Cyclic volatile methylsiloxane (cVMS) compounds are volatile, low-viscosity
silicone fluids used as precursors in the synthesis of high molecular weig
ht PDMS and as ingredients in certain personal care products. This study in
vestigates cVMS degradation and evaporation rates in soils as influenced by
molecular size, soil type, and moisture level. A temperate Michigan soil a
nd a highly weathered Hawaiian soil were incubated with similar to 40 mu g
of C-14-labeled cVMS/g of soil at similar to 22 degrees C; samples were kep
t at 32%, 50%, 92%, and 100% relative humidity (RH) both in open and closed
tubes. At each designated incubation time (from 0 to 21 days), the cVMS-co
ntaining soils were extracted, and the extra cts were analyzed by liquid sc
intillation counting (LSC) and reverse-phase high-performance liquid chroma
tography (RP-HPLC). The results showed that cVMS degradation was more signi
ficant than loss by volatilization in soil with low moisture levels. Degrad
ation reactions followed pseudo-first-order kinetics. The half-life of cVMS
fluids in air-dried soils ranged from 50 min to 5 days, depending on soil
type and cVMS molecular sizes. At high humidity (particularly at 100% RM),
the degradation slowed, while volatilization was accelerated and became a p
redominant process in regulating the cVMS removal from sail. At any given m
oisture level, the degradation rates of cVMS were much greater in highly we
athered soils (e.g., Oxisols) than in temperate soils, and the differences
were more profound for small cVMS (e.g., D-4) These findings demonstrate th
at cVMS fluids are unlikely to persist in any soils within the wide range o
f moisture conditions tested.