SLIDE 12 h = release height u = mean windspeed u* = RMS vertical air motion vs = sedimentation velocity u*/u = turbulence intensity, i
u*/u xpeak h
HIGH TURBULENCE
thin tail vs/u u
plume centreline
thick tail h
LOW TURBULENCE
u xpeak
h = release height u = mean windspeed u* = RMS vertical air motion vs = sedimentation velocity u*/u = turbulence intensity, i h = release height u = mean windspeed u* = RMS vertical air motion vs = sedimentation velocity u*/u = turbulence intensity, i
u*/u xpeak h
HIGH TURBULENCE
thin tail vs/u u
plume centreline
u*/u xpeak h
HIGH TURBULENCE
thin tail vs/u u
plume centreline
thick tail h
LOW TURBULENCE
u xpeak thick tail h
LOW TURBULENCE
u xpeak
Best Management Practice (BMP) for the Australian Cotton Industry
- getting pilots to understand the effect of the Australian summer Dusk Surface
Temperature Inversion (DUSTI), so they that they avoid spraying at dusk !
downwind deposition can be up to 20 times greater in highly stable conditions
http://www.depi.vic.gov.au/agriculture-and-food/farm-management/chemical-use/agricultural-chemical- use/spraying-spray-drift-and-off-target-damage/surface-temperature-inversions
Craig, I.P. 2004 The GDS model – a rapid computational technique for the calculation of aircraft spray drift buffer distances. Computers and Electronics in Agriculture 43 3 235-250