A mixing rule for imaginary parts of refractive indices of aerosols or colloids in the Rayleigh regime

• A mixing rule for imaginary parts of refractive indices is derived • This Rayleigh Mixing Rule is valid for small particles in the Rayleigh regime • In certain limits, it is in good agreement with established mixing rules • The Rayleigh Mixing Rule retrieves imaginary parts of refractive index spectra • Retrieved imaginary parts of refractive indices are weakly dependent on morphology A Rayleigh mixing rule that relates the effective imaginary part of the refractive index of a composite medium, such as an aerosol or colloid, to the complex refractive index of the Rayleigh particles is derived using Rayleigh scattering theory. The derivation is simple, straightforward, and only weakly dependent on particle morphology. The Rayleigh mixing rule offers an opportunity to derive the imaginary part of refractive index spectra of Rayleigh particles, suspended in a non-absorbing medium with known refractive index spectrum, from an extinction spectrum of the composite medium. However, for this application, the real refractive index spectrum of the particle must be known reasonably well and the imaginary part must be known well enough to decide between two mathematical solutions for it. The Rayleigh mixing rule is compared with widely used mixing rules (i.e., volume, Maxwell Garnett, and Bruggeman mixing rules) and we show that in the small volume fraction regime both the Maxwell Garnet and Bruggeman mixing rules agree with the Rayleigh mixing rule.

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Publication Details

Journal
Journal of Quantitative Spectroscopy and Radiative Transfer
Published
2024-11-07
DOI
https://doi.org/10.1016/j.jqsrt.2024.109254
Citations
2
Primary Topic
Atmospheric aerosols and clouds
Type
article
Field-Weighted Citation Impact
0.57

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article

A mixing rule for imaginary parts of refractive indices of aerosols or colloids in the Rayleigh regime

Justin B. Maughan, Hans Moosmüller, C. M. Sorensen, Prakash Gautam
2 citations
Journal of Quantitative Spectroscopy and Radiative Transfer
Atmospheric aerosols and clouds
0.57
article

A mixing rule for imaginary parts of refractive indices of aerosols or colloids in the Rayleigh regime

Justin B. Maughan, Hans Moosmüller, C. M. Sorensen, Prakash Gautam
article en
2 citations

Abstract

• A mixing rule for imaginary parts of refractive indices is derived • This Rayleigh Mixing Rule is valid for small particles in the Rayleigh regime • In certain limits, it is in good agreement with established mixing rules • The Rayleigh Mixing Rule retrieves imaginary parts of refractive index spectra • Retrieved imaginary parts of refractive indices are weakly dependent on morphology A Rayleigh mixing rule that relates the effective imaginary part of the refractive index of a composite medium, such as an aerosol or colloid, to the complex refractive index of the Rayleigh particles is derived using Rayleigh scattering theory. The derivation is simple, straightforward, and only weakly dependent on particle morphology. The Rayleigh mixing rule offers an opportunity to derive the imaginary part of refractive index spectra of Rayleigh particles, suspended in a non-absorbing medium with known refractive index spectrum, from an extinction spectrum of the composite medium. However, for this application, the real refractive index spectrum of the particle must be known reasonably well and the imaginary part must be known well enough to decide between two mathematical solutions for it. The Rayleigh mixing rule is compared with widely used mixing rules (i.e., volume, Maxwell Garnett, and Bruggeman mixing rules) and we show that in the small volume fraction regime both the Maxwell Garnet and Bruggeman mixing rules agree with the Rayleigh mixing rule.

Journal of Quantitative Spectroscopy and Radiative TransferVol. 331
Kansas State University (US), Pratt Institute (US), Desert Research Institute (US)
National Science Foundation, U.S. Department of Energy, National Aeronautics and Space Administration, Columbia University, Kansas State University, Los Alamos National Laboratory
Climate action
Openalex Percentile: Top 33%
Atmospheric aerosols and clouds
0.57
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