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Soil Respiration / Soil CO2 Efflux Measurements in situ

Q-SR1LP Soil Respiration Package

Q-SR1LP Soil Respiration Package

Q-SR1LP Soil Respiration Package, for measurements of soil respiration and water loss under field conditions. This package also measures soil temperature, soil moisture and atmospheric pressure. The included battery pack provides ~11 hours of field use. Soil samples can be analysed in the laboratory by placing them in the included flow-through chamber. Due to its modularity, the SR1LP Soil Respiration System has a broad application spectrum. 

Soil Respiration Chamber
Q-G180 - Soil Respiration Chamber, with collar for field use

The Q-SR1LP uses the Q-S151 CO2 analyser to quantify soil respiration by measuring the rate of CO2 accumulation. Under field conditions, soil respiration (RS) is measured in situ by placing a chamber directly on the soil or prepared soil respiration rings (allowing for repeated measurements on the same location; optional). Soil temperature can be measured with the Q-S132 Temperature Probe, and soil water loss (evaporation) is measured with the internal Q-S161 Temperature/Relative Humidity Sensor. In addition, soil moisture can be measured with the included Q-S135 Soil Moisture Sensor. Measuring both soil moisture and temperature in conjunction with CO2 efflux measurements is key, as these are the two main abiotic factors affecting RS. Atmospheric pressure is automatically measured with an absolute pressure sensor (Q-S181) to achieve correct CO2 concentrations, while the Q-G266 flow monitor accurately regulates the gas flow through the system.

Alternatively to field campaigns, soil samples (sampled e.g. carefully into soil rings) can be transported to the laboratory for assessment using the included flow-through chamber (Q-G115); the chamber can be placed in a climate-controlled room/climate chamber/water bath for measurements under defined, stable temperature conditions. Continue reading

Analogue signals from all sensors and analysers are converted to digital signals via two built-in LabQuest mini interfaces and a single USB interface, for a total of 7 channels. Data can be viewed, recorded and manipulated on a PC or Mac using the included Logger Pro software (with experimental files for soil respiration measurements).

 

The modularity of the Q-Box SR1LP package leads to different applications in both open flow and closed gas exchange systems within its CO2 measurement range of 0-2000 ppm. The Q-SR1LP can measure CO2 exchange from any organism or sample placed in a flow chamber and even in aqueous suspensions (by bubbling air or N2 through the liquid and analysing the effluent gas).

Q-SR1LP Soil CO2 Package - Features

  • Self-contained gas analyser for in situ soil respiration measurements
  • Measures CO2 exchange of soil in a flow-through chamber in the laboratory
  • Soil moisture and temperature sensors included
  • Soil evaporation measurements
  • Modular system with replaceable and expandable components
  • Housed in a rugged case for easy transport and field use
  • Battery pack for 11 hours of field operation included
  • Dedicated software package

Options:

  • Soil collars for field placement (optional), customized
  • Custom (soil) Respiration Chambers (field and lab), optional
  • GF-500 Gas Flux Autosampler
Components Soil Respiration Package
Q-SR1LP
OPEN

 

Product No.  Description
Q-SR1LP Q-Box Soil Respiration Package Q-SR1LP, includes the following individual components:
Q-S151 CO2 IRGA Q-S151 (0-2000 ppm), includes CO2 and H2O scrubbers
Q-P103 Gas Pump, 1 L min-1
Q-G266 Flow Monitor (0-1 L per min)
Q-G180 Soil Chamber with Collar (10.2 cm x 20 cm high), field use
Q-G115 Flow Through Chamber (3.8 cm x 20 cm), for lab use
Q-S135 Soil Moisture Sensor
Q-S132 Temperature Probe
Q-S161 RH/Temperature Sensor
Q-S181 Absolute pressure sensor, with a single channel USB data interface (GoLink)
Q-G122 Gas Bags, large (2x 30 Liter)
Q-A249 Battery Pack and Charger
Q-C610 2x LabQuest Mini interface, integrated
Q-C901 Logger Pro Software
Q-C404 Customized Setup Software. Files
Q-SR1LP-Kit Q-Box Accessory Kit (tubing, connectors, seales, etc)
Q-SR1LP-Case Rugged water proof case, housing all sensors and analyzers
Q-SR1LP-Manual Manual
Q-SR1LP-Power Individual power supplies, for stand alone use of analysers and sensors
   
