Volatile methyl siloxanes (VMS) are
ubiquitous anthropogenic pollutants
that have recently come under scrutiny for their potential toxicity
and environmental persistence. In this work, we determined the rate
constants for oxidation by OH radicals and Cl atoms at 297 ±
3 K and atmospheric pressure in Boulder, CO (∼860 mbar) of
hexamethyldisiloxane (L2), octamethyltrisiloxane (L3), decamethyltetrasiloxane
(L4), dodecamethylpentasiloxane (L5), hexamethylcyclotrisiloxane (D3),
octamethylcyclotetrasiloxane (D4), and decamethylcyclopentasiloxane
(D5). Measured rate constants with OH radicals were (1.20 ± 0.09)
× 10–12, (1.7 ± 0.1) × 10–12, (2.5 ± 0.2) × 10–12, (3.4 ± 0.5)
× 10–12, (0.86 ± 0.09) × 10–12, (1.3 ± 0.1) × 10–12, and (2.1 ±
0.1) × 10–12 cm3 molec–1 s–1, for L2, L3, L4, L5, D3, D4, and D5, respectively.
The rate constants for reactions with Cl atoms with the same compounds
were (1.44 ± 0.05) × 10–10, (1.85 ±
0.05) × 10–10, (2.2 ± 0.1) × 10–10, (2.9 ± 0.1) × 10–10, (0.56 ± 0.05) × 10–10, (1.16 ±
0.08) × 10–10, and (1.8 ± 0.1) ×
10–10 cm3 molec–1 s–1, respectively. Substituent factors of F(−Si(CH3)2OR) and F(−SiCH3(OR)2) are proposed for use in
AOPWIN, a common model for OH radical rate constant estimations. Cl
atoms can remove percentage levels of VMS globally with potentially
increased importance in urban areas.