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I'r - Memorial University of Newfoundland

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ange <strong>of</strong> Slatistica1 variat ion <strong>of</strong> the end members aodIor within their mixing arrays.<br />

Consequently. only these plots aJlowed the relative cootnbWon <strong>of</strong>prominc:nt primary and<br />

secondary sourcesto bequantitatively estimated in the present stUdy.<br />

Further, a comparison <strong>of</strong> the results <strong>of</strong> principa.I compooents analysis for both<br />

molecular andisotopic composition enables the relative usefulness <strong>of</strong>botb data sets to be<br />

quant ified. As it was shown in the previous discussion, the first two components in the<br />

principal components anal ysis for molecular composition account for the alteration <strong>of</strong>the<br />

PAH asse mblage by weathering processes. These two co mponents represent as much as<br />

76.5% <strong>of</strong> total variance in samp les. Thus, only the third component in analysis for<br />

molecular composition is responsible forthe actual relative contribution<strong>of</strong>different<br />

combust ion and petroleum sources. This component explains only 11.4% <strong>of</strong>total<br />

variability. On the contrary, in isotopic composition. the first component ex plains the<br />

relative contribution <strong>of</strong> the two primary sources. This component takes as much as<br />

66,4% cf nxal variabil ity. A simple calculation brin gs one to conc lude that the isoIopic<br />

data in this procedure was 5.8 times as useful as the molecular.<br />

The above examples demonstralc that identification <strong>of</strong>PAH isotopic co mposition<br />

should be considered as a technique highJy suppl ementary to the conventional molecular<br />

analysis. A similar conclusion was made by O 'Malley (1994), who studiedthe sources <strong>of</strong><br />

polycyclic aromatic hydrocarbons in two areas<strong>of</strong>eastern Canada.

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