Gravimetrically prepared carbon dioxide standards in support of atmospheric research
- 1Global Monitoring Division, National Oceanic and Atmospheric Administration, 325 Broadway, Boulder, Colorado 80305, USA
- 2Cooperative Institute for Research in Environmental Science, University of Colorado, Boulder, Colorado 80309, USA
- 3Climate and Environmental Physics, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
Correspondence: Bradley D. Hall (firstname.lastname@example.org)
We have explored a one-step method for gravimetric preparation of CO2-in-air standards in aluminum cylinders. We consider both adsorption to stainless steel surfaces used in the transfer of highly pure CO2 and adsorption of CO2 to cylinder walls. We demonstrate that CO2-in-air standards can be prepared with relatively low uncertainty (∼ 0.04 %, ∼95 % confidence level) by introducing aliquots whose masses are known to high precision and by using well-characterized cylinders. Five gravimetric standards, prepared over the nominal range of 350 to 490 µmol mol−1 (parts per million, ppm), showed excellent internal consistency, with residuals from a linear fit equal to 0.05 ppm. This work compliments efforts to maintain the World Meteorological Organization, Global Atmosphere Watch, mole fraction scale for carbon dioxide in air, widely used for atmospheric monitoring. This gravimetric technique could be extended to other atmospheric trace gases, depending on the vapor pressure of the gas.
Numerous laboratories make routine measurements of atmospheric carbon dioxide to better understand its sources, sinks, and temporal variability. These measurements are typically calibrated using high-pressure gas standards containing CO2 in air (typically natural air with assigned CO2 mole fractions), traceable to primary standards prepared or analyzed using absolute methods, such as manometry (Keeling et al., 1986; Zhao and Tans, 2006) and gravimetry (Machida et al., 2011; Rhoderick et al., 2016; Brewer et al., 2014), which provide traceability to the International System of Units (SI). The World Meteorological Organization (WMO) Global Atmosphere Watch (GAW) initially adopted the Scripps Institution of Oceanography scale (Keeling et al., 1986) and subsequently the National Oceanic and Atmospheric Administration (NOAA) scale (Zhao et al., 1997), both of which are based on repeated manometric measurements of a suite of primary standards, for WMO-affiliated monitoring networks. The WMO scale has been updated over the years as understanding has improved and measurement records of primary standards have increased (Keeling et al., 2002, 1986; Zhao and Tans, 2006).
Determining the absolute amount of CO2 in air is a challenge for both gravimetric and manometric methods, particularly since the relative uncertainties must be very small (∼0.006 % 1σ, or about a factor of 4 lower than the WMO network compatibility goal of 0.1 ppm – WMO, 2018) in order to assess changes (drift) in cylinders over many years. Long-term monitoring of atmospheric CO2 requires a stable reference, sufficient to identify small atmospheric gradients (of the order of 0.1 µmol mol−1, or 0.1 ppm, in the remote troposphere). Hereafter we will use parts per million for micromoles per mole. Both methods can be influenced by the adsorption of CO2 to surfaces. There is increasing evidence that CO2 can adsorb to the internal surfaces of cylinders and desorb with decreasing pressure (Langenfelds et al., 2005; Miller et al., 2015; Leuenberger et al., 2015; Brewer et al., 2018; Schibig et al., 2018). This impacts both the gravimetrically assigned mole fraction and the mole fraction of CO2 in air withdrawn from cylinders over time. Further, since cylinder characteristics may differ among cylinder manufacturers, understanding the behavior of CO2 in cylinders is critical to maintaining stable scales over time.
The gravimetric technique can employ multiple steps, in which the target gas (CO2 in this case) is diluted to the desired amount fraction. For example, Brewer et al. (2014) first prepared standards with mole fractions of a few percent, then made dilutions of those to the range needed for ambient monitoring (∼400 ppm). Others have opted to dilute CO2 to part per million levels in one step (Machida et al., 2011). Matrix gases can also be added in different ways: CO2 can be mixed with individual gases (N2, O2, Ar) to form an air-like matrix, or CO2 can be added to natural air from which the CO2 has been removed. Methods of targeting stable isotopes of CO2 (e.g., 13C-CO2) to better match natural abundances have also been explored (Brewer et al., 2014).
