618-13 Using FTIR to Measure Greenhouse Gas Emissions from Agricultural Sources.

See more from this Division: A03 Agroclimatology & Agronomic Modeling
See more from this Session: Symposium --Integrating Instrumentation, Modeling, and Remote Sensing in Honor of John Norman

Tuesday, 7 October 2008: 2:30 PM
George R. Brown Convention Center, 362DE

Owen Denmead1, David W.T. Griffith2, Glenn Bryant2, Stephen Wilson2, Travis Naylor2, Mei Bai3, Ben C.T. Macdonald4 and Barry Salter5, (1)CSIRO, Canberra, Australia
(2)Chemistry, Univ. of Wollongong, Wollongong, Australia
(3)Chemistry, University of Wollongong, Wollongong, Australia
(4)The Fenner School of Environment and Society, Australian National Univ., Canberra, Australia
(5)Central Experiment Station, BSES Limited, Mackay, Australia
Abstract:
Inventory improvement and the development of regulatory measures, trading options and mitigation strategies for greenhouse gas emissions all require precise measurements of atmospheric concentrations and fluxes of greenhouse gases.  The main emissions from agriculture are those of CH4, N2O, CO2 and the indirect greenhouse gas NH3.  Fourier Transform Infrared (FTIR) Spectroscopy identifies and quantifies concentrations of infrared absorbing gases by examining transmission spectra from a broad-band infrared source and using a non-linear least-squares algorithm that iteratively calculates the spectrum from a database of spectral line parameters until best fit to the recorded spectrum is obtained.  The relative precision (1std) of the measurements is 0.1–0.2%, giving 1std errors in CH4, N2O, CO2 and NH3 measurements of around 4 ppb, 0.5ppb, 1ppm and 0.5ppb respectively.  Attractions of FTIR spectroscopy are that it can measure the concentrations of all the infrared gases of interest simultaneously and it can be employed in both closed- and open-path systems.  Closed path systems are used for chamber, flux-gradient and backward Lagrangian stochastic dispersion (bLs) techniques of flux measurement and open-path systems are employed for measurement of fluxes from small, well-defined source areas such as feedlots, fertilised fields and grazed pastures, using the bLs technique.  The use of FTIR spectroscopy in both systems will be discussed.

See more from this Division: A03 Agroclimatology & Agronomic Modeling
See more from this Session: Symposium --Integrating Instrumentation, Modeling, and Remote Sensing in Honor of John Norman