Atmospheric radiocarbon (14C) and CO2 mole fractions observed at Cape Ochiishi

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This dataset comprises radiocarbon ratios in atmospheric carbon dioxide (CO2), expressed as Δ14C, and CO2 mole fractions in air samples collected through monthly flask sampling at Cape Ochiishi, Japan, since 2004.

Description

Creator
Release date
2026/10/02
Temporal coverage
2004/07/14 - 2021/04/15
Data provider
NIES
Email: cgerdb_admin(at)nies.go.jp
DOI
File format
Data volume
17 KB
Version
ver.1.0 (Last updated: 2026/10/02)
Language
English

Data Set

Parameters
Δ14C, CO2 mole fraction
Observation period
2004/07/14 Start (ongoing)
Location
43.16028°N, 145.49739°E
Altitude
Elevation: 42.4 m
Sampling height: 51.5 m
Altitude: 93.9 m
Measurement method
Air samples have been collected every month since 2004 to observe background atmospheric 14CO2. The air samples were drawn from the inlet by a diaphragm pump. The air was then passed through a cold trap (–45°C) and collected in Pyrex glass flasks equipped with two glass stopcocks sealed by Viton O-rings at 0.2 MPa in gauge pressure, after a 10-min purge. CO2 mole fractions in the air samples were measured using a non-dispersive infrared gas analyzer (NDIR). CO2 was extracted from the remaining whole air in the flask by passing it through a vacuum line. Water vapor was removed using a spiral trap cooled to –110 °C, and CO2 was cryogenically trapped at –196 °C. The CO2 samples were subsequently converted into graphite by reduction with hydrogen over an iron catalyst at 650 °C. The 14C/C ratios were measured using Compact Carbon AMS (CAMS, National Electrostatics Corp., 1.5SDH). Samples collected before 2013 were analyzed at Paleo Labo Co., Ltd., Japan and those collected after 2013 at NIES.
Calculation method
The 14CO2 results were reported as Δ14C values relative to the OXII standard. Corrections were applied for radioactive decay between 1950 and the analysis date and mass-dependent fractionation using δ13C (normalized to −25‰) according to Stuiver and Polach (1977). Blank corrections were also applied. The Δ14C value and its uncertainty were calculated for each run, then final values were obtained by averaging repeated measurements. The analytical precision of Δ14C measurements (counting statistics and the standard deviation of OXII standards) was 2.1‰, ranging from 1.5‰ to 2.8‰. CO2 mole fractions were determined against four working standard gases calibrated to the NIES 09 CO2 standard scale (Machida et al., 2011). The analytical precision of CO2 mole fractions (the average value of standard deviations for working standard gases) was ~0.02 ppm.
Keywords
[GCMD_Platform]
Platforms > Land-based Platforms > Permanent Land Sites >GROUND STATIONS
[GCMD_Science]
EARTH SCIENCE > ATMOSPHERE > ATMOSPHERIC CHEMISTRY > CARBON AND HYDROCARBON COMPOUNDS > ATMOSPHERIC CARBON DIOXIDE > CARBON DIOXIDE SURFACE
[Free keywords]
Carbon Cycle
Update history
[2026/10/02]
The data from July 2004 to April 2021 have been compiled. Ver.1.0.

Contributors

Acknowledgements

Acknowledgements
This research was financially supported by the Global Environmental Research Coordination System from the Ministry of the Environment of Japan (E0955, E1451, E1951, and E2452) and the Environment Research and Technology Development Fund (JPMEERF24S12200) of the Environmental Restoration and Conservation Agency, provided by the Ministry of the Environment of Japan.

Reference Information

References
Terao Y., Mukai H., Niwa Y., Sasakawa M., Machida T., Tohjima Y. (2026) Contributions of Fossil Fuel and Biospheric CO2 Emissions to Seasonal and Interannual Variability of Δ14CO2 in the Background Atmosphere Observed at Hateruma Island and Cape Ochiishi, Japan (2004–2021), submitted to Tellus.

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         Terao Y., Mukai H., Sasakawa M. (2026), Atmospheric radiocarbon (14C) and CO2 mole fractions observed at Cape Ochiishi,  ver.x.x*1, NIES, DOI:10.17595/20261002.002. (Reference date*2: YYYY/MM/DD)
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