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

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Appendix D<br />

Table D.2<br />

Lower Quantile Values <strong>of</strong> Cumulative Frequency Distribution <strong>for</strong> Dilution<br />

Factor<br />

Percentile<br />

Dilution Factor<br />

0 3.28<br />

5 40.26<br />

10 66.04<br />

15 88.39<br />

20 113.28<br />

25 139.73<br />

In this region a quasi-linear relationship exists between <strong>the</strong> modelled magnitude <strong>of</strong> dilution <strong>and</strong> its<br />

expected frequency <strong>of</strong> occurrence at contaminated sites. A dilution factor <strong>of</strong> 65 or less is expected to<br />

occur at about 10% <strong>of</strong> sites con<strong>for</strong>ming to <strong>the</strong> model assumptions, whereas only 5% <strong>of</strong> con<strong>for</strong>ming sites<br />

should have dilutions less than about 40.<br />

A 5% probability <strong>of</strong> accepting an incorrect decision has a long tradition in statistical evaluation <strong>of</strong><br />

scientific <strong>and</strong> engineering data (Steel <strong>and</strong> Torrie 1980) <strong>and</strong>, in <strong>the</strong> absence <strong>of</strong> catastrophic<br />

consequences <strong>of</strong> an error, is a reasonable point <strong>of</strong> departure here. In view <strong>of</strong> <strong>the</strong> uncertainty in <strong>the</strong><br />

design <strong>of</strong> <strong>the</strong> model itself, which by virtue <strong>of</strong> assumed stratigraphy <strong>and</strong> contaminant distribution is<br />

probably conservative, a dilution factor <strong>of</strong> 50 is recommended to protect against excessive leaching <strong>of</strong><br />

organic contaminants to groundwater.<br />

3.0 Application <strong>of</strong> Dilution Factor to Groundwater Check<br />

At equilibrium, <strong>the</strong> relationship between <strong>the</strong> contaminant concentration in soil pore water (C ws ) <strong>and</strong> in<br />

<strong>the</strong> aquifer (C wa ) is:<br />

C ws = DF × C wa [14]<br />

And a final check on PSQC HH can be per<strong>for</strong>med by substituting equation [14] above into equation [6]<br />

from Appendix C, setting C wa equal to <strong>the</strong> relevant drinking water guideline, <strong>and</strong> calculating <strong>the</strong> critical<br />

soil concentration, Y:<br />

Y = DF × C wa (K d + ? m ) [15]<br />

152

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