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health and safety plan solid waste management unit assessment

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HYDRAULIC FLUID 68-21<br />

molecular weight (more liquid) const.ituents would tend to volatilize<br />

first, the remaining material would generally have lower volatilities<br />

<strong>and</strong> lower water solubilities.<br />

68.2.2 Transformation Processes in Soil/Ground-water Systems<br />

An <strong>assessment</strong> of environmental persistence for hydraulic fluids is<br />

difficult given the variety of materials involved <strong>and</strong> the lack of<br />

pertinent data. Thus, most of the statements given below are both<br />

general <strong>and</strong> speculative in nature. Only the phosphate esters have been<br />

the subject of several environmental studies (see Chapter 49 of this<br />

Guide <strong>and</strong> references 1490 <strong>and</strong> 1496).<br />

Hydraulic fluid oils are expected to be moderately persistent in<br />

the soil/ground-water environment because of their resistance to hydrolysis,<br />

oxidation <strong>and</strong> biodegradation. The general resistance to<br />

hydrolysis (for saturated <strong>and</strong> unsaturated hydrocarbons) is described by<br />

Harris (529). However, the organic esters, phosphate esters <strong>and</strong><br />

polyglycols would be somewhat more susceptible to hydrolysis, especially<br />

under basic conditions.<br />

The <strong>assessment</strong> of the resistance to biodegradation is more com-<br />

.plex. Most of the molecules are so large that passage through cell<br />

walls (where metabolism or degradation is relatively easy) is hindered<br />

<strong>and</strong> much of the biodegradation must be carried out by extracellular<br />

enzymes secreted by the microbes. Such difficulties aside, many<br />

studies on petroleum hydrocarbon materials (oils as well as light<br />

distillates) have showed moderate to high eventual susceptibility to<br />

biodegradation for the bulk of the material (1842). A period of microbial<br />

adaptation may be required. The organic esters, phosphate esters<br />

<strong>and</strong> polyglycols would be expected to be more readily biodegraded.<br />

Different constituents of the oil will differ significantly in<br />

their biodegradability for reasons related to molecular size, structure<br />

<strong>and</strong> toxicity. For example, highly branched alkanes are much less<br />

biodegradable than linear alkanes, <strong>and</strong> polycyclic aromatic hydrocarbons<br />

with three or more rings are very resistant to biodegradation (515).<br />

For all hydrocarbons, aerobic biodegradation would be expected to be<br />

much more important than anaerobic biodegradation (1841). Because of<br />

this, <strong>and</strong> because of the decrease in microbiological activity with<br />

increasing soil depth, oil constitutents reaching deep anaerobic soils<br />

could persist for very long time periods.<br />

68.2.3 Primary Routes of Exposure from Soil/Ground-water Systems<br />

The above discussion of fate pathways suggests that the components<br />

of hydraulic fluids will vary widely in their volatility, tendency to<br />

sorb to soil, <strong>and</strong> potential for bioaccumulation. However, the base<br />

stock of hydraulic fluids manufactured with mineral oils are expected<br />

to be very strongly sorbed to soil because of their high molecular.<br />

weight <strong>and</strong> low water solubility. These compounds have extremely low<br />

volatility in pure form, but when present in water may have relatively<br />

6/87

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