Opacity of black smoke: calculated variation with particle size and refractive index
- 1 May 1979
- journal article
- Published by Optica Publishing Group in Applied Optics
- Vol. 18 (9), 1399-1403
- https://doi.org/10.1364/ao.18.001399
Abstract
The opacity of a black smoke (an aerosol of carbon spheres) is calculated from the Mie theory for several log-normal particle distributions. Calculations are presented at a wavelength of 0.55 μm for particle geometric mean diameters in the 10−3–1-μm range and geometric mean standard deviations in the 0 (monodisperse) to 0.4 range. For-a given mass concentration the extinction coefficient and, therefore, the opacity can vary by a factor of 2 or more as the size distribution is varied. For absorptive indexes (m2) near 0.7, typical of carbon, the smoke opacity is only weakly dependent on the real part of the particle refractive index.This publication has 4 references indexed in Scilit:
- Carbon aerosol visibility vs particle size distributionApplied Optics, 1978
- Calculation of Smoke Plume Opacity from Particulate Air Pollutant PropertiesJournal of the Air Pollution Control Association, 1971
- Atmospheric visibility related to aerosol mass concentration: reviewEnvironmental Science & Technology, 1969
- Visibility Reduction due to Jet-Exhaust Carbon ParticlesJournal of Applied Meteorology, 1962