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NEL OILS 66-11<br />

66.2 ENVIRONMENTAL FATE AND EXPOSURE PATHWAYS<br />

A discussion of the environmental behavior of fuel oil is limited<br />

by the lack of data defining its major components. The environmental<br />

behavior of hydrocarbons selected from 'the major classes will be<br />

addressed; however, trace elements <strong>and</strong> the many diverse additives will<br />

not be specifically addressed. Many of the hydrocarbons characteristic<br />

of diesel fuel have been addressed previously in the more extensive<br />

environmental fate section of the JP-4 chapter since these hydrocarbons<br />

are common to both petroleum fuels. The general discussions of<br />

aliphatic <strong>and</strong> aromatic hydrocarbons <strong>and</strong> their behavior in<br />

soil/ground-water systems will not be repeated here; the reader is<br />

referred to the relevant sections of Chapter 64.<br />

66.2.1 Equilibrium Partitioning Model<br />

In general, soil/ground-water transport pathways for low<br />

concentrations of pollutants in soil can be assessed by using an<br />

equilibrium partitioning model. For the purposes of assessing the<br />

environmental transport of diesel fuel, a group of specific<br />

hydrocarbons was selected from the dominant hydrocarbon classes, i.e.,<br />

alkanes, cycloalkanes, <strong>and</strong> aromatics: there were no availatile data to<br />

confirm the presence of the selected compounds in a typical diesel fuel<br />

sample. Table 66-3 identifies the selected hydrocarbons <strong>and</strong> presents<br />

the predicted partitioning of low soil concentrations of those<br />

hydrocarbons among soil particles, soil water, <strong>and</strong> soil air. The<br />

portions associated with the water <strong>and</strong> air: phases of the soil are<br />

expected to have higher mobility than the adsorbed portion.<br />

Estimates for the unsaturated topsoil indicate that sorption is<br />

expected to be an important process for all the dominant hydrocarbon<br />

categories. Partitioning to the soil-vapor phase is much less<br />

important than for other petroleum distillates since many of the lower<br />

molecular weight aliphatic hydrocarbons (C, -C,) characterized by high<br />

vapor pressure <strong>and</strong> low water solubility are not expected to be major<br />

components of diesel fuel. The aromatics have slightly higher water<br />

solubilities <strong>and</strong> transport with infiltrating water may be more<br />

important for these compounds; volatilization, on the other h<strong>and</strong>, is<br />

not expected to be important. In saturated, deep soils (containing no<br />

soil air <strong>and</strong> negligible soil organic carbon), a significant percent of<br />

the aromatic hydrocarbons is predicted to be present in the soil-water<br />

phase <strong>and</strong> available for transport with flowing ground water.<br />

Partitioning to the air <strong>and</strong> water phases is expected to be even less<br />

important for the organic components of residual fuel oils compared to<br />

components of diesel oil; sorption to soil particles is expected to be<br />

significant;<br />

In interpreting these results, it must be remembered that this<br />

model is valid only for low soil concentrations (below aqueous<br />

solubility) of the components. Large releases of diesel fuel (spills,<br />

leaking underground storage tanks) may exceed the sorptive capacity of<br />

the soil, thereby filling the pore spaces of the soil with the fuel.<br />

6/87<br />

.<br />

.-1<br />

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