X | = | distance from the planar source to the location of concern, along the centerline of the groundwater plume (i.e., y = 0, z = 0) |
Cx | = | the concentration of the contaminant at a distance X from the source, along the centerline of the plume |
Csource | = | the greatest potential concentration of the contaminant of concern in the groundwater at the source of the contamination, based on the concentrations of contaminants in groundwater due to the release and the projected concentration of the contaminant migrating from the soil to the groundwater. As indicated above, the model assumes a planar source discharging groundwater at a concentration equal to Csource. |
[ALPHA]x | = | dispersivity in the x direction (i.e., Equation R16) |
[ALPHA]y | = | dispersivity in the y direction (i.e., Equation R17) |
[ALPHA]z | = | dispersivity in the z direction (i.e., Equation R18) |
U | = | specific discharge (i.e., actual groundwater flow velocity through a porous medium; takes into account the fact that the groundwater actually flows only through the pores of the subsurface materials) where the aquifer hydraulic conductivity (K), the hydraulic gradient (I) and the total soil porosity [THETA]T must be known (i.e., Equation R19) |
[LAMBDA] | = | first order degradation constant obtained from Appendix C, Table E or from measured groundwater data |
Sw | = | width of planar groundwater source in the y direction |
Sd | = | depth of planar groundwater source in the z direction |
Ill. Admin. Code tit. 35, § 742.810
Amended at 37 Ill. Reg. 7506, effective May 15, 2013