Abstract
A dynamic chamber method was developed to measure fluxes of N2O from soils with greater accuracy than
previously possible, through the use of a quantum cascade laser (QCL). The dynamic method was compared
with the conventional static chamber method, where samples are analysed subsequently on a gas chromatograph.
Results suggest that the dynamic method is capable of measuring soil N2O fluxes with an uncertainty of typically
less than 1–2 μgN2O-Nm−2 hour−1 (0.24–0.48 gN2O-N ha−1 day−1), much less than the conventional static
chamber method, because of the greater precision and temporal resolution of the QCL. The continuous record
of N2O and CO2 concentration at 1 Hz during chamber closure provides an insight into the effects that enclosure
time and the use of different regression methods may introduce when employed with static chamber systems
similar in design. Results suggest that long enclosure times can contribute significantly to uncertainty in chamber
flux measurements. Non-linear models are less influenced by effects of long enclosure time, but even these do
not always adequately describe the observed concentrations when enclosure time exceeds 10 minutes, especially
with large fluxes.
Original language | English |
---|---|
Pages (from-to) | 643 - 652 |
Number of pages | 10 |
Journal | European Journal of Soil Science |
Volume | 65 |
Issue number | 5 |
DOIs | |
Publication status | Print publication - 2014 |
Bibliographical note
2047560Keywords
- Flux
- Gas chromatograph
- Nitrogen dioxide
- Quantum cascade laser
- Soil