Page 184 - Materials Chemistry, Second Edition
P. 184

Vadose Zone Soil Remediation                                     167



              Discussion:
              All three approaches yield the same result.


           5.2.4   Vapor Flow Rates

           The radial Darcy velocity, u , in homogeneous soil systems can be expressed
                                    r
           as [2]:
                                                   −
                                                      P RI
                                            P w
                                   k      r ln( w  R    1 ( ) 2   
                                            R / ) I   
                                                      P w
                              u r =                     0.5              (5.4)
                                   2µ
                                 
                                                      rR )
                                       1+  1 ( ) 2   ln(/ w
                                            −
                                               P RI
                                                     R / ) I
                                             P w     ln( w  R
           where u  is the vapor flow velocity at a radial distance r away from the extrac-
                   r
           tion well. The velocity at the wellbore, u , can be found by replacing r with
                                               w
           R  in Equation (5.4):
             w
                                   k                P RI  2 
                            u w =       P w      1−               (5.5)
                                               R I   
                                             w
                                        w
                                  2µ  R ln( R /)     P w    
             The volumetric vapor flow rate entering the extraction well, Q , can then
                                                                     w
           be found as:
                                        )(
                            Q w = (2π R Hu )
                                           w
                                      w
                                     π k    P w       P RI  2      (5.6)
                                =  H   µ     ln( R / )   1−    P w    
                                           w  R I        
           where H is the perforation interval of the extraction well.
             To convert the vapor flow rate entering the well to the flow rate discharged
           to the atmosphere (Q atm ), where P = P atm  = 1 atm, the following relationship
           can be used:
                                             P well 
                                     Q atm =      Q well                 (5.7)
                                             P atm 
           Example 5.10:   Estimate the Extracted Vapor Flow
                         Rate of a Soil-Venting Well
           A soil-venting well (4-in. diameter) was installed at a site. The pressure in the
           extraction well is 0.9 atm and the radius of influence of this soil-venting well
           has been determined to be 50 ft.
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