Measurements of N 2 O fluxes from fertilized grassland using a fast response tunable diode laser spectrometer
Author(s) -
Wienhold F. G.,
Frahm H.,
Harris G. W.
Publication year - 1994
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/93jd03279
Subject(s) - spectrometer , eddy covariance , anemometer , laser , time delay and integration , optics , environmental science , analytical chemistry (journal) , physics , computational physics , remote sensing , wind speed , chemistry , meteorology , geology , chromatography , ecology , ecosystem , biology
A fast response tunable diode laser spectrometer was used to make N 2 O flux measurements by both eddy correlation and concentration gradient techniques during a methods intercomparison field program in April 1992 at a site in Stirling, Scotland. A description of the site and the results of the intercomparison are presented in companion papers. Sufficient instrumental precision and time resolution for N 2 O flux determination using both techniques were obtained by application of the recently developed two‐tone frequency modulation coupled with fast scanning of the laser. The use of a dedicated digital signal processor allowed zero‐overhead on‐line data handling at a rate of 10 Hz such that the time response of the system was only limited by the gas exchange time in the multipass sample cell (200 ms). Vertical concentration gradients that lead to a difference of ≤1 part per billion by volume in the N 2 O mixing ratio at 0.06‐ and 1.05‐m elevation were statistically resolved within 1 min. Eddy correlation measurements with intake heights of 2.25 m and 2.75 m were made in conjunction with two different sonic anemometers. The software developed for reduction and analysis of the 10‐Hz eddy correlation data was based on time efficient FFT methods and performed time‐base matching of the data set, drift correction, coordinate rotation, and evaluation of the covariances and the frequency power distributions. N 2 O fluxes determined with this technique were in the range of 38–113 ng N m −2 s −1 . An unusual shape of the N 2 O concentration covariance function can be ascribed to fetch inhomogeneities, and we conclude that the eddy correlation data set contains information that can be used to characterize the spatial variability in N 2 O emission in addition to its spatial integral.
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