By A.G.Akimov, M.Yu.Barabanenkov, M.L.Baranochnikov, A.V.Leonov, A.D.Mokrushin, and N.M.Omel'yanovskaya
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Extra info for A Controllable Resistor with Features of a Field-Effect Transistor and Field Hall-Effect Sensor.
G. Nicholson, 1988a). The uptake of gases or particles at a surface relies on the afﬁnity of that surface for the depositing species. 0 100 Particle Diameter (µm) Figure 2 Representation of the dry deposition velocity measurements of particles to grass. Note: The points represent reported experimental data and the solid line represents the sedimentation velocity. The Dispersion, Deposition and Resuspension of Atmospheric Contamination 29 very low or zero for particles. In effect, particles can sometimes bounce off surfaces, although this process is poorly understood and is thought to be important only for quite large particles in windy conditions.
This is because the complexities associated with in-cloud chemistry and aqueous reactions subsequent to The Dispersion, Deposition and Resuspension of Atmospheric Contamination 35 collection mean that it is can be difﬁcult to distinguish whether the depositing species was scavenged in a particulate or a gaseous form. The use of W to describe contamination from a single episode is likely to be of limited use, since ground-level and in-cloud air concentrations are likely to vary signiﬁcantly according to meteorological conditions.
2. 3. Resuspension from roads References 22 23 24 26 26 29 30 34 35 38 38 39 40 41 42 44 47 ÃCorresponding author. V. All rights reserved. 21 22 Ken W. Nicholson 1. Introduction Atmospheric transport can be broken down into dispersion and deposition. Dispersion is the dilution process that occurs when material is transported downwind from a source and it is important in determining atmospheric concentration. In turn, atmospheric concentration is important in determining inhalation dose. Deposition is the process that results in the surface uptake of atmospheric material.