Terminology¶
This is a non-exhaustive list of terms and acronyms used in papers [1] [7] [10] on microplastics and nanoplastics (MnP) in the ocean-atmosphere system.
Microplastic / Nanoplastic¶
MP: microplastics, particles 1 \(\mu m\) to 5 \(mm\) in diameter.
NP: nanoplastics, plastic particles smaller than 1 \(\mu m\) in diameter.
MnP: micro(nano)plastics, collective term for all particles \(\le\) 5 \(mm\), including MPs and NPs.
Primary MnP: Intentionally manufactured micro/nano-sized plastics.
Secondary MnP: Plastics formed by degradation of larger items.
Flux¶
LOD: Limit of Detection, smallest detectable concentration.
LOQ: Limit of Quantification, smallest quantifiable concentration.
SSA: Sea Spray Aerosol, aerosol particles ejected into the atmosphere when air bubbles formed by breaking waves burst at the ocean surface.
SML: Surface Microlayer, the uppermost ~1000 µm of the ocean surface where floating MNP like PE accumulate.
MART: Marine Aerosol Reference Tank, to simulate SSA production and measure MNP aerosolization.
\([\text{MNP}]_{\text{air}}\) or \([\text{MNP}]_{\text{water}}\): Airborne or Waterborne MNP Concentration, number of MNP particles per unit volume of air or water
Units: particles \(m^{-3}\) (alternatively particles \(L^{-1}\))
\(U_{10}\): Wind speed at 10 m height, standard reference wind speed used in ocean-atmosphere modeling
Units: \(m \cdot s^{-1}\)
\(E_f\): Emission Factor, empirical coefficient relating water MNP concentration to emission flux
Units: \(m^{3} \cdot m^{-2} \cdot s^{-1}\)
Values vary by particle size and type (e.g., \(10^{-9} - 10^{-8}\) for typical MnPs)
\(Q\): Volumetric flow rate of incoming or outgoing air
Units: \(m^3 \cdot s^{-1}\)
\(\mathcal{C}\): Particle number concentration of MnP
Units: particles \(m^{-3}\)
\(E\): Emission Rate
Definition: Total number of MNP particles emitted per second
In the MART setup, the change in concentration of particles in the air over time can be written as:
\[ \frac{d\mathcal{C}}{dt} = Q_{\text{in}} \cdot \mathcal{C}_{\text{in}} - Q_{\text{out}} \cdot \mathcal{C}_{\text{out}} + E - L \]Where:
\(\mathcal{C}\) = particle concentration in the chamber (air)
\(Q_{\text{in}}\) = air inflow rate
\(\mathcal{C}_{\text{in}}\) = particle concentration in inflow air
\(Q_{\text{out}}\) = air outflow rate
\(\mathcal{C}_{\text{out}}\) = particle concentration in outflow air
\(L\) = loss of particles (e.g., deposition on walls; often neglected in basic cases)
When steady state is reached, i.e., the particle concentration in the chamber becomes constant over time:
\[ \frac{d\mathcal{C}}{dt} = 0 \]Also assume:
Clean air inflow: \(\mathcal{C}_{\text{in}} = 0\)
Losses are negligible: \(L \approx 0\)
So the mass balance simplifies to:
\[ E = Q_{\text{out}} \cdot \mathcal{C}_{\text{out}} \]Units: particles \(s^{-1}\)
\(F\): Emission Flux
Definition: Number of MNP particles emitted per unit area per unit time
Formula:
\[ F(U_{10}, \mathcal{C}) = (3.84 \times 10^{-6} \cdot U_{10}^{-3.41}) \cdot (E_f \cdot \mathcal{C}) \]Units: particles \(m^{-2} \cdot s^{-1}\)
Note that \(3.84 \times 10^{-6} \cdot U_{10}^{-3.41}\) is a dimensionless coefficient.
\(AF\): Aerosolization Factor
Definition: Ratio of MNP concentration in air to that in water
Formula:
\[ AF = \frac{[\text{MNP}]_{\text{air}}}{[\text{MNP}]_{\text{water}}} \]Dimensionless (ratio of concentrations)
Aerosol¶
Aerosol Size Modes: grouped log-normal size distributions, each has a characteristic size range and composition:
Nucleation Mode
Diameter < 5 nm
Represents the smallest aerosols (e.g., newly formed sulfate particles).
No microplastics allowed due to their larger size.
Aitken Mode
Diameter ~5–50 nm
Small particles that can grow via condensation/coagulation.
Subdivided into soluble and insoluble.
Accumulation Mode
Diameter ~50-250/500 nm
Intermediate-size aerosols where particles tend to “accumulate.”
Important for cloud formation and light scattering.
Coarse Mode
Diameter >250 nm
Larger particles that deposit faster.
Includes both soluble and insoluble variants.
Super-Coarse Mode
Diameter >2500 nm
Largest particles (like microplastic fibres).
Only insoluble; no soluble version exists in the model.
MnP Particle Types
Fragment:
Small broken-down pieces of plastic; emitted across all insoluble modes (except nucleation).
Fibre:
Thread-like plastic particles (e.g., from textiles); emitted only into the super-coarse insoluble mode.
Currently modeled as spheres, which underrepresents their atmospheric behavior.
CCN: Cloud Condensation Nuclei
Particles that can initiate cloud droplet formation when in the soluble mode and in the presence of supersaturation.
AOD: Aerosol Optical Depth
A measure of how much aerosol particles in the atmosphere block or scatter sunlight.
CDNC: Cloud Droplet Number Concentration
The number of cloud droplets per unit volume of air, influenced by aerosol concentration and type.
Radiative Effects:
The influence of particles on Earth’s energy balance via scattering or absorbing radiation.
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