Preparation of primary standard mixtures for atmospheric oxygen measurements with less than 1&thinsp;µmol&thinsp;mol<sup>−1</sup> uncertainty for oxygen molar fractions

<p>Precise monitoring of changes in atmospheric <span class="inline-formula">O<sub>2</sub></span> levels was implemented by preparing primary standard mixtures with less than 1&thinsp;<span class="inline-formula">µ</span>mol&thins...

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Bibliographic Details
Main Authors: N. Aoki, S. Ishidoya, N. Matsumoto, T. Watanabe, T. Shimosaka, S. Murayama
Format: Article
Language:English
Published: Copernicus Publications 2019-05-01
Series:Atmospheric Measurement Techniques
Online Access:https://www.atmos-meas-tech.net/12/2631/2019/amt-12-2631-2019.pdf
Description
Summary:<p>Precise monitoring of changes in atmospheric <span class="inline-formula">O<sub>2</sub></span> levels was implemented by preparing primary standard mixtures with less than 1&thinsp;<span class="inline-formula">µ</span>mol&thinsp;mol<span class="inline-formula"><sup>−1</sup></span> standard uncertainty for <span class="inline-formula">O<sub>2</sub></span> molar fractions. In this study, these mixtures were crafted in 10&thinsp;L high-pressure aluminium alloy cylinders using a gravimetric method in which unknown uncertainty factors were theoretically determined and subsequently reduced. Molar fractions of the constituents (<span class="inline-formula">CO<sub>2</sub></span>, Ar, <span class="inline-formula">O<sub>2</sub></span>, and <span class="inline-formula">N<sub>2</sub></span>) in the primary standard mixtures were mainly resolved using masses of the respective source gases (<span class="inline-formula">CO<sub>2</sub></span>, Ar, <span class="inline-formula">O<sub>2</sub></span>, and <span class="inline-formula">N<sub>2</sub></span>) that had been filled into the cylinders. To precisely determine the masses of the source gases, the difference in mass of the cylinder before and after filling the respective source gas was calculated by comparison with an almost identical reference cylinder. Although the masses of the cylinders filled with the source gas with respect to the reference cylinder tended to deviate in relation to temperature differences between the source-gas-filled cylinder and surrounding air, the degree of the deviation could be efficiently reduced by measuring the two cylinders at the exact same temperature. The standard uncertainty for the cylinder mass obtained in our weighing system was determined to be 0.82&thinsp;mg. The standard uncertainties for the <span class="inline-formula">O<sub>2</sub></span> molar fractions in the primary standard mixtures ranged from 0.7 to 0.8&thinsp;<span class="inline-formula">µ</span>mol&thinsp;mol<span class="inline-formula"><sup>−1</sup></span>. Based on the primary standard mixtures, the annual average molar fractions of atmospheric <span class="inline-formula">O<sub>2</sub></span> and Ar in 2015 at Hateruma island, Japan, were found to be <span class="inline-formula">209339.1±1.1</span> and <span class="inline-formula">9334.4±0.7</span>&thinsp;<span class="inline-formula">µ</span>mol&thinsp;mol<span class="inline-formula"><sup>−1</sup></span>, respectively. The molar fraction for atmospheric Ar was in agreement with previous reports.</p>
ISSN:1867-1381
1867-8548