Sunlight-driven degradation of plastic in the environment is photooxidation, not simple erosion. UV photons (mainly UV-B, 280–315 nm) are absorbed by chromophores in the polymer backbone, homolytically cleaving a C–C or C–H bond and producing a carbon radical. In the presence of O₂ that radical propagates a chain reaction (Norrish I/II photolysis) that ends in chain scission — the backbone snaps — steadily lowering the polymer's molecular weight until the material embrittles and fragments into smaller pieces, one route by which primary microplastics generate secondary micro- and nanoplastics.
This sim models the particle as a network of bonded monomer units. Each incoming photon that strikes the surface has a probability of breaking a nearby bond, set by an Arrhenius-type scission rate:
k = Φ · I_UV · exp(−Ea / RT) · f(O₂)
Φ = quantum yield of chain scission per absorbed photon
I_UV = UV irradiance (intensity slider)
Ea = 42 kJ/mol, activation energy of the radical propagation step
R,T = gas constant, absolute temperature (temperature slider)
f(O₂)= 0 in anoxic conditions, rising to 1 as O₂ availability increases
(photo-oxidation stalls without dissolved oxygen to trap the radical)
- UV intensity — sets how often photons strike the particle (shaded water vs. full midday sun).
- Temperature — accelerates the radical propagation step through the Arrhenius exponential; warm, sunlit sand degrades plastic far faster than cold, deep water.
- O₂ availability — without dissolved oxygen the radical can't propagate to a full scission; buried or anoxic sediment plastics persist far longer than surface-floating ones.
- When enough bonds around a region break, that cluster mechanically detaches and drifts free as its own particle — a new, smaller piece of secondary microplastic that can itself keep fragmenting.