Pure gases and mixtures containing
stable isotopes are used in
a wide variety of applications including health care, food authentication,
geochemistry, and environmental monitoring. It is therefore important
to understand the role of moisture, which is one of the most critical
impurities in compressed gas mixtures and pure gases, in their stability.
Gaseous carbon dioxide (CO
2
) was used as a proxy for the
evaluation of the effects of its isotopic composition, when in contact
with moisture throughout the depletion of a cylinder’s contents,
as well as pressure regulation and long-term stability. To accentuate
the detrimental effects of moisture on CO
2
isotopic stability,
enriched
18
O-water was added to natural-abundance, gaseous
carbon dioxide. The δ
18
O–CO
2
changed
from −23.16‰ vs Vienna Pee Dee Belemnite (VPDB) to +109‰
vs VPDB. It was further demonstrated that with appropriate cylinder
preparation to reduce residual moisture, source material purity with
low moisture content, and pressure regulation (from 57.0 down to 0.5
bar), both δ
13
C and δ
18
O remained
consistent within ±0.04 and ±0.06‰, respectively,
throughout the entire cylinder contents. Pressure reduction using
a dual-stage regulator yielded statistically consistent results at
the 99% confidence level from delivered pressures of 0.1–0.8
bar. Furthermore, the isotopic values remained consistent during a
1 year shelf-life study, illustrating the ability to utilize and regulate
pressurized gases as working reference standard gases.