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Protocol for the Derivation of Environmental and Human ... - CCME

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Appendix D<br />

R = recharge, m/yr<br />

A = area <strong>of</strong> contaminated site, m 2<br />

Neglecting lateral dispersion, <strong>the</strong> horizontal contaminant flux in groundwater is approximated by<br />

Q ch = C gw [(W × B × q) + (R × A)] [2]<br />

where<br />

Q ch = horizontal contaminant flux, mg/yr<br />

C gw = concentration <strong>of</strong> contaminant in groundwater, mg/m 3<br />

W = width <strong>of</strong> contaminated zone, m<br />

B = effective mixing depth in aquifer, m<br />

q = Darcy velocity <strong>of</strong> aquifer, m/yr<br />

Applying mass balance considerations, contaminant transport in <strong>the</strong> vadose <strong>and</strong> saturated zones is set<br />

equal:<br />

C sw × R × A = C gw [(W × B × q) + (R × A)] [3]<br />

And a dilution factor (DF) may be defined as:<br />

Which reduces to<br />

By definition<br />

DF = C sw /C gw = [(W × B × q) + (R × A)]/R × A [4]<br />

DF = (W × B × q/R × A) + 1 [5]<br />

A = W × L [6]<br />

where<br />

L = length <strong>of</strong> contaminated site, m<br />

Substituting [6] into [4] yields<br />

DF = (B × q/R × L) + 1 [7]<br />

146

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