An introduction to CAN - download pdf or read online

By Bagschik P.

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G. Sehmel, 1976a; Nicholson, 1988b). Consequently, the ease at which a contaminant can become resuspended in the atmosphere is related often to the characteristics of the resident surface material, rather than the depositing species. Even the largest of particles can lift off from or move across a surface. However, gravitational effects may restrict the material from becoming resuspended properly in the atmosphere and it might be deposited very soon after becoming airborne. , 1974), which is a measure of the tangential velocity of the turbulent eddies in the free air.

Consequently, the ease at which a contaminant can become resuspended in the atmosphere is related often to the characteristics of the resident surface material, rather than the depositing species. Even the largest of particles can lift off from or move across a surface. However, gravitational effects may restrict the material from becoming resuspended properly in the atmosphere and it might be deposited very soon after becoming airborne. , 1974), which is a measure of the tangential velocity of the turbulent eddies in the free air.

Turbulence in the free atmosphere increases with increasing surface roughness and with increasing height of the individual surface elements. g. Garland, 1977), as well as the more frequent penetration of turbulent eddies into this layer. In addition, long surface elements can penetrate further into the free turbulent atmosphere, and deposition of particles via interception or impaction can occur, with both of these processes becoming increasingly important with increasing wind speed. g. g. Garland, 1977).

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