2020
DOI: 10.1002/jpln.201900493
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Application of a low‐cost NDIR sensor module for continuous measurements of in situ soil CO2 concentration

Abstract: We tested the performance of a newly developed CO 2 probe, K33SOIL [based on the sensor module K33 (Senseair, Sweden)], under harsh temperature and humidity conditions in a laboratory experiment. The K33SOIL, competed well (RMSE = 0.032% CO 2) with the often used GMP343 (Vaisala, Finland) in precision and accuracy. A field experiment showed that the K33SOIL is also suitable for in situ applications. Thus, the K33SOIL is a valuable and cost-efficient tool for measurement of soil CO 2 concentration.

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Cited by 5 publications
(2 citation statements)
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“…Several research groups (Jassal et al, 2005;Hirano, 2003;Tang et al, 2003) used compact nondispersive infrared (NDIR) CO 2 sensors to install them directly in the soil after this technology became available. The availability of low-cost microcontrollers and NDIR sensors stimulates further applications in soil gas research (Blackstock et al, 2019;Heger et al, 2020).…”
Section: Introductionmentioning
confidence: 99%
“…Several research groups (Jassal et al, 2005;Hirano, 2003;Tang et al, 2003) used compact nondispersive infrared (NDIR) CO 2 sensors to install them directly in the soil after this technology became available. The availability of low-cost microcontrollers and NDIR sensors stimulates further applications in soil gas research (Blackstock et al, 2019;Heger et al, 2020).…”
Section: Introductionmentioning
confidence: 99%
“…We assumed that the manometric procedure could be improved by the recent development of low‐cost CO 2 sensors and microcontrollers (e.g. Greenspan et al., 2016; Harmon et al., 2015; Heger et al., 2020), and adapted to also measure DIC. The new device was used to test the following research hypotheses: (a) the calcite‐specific surface area (SSA, calcite RSA per weight of calcite) should increase over the ecological succession of biocrusts due to a gradual increase in small‐size secondary carbonates during soil development; (b) the colonization of the soil by lichens and plants should decrease the CCE due to their ability to enhance mineral weathering and (c) in a spring‐cave‐downstream river continuum, the DIC content should increase progressively due to the enhanced dissolution of CO 2 in CO 2 ‐rich caves, combined with the accumulation of aqueous carbonate species during CaCO 3 weathering.…”
Section: Introductionmentioning
confidence: 99%