Characterising the methane gas and environmental response of the Figaro Taguchi Gas Sensor (TGS) 2611-E00
In efforts to improve methane source characterisation, networks of cheap high-frequency in situ sensors are required, with parts-per-million-level methane mole fraction ([CH4]) precision. Low-cost semiconductor-based metal oxide sensors, such as the Figaro Taguchi Gas Sensor (TGS) 2611-E00, may sati...
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Veröffentlicht in: | Atmospheric measurement techniques 2023-07, Vol.16 (13), p.3391-3419 |
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Zusammenfassung: | In efforts to improve methane source characterisation, networks of cheap high-frequency in situ sensors are required, with parts-per-million-level methane mole fraction ([CH4]) precision. Low-cost semiconductor-based metal oxide sensors, such as the Figaro Taguchi Gas Sensor (TGS) 2611-E00, may satisfy this requirement. The resistance of these
sensors decreases in response to the exposure of reducing gases, such as
methane. In this study, we set out to characterise the Figaro TGS 2611-E00
in an effort to eventually yield [CH4] when deployed in the field. We
found that different gas sources containing the same ambient 2 ppm
[CH4] level yielded different resistance responses. For example,
synthetically generated air containing 2 ppm [CH4] produced a lower
sensor resistance than 2 ppm [CH4] found in natural ambient air due to possible interference from supplementary reducing gas species in ambient
air, though the specific cause of this phenomenon is not clear. TGS 2611-E00
carbon monoxide response is small and incapable of causing this effect. For
this reason, ambient laboratory air was selected as a testing gas standard
to naturally incorporate such background effects into a reference
resistance. Figaro TGS 2611-E00 resistance is sensitive to temperature and
water vapour mole fraction ([H2O]). Therefore, a reference resistance
using this ambient air gas standard was characterised for five sensors (each inside its own field logging enclosure) using a large environmental chamber, where logger enclosure temperature ranged between 8 and
38 ∘C and [H2O] ranged between 0.4 % and 1.9 %.
[H2O] dominated resistance variability in the standard gas. A linear
[H2O] and temperature model fit was derived, resulting in a
root mean squared error (RMSE) between measured and modelled resistance in
standard gas of between ±0.4 and ±1.0 kΩ
for the five sensors, corresponding to a fractional resistance uncertainty
of less than ±3 % at 25 ∘C and 1 % [H2O]. The TGS 2611-E00 loggers were deployed at a landfill site for 242 d before and
96 d after sensor testing. Yet the standard (i.e. ambient air) reference
resistance model fit based on temperature and [H2O] could not replicate
resistance measurements made in the field, where [CH4] was mostly
expected to be close to the ambient background, with minor enhancements.
This field disparity may have been due to variability in sensor cooling
dynamics, a difference in ambient air composition during environmental
chamber testing compared to |
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ISSN: | 1867-8548 1867-1381 1867-8548 |
DOI: | 10.5194/amt-16-3391-2023 |