Here we describe one-step preparation of CO2-in-air compressed gas standards in aluminum cylinders. We used information gained from recent decanting experiments (Schibig et al., 2018) to correct for CO2 adsorption to the cylinder walls. This work was undertaken to support NOAA manometric efforts and learn more about the behavior of CO2 in aluminum cylinders.
Standards were prepared in 29.5 L Luxfer aluminum cylinders (∼22 kg empty) (Scott Marrin, Inc., Riverside, CA), with brass packless valves (Ceodeux). We chose these cylinders for two reasons. First, we wanted to perform the dilutions in one step and therefore needed relatively large cylinders. Second, we wanted to use cylinders that were well characterized. We have considerable experience with CO2 in air in this type of cylinder. Specific to this work, all cylinders used were filled with natural air and decanted several times for CO2 adsorption studies (Schibig et al., 2018) prior to being used for gravimetric standards described here.
For this gravimetric work, each cylinder was evacuated to ∼30 mtorr (4 Pa) and weighed on a mass comparator (Sartorius CCE40K3: 40 kg capacity, 2 mg readability) relative to a control cylinder of similar mass and volume. The mass comparator was calibrated using a 10 kg mass (Troemner), and linearity over the working range was confirmed by adding a 5 kg mass (Mettler Toledo) to the reference cylinder. We then added ∼50 psi (0.34 MPa) natural air containing 402 or 408 ppm CO2 determined by analysis (WMO X2007 scale). Cylinders were then vented, partially evacuated to ∼400 torr (53 kPa), and weighed. The mass of residual air along with the mole fraction of CO2 was used to calculate the initial mass of CO2 in the cylinder. We did not evacuate the cylinders further because CO2 adsorption studies (Schibig et al., 2018) were performed at pressures ranging from 0.1 to 13.8 MPa. The Schibig et al. (2018) work provided a means to determine the amount of CO2 adsorbed to cylinder walls, and we wanted to perform the gravimetric addition with a small amount of residual CO2 in the cylinders, consistent with that work. For the standards presented here, the initial CO2 in the cylinder corresponds to <0.8 % of the total CO2, and so the uncertainty associated with the mole fraction of initial CO2, derived from an independent CO2 calibration (Zhao and Tans, 2006), makes a negligible contribution to the total uncertainty (Table 1). The majority of the uncertainty in the mass of CO2 originally in the cylinder results from uncertainty in the mass determination of the residual air. Nevertheless, we include a standard uncertainty of 0.025 % on the WMO X2007 CO2 scale (https://www.esrl.noaa.gov/gmd/ccl/ccl_uncertainties_co2.html, last access: August 2018).
Note: Entries preceded by “μ_” represent standard uncertainties (∼68 %
CO2_a: mass of CO2 aliquot in a 5 mL container, added to cylinder.
CO2_b: initial mass of CO2 in the cylinder (based on analyzed mole fraction and mass of residual air).
Air: mass of air (includes 10–15 g residual air initially present in cylinder).
: total amount of CO2 (moles) (0.99997 purity correction applied).
nair: total amount of air (moles).
: correction applied to account for adsorption to cylinder walls.
: correction applied to account for CO2 in the dilution gas.
: mole fraction of CO2.