Optional  
Soil respiration collars Collars for permanent placement in the field (to place the respiration chamber Q-G180 on without repeated soil disturbance), custom material and dimensions, fixation hooks
Custom respiration chamber Custom soil respiration chambers, user defined material, dimensions and features
GF-500 Soil Respiration Autosampler, lab
References Q-SR1LP OPEN

  • Eaton WD, et al. (2012) The impact of Pentaclethra macroloba on soil microbial nitrogen fixing communities and nutrients within developing secondary forests in the Northern Zone of Costa Rica. Tropical Ecology 53:207-214
  • Li X, et al. (2015) Establishing microbial diversity and function in weathered and neutral Cu-Pb-Zn tailings with native soil addition. Geoderma 247-248: 108-116 doi: 10.1016/j.geoderma.2015.02.010
  • Prasad S, Baishya R (2019) Interactive effects of soil moisture and temperature on soil respiration under native and non-native tree species in semi-arid forest of Delhi, India. Tropical Ecology 60: 252-260. doi: 10.1007/s42965-019-00028-x
  • Robertson LM et al. (2020) Geochemical and mineralogical changes in magnetite Fe-ore tailings induced by biomass organic matter amendment. Science of the Total Environment 724: 138196 doi: 10.1016/j.scitotenv.2020.138196
  • Smorkalov IA, Vorobeichik EL (2015) The impact of a large industrial city on the soil respiration in forest ecosystems. Eurasian Soil Science 48:106-114. doi: 10.1134/S1064229315010147
  • Tomar U, Baishya R (2020) Seasonality and moisture regime control soil respiration, enzyme activities, and soil microbial biomass carbon in a semi-arid forest of Delhi, India. Ecological Processes 9: 50 doi: 10.1186/s13717-020-00252-7
  • You F, Dalal R, Huang L (2018) Biochar and biomass organic amendments shaped different dominance of lithoautotrophs and organoheterotrophs in microbial communities colonizing neutral copper (Cu)-molybdenum (Mo-gold (Au) tailings. Geoderma 309, 100-110. doi: 10.1016/j.geoderma.2017.09.010
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Contact us to receive the Q-SR1LP Soil Respiration Manual.



Why to measure Soil CO2 Efflux rates?

Measuring soil respiration and CO2 emission rates on site is crucial for comprehending and managing the intricate dynamics of carbon cycles in ecosystems. This phenomenon, whereby microorganisms respire and discharge carbon dioxide while decomposing organic matter, functions as an important interface between terrestrial ecosystems and the atmosphere. Continue reading

The significance of these measurements lies in their capacity to offer instantaneous insights into the carbon cycle of a given environment. Soil respiration indicates microbial activity, influencing carbon storage, and release. Scientists can evaluate the impacts of land-use changes, climate variations and management practices on carbon storage by measuring CO2 efflux rates.

Significantly, temporal variability in soil respiration rates offers insight. Recognising the fluctuations of respiration over time allows for the identification of seasonal patterns and the influence of climatic factors. This information assists in forecasting how ecosystems will react to future environmental alterations, leading to better-informed conservation and land management choices.

Additionally, soil respiration functions as a dependable gauge of soil health. Flourishing microbial communities active in decomposition assist in the recycling of nutrients, promoting plant growth and the overall vitality of the ecosystem. Monitoring respiration rates provides a valuable indicator of the biological activity within the soil, aiding the assessment of its resilience and ability to support diverse forms of life.

In summary, measuring soil respiration and CO2 efflux rates in situ is essential for unravelling the complexities of carbon cycling, evaluating temporal variations and determining the overall health of ecosystems. Such knowledge is essential for sustainable land management and preserving the fragile equilibrium between carbon sources and sinks in our dynamic environment.

