--> Abstract: Combining Hydropyrolysis and Compound Specific Stable Isotope Measurements to Identify Sources of Biodegraded PAHs in Sediments, by Gbolagade A. Olalere, Cheng-Gong Sun, Mick Cooper, Colin E. Snape, and Christopher Vane; #90124 (2011)

Datapages, Inc.Print this page

AAPG ANNUAL CONFERENCE AND EXHIBITION
Making the Next Giant Leap in Geosciences
April 10-13, 2011, Houston, Texas, USA

Combining Hydropyrolysis and Compound Specific Stable Isotope Measurements to Identify Sources of Biodegraded PAHs in Sediments

Gbolagade A. Olalere1; Cheng-Gong Sun2; Mick Cooper2; Colin E. Snape2; Christopher Vane3

(1) Delta (FEWEN) Consultants Ltd, London, United Kingdom.

(2) Nottingham Fuel and Energy Centre, University of Nottingham, Nottingham, United Kingdom.

(3) Geochemistry, British Geological Survey, Nottingham, United Kingdom.

Compound-specific 13C/12C isotope ratio measurements have successfully been demonstrated as a useful technique for polycyclic aromatic hydrocarbons (PAHs) source apportionment in a number of studies. However, where the PAHs matrix have been subjected to heavy biodegradation, and the isotopic signatures for PAHs are overlapping for some sources, further constraints are needed for unambiguous source apportionment.

Given that stable carbon isotopic ratios (δ13C) of PAHs are not significantly affected by biodegradation and that hydropyrolysis of asphaltenes can generate representative molecular profiles expected for non-biodegraded oils, this methodology has been used for source apportioning hydrocarbons in biodegraded environmental samples.

This protocol has been applied to river sediments, to reveal the variations in isotopic ratio (13C/12C) (-24 to -28 ‰) in Clyde River sediments, suggesting that the sources of PAHs are numerous, with (petroleum and combustion sources- biomass burning, coal derived, and vehicle particulate) are providing major inputs of the parent PAHs.

The core sample studies have revealed that the quantities of asphaltene as small as 0.6 mg - 1 mg are good enough to generate enough hydrocarbons for reliable geochemical studies. The molecular and isotopic profiles of the core samples have suggested that PAHs input varied both qualitatively, quantitatively and in distribution. But the protocol has allowed an unambiguous specific source-apportionment of the PAHs in Glasgow area.

It appeared that the core samples derived their PAHs from coal, petroleum, and combustion of coal, biomass and petroleum. The historical shift in energy use, with time, from coal and coal utilization (-23 to -26‰), coal combustion (-25 to -26‰) and for values (-27 to -30‰), abundant petroleum (-27 to -29‰) and (-30‰) biomass combustion has been revealed.

The localized high level of concentrations of Benzo(a)Pyrene (BaP) and Benzo(k)fluoranthene- (32 - 4225 μg/g) generally, has been ascribed to dumping, and therefore, needs attention. Also, the exceptionally high concentrations of Benzo(k)fluoranthene and BaP with 758.4 µg/g and 846.2 µg/g respectively, in sample 608, has specifically allowed for suggesting petrol and diesel exhausts as major sources of PAHs in Glasgow area.

Finally, this combined technique has proved successful in an unambiguous source apportionment of PAHs in river and estuarine sediments in which hydrocarbons have been biodegraded.