A simple model based on canopy structure is developed to explain the vertical distribution of clouds of droplets in a crop canopy. An attenuation coefficient derived from experiments in cotton was insensitive to droplet size in the range 40--200 ~zm and to the microclimate.
Transport of aerial spray, I. A model of aerial dispersion
โ Scribed by D.H. Bache; W.J.D. Sayer
- Publisher
- Elsevier Science
- Year
- 1975
- Weight
- 609 KB
- Volume
- 15
- Category
- Article
- ISSN
- 0002-1571
No coin nor oath required. For personal study only.
โฆ Synopsis
A simple model representing deposition from a sedimenting cloud diffusing about its centre of gravity was compared with tracer distributions obtained from aerially released line sources in the lowest 15 m of the atmosphere. An estimate of linear growth in cloud dimensions was derived for its initial phase of dispersion. Comparison of the model with independent data corroborated the growth law and demonstrated its response to changes in atmospheric turbulence intensity. For clouds of light particles, it was shown that the distribution was characterised by the position of maximum concentration, which occurs at a distance proportional to the release height and inversely proportional to the turbulent intensity. Estimates were provided for ground deposition from line sources oriented parallel to and perpendicular to the wind direction.
๐ SIMILAR VOLUMES
Based on a model of aerial dispersion of spray clouds released from aircraft, criteria are given for choosing droplet sizes and flying heights in practical crop-spraying situations. There are advantages in using sprays composed of small droplets; micrometeorological measurements over cotton suggest