TY - JOUR
T1 - Relationships between visible extinction, absorption and mass concentration of carbonaceous smokes
AU - Jennings, S. G.
AU - Pinnick, R. G.
PY - 1980
Y1 - 1980
N2 - A linear relation, independent of the size distribution, between visible and near-i.r. extinction coefficient σe(m-1) and mass concentration M (gm-3) of carbonaceous smokes is predicted. For a wavelength λ = 0.55μm the relation is σe/M = 9.5m2g-1, assuming a particle density of 2gcm-3. The relation is in good agreement with measurements on coal-fired stack plumes, oil smoke, soot and diesel exhaust that are available in the literature. A similar relationship between carbonaceous smoke visible and near-i.r. absorption coefficient σa, and mass concentration is also derived. The relations suggest that integrated mass concentration along a path within a carbonaceous smoke cloud can be inferred from measurement of the transmission from one end of the path to the other, and that the mass concentration at a particular location in the cloud can be determined from an in situ measurement of aerosol absorption at that location with a visible or near-i.r. laser spectrophone.
AB - A linear relation, independent of the size distribution, between visible and near-i.r. extinction coefficient σe(m-1) and mass concentration M (gm-3) of carbonaceous smokes is predicted. For a wavelength λ = 0.55μm the relation is σe/M = 9.5m2g-1, assuming a particle density of 2gcm-3. The relation is in good agreement with measurements on coal-fired stack plumes, oil smoke, soot and diesel exhaust that are available in the literature. A similar relationship between carbonaceous smoke visible and near-i.r. absorption coefficient σa, and mass concentration is also derived. The relations suggest that integrated mass concentration along a path within a carbonaceous smoke cloud can be inferred from measurement of the transmission from one end of the path to the other, and that the mass concentration at a particular location in the cloud can be determined from an in situ measurement of aerosol absorption at that location with a visible or near-i.r. laser spectrophone.
UR - https://www.scopus.com/pages/publications/0019227602
U2 - 10.1016/0004-6981(80)90176-6
DO - 10.1016/0004-6981(80)90176-6
M3 - Article
AN - SCOPUS:0019227602
SN - 0004-6981
VL - 14
SP - 1123
EP - 1129
JO - Atmospheric Environment (1967)
JF - Atmospheric Environment (1967)
IS - 10
ER -