1983
DOI: 10.1016/0002-1571(83)90065-1
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Verification of a simple micrometeorological method for estimating the rate of gaseous mass transfer from the ground to the atmosphere

Abstract: Wilson, J.D., Catchpole, V.R., Denmead, O.T. and Thurtell, G.W., 1983. Verification of a simple micrometeorological method for estimating the rate of gaseous mass transfer from the ground to the atmosphere. Agric. Meteorol., 29: 183--189.Wilson et al. proposed a simple micrometeorological method of estimating the rate of gaseous mass transfer to the atmosphere from a small circular plot which required measurements of time-average species-concentration and horizontal windspeed at a single height. This method ha… Show more

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Cited by 105 publications
(67 citation statements)
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“…In order to be independent of wind direction, it is usually used with slurry spread onto circular plots (Denmead, 1983;Wilson et al, 1983;Denmead and Raupach, 1993). With a mast in the centre of the circle with radius X R , the horizontal (advection) flux F of the upwind emitted NH 3 is determined from the measured vertical (z) profiles of concentration (c) and horizontal wind speed (u):…”
Section: Integrated Horizontal Flux Approachmentioning
confidence: 99%
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“…In order to be independent of wind direction, it is usually used with slurry spread onto circular plots (Denmead, 1983;Wilson et al, 1983;Denmead and Raupach, 1993). With a mast in the centre of the circle with radius X R , the horizontal (advection) flux F of the upwind emitted NH 3 is determined from the measured vertical (z) profiles of concentration (c) and horizontal wind speed (u):…”
Section: Integrated Horizontal Flux Approachmentioning
confidence: 99%
“…Lockyer, 1984) and the integrated horizontal flux (IHF) measurement technique (Wilson et al, 1983;Denmead, 1995). Wind tunnel measurements are generally performed on a small-scale plots (<10 m 2 ), while the IHF is applied on medium-scale circular plots between 20 m and 50 m radius.…”
Section: Introductionmentioning
confidence: 99%
“…The integrated horizontal flux method (Beauchamp et al, 1978;Wilson et al, 1983;Wilson & Shun, 1992) is a relatively simple micrometeorological method that can be used to estimate the rate of gas transfer from the ground to the atmosphere. The method requires a small circular plot (radius f50 m) in which the average horizontal wind speed ( -u s ) and concentration ( -c) profile are determined in the center of the plot in such a way that the average emission rate or upward vertical flux (F) can be determined as [28] Although this method cannot be used to determine fluxes from the atmosphere to the surface.…”
Section: Integrated Horizontal Mass Fluxmentioning
confidence: 99%
“…A simplification of the trajectory simulation model is the theoretical profile shape (TPS) technique (Wilson et al 1983). …”
Section: Theoretical Profile Shape Techniquementioning
confidence: 99%