References Soil Respiration
Methods and Application
OPEN

  • Barba, J., Cueva, A., Bahn, M., Barron-Gafford, G. A., Bond-Lamberty, B., Hanson, P. J., ... & Vargas, R. (2018). Comparing ecosystem and soil respiration: Review and key challenges of tower-based and soil measurements. Agricultural and Forest Meteorology, 249, 434-443.
  • Ben-Noah, I., & Friedman, S. P. (2018). Review and evaluation of root respiration and of natural and agricultural processes of soil aeration. Vadose Zone Journal, 17(1), 1-47.
  • Brændholt, A., Steenberg Larsen, K., Ibrom, A., & Pilegaard, K. (2017). Overestimation of closed-chamber soil CO2 effluxes at low atmospheric turbulence. Biogeosciences, 14(6), 1603-1616.
  • Hanson, P. J., Edwards, N. T., Garten, C. T., & Andrews, J. A. (2000). Separating root and soil microbial contributions to soil respiration: a review of methods and observations. Biogeochemistry, 48, 115-146.
  • Janssens, I. A., Dieleman, W., Luyssaert, S., Subke, J. A., Reichstein, M., Ceulemans, R., ... & Law, B. E. (2010). Reduction of forest soil respiration in response to nitrogen deposition. Nature geoscience, 3(5), 315-322.
  • Kuzyakov, Y. (2006). Sources of CO2 efflux from soil and review of partitioning methods. Soil biology and biochemistry, 38(3), 425-448.
  • Kuzyakov, Y., & Larionova, A. A. (2005). Root and rhizomicrobial respiration: a review of approaches to estimate respiration by autotrophic and heterotrophic organisms in soil. Journal of Plant Nutrition and Soil Science, 168(4), 503-520.
  • Mayer, M., Sandén, H., Rewald, B., Godbold, D. L., & Katzensteiner, K. (2017). Increase in heterotrophic soil respiration by temperature drives decline in soil organic carbon stocks after forest windthrow in a mountainous ecosystem. Functional Ecology, 31(5), 1163-1172.
  • Metcalfe, D. B., Fisher, R. A., & Wardle, D. A. (2011). Plant communities as drivers of soil respiration: pathways, mechanisms, and significance for global change. Biogeosciences, 8(8), 2047-2061.
  • Mei-Yee, C. H. I. N., LAU, S. Y. L., MIDOT, F., JEE, M. S., LO, M. L., SANGOK, F. E., & MELLING, L. (2023). Root exclusion methods for partitioning of soil respiration: Review and methodological considerations. Pedosphere, 33(5), 683-699.
  • Phillips, C. L., Bond-Lamberty, B., Desai, A. R., Lavoie, M., Risk, D., Tang, J., ... & Vargas, R. (2017). The value of soil respiration measurements for interpreting and modeling terrestrial carbon cycling. Plant and Soil, 413, 1-25.
  • Reichstein, M., & Beer, C. (2008). Soil respiration across scales: The importance of a model–data integration framework for data interpretation. Journal of Plant Nutrition and Soil Science, 171(3), 344-354.
  • Rochette, P., & Hutchinson, G. L. (2005). Measurement of soil respiration in situ: chamber techniques. Micrometeorology in agricultural systems, 47, 247-286.
  • Ryan, M. G., & Law, B. E. (2005). Interpreting, measuring, and modeling soil respiration. Biogeochemistry, 73, 3-27.
  • Schlesinger, W. H., & Andrews, J. A. (2000). Soil respiration and the global carbon cycle. Biogeochemistry, 48, 7-20.
  • Xu, M., & Shang, H. (2016). Contribution of soil respiration to the global carbon equation. Journal of plant physiology, 203, 16-28.

 


Gas Analyzers

For a large selection of individual gas flux components, see pages on Gas Analysers, Flow Monitors & Pumps, Pressure Sensors, and Gas Control Systems. 


Photosynthesis Measurements

For CO2 exchange measurements on plant leaves, consider the competitively priced Q-CO650 Plant Photosynthesis Package. 



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