Technical note: Facilitating the use of low-cost methane (CH<sub>4</sub>)
sensors in flux chambers – calibration, data processing, and an open
source make-it-yourself logger
Abstract:Abstract. A major bottleneck regarding the efforts to better quantify greenhouse gas fluxes, map sources and sinks, and understand flux regulation, is the shortage of low-cost and accurate-enough measurement methods. The studies of methane (CH4) – a long-lived greenhouse gas increasing rapidly but irregularly in the atmosphere for unclear reasons, and with poorly understood source-sink attribution – suffer from such method limitations. This study present new calibration and data processing approaches for use o… Show more
“…The Python code needs modifications for use with other data, and the CH 4 sensor data cannot represent results from other sensors as sensor-specific calibration is needed. The Arduino code for the CH 4 -CO 2 -RH-T logger described in the Supplement is available at http://urn.kb.se/resolve?urn=urn:nbn: se:liu:diva-162780 (Bastviken and Duc, 2020).…”
Abstract. A major bottleneck regarding the efforts to better quantify greenhouse gas fluxes, map sources and
sinks, and understand flux regulation is the shortage of low-cost and accurate-enough measurement
methods. The studies of methane (CH4) – a long-lived greenhouse gas increasing rapidly
but irregularly in the atmosphere for unclear reasons, and with poorly understood source–sink
attribution – suffer from such method limitations. This study presents new calibration and data
processing approaches for use of a low-cost CH4 sensor in flux chambers. Results show
that the change in relative CH4 levels can be determined at rather high accuracy in the
2–700 ppm mole fraction range, with modest efforts of collecting reference samples
in situ and without continuous access to expensive reference instruments. This opens
possibilities for more affordable and time-effective measurements of CH4 in flux
chambers. To facilitate such measurements, we also provide a description for building and using an
Arduino logger for CH4, carbon dioxide (CO2), relative humidity, and
temperature.
“…The Python code needs modifications for use with other data, and the CH 4 sensor data cannot represent results from other sensors as sensor-specific calibration is needed. The Arduino code for the CH 4 -CO 2 -RH-T logger described in the Supplement is available at http://urn.kb.se/resolve?urn=urn:nbn: se:liu:diva-162780 (Bastviken and Duc, 2020).…”
Abstract. A major bottleneck regarding the efforts to better quantify greenhouse gas fluxes, map sources and
sinks, and understand flux regulation is the shortage of low-cost and accurate-enough measurement
methods. The studies of methane (CH4) – a long-lived greenhouse gas increasing rapidly
but irregularly in the atmosphere for unclear reasons, and with poorly understood source–sink
attribution – suffer from such method limitations. This study presents new calibration and data
processing approaches for use of a low-cost CH4 sensor in flux chambers. Results show
that the change in relative CH4 levels can be determined at rather high accuracy in the
2–700 ppm mole fraction range, with modest efforts of collecting reference samples
in situ and without continuous access to expensive reference instruments. This opens
possibilities for more affordable and time-effective measurements of CH4 in flux
chambers. To facilitate such measurements, we also provide a description for building and using an
Arduino logger for CH4, carbon dioxide (CO2), relative humidity, and
temperature.
“…In case of missing temperature and RH for a given AFC (due to K33 ELG sensor malfunction), values of temperature and RH from the closest AFC and closest in time were used, assuming the same temperature and RH in both chambers. Afterward, each CH 4 sensor was calibrated separately by following a procedure described in detail in Bastviken et al (45) using background air concentrations under different humidity and well mixed atmospheric conditions (wind speed higher >2 m/s) as reference data. Finally, including volume and area of the chamber, CH 4 flux (μmol•m −2 •h −1 ) was calculated as a relative change in CH 4 levels in a chamber over time.…”
Lakes are considered the second largest natural source of atmospheric methane (CH4). However, current estimates are still uncertain and do not account for diel variability of CH4 emissions. In this study, we performed high-resolution measurements of CH4 flux from several lakes, using an automated and sensor-based flux measurement approach (in total 4,580 measurements), and demonstrated a clear and consistent diel lake CH4 flux pattern during stratification and mixing periods. The maximum of CH4 flux were always noted between 10:00 and 16:00, whereas lower CH4 fluxes typically occurred during the nighttime (00:00–04:00). Regardless of the lake, CH4 emissions were on an average 2.4 higher during the day compared to the nighttime. Fluxes were higher during daytime on nearly 80% of the days. Accordingly, estimates and extrapolations based on daytime measurements only most likely result in overestimated fluxes, and consideration of diel variability is critical to properly assess the total lake CH4 flux, representing a key component of the global CH4 budget. Hence, based on a combination of our data and additional literature information considering diel variability across latitudes, we discuss ways to derive a diel variability correction factor for previous measurements made during daytime only.
“…Based on existing knowledge of the expected air temperature variations at the in situ sampling point at the GrIS (Christiansen and Jørgensen, 2018), the humidity calibration was only carried out at a single temperature in this study. However, variations in the ambient air temperature are also expected to have a linear scaling effect for the type MOS system tested in this study (Bastviken et al, 2020;van den Bossche et al, 2017).…”
Section: Data Processingmentioning
confidence: 97%
“…Future tests should aim to investigate if the differences between the results from the laboratory and field calibration can be minimized by using the same type of datalogger and identical power supply (FX rechargeable lithium ion battery pack) both in the laboratory and in the field. Results from this type of test could reveal if field calibration for each individual MOS system is needed, similar to the approach in Bastviken et al (2020), or if batch calibrations of several identical MOS systems can be performed in the laboratory without the need for timeconsuming field calibration.…”
Section: Field Calibration Of the Metal Oxide Sensormentioning
confidence: 99%
“…One of the main obstacles previously reported concerning the use of MOSs for monitoring of gases in ambient air is the possible effect of variations in air temperature and humidity in the sampling environment (Bastviken et al, 2020;Eugster et al, 2019;Masson et al, 2015;Sohn et al, 2008). Different approaches exist to compensate for this potential measurement error and are related to post-correcting for variations in temperature and humidity, based on either generic temperature and humidity dependency curves supplied by the sensor company (Eugster and Kling, 2012).…”
Section: Post-correction and Cross-interference Evaluationmentioning
Abstract. In this paper, the performance of a low-cost and low-power methane
(CH4) sensing system prototype based on a metal oxide sensor (MOS)
sensitive to CH4 is tested in a natural CH4-emitting environment at the Greenland ice sheet (GrIS). We investigate if the MOS could be used as a supplementary measurement technique for monitoring CH4 emissions from the GrIS with the scope of setting up a CH4 monitoring network along the GrIS. The performance of the MOS is evaluated on the basis of simultaneous measurements using a cavity ring-down spectroscopy (CRDS) reference instrument for CH4 over a field calibration period of approximately 100 h. Results from the field calibration period show that CH4 concentrations measured with the MOS are in very good agreement with the reference CRDS. The absolute concentration difference between the MOS and the CRDS reference values within the measured concentration range of approximately 2–100 ppm CH4 was generally lower than 5 ppm CH4, while the relative concentration deviations between the MOS and the CRDS were generally below 10 %. The calculated root-mean-square error (RMSE) for the entire field calibration period was 1.69 ppm (n=37 140). The results confirm that low-cost and low-power MOSs can be effectively used for atmospheric CH4 measurements under stable water vapor conditions. The primary scientific importance of the study is that it provides a clear example of how the application of low-cost technology can enhance our future understanding on the climatic feedbacks from the cryosphere to the
atmosphere.
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