other CH4 sources that will be measured in the future. (Please see electronic version for color figures.)
The procedure can be divided in four main steps: field sampling, preconcentration, purification and 14C measurement. As shown by the black dashed lines in Figure 1, the possibility to measure CH4 from aquatic and terrestrial environments will be implemented soon. However, the system has been developed and optimized for 14C measurements of atmospheric CH4, as this task remains the biggest challenge given the low concentration of CH4 in air (< 2 ppm) and the overwhelming presence of CO2 (> 400 ppm). First, 50–100 L of atmospheric air is collected in an aluminum bag which is brought to the lab, where it is connected to a methane preconcentration line (PRECON), to dramatically decrease the sample size by removing CO2 and most of the bulk air (i.e. N2, O2 and Ar). The preconcentrated sample is then transferred to a GC column, where CH4 is chromatographically purified and subsequently trapped as pure CH4. The purity can be checked by re-injection of the trapped CH4 into the GC. It is then combusted to CO2, manometrically quantified and flame-sealed in a glass ampoule. Finally, the 14C measurement of the CH4-derived CO2 is performed with a MICADAS AMS (Szidat et al. Reference Szidat, Salazar, Vogel, Battaglia, Wacker, Synal and Türler2014).
The individual steps involved in a 14C measurement of atmospheric CH4 are described in the following subsections, with a special emphasis on the PRECON and the PURIF analytical setups.
Sampling
It is necessary to extract CH4 from 50–100 L of air, as its concentrations are less than 2 ppm in atmospheric background air and the target amount for reliable 14C gas measurements is 50 µg C. Therefore, atmospheric air samples are collected by pumping 50-100 L air (STP) into an aluminum bag (100 L PE-AL-PE, Tesseraux, Germany) using a small membrane pump (N838ANE, KNF, Germany).
Methane Preconcentration Setup (PRECON)
Description
A new methane preconcentration setup was developed in our laboratory. It facilitates a drastic reduction of the size of atmospheric air samples from 50–100 L down to 10–15 mL by removing most of the bulk air and CO2, while preserving the original CH4 content. This setup (see Figure 2a) is coupled to a methane purification setup (see Figure 2b), which will be described in the next section. The main components are three cryogenic traps cooled to liquid nitrogen temperature (–196ºC), of which the first (Russian doll trap, RDT) removes CO2, while the second (charcoal trap, CT1) and the third (CT2) allow two successive CH4 preconcentration steps.
(a) Methane preconcentration setup (PRECON). The traps RDT, CT1 and CT2 are used for CO2 removal, first and second CH4 preconcentration steps, respectively. (b) Methane purification setup (PURIF), shown when trapping pure CO, CH4 and CO2 provided from either a syringe injection or the PRECON.
The line consists of 1/4” stainless steel (SS) tubing with Swagelok connections (Swagelok, USA) and a central part between V2 and V7 made of 12 mm OD glass with grease-free Rotulex joints. These two parts are connected using Ultra-Torr (UT) fittings on the glass side and SS tube adapters on the metal side (Swagelok, USA). The gas flow rates in the line, all given in normal conditions (1013 mbar, 0ºC), are regulated by two mass flow controllers MFC1 (SLA5850S, 0–5 L min–1, Brooks, USA) and MFC2 (SLA5850S, 0–150 mL min–1, Brooks, USA). MFC1 and MFC2 regulate the flow for the first and second preconcentration step, respectively. The absolute pressure along the line is monitored by four pressure sensors (P1–P3: PBMN Industrial Low Pressure, 0–2 bar; P4: PBMN flush, 0–2 bar, Baumer, Switzerland).
An aluminum bag (sample bag), which contains an atmospheric air sample collected in the field, is connected to the preconcentration line. The sample is dried in the trap “Drierite,” a plastic tube (24 mm ID, L = 160 mm) filled with 70 g of Drierite™ (CaSO4, 10–20 mesh, Sigma-Aldrich, USA) which turns from blue to pink when it should be regenerated (60 min, 210ºC). V1 allows to switch to a nitrogen supply to clean the system (N2, purity = 99.999%, Carbagas, Switzerland).
