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health and safety plan solid waste management unit assessment

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STODDARD SOLVENT 67-11<br />

67.2.2 Transport <strong>and</strong> Transformation Processes<br />

Transport <strong>and</strong> transformation of Stoddard solvent constituents will<br />

depend on the physicochemical (<strong>and</strong> biological) properties of the<br />

constituents. Some constituents will dissolve more quickly in the<br />

percolating ground waters <strong>and</strong> be sorbed less strongly on the soils,<br />

thus being transported more rapidly, <strong>and</strong> may or may not be susceptible<br />

to degradation by chemical or biological action. Thus, as was shown in<br />

Figure 65-1, the relative concentrations of the constituents of the<br />

solvent will vary with time <strong>and</strong> distance from the site of<br />

contamination. This effect is called "weathering." (This term is also<br />

used to describe the changes to petroleum materials following spills<br />

into surface waters where film spreading <strong>and</strong> breakup, <strong>and</strong> differential<br />

volatilization, dissolution <strong>and</strong> degradation are all involved.)<br />

There are no available data specific to the transport <strong>and</strong><br />

transformation of Stoddard solvent in soil/ground-water systems. In<br />

general, the low water solubility <strong>and</strong> moderate vapor pressure of<br />

Stoddard solvent suggest that volatilization with subsequent<br />

photooxidation in the atmosphere may be important. Even though the<br />

most volatile hydrocarbons (i.e., < C,) are not expected to be major<br />

components of Stoddard solvent, volatilization from surface soils is<br />

expected to be a major fate process for the alkanes which have very low<br />

water solubility. The aromatic hydrocarbons likely to be present in<br />

Stoddard solvent are moderately soluble in water <strong>and</strong> may be available<br />

to be dissolved in <strong>and</strong> transported with infiltrating water. Sorption<br />

to organic materials may limit the actual rates of leaching <strong>and</strong><br />

volatilization from soils.<br />

As discussed in detail in Chapter 64, large surface spills or<br />

subsurface discharges of petroleum distillates may result in a separate<br />

organic phase on the surface of the ground water. Migration of the<br />

organic phase may be very different from that of the ground water<br />

itself <strong>and</strong> the solvent hydrocarbons dissolved in the ground water.<br />

Biodegradation may be an important transformation process for .<br />

Stoddard solvent in soil/ground-water systems; some photooxidation of<br />

surface spills may also occur. Data presented in Chapter 64 suggest<br />

that microorganisms capable of degrading C, to Cl2 aliphatic <strong>and</strong><br />

aromatic hydrocarbons are not uncommon in the environaant, <strong>and</strong> under<br />

conditions favorable to microbial activity, biodegradation may be<br />

rapid. It should be mentioned that Walker & A. (2257) state that<br />

even under optimum conditions, total <strong>and</strong> complete biodegradation of<br />

petroleum hydrocarbons is not expected to occur except possibly over an<br />

extremely long time period.<br />

Overall, ground water underlying soil contaminated with Stoddard<br />

solvent hydrocarbons may be vulnerable to contamination by at least<br />

some of these components. The type of spill (surface vs. sub-surface)<br />

is of importance since volatilization from the surface may be a<br />

significant removal process particularly for the lower molecular weight<br />

6/87

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