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The boundary conditions for steady-state radial flow of LFG are: <br />P=PW r=R,, <br />P = PL r = RILFG <br />The term RILFG is the radius of influence of a LFG collection well, and denotes the radial <br />distance from the collection well where the pressure induced by the well is equal to the <br />positive pressure PL within the landfill. <br />Substituting the above boundary conditions for steady-state radial flow of LFG into the <br />above steady-state radial pressure distribution equation results in a steady-state radial LFG <br />pressure distribution equation: <br />In(r R ) <br />I'2(�) — Pw2 = \PiFG — 1'w) In( RI FG) Eauation 3 <br />RW <br />Where: <br />Pr = Absolute pressure measured at a distance r from the collection well (g/cm-s2) <br />PLFG = Absolute internal LFG pressure (Pa,m + PL) (9/cm-s2) <br />Pte, = Absolute pressure applied to the collection well (g/cm-s2) <br />RILFG = Radius of influence of the landfill gas collection well (cm) <br />Rw = Radius of the gas collection well (cm) <br />r = Distance from the collection well to pressure monitoring probe (cm) <br />The Radius of Influence (RI) is one of the most important parameters to be considered in <br />the design of a LFG collection system. Extraction wells should be placed so that the overlap <br />of their radii of influence covers the entire landfill surface. <br />The radius of influence (Rl,,,,) calculated using equation (1) represents the radial distance <br />from the collection well where the induced pressure equals the atmospheric pressure. The <br />radius of influence (RILFG) calculated by equation (3) represents the radial distance from the <br />collection well where the pressure induced by the collection well equals the internal <br />positive pressure of the landfill. The relationship of these two radii is shown in the following <br />boundary flow conditions figure. As this figure illustrates, in a landfill, the atmospheric <br />radius of influence also denotes the area surrounding the collection well where air intrusion <br />is able to occur. It must be noted that both radii of influence (RI atmospheric and RILFG) are <br />not constant parameters, but will vary depending on the amount of vacuum applied to the <br />collection well and, in the case of RILFG , on the magnitude of the internal LFG pressure PL . <br />It also must be noted that both radii of influence calculated by equations 1 and 3 represent <br />averages over all the flow paths. These radii of influence should not be considered the <br />maximum extent of any pressure gradient created by the collection well. <br />6 <br />Installation Work Plan to Remediate Landfill Gas Migration <br />J:\Allied\Forward\Workplan\Forward Evaluation - rev4.doc:9/15/2004 <br />Ll <br />