RDT is a custom-made “Russian doll” glass trap of a concentric design, similar to the one described by Brenninkmeijer and Röckmann (Reference Brenninkmeijer and Röckmann1996). When immersed into liquid nitrogen, the undulations of its inner part and three nested glass fiber thimbles (Whatman 33 × 94 mm and 25 × 100 mm, GE Healthcare, USA) at its bottom section ensure a very efficient trapping of CO2 and other lower volatility gases through the mechanisms of condensation and adsorption. This configuration allows an efficient removal of substantial amounts of CO2 at high flow rates. Atmospheric CO2, which has been scavenged from the air sample and trapped in RDT, can be recovered after the end of the preconcentration by cryogenically transferring it into the glass bottle “CO2 flask.” An automated graphitization equipment (Němec et al. Reference Němec, Wacker and Gäggeler2010) is then used for the production of solid targets for 14CO2 measurements.
CT1 is a custom-made U-shaped glass trap (13 mm ID) filled with 12 g activated charcoal (Fluka 05112, grain size 0.3–0.5 mm, 0.41 g/cm3, Sigma-Aldrich, USA). P2 and P3 are used to monitor the pressure drop across the trap and the stability of the system throughout the first preconcentration step. A bypass allows excluding this trap from the flow path when necessary.
The second CH4 preconcentration step is achieved in CT2, a custom-made 1/8” OD SS U-shaped trap (2.16 mm ID, L = 40 cm) filled with 0.5 g charcoal. The trap is connected to the valve V11, an electrically actuated 2-position 6-port valve with 1/8′′ fittings (VICI, USA), which is used in “load” mode when CH4 is preconcentrated into CT2 (as shown in Figure 2a) or in “injection” mode when the sample in CT2 is transferred to the GC column of the PURIF.
The sample is pumped from the aluminum bag through the preconcentration line with a membrane pump MP (MZ 2C NT, Vacuubrand, Germany), which is well suited for the handling of high gas flow rates in the line. The pump has an ultimate vacuum of 7 mbar and is also used for cleaning purposes, as it can easily tolerate the removal of potential moisture in the line. Finally, V13 is a needle valve which allows to stop pumping the line gently when required.
Procedure
Cleaning
Before the preconcentration of an air sample, the line and particularly the traps are cleaned thoroughly to remove any contamination from the previous sample or from eventual leaks in the line. First, RDT is cleaned at 95ºC (hot water bath) in a N2 flow of 1.5 L min–1 for 3 min, to remove water vapor and other condensable gases that could remain adsorbed onto the glass fiber thimbles. In this step, CT1 is bypassed and the impurities are directly removed by the pump. As CT1 contains a significant amount of charcoal, care is taken to ensure that CH4 previously adsorbed is comprehensively eliminated. To do so, CT1 is heated to 95ºC, evacuated for 10 min and then flushed with N2 (20 min, 1.5 L min–1). The trap is then pressurized to slightly above ambient pressure with N2 and closed. Finally, CT2 is heated to 95ºC and evacuated for 3 min, flushed for three additional minutes with 50 mL min–1 N2, pressurized to ∼1.2 bar and closed.
First Preconcentration
A N2 flow of 1.5 L min–1 is established in the line with CT1 bypassed and V9 positioned toward the pump. The sample bag is then opened and V1 is switched to connect the sample to the line. RDT is cooled to –196ºC to scrub CO2, and after 1 min, CT1 is included into the flow path by cooling it to –196ºC, opening its inlet (V6) and outlet (V7) and closing the bypass (V5). At that time, CT1 starts trapping CH4 and the flow integrator of MFC1 is initiated to determine the total volume of air. During the 40 min of sample transfer at a flow rate of 1.5 L min–1, the pressures in the lines are monitored (P1, P2 and P3) to avoid a pressure rise due to a leak or a shortcoming of the pump that could trigger O2 condensation (Brenninkmeijer Reference Brenninkmeijer1991). The pressure in the line is usually very stable, with typical values at gauges P2 and P3 of 205 mbar and 85 mbar, respectively. When the pressure at P1 drops below 200 mbar, indicating that the sample has been almost totally transferred to CT1, the inlets of RDT and CT1 are closed and V1 is switched to the N2 bottle. CT1 is evacuated until the pressure at its outlet is stable (i.e. P3 = 10–12 mbar). The liquid nitrogen bath is then replaced by a dry ice/ethanol slurry (–72ºC) for 5 min 30 sec to desorb and pump away excess air trapped together with CH4 into CT1. As shown below, there is no loss of CH4 when bulk air is removed from the trap at –72°C. V8 is then closed, and the dry ice/ethanol bath is replaced with an ambient temperature water bath to manometrically quantify the amount of gas still trapped in the enclosed volume delimited by V6 and V8. Typical sample volumes after the first preconcentration step are 80–100 mL, which is too high to be directly transferred to the GC column for the CH4 purification.
