Table 1 Comparison of aerosol viscosity measurement techniques and capabilities
From: The viscosity of atmospherically relevant organic particles
Technique | Viscosity range (Pa s) | Particle diameter range (μm) | Temperature range (°C) | Notes | References |
|---|---|---|---|---|---|
Fluorescence lifetime imaging (FLIM) | 10−3–103 | 0.5–100 | Ambient | T range can be extended by using a cooled/heated microscope stage. The upper viscosity limit could be extended using different molecular rotors | |
Particle rebound | 100–102 | <0.4 | Ambient | RH dependence of rebound fraction measured to identify moisture content that gives rise to viscosity range specified | |
Dimer relaxation | 5 × 105–2 × 107 | ~0.05–0.2 | −15 to +80 °C | Identify T/RH conditions for transition in viscosity. Extrapolation to find Tg possible. Exact size and temperature ranges depend on many parameters | |
Light scattering | ~107 | ~0.1–0.9 | −38 to +10 °C | Transition in depolarisation ratio (minimum size limit specified) from non-spherical to spherical shape on measurement timescale occurs at the viscosity indicated | |
Shape relaxation | 105–1011 | <0.2 | Ambient | Combination of particle diameter and mass measurements used to estimate shape factor | |
SEM imaging | 10−1–1012 | 0.3–2 | Ambient | Qualitative distinction between ‘solid’, ‘semi-solid’ and ‘liquid’ particles for complex field and laboratory-generated samples | |
Aerosol optical tweezers | 10−3–109 | 5–20 | Ambient | Requires mL of sample. Measurable coalescence timescales span 10−6 to 105 s. RH dependence of viscosity | |
Bead mobility | 10−3–103 | 30–50 | Ambient | Samples collected with impactors can be analysed. RH dependence on viscosity can be determined | |
Poke flow | 103–107 | 25–75 | Ambient | Samples collected with impactors can be analysed. Uncertainties in the measured viscosities are large due to assumptions used when determine viscosity | |
Bulk viscometry/rheology | 10−3–108 typical | Bulk | −40 to 200 oC typical | Crossover in storage and loss modulus allows identification of any phase state change |