An initial aliquot of high-purity CO2 was added to an evacuated 50 mL stainless steel container with a single metal bellows valve (Swagelok, model SS-4H) (pressure rated to 1000 psi, or 6.90 MPa, at 37 ∘C). After CO2 was loaded into the 50 mL container at the desired pressure, it was cryogenically transferred to a 5 mL stainless steel container, also with a metal bellows valve (total mass ∼150 g) that had been evacuated and weighed previously. The CO2 was cryogenically purified by freezing at −197 ∘C and pumping off non-condensible gases. We estimate the purity of the CO2 source at 99.994 % and that of the cryogenically purified CO2 aliquots at 99.997±0.002 % (Table 2). In this smaller volume, both liquid and vapor phases of CO2 would be present at room temperature (18 ∘C in this case). Note that the vapor pressure of CO2 at 18 ∘C is ∼795 psi (5.48 MPa) and that our 5 mL container and valve was rated to 1000 psi (6.89 MPa). We employed this secondary transfer to a smaller container so that we could weigh ∼1.5 g of CO2 on a balance with 0.01 mg readability (Mettler Toledo AT201, 200 g capacity). The 50 mL container used in the first step is too large to be weighed on the AT-201. This is an important aspect of this work. Without this secondary step, our uncertainties would have been about a factor of 10 larger. The mass of CO2 in each 5 mL aliquot was determined by weighing the 5 mL container relative to a control object of similar mass and density (sequence ABABA…). The AT-201 was calibrated using internal weights and span-checked by adding a 2.0000 g mass to the 5 mL container.
a Since the CO2 aliquots were cryogenically purified to remove
we calculate the aliquot purity based on H2O only. Non-condensibles
O2, Ar, H2, CO, and CH4.
b Gas Chromatography with Electron Capture Detection
c Gas Chromatography with Mass Selective Detection
Each purified CO2 aliquot was transferred from the 5 mL container to a partially evacuated cylinder on a stainless steel vacuum manifold using a pressurization–expansion method (Fig. 1) (Dlugokencky et al., 2005). The cylinder was connected to the vacuum manifold using a 1∕8 in. o.d. AT-steel transfer line. AT steel, also known as “activity tested steel” (Grace Discovery Science, Columbia, MD), is treated using vapor deposition to improve surface inertness. In initial tests we found that AT steel performed better than other types of stainless steel, but in subsequent tests both 1∕8 in. o.d. stainless steel and 1∕8 in. o.d. AT steel performed similarly (see Sect. 3).
To transfer the aliquot to the cylinder, the manifold and transfer lines were preheated to ∼60 ∘C and evacuated to 5 mtorr (0.7 Pa). In quick succession, the cylinder valve was opened and the valve on the 5 mL container was opened, allowing CO2 to expand into the cylinder. The expansion of CO2 resulted in significant cooling of the 5 mL container, so we heated the 5 mL container, manifold, and transfer lines to ∼60 ∘C while alternately pressurizing the 5 mL container to ∼200 psi (1.38 MPa) with CO2-free air (dilution gas) and expanding into the cylinder. After about 20 pressurization–expansion cycles, the valve on the 5 mL container was closed and the cylinder pressurized with dilution gas. The 5 mL container was removed from the manifold at a cylinder pressure of ∼500 psi (3.45 MPa), and the cylinder was then further pressurized to 1000 psi (6.90 MPa) with dilution gas. Dilution gas consisted of scrubbed natural air (cryogenic ultrapure grade, Scott Marrin, Inc.; now Praxair, Los Angeles, CA). This gas was analyzed for CO2 by nondispersive infrared analysis (NDIR; LI-COR Li-7000). Samples of dilution gas were compared to a reference of dry nitrogen (99.999 %) scrubbed using Ascarite II (Sigma Aldrich). All cylinders of dilution gas contained 0.01±0.01 ppm CO2. After cylinders cooled to room temperature, they were weighed on the mass comparator relative to the control cylinder.
The mole fraction of CO2, , was calculated using Eq. (1), where na is the moles of CO2 transferred from the 5 mL container, nb is the moles of CO2 initially present in the cylinder, nair is the total moles of air (sum of natural air initially present and dilution air), p is the purity coefficient, f is the transfer efficiency, is a correction for the amount of CO2 adsorbed to the cylinder walls () expressed in parts per million, and is the amount of CO2 in the dilution air, also expressed in parts per million.