Second Preconcentration
The second preconcentration step, which aims at further reducing the sample volume by removing excess air, is executed in a similar way and transfers the sample from CT1 to CT2. To do so, V9 is switched toward CT2 and the line until V8, including CT2, is evacuated. The valve to the pump V13 is then closed and CT2 is cooled to –196ºC. CT1 is heated to 95ºC to desorb CH4 together with excess air and all gases are then transferred to CT2 at a flow rate of 20 mL min–1 (MFC2) by opening V8. When the pressure after CT2 starts rising (P4), which indicates a breakthrough of air at CT2, V13 is opened to pump away excess air. When P3 drops below 50 mbar, CT1 is flushed with 20 mL min–1 N2 through CT2 for 15 min to guarantee that all the CH4 adsorbed onto CT1 is carried to CT2. The transfer is stopped by closing V8 and CT2, still at –196ºC, is evacuated for 1 min. CT2 is then heated to –72ºC for exactly 1 min 30 sec to desorb and remove excess air.
Transfer to the PURIF
The preconcentrated air sample, still trapped in CT2, is carried to the GC column by first switching V11 to position B (injection), which enables the He carrier gas from the GC to flush CT2 to the column. The dry ice/ethanol bath under CT2 is then removed, the trap is heated to 95ºC to comprehensively desorb CH4 and other trapped gases and the GC run is started immediately afterwards.
Methane Purification Setup (PURIF)
Description
The methane purification setup (PURIF) is schematically shown in Figure 2b. Small (<10 mL) CH4-containing gas mixtures are chromatographically purified and pure CH4 subfractions are recovered as CH4-derived CO2 in a glass ampoule. Although the setup mainly aims at preparing pure CH4 samples for subsequent 14C analysis, this preparative GC technique allows even compound-specific radiocarbon analyses of CH4, CO, CO2 and eventually C2H6. The gas sample is first chromatographically separated before pure CH4 is isolated in an individual trap. It is then transferred to a CuO oven where CH4 is converted into CO2, quantified manometrically and finally flame-sealed in a glass ampoule. The system can handle two different types of sample feed: (1) a manual syringe injection into the GC inlet (SYRINGE) and (2) an on-line injection of a preconcentrated air sample (PRECON).
The GC (7890B, Agilent, USA) is equipped with a purged packed (PP) inlet, a packed column (ShinCarbon ST 80/100, 2 mm ID, L = 2 m, Restek, USA) and a thermal conductivity detector (TCD). The PP inlet was modified such that the injection valve V11 of the PRECON was included into the flow path of the He carrier gas which feeds the inlet (see Figure 2a). The column is thus constantly flushed with He (purity = 99.999%, Carbagas, Switzerland), and the flow is regulated by the electronic pneumatic control module of the GC. Hence, the option is kept to either perform a direct syringe injection of a gas mixture through the septum of the inlet (V11 in “load” mode, as shown in Figure 2a) or to transfer a preconcentrated sample from CT2 (PRECON) to the column (V11 in position “inject”). The column was chosen for its ability to handle large injection volumes at low bleeding and high efficiency of separating permanent gases and hydrocarbons. According to the physical properties of the packing material, the gases are mainly separated according to their volatility. Therefore, bulk air (O2, N2 and Ar) elutes first, followed by CO, CH4, CO2 and finally trace gases of lower volatility. The oven is kept at 40ºC for 4 min and is then heated to 250ºC with a temperature ramp of +10ºC/min. The column is finally cleaned at 280ºC for three additional minutes. The PP inlet is operated in constant pressure mode (20 psig), which causes a gradual decrease of the He carrier gas flow rate from 14 mL min–1 down to 9 mL min–1 as the temperature of the oven rises and the He viscosity increases consequently.
All the tubing is 1/8” SS with Swagelok fittings. The exhaust of the TCD is connected to V14, a 2-position 6-port valve (VICI, USA). When V14 is in position B, as shown in Figure 2b, the gases eluting from the column are carried to V15, a 6-position selector valve (EUTA-2ST6MWE-CU, VICI, USA). The trapping consists of 6 identical custom-made 1/8” OD SS U-shaped traps (2.16 mm ID, L = 35 cm), each of which filled with 0.4 g charcoal and connected to a port of V15. Although V15 was chosen for its small internal volume, intermediary traps are used to ensure a minimal cross contamination when V15 is switched from one collecting trap to the next. Each trap is also equipped with a septum injector nut (VICI, USA) holding a 6 mm septum (TCSD, Trajan, Australia) and connected to a union tee, allowing the collection of pure CH4 (in He) aliquots with a syringe (Pressure-Lok Series A-2, 2 ml, VICI, USA).
