Theoretical Background
This section introduces the aerosol science theories and calculation methods used in AeroViz.
Optical Properties
Mie Scattering Theory
Mie theory describes the scattering and absorption of electromagnetic waves by spherical particles and is the foundation for calculating aerosol optical properties.
- Extinction, scattering, and absorption efficiency factors
- Internal mixing vs external mixing vs core-shell structure
- Effects of refractive index and particle size
IMPROVE Extinction Equation
The IMPROVE (Interagency Monitoring of Protected Visual Environments) equation is used to estimate extinction coefficients from chemical composition.
- Original version vs revised version
- Hygroscopic growth factor f(RH)
- Mass extinction efficiency of each component
Size Distribution
Log-normal Distribution
Aerosol size distributions typically follow log-normal distributions and can be characterized by geometric mean diameter (GMD) and geometric standard deviation (GSD).
- Number/surface area/volume distribution conversion
- Modal analysis (Nucleation, Aitken, Accumulation, Coarse)
- Size distribution statistics
ICRP 66 Lung Deposition Model
The International Commission on Radiological Protection (ICRP) human respiratory tract model is used to calculate regional deposition of inhaled aerosols.
- Head airways (HA), tracheobronchial (TB), and alveolar (AL) regions
- Activity intensity and breathing patterns
- Deposition fraction calculation
Chemical Properties
kappa-Kohler Theory
kappa-Kohler theory describes the hygroscopicity of aerosol particles, where the kappa value reflects the particle's ability to act as cloud condensation nuclei.
- Single-parameter kappa definition
- Relationship between chemical composition and kappa
- Hygroscopic growth factor calculation
Mass Reconstruction
Reconstructing PM2.5 mass from chemical composition to verify analytical completeness.
- Major components: SIA, OM, EC, Soil, SS
- Ammonium status determination
- OM/OC ratio selection
VOC Analysis
Ozone Formation Potential (OFP)
Assessment of volatile organic compounds (VOC) contribution to ozone formation.
- Maximum Incremental Reactivity (MIR)
- Species-specific OFP calculation
- Secondary Organic Aerosol Potential (SOAP)