Cyclic volatile methyl siloxanes (cVMS) are present in technical applications and personal care products.They are predicted to undergo long-range atmospheric transport, but measurements of cVMS in remote areas remain scarce. An active air sampling method for decamethylcyclopentasiloxane (D5) was further evaluated to include hexamethylcyclotrisiloxane (D3), octamethylcyclotetrasiloxane (D4), and dodecamethylcyclohexasiloxane (D6). Air samples were collected at the Zeppelin observatory in the remote Arctic (79°N, 12°E) with an average sampling time of 81 ± 23 hours in late summer (AugustOctober) and 25 ± 10 hours in early winter (November -December) 2011. The average concentrations of D5 and D6 in late summer were 0.73 ± 0.31 ng/m 3 and 0.23 ± 0.17 ng/m 3 respectively, and 2.94 ± 0.46 ng/m 3 and 0.45 ± 0.18 ng/m 3 in early winter respectively. Detection of D5 and D6 in the Arctic atmosphere 2 confirms their long range atmospheric transport. The D5 measurements agreed well with predictions from an Eulerian atmospheric chemistry-transport model, and seasonal variability was explained by the seasonality in the OH radical concentrations. These results extend our understanding of the atmospheric fate of D5 to high latitudes, but question the levels of D3 and D4 that have previously been measured at Zeppelin with passive air samplers.
IntroductionCyclic volatile methyl siloxanes (cVMS) are high-volume production chemicals used in the production of silicone polymers, in personal care products, and in a range of technical applications. cVMS have been found in both the physical environment and in biota, and have lately become subject to increasing scientific scrutiny by environmental scientists and regulators.
1-3The three congeners, and dodecamethylcyclohexasiloxane (D6) have specifically been the focus of the attention.e.g.1-3Hexamethylcyclotrisiloxane (D3) is an additional member of the group of cVMS. The physical-chemical properties of cVMS differ from many known organic pollutants, as they combine high volatility with extreme hydrophobicity and a considerable affinity for organic phases like octanol (Table S1).
4Volatilization to the atmosphere is the main emission pathway of cVMS to the environment. 1-3 Hence the atmosphere is a key compartment for understanding the environmental fate and behavior of cVMS. Once in the atmosphere, cVMS are predicted to be mainly present in the gas phase, and degradation by reaction with hydroxyl radicals is understood to be the main removal mechanism. 5 The atmospheric half-lives due to reaction with hydroxyl radicals are 20.0 days for D3, 10.3 days for D4, 6.7 days for D5, and 5.8 days for D6 (Table S1). The estimated levels of D5 from these models correspond well with observed atmospheric concentrations in the environment. 9, 11 The predicted seasonality of D5 was a consequence of the strong seasonality of the hydroxyl radical concentrations at high latitudes. During the polar night low levels of hydroxyl radicals slow down the atmospheric degradation of D5 and allow it to ...