V16 is a 4-position dead-end selector (EUTA-2SD4MWE-CU, VICI, USA). An external He supply (V14 in position A), flow-regulated by MFC3 (SLA5850S, 0–50 mL min–1, Brooks, USA) is used to either clean the 6 traps (V16 in position 2) or to transfer CH4 to the combustion oven (V16 in position 1). The methane combustion line consists of a quartz tube (4 mm ID, L = 40 cm) filled with 5.4 g copper oxide wires (0.5 mm diameter, Elementar, Germany) in its central part and connected on both ends to the SS line by means of UT fittings. The quartz tube stands in the middle of a custom-made combustion furnace heated to 950ºC.
The recovery part, where CH4-derived CO2 is quantified and sealed in an ampoule, is an adaptation of the THEODORE system described by Szidat et al. (Reference Szidat, Jenk, Gäggeler, Synal, Hajdas, Bonani and Saurer2004). T1 and T2 are helicoidally-shaped 1/8” SS lines cooled to –72ºC and –196ºC when trapping the combustion products H2O and CO2, respectively. The line is evacuated with a scroll pump SP (IDP-3, Agilent, USA) which allows to evacuate the line down to 1 × 10–1 mbar. The amount of CO2 recovered after CH4 combustion is quantified with the pressure sensor P5 (PBMN Industrial Low Pressure, 0–1 bar, Baumer, Switzerland) in the calibrated volume (CV) of 7.94 cm3. The CH4-derived CO2 is finally flame-sealed into a glass ampoule (4 mm OD, L = 6–7 cm).
Procedure
When not in use, the recovery part remains evacuated to minimize contamination and to shorten the cleaning procedure preceding a sample processing. For similar reasons, CT3 to CT8 are always kept pressurized with He. The combustion oven is gradually heated to 950ºC while flushing with 20 mL min–1 He. Meanwhile, the GC column is baked out to remove any potential contamination and enable the TCD to reach a stable condition. The charcoal U-traps CT3 to CT8 are flushed one by one for 3 min each, and an overpressure (1.5 bar) is applied in each trap to prevent any external contamination. Just before the sample injection, the six traps are immersed into liquid nitrogen and are again individually pressurized to 1.5 bar with He. The valve V14 is then switched to position B and V16 to position 2 (see Figure 2b), so that the gases eluting from the GC column are transferred to the selected trap.
As stated above, the purification setup can either be used as a stand-alone unit, by directly injecting a gas mixture, or together with the PRECON. In the first case, the sample is injected with a syringe through the septum of the PP inlet and the GC run is started immediately after. When used together with the PRECON, the GC method is started just after heating the second preconcentration trap CT2 to 95ºC.
CT4, CT6 and CT8 are used to trap CO, CH4 and CO2, respectively. The GC effluent is directed through the traps CT3, CT5 and CT7 between the peaks of the three target gases to avoid any cross contamination between the carbon-containing gases eluting from the column. The selector valve V15 is switched to the position of the chosen trap 30 s before the onset of the peak at the TCD and 45 s after the TCD signal has reached baseline to account for the transfer time between the detector and the traps (around 12 s) and to ensure a comprehensive trapping of the pure subfractions. After the elution and adsorption of CO2 on CT8, V14 is switched to position A so that the GC flow is disconnected from the trapping part to avoid any low volatile gas eluting from the column to be adsorbed in a trap.
The six traps are heated to 95ºC to desorb CH4, CO and CO2, the combustion line is flushed (35 mL min–1 He, 2 min) to a vent (V22) and T1 and T2 are cooled down to –72ºC and –196ºC, respectively. CT6 is selected and CH4 is combusted in a He flow of 10 mL min–1 for 10 min and the CH4-derived CO2 is trapped in T2. When the combustion is completed, remaining He in T2 is pumped away and the CH4-derived CO2 is manometrically quantified in the calibrated volume CV before it is flame-sealed in a glass ampoule, ready for a 14C-AMS gas measurement.
Methane Preconcentration and Purification Setup (MPPS)
When the PRECON and the PURIF are used together for 14C measurements of atmospheric CH4 samples, time can be saved by handling both setups simultaneously. During preconcentration of the sample, the PURIF is started up and cleaned. If a second sample needs to be processed, the cleaning of the PRECON is started (RDT, CT1 and CT2) while the first sample is purified in the GC column. A single preconcentration followed by a purification lasts ∼3 hr, two samples can be prepared for 14C measurements in ∼5.5 hr so that three samples may be handled in one working day.
