Table 1 Summary of the physiochemical properties of LACs.

From: Lifecycle of light-absorbing carbonaceous aerosols in the atmosphere

LAC type

Black carbon (BC)

Brown carbon (BrC)

Highly absorbing BrC

Moderately absorbing BrC

Weakly absorbing BrC

Common present forms or other names

Soot, elemental carbon (EC), involatile carbon

Tar ball

(in continuous state)

Atmospheric humic-like substances

(HULIS, in continuous state)

Water-soluble BrC

Sources

(formation mechanism)

High-temperature combustion (flame synthesis of PAHs)

More absorbing BrC from flaming biomass or solid fuel burning than lower-temperature smoldering combustion

(pyrolysis and near-source condensation, oxidation, functionization after emission)

Some primary OA after photobleaching; some secondary OA from VOC condensation

Carbon bonding

sp2 dominated

A range of sp2/sp3

Moderate sp2/sp3

Low sp2

Composition

Graphite layers

Chromophores, e.g., aromatics associated with nitrated, carbonyl, and unsaturated function groups

Chromophores being decomposed or newly formed

Morphology

 Shape and particle size

Aggregates of monomers in diameter 10–50 nm, overall diameter 80–220 nm

Sphere mainly at accumulation mode in diameters of hundreds of nanometers; or as coatings

Secondary species, size depending on the condensed substrate

 Volatility

 (vaporization temperature)

Refractory

(~4000 K)

Extremely low volatility (~1000 K)

Low to medium volatile

Semi-volatile

 Viscosity

Solid

Amorphous solid

Amorphous, semi-solid or liquid depending on temperate and RH

Mostly liquid

Optical properties

 Imaginary refractive indexa

Weak spectral dependence ~0.7–0.8

~0.3–0.5, slightly enhanced near-UV, also near-IR

In the order of 0.01–0.1, mainly near-UV

In the order of 0.001–0.01, only near-UV

 Absorption Ångström exponent (AAE)

AAE ~1

AAE slightly >1

Moderate AAE 2–4

High AAE ~3–8

Hygroscopic properties

 Solubility

Insoluble to any solvents

Mostly insoluble

Partly soluble (usually more in organic solvents)

Soluble

 Cloud condensation nuclei

Hard CCN;

enhanced CCN after aging

Barely CCN but may enhance through oxidation

More CCN

 Ice nuclei

Maybe deposition IN

Maybe deposition/immersion IN when glassy-solid/semi-solid

Hard IN

 Atmospheric evolution

Chemically inert; more compact shape after aging, possible absorption enhancement

Chemically unstable; subject to photolysis/photooxidation degradation; may enhance absorption by NO3 oxidation or ammonia uptake

  1. aOnly values for most model applications (shown in Fig. 3) are given.