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MM M 1=1rllr lM M <br /> r r lifil� <br /> 0Benzene parameters i <br /> A [m2] 40 000 plan view of the source area <br /> b [m] 2000 aquifer thickness <br /> Cs [mgAgsoo] concentration of chemical'Y'sorbed to soil particle surfaces <br /> CT [mgAgsod total soil concentration(all phases)of chemical' ' <br /> C°r [mgJkgso,i] <br /> 13 000 total soil concentration (all phases) of chemical'T'at time t=O <br /> CT max [mgm,xture/kgsod] total soil concentration of a multi-component mixture <br /> Cv [mg,/Lair] vapor phase concentration of chemical'Y' in the sod matrix <br /> Ci [mgJkgso,i] <br /> immiscible(free-phase) concentration of'Y'in the source zone <br /> C°cs(LR,O,z, [dimensionless] steady-state normalized concentration distribution along the dissolved plume centedine <br /> «CR>z>t,max [mgJLH20] 12 000 time-averaged solute concentration at the receptor location <br /> DAF [dimensionless] dilution attenuation factor (chemical specific) <br /> Des [m2/yj 0 600 effective gas phase diffusion coefficient in sod matrix (chemical specific) <br /> foc [kgcaftn/kgso,i] 1 330 fraction of organic carbon in soil matrix <br /> H [m] 2000 source zone thickness[in] <br /> Hw [m] 2000 well screen interval (screen interval is assumed to extend from the water table downwards) [m] <br /> [M3/M2-dl 0 000 water flux through the source zone <br /> If [mld] 0000411 water infiltration rate through source zone 15 0 000411 <br /> Kd ((mgJkgso,i)/ sod/water partition coefficient(chemical specific) <br /> (mgJLH2o)] 0114 <br /> Kd,s 0 114 <br /> Kd,vz 0 114 <br /> KH [(mgJLa,r)1 Henrys law coefficient(chemical specific) <br /> (mgJLH20)] 0 220 <br /> Koc [(mgJkgso,i)/ organic carbon partition coefficient(chemical specific) <br /> (mgJLH20)] 57 000 <br /> KxY cm/sec 000020 Horizontal hydraulic conductivity KW 00001 00864 <br /> Kz cm/sec 008640 Vertical hydraulic conductivity cm/s m/d <br /> L [m] 10 000 length of the source zone parallel to groundwater flow direction <br /> Lc [m] 13 000 depth of sod cover overlaying the source zone <br /> Ld [m) 14 000 diffusion path length for volatile source zone losses= Lc+Y2H <br /> Lvz [m] 0 000 distance from the bottom of the source zone to the aquifer <br /> Ls [m] <br /> LR [m] 30 000 distance downgradient to receptor <br /> ML [Mg.] mass of compound in the source zone soil pore water(chemical specific) <br /> Ms [mg[] mass of compound sorbed onto source zone soil particles(chemical specific) <br /> My [mgr] mass of compound in the source zone vapor space(chemical specific) <br /> Mw [glmoles,] molecular weight of a single component in a mixture(chemical specific) <br /> Mw,avg [gm,xwrelmolesm,xture] 90 000 average molecular weight of the mixture(mixture specific) <br /> n [LvoidslLswl 0 440 total soil porosity <br /> Pv [atm] pure phase vapor pressure of compound (chemical specific) <br /> R [0 0821 L-atm/mole-K) 0 082 Universal Gas Constant <br /> S [mgJLH20) 1780 000 pure phase aqueous solubuty of chemical 'T'(chemical specific) <br />