Methane 14C Measurement
The CH4-derived CO2 ampoules are measured using the ampoule cracker of the gas handling system of the MICADAS at the University of Bern. The precision achieved during 14C measurements of CO2 samples amounting 50–80 µg C is typically 1% for a modern sample. Two standards, a 14C-free CO2 blank and the NIST Standard Reference Material 4990C (Oxa-II, F14C = 1.3407 ± 0.0005), are measured before and after the samples for blank subtraction, standard normalization and correction of isotopic fractionation (Szidat et al. Reference Szidat, Salazar, Vogel, Battaglia, Wacker, Synal and Türler2014).
RESULTS AND DISCUSSION
Optimization and Performance of the PRECON
The PRECON was tested and optimized using a “pressurized air sample” from a commercially available pressurized air bottle (C017E5R, Druckluft, Carbagas, Switzerland), with measured concentrations of 426 ppm CO2 and 2.10 ppm CH4. It does contain neither water vapor nor CO, as these gases were removed when atmospheric air was pressurized into the bottle. A cavity ring-down spectroscopy analyzer (G2401, PICARRO, USA) was connected to the exhaust of the membrane pump to control the concentrations of CO, CO2, CH4 and H2O during the different steps of the procedure. Finally, the preconcentrated samples were transferred to the GC and the TCD was used to assess the performance of the preconcentration.
The RDT removes over 99.8% CO2 for atmospheric air samples up to a total volume of 400 L without any CO2 breakthrough. As the preconcentrated sample is subsequently purified in the GC column, the scavenging of CO2 does not need to be quantitative. Hence, the usage of a single RDT is sufficient and simplifies the system operation compared to the setups from others, which apply multiple successive traps for this purpose (Wahlen et al. Reference Wahlen, Tanaka, Henry, Deck, Zeglen, Vogel, Southon, Shemesh, Fairbanks and Broecker1989; Brenninkmeijer and Röckmann Reference Brenninkmeijer and Röckmann1996; Röckmann Reference Röckmann1998; Kessler and Reeburgh Reference Kessler and Reeburgh2005; Petrenko et al. Reference Petrenko, Smith, Brailsford, Riedel, Hua, Lowe, Severinghaus, Levchenko, Bromley and Moss2008).
No measurable CH4 breakthrough (< 2‰) was observed in the first preconcentration trap (CT1, 12 g charcoal, 13 mm ID) for air samples up to 200 L, corresponding to a total amount of 210 µg C (CH4) successively trapped, which is four times the targeted sample size. During the preconcentration of larger air volumes, the trapping efficiency drops gradually over time and reaches 50% CH4 breakthrough after 430 L air. Thus, this trap should not be used for sample sizes over 200 L, as isotopic fractionation may occur and would make eventual CH4 stable isotope measurements useless (Wahlen et al. Reference Wahlen, Tanaka, Henry, Deck, Zeglen, Vogel, Southon, Shemesh, Fairbanks and Broecker1989; Kessler and Reeburgh Reference Kessler and Reeburgh2005).
The dimensions of the second preconcentration trap CT2 (0.5 g charcoal, 2.16 mm ID) were chosen as a downscaling of CT1 to further remove excess air while trapping the total amount of CH4 transferred from CT1. From an original air volume of 60 L, the sample size is typically 80–100 mL after the first preconcentration step in CT1 and 10–15 mL after the second step in CT2, corresponding to successive CH4 enrichment factors of approximately 650 and 8, respectively. Thus, CH4 is enriched to a concentration of 8–12‰ after the two preconcentration steps, which is in agreement with the values obtained by Bergamaschi et al. (Reference Bergamaschi, Brenninkmeijer, Hahn, Röckmann, Scharffe, Crutzen, Elansky, Belikov, Trivett and Worthy1998) for a similar procedure. The enrichment factor is lower in CT2, which can be explained by the higher O2/N2 ratio in the sample in CT1 compared to the original ratio in atmospheric air. This O2 enrichment after the first preconcentration step is due to its lower volatility compared to N2, which causes a more efficient adsorption of O2 onto the charcoal. This discrimination over N2 is further enhanced in CT2, resulting in a larger proportion of the sample trapped in CT2. However, the slightly oversized CT2 prevents any CH4 loss during the preconcentration, and the final sample volume (10–15 mL) is still appropriate for a chromatographic separation in the GC column of the PURIF.
The performance of the PRECON was also evaluated by TCD measurements during the preconcentration of 60 L of the pressurized air sample, with known concentrations of CO, CH4 and CO2. The results are detailed in the next section, together with the performance of the PURIF (see Figure 3 below).
