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t <br /> �k <br /> _UTCMOT=- GASOL=M <br /> 65-13 <br /> aydrocarbons was selectad from the daminaat hydrocarbon c' . . s, i.e. . <br /> alkaaas. cycloa1 kanes. and aromatics- glass specific were E <br /> r chosen an the .basis of their relative concentrations. ar.; mere tended <br /> :o span tha boiling point average of the gasoline ..ydr _Mons. <br /> :able 65-3 identifies the selected hydrocarbons and <br /> � y pres the <br /> ?redicted partitioning of low soil concentrations o£ those hydrocarbons <br /> k among soil particles. soil water. and soil air. The portions <br /> associated with the wacer and air phases of the soil are expected to <br /> naveahigher mobility than the adsorbed portion. <br /> : <br /> 1 <br /> � . Estimates for the unsaturated topsoil indicate that sorption is <br /> expected to be an important process for all the dominant hydrocarbon <br /> catagaries. Partitioning to the soil-vapor phase is also expected to <br /> be important for the- lover molecular weight aliphatic hydrocarbons <br /> (C,1-Cs) which are characterized by high vapor pressure and Low watar <br /> solubility. The alkyl benzenes have higher water solubilities and <br /> cransporz with infiltrating Water may be important for these compounds: <br /> volatilization. ort the other hand. may be less important. In i <br /> saturated. deep soils (containing no soil air and negligible soil <br /> I organic .carbon) , a significant percent of both aliphatic (particularly <br /> " less than Cr) and aromatic hydrocarbons is predicted co be present in <br /> chaasoil-wacer phase and available for transport with flowing ground <br /> tater. <br /> In interpreting chase results. it must be remembered that this <br /> modal is valid only for Low soil concentrations (below aqueous <br /> + N. solubility) of the components. Targe releases of gasoline (spills. <br /> leaking underground storage tanks) may exceed the sorptive capacity of <br /> the soil. thereby filliog -the pore spaces of the soil with the fuel. <br /> In chis situation, the hydrocarbon mixture would move as a bulk fluid <br /> r and the equilibrium partitioning model would not be applicable. i <br /> Overall, ground water underlying soil concaminacad with gasoline <br /> hydrocarbons is expected to be vulnerable to contamination by ac least <br /> some of these components. The type of spill (surface vs. sub-surface) <br /> is ;.of particular importance. since volatilisation from the surface is <br /> expected to be a significant removal process for low molecular weight <br /> aliphaties. At this point. it should be mentioned that enviror%manul 4 <br /> fate/exposure/toxicology chapters for several of the components in <br /> table 65-3 Were included in Volume 1 of the IRP Toxicology Guide. The <br /> 4 gasoline components addressed in Volume 1 include: bensene. eoluene. <br /> xylenes. 'ethyl benzene, and naphthalene. Three major gasoline <br /> additives - TOCP. tatraathyL lead and ethylene dibromide were addressed <br /> in Volume 2 of the IRP Toxicology Guide, while ethylene dichloride was <br /> addressed in Volume 1. <br /> 6512.1.2 Transport Studies <br /> Hundreds of thousands of underground gasoline storage tanks are <br /> a currently used ac service stations, commercial locations, residences. <br /> w and petroleum depots,. and almost all the gasoline used for <br /> r,7 a <br /> cransporzation purposes in the U.S. is stored underground at least once <br /> s 6/87 <br /> � k ; <br /> } <br /> 7 S£ <br />