The amount of each component was determined from the mass and molecular weight. For CO2 we used a molecular weight of 44.0096±0.0006 g mol−1 (consistent with a 13C-CO2 content of −29 ‰ on the Vienna Peedee belemnite (VPBD) scale, determined using off-axis integrated cavity output spectroscopy (Los Gatos Research) traceable to the University of Colorado (INSTAAR) Stable Isotope Laboratory realization of VPDB; Trolier et al., 1996; Tans et al., 2017). For the dilution gas, we used a molecular weight of 28.9602±0.0042 g mol−1. The oxygen content of the dilution gas was measured using a paramagnetic method (Beckman, E2) traceable to NIST SRM 2659A (20.863±0.011 % O2 in N2). Argon was taken as 0.933 % (Sutour et al., 2007), and the noble gases Xe, Ne, and Kr were taken as 0.09, 18.0, and 1.14 ppm, respectively. Nitrogen was assumed to comprise the remaining fraction. We assumed 100 % transfer efficiency (f=1.0) with an uncertainty of 0.01 % (rectangular distribution) (see Sect. 3).
The mole fraction correction for CO2 adsorbed to the cylinder walls () was determined from multiple decanting experiments (Schibig et al., 2018). Briefly, in those experiments, cylinders were filled with dry natural air (∼ 400 ppm) and drained at 0.3 L min−1 and analyzed continuously for CO2 by NDIR. These studies showed remarkably consistent results: that the mole fraction of CO2 exiting the cylinder increased as the cylinder pressure decreased and that the data can be described with a Langmuir isotherm (Fig. 2). By fitting the data with a Langmuir isotherm as derived by Leuenberger et al. (2015), and integrating the area between the Langmuir fit and the initial , we determined the amount of CO2 that desorbs from the walls as the cylinder is vented slowly to near-ambient pressure (Fig. 2). The amount of CO2 adsorbed to the walls, expressed as a fraction of the total amount of CO2 in the cylinder, was typically about 0.004 % (Table 3). Although the low-flow data show very good reproducibility (Table 3), we assumed a standard uncertainty of 0.01 ppm.
Five standards were prepared gravimetrically, with CO2 mole fractions ranging from 357 to 492 ppm. Preparation uncertainties were determined by propagating uncertainties associated with variables in Eq. (1) (Table 1), using software available from the National Institute of Standards and Technology (NIST) (https://www.nist.gov/programs-projects/metrology-software-project, last access: May 2014). The two most important factors influencing uncertainty are repeatability associated with weighing the purified CO2 aliquot (contributing ∼25 %) and the molecular weight of air (contributing ∼65 %). For MWair, the uncertainty is partially limited by our ability to measure O2 and calibrate the O2 analyzer.
Following preparation, standards were analyzed using laser spectroscopy (Tans et al., 2017). Each standard was analyzed twice over a period of 2 weeks. The response was expressed as the mole fraction of CO2, calculated on the WMO X2007 CO2 scale, relative to that of CB11941. We use this relative response because mole fraction assignments on the X2007 scale account for differences in the abundances of stable isotopes of CO2 (mainly 13C-CO2) between the gravimetric standards and secondary standards used for calibration (Tans et al., 2017). For comparison, we also calculated the response based on the analyzer signal derived from a single CO2 isotopologue (16O-12C-16O, 626). Both methods give similar results with respect to consistency of the standard set.
Table 4 and Fig. 3 show the best-fit results and residuals (difference between best fit and prepared mole fraction). All standards agree (within expanded uncertainties) with the regression line. The standard deviation of residuals is 0.05 ppm and the largest residual is 0.09 ppm. Since the uncertainty associated with the molecular weight of air is the largest contributor to the total uncertainty, but is common to all standards, it is worth recalculating uncertainty without this contribution in order to assess consistency. Without μ_MWair, standard uncertainties for each standard are 40 %–60 % lower than when μ_MWair is included. Recalculating the regression using these lower uncertainties, we find that the residuals do not change appreciably. However, the residual for cylinder CB11941 becomes 0.098 ppm. With a standard uncertainty of 0.046 ppm, CB11941 is not consistent with the rest of the standards. This may be the result of preparation. Cylinder CB11941 was the first standard prepared and followed testing that involved injecting high concentrations of CO2 into the manifold and transfer lines. It is possible that some residual CO2 remained in the manifold and transfer lines and was introduced into CB11941 when the manifold and transfer lines were heated. The other standards were prepared following several heating cycles and are less likely to be influenced by any residual CO2.
