Silicone (polydimethylsiloxane, or PDMS) fluids are widely used in ind
ustrial and consumer products and may find their way into municipal sl
udges that are eventually applied to the land. Earlier studies showed
that PDMS degrades in soil to low-molecular-weight, water-soluble sila
nols of the formula HO-[Si(CH3)(2)O](n)-H. In this study, 200-cs [C-14
]PDMS (1, 10, 100 mg kg(-1)) was placed in 50 g Londo sandy clay loam,
and the soil was dried to generate the desired silanols in situ. The
soil was remoistened and incubated at 25 degrees C, 12% moisture, and
21% O-2. The ultimate PDMS degradation product was identified by GC-MS
as dimethylsilanediol. During the next 4 months, from 25 to 50% of th
is substance was either volatilized from the soil, incorporated into t
he humus, or to a lesser extent oxidized to (CO2)-C-14. The latter two
processes increased with addition of alfalfa to the soil. No trend wa
s seen in the loss of dimethylsilanediol over different concentrations
.