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Inter-comparison of O2/N2 Ratio Scales Among AIST, NIES, TU, and SIO Based on Round-Robin Using Gravimetric Standard Mixtures.

Authors :
Nobuyuki Aoki
Shigeyuki Ishidoya
Yasunori Tohjima
Shinji Morimoto
Keeling, Ralph F.
Cox, Adam
Shuichiro Takebayashi
Shohei Murayama
Source :
Atmospheric Measurement Techniques Discussions; 1/6/2021, p1-26, 26p
Publication Year :
2021

Abstract

A study was conducted to compare the d(O<subscript>2</subscript>/N<subscript>2</subscript>) scales used by four laboratories engaged in atmospheric d(O<subscript>2</subscript>/N<subscript>2</subscript>) measurements. These laboratories are the Research Institute for Environmental Management Technology, Advanced Industrial Science and Technology (EMRI/AIST), the National Institute for Environmental Studies (NIES), Tohoku University (TU), and Scripps Institution of Oceanography (SIO). Therefore, five high-precision standard mixtures for O<subscript>2</subscript> molar fraction gravimetrically prepared by the National Metrology Institute of Japan (NMIJ), AIST (NMIJ/AIST) with a standard uncertainty of less than 5 per meg were used as round-robin standard mixtures. EMRI/AIST, NIES, TU, and SIO reported the analysed values of the standard mixtures on their own d(O<subscript>2</subscript>/N<subscript>2</subscript>) scales, and the values were compared with the d(O<subscript>2</subscript>/N<subscript>2</subscript>) values gravimetrically determined by NMIJ/AIST (the NMIJ/AIST scale). The d(O<subscript>2</subscript>/N<subscript>2</subscript>) temporal drift in the five standard mixtures during the inter-comparison experiment was corrected based on the d(O<subscript>2</subscript>/N<subscript>2</subscript>) values analysed before and after the experiments by EMRI/AIST. The scales are compared based on offsets in zero and span. The span offsets from the NMIJ/AIST scale ranged from -0.17% to 3.3%, corresponding with the difference of 0.29 Pg yr<superscript>-1</superscript> in the estimates for land biospheric and oceanic CO<subscript>2</subscript> uptakes. The zero offsets from the NMIJ/AIST scale are -581.0 ± 2.2, -221.4 ± 3.1, -243.0 ± 3.0, and -50.7 ± 2.4 per meg for EMRI/AIST, TU, NIES, and SIO, respectively. The atmospheric d(O<subscript>2</subscript>/N<subscript>2</subscript>) values observed at Hateruma Island (HAT; 24.05°N, 123.81°E), Japan, by EMRI/AIST and NIES became comparable by converting their scales to the NMIJ/AIST scale. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
18678610
Database :
Complementary Index
Journal :
Atmospheric Measurement Techniques Discussions
Publication Type :
Academic Journal
Accession number :
147981202
Full Text :
https://doi.org/10.5194/amt-2020-481