Abstract

Abstract. Atmospheric trace gases such as dihydrogen (H2), carbon monoxide (CO) and methane (CH4) play important roles in microbial metabolism and biogeochemical cycles. Analysis of these gases at trace levels requires reliable storage of discrete samples of low volume. While commercial sampling vials such as Exetainers® have been tested for CH4 and other greenhouse gases, no information on reliable storage is available for H2 and CO. We show that vials sealed with butyl rubber stoppers are not suitable for storing H2 and CO due to release of these gases from rubber material. Treating butyl septa with NaOH reduced trace-gas release, but contamination was still substantial, with H2 and CO mixing ratios in air samples increasing by a factor of 3 and 10 after 30 d of storage in conventional 12 mL Exetainers. All tested materials showed a near-linear increase in H2 and CO mixing ratios, indicating a zero-order reaction and material degradation as the underlying cause. Among the rubber materials tested, silicone showed the lowest potential for H2 and CO release. We thus propose modifying Exetainers by closing them with a silicone plug to minimise contamination and sealing them with a stainless-steel bolt and O-ring as a secondary diffusion barrier for long-term storage. Such modified Exetainers exhibited stable mixing ratios of H2 and CH4 exceeding 60 d of storage at atmospheric and elevated (10 ppm) mixing ratios. The increase of CO was still measurable but was 9 times lower than in conventional Exetainers with treated septa; this can be corrected for due to its linearity by storing a standard gas alongside the samples. The proposed modification is inexpensive, scalable and robust, and thus it enables reliable storage of large numbers of low-volume gas samples from remote field locations.

Highlights

  • Dihydrogen (H2) and carbon monoxide (CO) are trace gases present in the atmosphere at 0.53 ppm and approximately 0.15 ppm (Ehhalt and Rohrer, 2009; Petrenko et al, 2013)

  • The gas chromatography system (GC) is field-deployable and measurements can be conducted in situ, which eliminates the problem of gas storage altogether (King and Weber, 2008; Meredith et al, 2017)

  • Our results clearly demonstrate that commercially available gas-sample vials sealed with butyl rubber are not suited for the storage of gas samples with trace levels of H2 and CO

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Summary

Introduction

Dihydrogen (H2) and carbon monoxide (CO) are trace gases present in the atmosphere at 0.53 ppm and approximately 0.15 ppm (Ehhalt and Rohrer, 2009; Petrenko et al, 2013). They are important intermediates in numerous biogeochemical reactions, with environmental equilibrium concentrations kept at trace levels by tightly controlled production and consumption reactions (Hoehler et al, 1998; Khalil and Rasmussen, 1990). A field laboratory or shipboard setup may allow for short-term (minutes to hours) storage of samples in syringes or gas-tight sampling bags

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