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.