To support our assumption of 100 % transfer efficiency, we examined both the potential for adsorption of CO2 in the manifold and transfer lines and the efficiency of transferring CO2 from the 5 mL container to a cylinder. We tested the transfer line by flowing air containing ∼0.1 ppm CO2 at 0.2 L min−1 through 1∕8 in. AT-steel tubing to an NDIR analyzer. Then we injected 0.6 mL of 10 % CO2 in air into this air stream. After the initial slug of CO2 was observed and the NDIR signal returned to baseline, we heated the transfer line and measured the additional CO2 coming off (Fig. 4). Comparing the area of the CO2 released upon heating with that of the main sample injected, we found that our AT-steel transfer line (length 1 m) retained about 0.04 % of CO2 in the sample. We were able to drive off most of this CO2 on the first heating cycle, with <0.01 % released on subsequent heating. Tests with stainless steel (not AT steel) showed similar results. By heating the lines multiple times and passing a large amount of CO2-free air through them, it is unlikely that a significant amount of CO2 would remain in the manifold or transfer line.
We tested the transfer efficiency from the 5 mL container by cryogenically moving aliquots of CO2 from one 5 mL container to another on a vacuum line (using liquid N2), without additional flushing, and measuring changes in mass. When both the initial 5 mL container and transfer line were heated, a transfer efficiency of 99.9±0.1 % was achieved. Without heating, the same test revealed only 99 % efficiency. We expect that repeated pressurization–expansion with CO2-free air, in addition to heating, would improve the transfer efficiency of the CO2 aliquot to near 100 %. The relatively good agreement among the four standards prepared after CB11941 supports this assumption. It seems unlikely that this level of agreement could be achieved with poor or variable transfer efficiency.
As mentioned earlier, we estimated the amount of CO2 adsorbed to the cylinder walls (∼0.004 %) from the results of low-flow decanting experiments. The Schibig et al. (2018) decanting tests reveal substantially less CO2 adsorbed compared to “mother–daughter” tests (Miller et al., 2015; Brewer et al., 2018), in which half the contents of one cylinder are transferred to an equal size cylinder and the adsorption determined based on the resulting mole fraction difference. From mother–daughter tests on 5.9 L cylinders from Airgas (Riverton, NJ) and 5 L cylinders from Air Products (Vilvoorde, Belgium), Miller et al. (2015) estimated that about 0.02 % of the CO2 was adsorbed to the walls. Brewer et al. (2018) performed similar tests on 10 L aluminum cylinders treated with the BOC Spectra Seal process and found CO2 adsorption fractions of about 0.05 %.
In preparation for this work, we performed mother–daughter tests on both 5.9 and 29.5 L aluminum cylinders (Scott Marrin, Riverside, CA), including cylinders CB11941 and CB11873 used in this work. Cylinders CB11941 and CB11873 were filled with natural air, vented, and then evacuated to 5 psia (0.03 MPa). Air from two mother cylinders containing natural air was transferred into CB11941 and CB11873. We found that the CO2 in daughter cylinders CB11941 and CB11873 was 0.16–0.19 ppm lower than their respective mothers after transfer (Table 5), similar to the results of Miller et al. (2015) and Brewer et al. (2018). Our tests with 5.9 L cylinders also showed differences of ∼0.2 ppm (not shown).
Mother–daughter tests suggest 5 to 10 times more adsorption than that determined from the Schibig et al. (2018) low-flow data. The difference between mother–daughter tests and the low-flow experiments could be related to thermal fractionation. Schibig et al. (2018) performed both low-flow (0.3 L min−1) and high-flow (5.0 L min−1) decanting experiments. They found that changes in CO2 at the high flow rate were 2.5 times those observed at the low flow rate and attributed the difference to thermal fractionation at the higher flow rate. During our mother–daughter tests, the mother cylinders experienced significant cooling during transfer, which could have caused fractionation as cooler air sinks in the center core of the cylinder, with CO2 preferentially remaining in the mother cylinder. In fact, after transferring half of the gas from a mother cylinder to a respective daughter cylinder, the mole fraction of CO2 in each mother cylinder increased 0.06±0.01 ppm relative to its value determined prior to transfer (Table 5). From Fig. 2, which represents a typical low-flow decanting result, the increase due to desorption from the cylinder walls should be far smaller than 0.06 ppm at 50 % of the original cylinder pressure.