Chromatographic separation of a gas mixture. Dashed red line: injection into the PP inlet of 2 mL standard gas mixture (79% N2, 12% CO2, 5% O2, 2% CO and 2% CH4). Blue line: on-line injection from the PRECON of the preconcentration of 60 L pressurized air sample (2.10 ppm CH4, 426 ppm CO2). Grey dotted line: oven temperature program.
Optimization and Performance of the PURIF
Separation
The main physical parameters that influence the quality of the chromatographic separation are the carrier gas flow rate and the temperature of the oven. The GC method optimization was carried out with a standard gas mixture (79% N2, 12% CO2, 5% O2, 2% CO and 2% CH4) that contains higher concentrations of the main trace gases, as the TCD is not sensitive enough for the detection of low concentration compounds. The chromatogram of the syringe injection of 2 mL standard gas mixture, corresponding to approximately 20 µg C (CH4), is shown in Figure 3. Methane is well separated from CO and CO2 even when using a temperature ramp to shorten the method.
An overload of the column causes a broadening and tailing of the peaks, as the column is not designed for such large gas volumes. The effect is enhanced when larger samples are injected, which causes further peak broadening and reduced retention times. This behavior does not affect the collection of pure CH4, as the peaks of CO, CH4 and CO2 are still well separated. However, it causes a poor separation of CO from bulk air, which is partially counterbalanced by the low oven temperature of 40ºC for the first 4 min of the run. Unfortunately, these two peaks start to overlap for samples bigger than 2 mL. A longer column combined with a cooling of the oven could solve this issue if 14CO measurements are of interest, but it would come at the cost of an extended time for the chromatographic separation and the column cleaning. As atmospheric CO is very low in concentration and hard to separate from ambient air due to a similar volatility to O2 (Brenninkmeijer Reference Brenninkmeijer1993), the required modifications are currently not considered.
Figure 3 additionally shows the result of the preconcentration and chromatographic purification of 60 L of the pressurized air sample, when the PRECON and PURIF are jointly used. It should first be noticed that the retention times of the gases are 1–1.5 min longer compared to a direct injection. This is partly due to the sample transfer time between CT2 and the PP inlet, but also to a strongly reduced carrier gas flow rate when the preconcentrated sample in CT2 is heated, as it expands and creates an overpressure in the PP inlet. Fortunately, the shift of the retention times is reproducible and can be accounted for when the pure subfractions are collected in their respective traps. The sample volume after preconcentration is around 10–15 mL, resulting in a strong broadening of the bulk air peak. The TCD signal slowly drops to the baseline after the elution of O2 and N2, which is mainly caused by the dead volumes in the line between CT2 and the PP inlet of the GC.
The PRECON greatly decreased the amount of CO2 from the air sample. However, the GC results show that the PURIF remains a mandatory step for getting reliable 14CH4 results, as the CO2 amount after preconcentration is ∼20% the amount of CH4. The residual CO2 originates from an incomplete scavenging of CO2 in RDT along with some CO2 production in CT1 when it is heated to 95ºC (Bräunlich Reference Bräunlich2000).
Although CH4 is well separated from other carbon-containing gases, it unfortunately co-elutes with krypton (Kr), a noble gas that shows concentrations of ∼1 ppm in the atmosphere and similar physical properties with CH4. Since both separations in the charcoal traps of the PRECON and in the GC column are based on physical adsorption using carbon molecular sieves, Kr is preconcentrated together with CH4 in the PRECON and co-elutes with CH4. This issue was already documented by Schmitt et al. (Reference Schmitt, Seth, Bock, van der Veen, Möller, Sapart, Prokopiou, Sowers, Röckmann and Fischer2013). A full chromatographic separation may only be possible at the cost of cooling the GC oven or using a longer column, which would dramatically extend the whole procedure. As CH4 is ultimately combusted and recovered as CO2 in a glass ampoule, however, Kr is removed in this latter step. Consequently, co-eluting Kr impedes the ability to precisely quantify the amount of CH4 preconcentrated, but the manometric quantification of the CH4-derived CO2 can still be used to assess the yield and performance of the whole procedure involving PRECON and PURIF.
Trapping
Methane trapping efficiency after its chromatographic separation was measured by connection of the outlet of the CH4 trap (CT6) to the flame ionization detector (FID) of the GC, which is more sensitive to hydrocarbons than the TCD. Up to 2 mL pure CH4, which corresponds to an amount of ∼1000 µg C, could be trapped at –196ºC for 50 min, while the trap was flushed with a He flow rate of 35 mL min–1 to the FID without any detectable breakthrough. This result yields to a trapping efficiency of >99.99%.
