scholarly journals Application of a low-cost NDIR sensor module for continuous measurements of in situ soil CO2 concentration

Author(s):  
Adrian Heger ◽  
Volker Kleinschmidt ◽  
Alexander Gröngröft ◽  
Lars Kutzbach ◽  
Annette Eschenbach
2020 ◽  
Author(s):  
Adrian Heger ◽  
Volker Kleinschmidt ◽  
Alexander Gröngröft ◽  
Lars Kutzbach ◽  
Annette Eschenbach

<p>We applied the low-cost non-dispersive infrared sensor module K33 (ICB, Senseair, Sweden) for measurements of soil CO<sub>2</sub> concentration. We integrated the sensor module in a new soil probe suitable for in situ measurements of soil gas CO<sub>2</sub> concentration. Therefore, we covered the sensor module with epoxy resin. For continuous measurements, we connected our soil CO<sub>2</sub> probe to a microcontroller (MEGA 2560 Rev3, Arduino.cc, Italy) equipped with a data logging shield (Adalogger FeatherWing, Adafruit, USA). In a laboratory experiment, we evaluated the accuracy and precision of our soil CO<sub>2</sub> probe at changing temperature and humidity by comparison with the often used CO<sub>2</sub> probe GMP343 (Vaisala, Finland) as a reference. In a field experiment, we buried our soil CO<sub>2</sub> probe to test its performance under natural environmental conditions.</p><p>The result of the laboratory experiment is that our soil CO<sub>2</sub> probe compares well with the GMP343, even at maximum relative humidity. The accuracy (<0.1 % CO<sub>2</sub>) was below the accuracy given by the manufacturer. The field experiment demonstrated that our soil CO<sub>2</sub> probe provides high-quality measurements of soil CO<sub>2</sub> concentrations under in situ soil conditions. After retrieving it, it still measured with the same accuracy and precision as before.</p><p>In summary, we used the sensor module K33 for the first time to measure in situ soil CO<sub>2</sub> concentrations by integrating it into a newly developed probe. The cost-efficient availability of our CO<sub>2</sub> probe opens up the opportunity to carry out continuous soil CO<sub>2</sub> measurements over long time periods with simultaneously high spatial resolution.</p>


2020 ◽  
Vol 148 (3) ◽  
pp. 255-269 ◽  
Author(s):  
Kyungjin Min ◽  
Asmeret Asefaw Berhe ◽  
Chau Minh Khoi ◽  
Hella van Asperen ◽  
Jeroen Gillabel ◽  
...  

CATENA ◽  
2020 ◽  
Vol 185 ◽  
pp. 104280
Author(s):  
Min Cao ◽  
Yongjun Jiang ◽  
Yu Chen ◽  
Jiaxin Fan ◽  
Qiufang He

2019 ◽  
Vol 375 ◽  
pp. 43-56 ◽  
Author(s):  
M. Poret ◽  
A. Finizola ◽  
T. Ricci ◽  
G.P. Ricciardi ◽  
N. Linde ◽  
...  

1997 ◽  
Vol 20 (12) ◽  
pp. 1495-1505 ◽  
Author(s):  
T. J. BOUMA ◽  
K. L. NIELSEN ◽  
D. M. EISSENSTAT ◽  
J. P. LYNCH

2018 ◽  
Author(s):  
Jobin Joseph ◽  
Christoph Külls ◽  
Matthias Arend ◽  
Marcus Schaub ◽  
Frank Hagedorn ◽  
...  

Abstract. The short-term dynamics of carbon and water fluxes across the soil–plant–atmosphere continuum are still not fully understood. One important constraint is the lack of methodologies that enable simultaneous measurements of soil CO2 concentration and its isotopic composition at a high temporal resolution for longer periods of time. δ13C of soil CO2 can be used to derive information on the origin and physiological history of carbon and δ18O in soil CO2 aids to infer interaction between CO2 and soil water. We established a real-time method for measuring soil CO2 concentration, δ13C and δ18O values across a soil profile at higher temporal resolutions up to 1 Hz using an Off-Axis Integrated Cavity Output Spectrometer (OA-ICOS). We also developed a calibration method correcting for the sensitivity of the device against concentration-dependent shifts in δ13C and δ18O values under highly varying CO2 concentration. The deviations of measured data were modelled, and a mathematical correction model was developed and applied for correcting the shift. By coupling an OA-ICOS with hydrophobic but gas permeable membranes placed at different depths in acidic and calcareous soils, we investigated the contribution of abiotic and biotic components to total soil CO2 release. We found that in the calcareous Gleysol, CO2 originating from carbonate dissolution contributed to the total soil CO2 concentration at detectable degrees probably due to CO2 evasion from groundwater. Inward diffusion of atmospheric CO2 was found to be rather pronounced in the topsoil layers at both sites. No specific pattern was identified for δ18O in soil CO2 at the calcareous site, δ18O values reflected fairly well the δ18O of soil water at the acidic soil site.


SOIL ◽  
2019 ◽  
Vol 5 (1) ◽  
pp. 49-62 ◽  
Author(s):  
Jobin Joseph ◽  
Christoph Külls ◽  
Matthias Arend ◽  
Marcus Schaub ◽  
Frank Hagedorn ◽  
...  

Abstract. The short-term dynamics of carbon and water fluxes across the soil–plant–atmosphere continuum are still not fully understood. One important constraint is the lack of methodologies that enable simultaneous measurements of soil CO2 concentration and respective isotopic composition at a high temporal resolution for longer periods of time. δ13C of soil CO2 can be used to derive information on the origin and physiological history of carbon, and δ18O in soil CO2 aids in inferring the interaction between CO2 and soil water. We established a real-time method for measuring soil CO2 concentration, δ13C and δ18O values across a soil profile at higher temporal resolutions (0.05–0.1 Hz) using an off-axis integrated cavity output spectroscopy (OA-ICOS). We also developed a calibration method correcting for the sensitivity of the device against concentration-dependent shifts in δ13C and δ18O values under highly varying CO2 concentration. The deviations of measured data were modelled, and a mathematical correction model was developed and applied for correcting the shift. By coupling an OA-ICOS with hydrophobic but gas-permeable membranes placed at different depths in acidic and calcareous soils, we investigated the contribution of abiotic and biotic components to total soil CO2 release. We found that in the calcareous Gleysol, CO2 originating from carbonate dissolution contributed to the total soil CO2 concentration at detectable degrees, potentially due to CO2 evasion from groundwater. The 13C-CO2 of topsoil at the calcareous soil site was found reflect δ13C values of atmospheric CO2, and the δ13C of topsoil CO2 at the acidic soil site was representative of the biological respiratory processes. δ18O values of CO2 in both sites reflected the δ18O of soil water across most of the depth profile, except for the 80 cm depth at the calcareous site where a relative enrichment in 18O was observed.


2012 ◽  
Vol 63 (2) ◽  
pp. 261-271 ◽  
Author(s):  
N. Goutal ◽  
F. Parent ◽  
P. Bonnaud ◽  
J. Demaison ◽  
G. Nourrisson ◽  
...  

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