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I'r - Memorial University of Newfoundland

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It is difficult to differentiate between the relative importance <strong>of</strong>car soot and fire soot<br />

end members. As the car soot member demonstrates the widest range<strong>of</strong>statistical<br />

variation. it always overlaps with the range for fire soots. However. an increased<br />

influence <strong>of</strong>road sweeps can be established for a nwnber <strong>of</strong>stations. For example, the<br />

station at Buffalo consistently plots closer to the crankcase oil-road sweep mixing curve<br />

(Fig. 4.2.8, 4.2.11, 4.2.134.2. L7). The graphs demonstrate that as much as 80-90%<strong>of</strong><br />

PAH at this station derive from this secondary source. Contributi on from the road<br />

sweeps may also be important at sites 955, 84. %2, 23, and935 (Fig. 4.2.8, 4.2.1 L,<br />

4.2.15. 4.2.16).<br />

To conclude. the PAH assemblage in most samples can be attributed to mixing <strong>of</strong><br />

four primary and secondary sources. However, there are a few stations (especially 1021,<br />

946.966) where previously unidentified sources might influence the isotopic composition<br />

<strong>of</strong> PAH . The contribution from combustion sources seem to be predominant throughout<br />

the lake. Neverthe less, petroleum sources are important at some stations in the Western<br />

Basin and the northern part <strong>of</strong>the Central Basin. Finally, at stations located closer to the<br />

southern shore in the Central and Eastern Basins, the contribution <strong>of</strong>road sweeps can also<br />

be important (955. 84, 962, 23. and 935). This importance is especially well seen at<br />

Buffalo where it is close to 100"/0.<br />

4.2.2.1 Pet f or isotopiccomposition (source identification)<br />

As in the case with molecular composition, the final step to generalization <strong>of</strong>results<br />

was made through app lication <strong>of</strong>multivariate statistics (Appe ndix. 84; for more<br />

14

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