Estimation of Soil Respiration: Techniques for Measurement of Soil Gas

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Estimation of soil respiration: Techniques for measurement of soil gas Mark Blonquist Apogee Instruments Bruce Bugbee Utah State University Scott Jones Utah State University Two methods for soil respiration measurement Soil surface flux Gradient flux (chambers): (buried sensors): • widely used • not commercially available • commercially available ($3,000-$15,000) ($15,000-60,000) • provides subsurface data • must account for altered boundary • requires diffusion coefficient layer • challenging to measure sub- • doesn’t need diffusion coefficient surface gas concentration Photo from LI-COR Biosciences Photo from Turcu et al. (2003) Respiration: CH2O + O2 CO2 + H2O 20.95% 0.04% Advantage of O2 = 20.95% = 520 x CO = 0.04% measuring CO2 2 Advantage of 1 – No bicarbonate effects measuring O2 2 – Low cost (approx. $300 vs. $900) Once physical effects are accounted for, relationship between C flux and C metabolized (respiration) is 1:1 Respiratory quotient: CO2 / O2 Carbohydrate RQ = 1.0 Protein RQ = 0.8 Fat RQ = 0.6 Lignin RQ = 0.2 Nitrification: RQ = 0.0 + NH4 + 2O2 NO3 + 2H + H2O Two ways to express gas concentration Absolute Units Relative Units • partial pressure • percent gas in air [kPa] [%] • moles of gas per unit volume • mole fraction [mol m-3] [kPa kPa-1 air] • mass of gas per unit volume • parts per million [g m-3] [ppm] Gas sensors respond to absolute concentration, but are generally calibrated to read relative units Factors affecting gas concentration in soil • Barometric Pressure Factors affecting gas concentration in soil • Barometric pressure • Humidity (function of temperature) H2O Factors affecting gas concentration in soil • Pressure • Humidity • Temperature • effect on molar density and sensor electronics • gas / liquid partitioning Pure CO2 is 30 times more soluble in water than Pure O2 100 % CO2 100 % O2 Solubility is roughly equal when CO2 concentration is 0.6 % CO2 O2 Conclusions • Gradient flux approach warrants further consideration; in situ gas measurements need appropriate correction to account for physically-based fluxes • O2 measurements provide a useful supplement to CO2 measurements .

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