Finally, we compare these standards to the WMO X2007 CO2 scale. The mean ratio of gravimetrically assigned mole fractions to values assigned on the WMO X2007 scale is 1.00045 with a standard deviation of 0.00017. Thus, the WMO X2007 scale is ∼0.05 % lower than a scale based on these gravimetric standards. However, this difference is not outside the range of uncertainties (∼0.05 % for WMO X2007 and ∼0.033 % for this work, ∼95 % confidence level, or coverage factor k=2). While the 13C-CO2 content of these gravimetrically prepared standards is lower than that of natural air (−29 ‰, compared to about −8 ‰ for natural air), and these standards were compared to WMO secondary standards with 13C-CO2 at ambient levels during analysis, this introduces negligible bias because the analytical method compensates for different isotopic abundances (Tans et al., 2017). Further discussion on differences between the WMO X2007 scale and these gravimetric standards will be included in a subsequent publication.
Five gravimetric CO2-in-air standards, prepared at the parts per million level in one dilution step, show excellent internal consistency. Prepared mole fractions were adjusted for CO2 expected to adsorb to cylinder walls. This correction was determined from low-flow decanting studies and is a factor of 5–10 smaller than that inferred from mother–daughter tests. With improved understanding of CO2 adsorption characteristics, and by introducing condensed-phase aliquots of CO2 into small vessels that can be weighed with sufficient repeatability, CO2-in-air standards can be prepared with relatively low uncertainty. This work supports parallel efforts to maintain the WMO mole fraction scale for CO2.
Most relevant data are included in Tables 1–3. Data needed to calculate values in Table 3 are available in Schibig et al. (2018). Additional data are available in the Supplement.
The supplement related to this article is available online at: https://doi.org/10.5194/amt-12-517-2019-supplement.
BDH designed the experiment, carried out the laboratory work, and prepared the standards. AMC and BJM performed purity analysis. MS performed cylinder stability tests. BDH prepared the paper with contributions from all authors.
The authors declare that they have no conflict of interest.
This work was supported, in part, by NOAA's Atmospheric Chemistry, Carbon
Cycle, and Climate program (AC4). Michael Schibig was supported by an Early Postdoc
Mobility fellowship from the Swiss National Science Foundation (SNSF) while
working at NOAA in Boulder, CO. The authors thank Thomas Mefford for performing the analysis and Duane Kitzis for providing
cylinders of clean, unpolluted air.
Edited by: Marc von Hobe
Reviewed by: three anonymous referees
Brewer, P. J., Brown, R. J. C., Miller, M. N., Miñarro, M. D., Murugan, A., Milton, M. J. T., and Rhoderick, G. C.: Preparation and Validation of Fully Synthetic Standard Gas Mixtures with Atmospheric Isotopic Composition for Global CO2 and CH4 Monitoring, Anal. Chem., 86, 1887–1893, https://doi.org/10.1021/ac403982m, 2014.
Brewer, P. J., Brown, R. J. C., Resner, K. V., Hill-Pearce, R. E., Worton, D. R., Allen, N. D. C., Blakley, K. C., Benucci, D., and Ellison, M. R.: Influence of Pressure on the Composition of Gaseous Reference Materials, Anal. Chem., 90, 3490–3495, https://doi.org/10.1021/acs.analchem.7b05309, 2018.
Dlugokencky, E. J., Myers, R. C., Lang, P. M., Masarie, K. A., Crotwell, A. M., Thoning, K. W., Hall, B. D., Elkins, J. W., and Steele, L. P.: Conversion of NOAA atmospheric dry air CH4 mole fractions to a gravimetrically prepared standard scale, J. Geophys. Res.-Atmos., 110, https://doi.org/10.1029/2005JD006035, 2005.
