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Measurement of Particle Size Distribution in Turbid Solutions by Dynamic Light Scattering Microscopy
Published on: January 9, 2017
Using dynamic light scattering to characterize mixed phase single particles levitated in a quasi-electrostatic
1Institute for Atmospheric and Climate Science, ETH Zurich, 8092, Zurich, Switzerland. ulrich.krieger@env.ethz.ch
Faraday Discussions
|January 25, 2008
Summary
Dynamic Light Scattering (DLS) effectively sizes non-spherical aerosol particles by analyzing their rotational Brownian motion. This method provides quantitative measurements for solid salt and mixed-phase particles, overcoming limitations of traditional approaches.
Area of Science:
- Aerosol science
- Physical chemistry
- Optical physics
Background:
- Characterizing non-spherical aerosol particles is crucial for understanding atmospheric processes.
- Traditional sizing methods often struggle with irregular particle shapes.
- Electrodynamic and quasi-electrostatic balances offer controlled environments for single particle studies.
Purpose of the Study:
- To develop and validate a method for sizing non-spherical, micrometre-sized aerosol particles using Dynamic Light Scattering (DLS).
- To investigate the influence of particle shape and internal structure on DLS measurements.
- To assess the feasibility of characterizing particle dynamics within aerosol particles.
Main Methods:
- Levitation of single aerosol particles (solid salt or mixed-phase) in electrodynamic or quasi-electrostatic balances.
- Measurement of temporal intensity autocorrelation functions from far-field scattering patterns using DLS.
- Quantitative analysis of the shortest decay in autocorrelation functions, treating particles as equivalent Mie spheres.
- Attribution of intensity fluctuations to rotational Brownian motion.
Main Results:
- A quantitative method for sizing non-spherical aerosol particles based on DLS and rotational Brownian motion was established.
- The shortest decay of the autocorrelation function provides reliable particle size information.
- Deviations from Mie scattering patterns contribute to long tails in autocorrelation functions.
- Diffusional motion of inclusions within droplets is masked by rotational motion, preventing analysis.
Conclusions:
- DLS analysis of rotational Brownian motion is a viable technique for sizing non-spherical aerosol particles.
- The method allows for the characterization of both solid salt and mixed-phase aerosol particles.
- Internal particle dynamics, such as inclusion diffusion, cannot be resolved due to dominant rotational motion.

