Some Factors that Affect the Deposition Rates of Sulfur Dioxide and Similar Gases on Vegetation

TLDR

Deposition of sulfur dioxide on vegetation is governed by environmental factors such as aerodynamic resistance, surface roughness, heat flux, and stomatal resistance, which vary diurnally and spatially, with typical stomatal resistance around 0.7 s cm⁻¹ in midwestern U.S. crops.

Abstract

The deposition of sulfur dioxide on growing vegetation is affected by diverse environmental factors, many of which undergo large diurnal and spatial variations. The aerodynamic resistance to vertical transfer in the surface boundary layer can be formulated in terms of the friction velocity, height of observation, vertical heat flux, and surface roughness. Also important are the resistance in the air layer closest to the surface elements and, in dry vegetation, the average stomatal resistance of the plants. The latter variable is among the most difficult to estimate, but over many agricultural field crops like those in the midwestern U.S., a typical minimum value of average stomatal resistance to SO2 transfer is about 0.7 s cm-1, as is indicated by various experimental data. The deposition velocity can be estimated as the inverse of the sum of the resistances of the layers, necessarily down to where the concentrations are zero; in the surface boundary layer, any of the various resistances might be dominant. Above the surface layer, the micrometeorological relationships are known with less certainty, but reasonable approximations indicate that during unstable conditions the resistance to transfer is very small at heights of several tens of meters and during stable conditions the aerodynamic resistance is very large aloft.