The CH4 trap is heated to 95ºC when CH4 is transferred to the combustion oven. This temperature allows a comprehensive desorption of CH4 from the charcoal and thus prevents any isotopic fractionation (Bräunlich Reference Bräunlich2000). The traps CT4 and CT8 were also successfully tested for their ability to trap and desorb CO and CO2, respectively.
Combustion
The choice of CuO as a catalyst for the conversion of CH4 to CO2 was based on several aspects: it is cheap, easy to use, regenerate or replace and shows a good oxidation efficiency of hydrocarbons without any need of an additional oxidant, which simplifies the isolation of pure CH4-derived CO2 (Dumke et al. Reference Dumke, Faber and Poggenburg1989; Kessler and Reeburgh Reference Kessler and Reeburgh2005). A long and thin quartz tube allows a comprehensive combustion of CH4 while the oven cleaning is facilitated, which minimizes cross contamination from a sample to the next. Methane combustion efficiency was assessed by connection of the outlet of T2 to the FID. As CH4 is not trapped in T2, an empty tube cooled to –196ºC without any adsorbent, a potential incomplete combustion of CH4 can be detected by the FID. Aiming at a time-efficient method, the highest He carrier flow granting a complete combustion of CH4 was sought. This is achieved at a flow rate of 10 mL min–1 and breakthroughs of 0.2% and 1.8% are observed for flow rates of 20 mL min–1 and 35 mL min–1 He, respectively.
Validation of the MPPS
Performance
The constant contamination is a model of the procedural blank of a system (Brown and Southon Reference Brown and Southon1997; Salazar et al Reference Salazar, Zhang, Agrios and Szidat2015), which assumes that a constant amount of carbon with a fixed F14C value is added to the recovered CH4-derived CO2 when an air sample is preconcentrated and purified. It can be evaluated by processing CH4 standards of known mass and 14C content through the whole procedure. We use a modern methane standard that was produced through the reduction of CO2, which was released by the combustion of tree leaves. The pure modern methane standard was measured with the MICADAS after combustion of CH4 to CO2 and shows a F14C of 1.024 ± 0.003, which is consistent with the results from the direct 14C measurements of the CH4 with gas proportional counting (GPC) at the GPC Radiocarbon Lab at the Physics Institute of the University of Bern (Loosli et al. Reference Loosli, Heimann and Oeschger1980). In order to ease the handling of small volumes, the modern methane standard was diluted to 10% CH4 in He. The CH4 contained in the standard gas mixture was used as a fossil CH4 standard, as it is totally depleted in 14CH4 (i.e. F14C = 0). Different amounts of these two gases were injected with a septum injector nut at the preconcentration line before the RDT into a N2 flow of 60 L in total and the preconcentration and purification steps were performed as usually. The procedural blank (constant contamination) of the MPPS was determined to be 0.35 ± 0.10 µg C with an F14C of 0.35 ± 0.18 (see Table 1). These values were calculated using the statistical model developed by Salazar et al. (Reference Salazar, Zhang, Agrios and Szidat2015). The cross contamination from the previous sample, which is 0.4 ± 0.2%, most likely originates from an imperfect cleaning of the charcoal traps.
Quality assurance parameters of the Methane Preconcentration and Purification Setup (MPPS), with average uncertainty (1σ) and standard deviation (Std dev) of all measurements (both calculated referring to a single analysis). See Supplementary Materials for detailed results.
* Determined from repeated analysis of 60 L of the pressurized air sample.
# Determined from repeated analysis of the modern methane standard.
The system repeatability was determined from several preconcentration, purification and 14CH4 measurement of 60 L pressurized air sample (see Table 1). The MPPS exhibits a good repeatability, as the standard deviation of the F14C for all CH4 analyses of the pressurized air sample is 0.010, which is comparable to the average F14C measurement uncertainty of a single analysis (0.012). To assess the system accuracy, repeated 14C measurements of the modern methane standard that was processed through the MPPS were compared to the modern methane standard F14C reference value. The results, presented in Table 1, show that the mean F14C from the repeated measurements (F14C = 1.018 ± 0.008) is statistically indistinguishable from the reference value (F14C = 1.024 ± 0.003). The overall yield of the setup was calculated from the comparison of the amount of CH4-derived CO2 recovered in a glass ampoule with its corresponding theoretical amount of CH4 injected into the PRECON (see Table 1). The samples used for this evaluation were collected in aluminum bags at the Beromünster tall tower, Switzerland, as described by Berhanu et al. (Reference Berhanu, Szidat, Brunner, Satar, Schanda, Nyfeler, Battaglia, Steinbacher, Hammer and Leuenberger2017). The yield of the MPPS is 101.2 ± 1.4%, indicating a quantitative recovery of CH4 during the preconcentration and purification steps.