Keeling, C. D., Guenther, P. R., and Moss, D. J.: Scripps reference gas calibration system for carbon dioxide-in-air standards: revision of 1985, Gaw Report No. 42, WMO, Geneva, Switzerland, 1986.
Keeling, C. D., Guenther, P. R., Emanuele, G., Bollenbacher, A., and Moss, D. J.: Scripps reference gas calibration system for carbon dioxide-in-nitrogen and carbon dioxide-in-air standards: revision of 1999, Scripps Institution of Oceanography, La Jolla, CA, 2002.
Langenfelds, R. L., van der Schoot, M. V., Francey, R. J., Steele, L. P., Schmidt, M., and Mukai, H.: Modification of air standard composition by diffusive and surface processes, J. Geophys. Res.-Atmos., 110, https://doi.org/10.1029/2004JD005482, 2005.
Leuenberger, M. C., Schibig, M. F., and Nyfeler, P.: Gas adsorption and desorption effects on cylinders and their importance for long-term gas records, Atmos. Meas. Tech., 8, 5289–5299, https://doi.org/10.5194/amt-8-5289-2015, 2015.
Machida, T., Tohjima, Y., Katsumata, K., and Mukai, H.: A new CO2 calibration scale based on gravimetric one-step dilution cylinders in National Institute for Environmental Studies – NIES 09 CO2 Scale, Gaw Report No. 194, WMO, Geneva, Switzerland, 165–169, 2011.
Miller, W. R., Rhoderick, G. C., and Guenther, F. R.: Investigating Adsorption/Desorption of Carbon Dioxide in Aluminum Compressed Gas Cylinders, Anal. Chem., 87, 1957–1962, https://doi.org/10.1021/ac504351b, 2015.
Rhoderick, G. C., Kitzis, D. R., Kelley, M. E., Miller, W. R., Hall, B. D., Dlugokencky, E. J., Tans, P. P., Possolo, A., and Carney, J.: Development of a Northern Continental Air Standard Reference Material, Anal. Chem., 88, 3376–3385, https://doi.org/10.1021/acs.analchem.6b00123, 2016.
Schibig, M. F., Kitzis, D., and Tans, P. P.: Experiments with CO2-in-air reference gases in high-pressure aluminum cylinders, Atmos. Meas. Tech., 11, 5565–5586, https://doi.org/10.5194/amt-11-5565-2018, 2018.
Sutour, C., Stumpf, C., Kosinski, J. P., Surget, A., Hervouët, G., Yardin, C., Madec, T., and Gosset, A.: Determination of the argon concentration in ambient dry air for the calculation of air density, Metrologia, 44, 448–452, 2007.
Tans, P. P., Crotwell, A. M., and Thoning, K. W.: Abundances of isotopologues and calibration of CO2 greenhouse gas measurements, Atmos. Meas. Tech., 10, 2669–2685, https://doi.org/10.5194/amt-10-2669-2017, 2017.
Trolier, M., White, J. W. C., Tans, P. P., Masarie, K. A., and Gemery, P. A.: Monitoring the isotopic composition of atmospheric CO2: Measurements from the NOAA Global Air Sampling Network, J. Geophys. Res.-Atmos., 101, 25897–25916, https://doi.org/10.1029/96JD02363, 1996.
WMO: 19th WMO/IAEA Meeting on Carbon Dioxide, Other Greenhouse Gases and Related Tracers Measurement Techniques (GGMT-2017), Geneva, Switzerland, 2018.
Zhao, C. L., Tans, P. P., and Thoning, K. W.: A high precisionmanometric systemfor absolutecalibrations of CO2 in dry air, J. Geophys. Res., 102, 5885–5894, 1997.
Zhao, C. L. and Tans, P. P.: Estimating uncertainty of the WMO mole fraction scale for carbon dioxide in air, J. Geophys. Res., 111, https://doi.org/10.1029/2005JD006003, 2006.