1989
DOI: 10.1002/ps.2780250109
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Assessment of canopy and ground deposits of fenitrothion following aerial and ground application in a northern ontario forest

Abstract: Spray deposit patterns on simulated and live foliage of balsam fir and white birch were determined at different heights and at periphery and interior locations of the tree crown, following aerial and ground applications of fenitrothion formulations over a boreal forest near Searchmont, Ontario. Droplet size spectra and AI deposits were assessed at ground level with ‘Kromekote’ card/glass plate units. Aerial application was made with a Cessna 188 aircraft fitted with ‘Micronair’ AU3000 atomizers. For ground app… Show more

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Cited by 10 publications
(10 citation statements)
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“…Such large differences could be due to differences in various operational parameters encountered during the spray applications [e.g., possible swath offset and overlap, canopy Downloaded by [The University of British Columbia] at 17:18 26 November 2014 height (13.6 m vs 10.8 m), wind speed and direction (4.2 km/h, W vs 5.8 km/h, WSW), RH (32% vs 25%), ambient temperature (18.6°C vs 21.5°C), volume rate (9.4 L/ha vs47 L/ha), atomizer type (Micronair vs disccore), blade angle orientation (35° vs 90° down), aircraft speed, and micrometeorological conditions (including turbulence at the canopy level, which increases the kinetic energy of droplets affecting target impaction) (Matthews, 1984)]. These results generally appear to support the findings of Himel et al (1987), Sundaram et al (1989a) and Teske and Barry (1993).…”
Section: Droplet Density and Size Spectrasupporting
confidence: 85%
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“…Such large differences could be due to differences in various operational parameters encountered during the spray applications [e.g., possible swath offset and overlap, canopy Downloaded by [The University of British Columbia] at 17:18 26 November 2014 height (13.6 m vs 10.8 m), wind speed and direction (4.2 km/h, W vs 5.8 km/h, WSW), RH (32% vs 25%), ambient temperature (18.6°C vs 21.5°C), volume rate (9.4 L/ha vs47 L/ha), atomizer type (Micronair vs disccore), blade angle orientation (35° vs 90° down), aircraft speed, and micrometeorological conditions (including turbulence at the canopy level, which increases the kinetic energy of droplets affecting target impaction) (Matthews, 1984)]. These results generally appear to support the findings of Himel et al (1987), Sundaram et al (1989a) and Teske and Barry (1993).…”
Section: Droplet Density and Size Spectrasupporting
confidence: 85%
“…The D max values found on the horizontal disc samplers in Plot 1 were generally high at all three canopy levels (76 to 102 urn) due to gravitational sedimentation of droplets, compared to the values found on the vertical cylindrical samplers (51 to 58 urn) ( (Roltsch et al, 1994;MacNichol, 1995) and other conventional insecticides (Carman and Jeppson, 1974;Yates et al, 1974;Spillman and Joyce, 1978;Armstrong and Yule, 1978;1989a;Barry, 1984;Sundaram, 1987). The gradation observed was due to the canopy levels (NMD, 10.7 ± 1.8 to 12.6 ± 2.7 urn; VMD, 32.8 ± 3.0 to 35.3 ± 3.0 urn) were similar to the corresponding values obtained for the discs (NMD, 10.6 ± 1.9 to 11.7 ± 2.4 urn; VMD, 31.9 ± 2.7 to 43.1 ± 3.2 urn) [ANOVA P > 0.05 (Ryan et al, 1985)].…”
Section: Droplet Density and Size Spectramentioning
confidence: 90%
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“…If the layer could be made uniform and had a density of 1.0 g/cc, its thickness would be 0.05 //m [which is about 1/20 of the thickness of a spider web (Liu and Megaw, 1985)], and could not even be seen under an ordinary microscope. Furthermore, spray droplets seldom deposit uniformly on the entire foliar surfaces in the tree canopy (Armstrong and Yule, 1978;Sundaram, 1987) because droplets are usually filtered by the periphery of the canopy which is more exposed to the spray cloud than the interior parts. This leads to markedly higher deposits (up to ca.…”
Section: Dosage and Covermentioning
confidence: 99%