The chromatographic purification of CH4 after preconcentration is an essential step, as it guarantees the reliability of the 14C results. Such an approach has been previously employed by some other groups (e.g. Wahlen et al. Reference Wahlen, Tanaka, Henry, Deck, Zeglen, Vogel, Southon, Shemesh, Fairbanks and Broecker1989; Eisma et al. Reference Eisma, van der Borg, de Jong, Kieskamp and Veltkamp1994). However, their systems were used for the purification of much larger air volumes and thus required more traps and a long and labor-intensive procedure limiting their throughput. The simplified preconcentration line presented here drastically reduces the sample preparation time for a 14CH4 measurement, as three samples can be readily prepared within a working day. Hence, the MPPS is suited to the monitoring of atmospheric 14CH4.
Versatility
According to the research strategy depicted in Figure 1, the two systems presented in this work can be adapted to handle CH4 collected from many diverse environments (e.g. aquatic, wetland, marine etc.), where CH4 concentrations can be much higher than in atmospheric air. As methanogenesis is often intense in the carbon-rich sediments at the bottom of some lakes and ponds, typical concentrations in the samples collected can be high enough so that a few milliliters contain enough CH4 for a radiocarbon analysis (Rinta et al. Reference Rinta, Bastviken, van Hardenbroek, Kankaala, Leuenberger, Schilder, Stötter and Heiri2015). If so, the sample does not require preconcentration and the PURIF can be used alone as it can handle direct injections of gas mixtures up to 10 mL.
For intermediate concentration methane sources, such as arctic lakes or peatlands, gas samples are usually extracted with headspace techniques (Walter et al. Reference Walter, Chanton, Chapin, Schuur and Zimov2008; Garnett et al. Reference Garnett, Hardie and Murray2011). A methane 14C analysis of such samples often involves the extraction from gas samples of a few hundred milliliters. In this case, using the whole PRECON might be an overkill; hence, it may be possible to adapt the PRECON to use the second preconcentration step with CT2 alone before performing the CH4 purification.
Finally, CH4 dissolved in low concentration waters can be extracted with membrane contactors (Matsumoto et al. Reference Matsumoto, Han, Jaklitsch and Aggarwal2013; Sparrow and Kessler Reference Sparrow and Kessler2017), resulting in extracted gas volumes similar to the ones required for atmospheric air sampling. Thus, these samples can be handled as the atmospheric air samples by combination of the whole PRECON and the PURIF.
CONCLUSION
A new methane preconcentration and purification setup was developed for the preparation of atmospheric CH4 samples for 14C measurements. The system requires only ∼50 L of atmospheric air, which can be collected in an aluminum bag or pressurized in a gas bottle. A preparative gas chromatography technique is used for CH4 isolation, which confirms that methane has been successfully separated from any other carbon-containing gases such as CO or CO2 that could dramatically bias the 14CH4 results. A procedural blank of 0.35 ± 0.10 µg C with an F14C of 0.35 ± 0.18 was determined, which is low compared to the typical amounts of CH4 purified and measured. Methane is quantitatively extracted from the original air sample and isolated as pure CH4 for the AMS 14C measurement, which shows a good accuracy and repeatability. The system is therefore well suited to the radiocarbon analysis of atmospheric CH4. Since methane is not combusted before purification, CH4 aliquots can be collected for stable isotope measurements. Combined with 14C results, they should provide complementary information.
ACKNOWLEDGMENTS
We are grateful to the funding of the Dr. Alfred Bretscher Scholarship. Carina van der Veen and Henk Snellen (IMAU, Utrecht) assisted during the early steps of the setup development. Markus Leuenberger, Thomas Wagner and Peter Dürring (Climate and Environmental Physics, University of Bern) provided the methane modern standard, the air samples from Beromünster, the PICARRO and the pressurized air bottle. We further thank Robert Eichler (Paul Scherrer Institute) for the oven furnace and Gary Salazar for the assistance with the MICADAS and the evaluation of the data.
SUPPLEMENTARY MATERIAL
To view supplementary material for this article, please visit https://doi.org/10.1017/RDC.2019.76.
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