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25th International Meeting on Organic Geochemistry IMOG 2011

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P-015<br />

Can comprehensive analysis of degraded oil indicate the<br />

c<strong>on</strong>diti<strong>on</strong>s under which biodegradati<strong>on</strong> occurred in an oil<br />

reservoir?<br />

Thomas Oldenburg 1 , Steve Larter 1,2 , Melisa Brown 1 , Ben Hsieh 1 , Ian Head 2 , Martin<br />

J<strong>on</strong>es 2 , Caroline Aitkins 2 , Neil Gray 2<br />

1 University of Calgary, Calgary, Canada, 2 Newcastle University, Newcastle up<strong>on</strong> Tyne, United Kingdom<br />

(corresp<strong>on</strong>ding author:toldenbu@ucalgary.ca)<br />

Most of the world petroleum reserves are<br />

biodegraded with the largest oil reserves being found<br />

<strong>on</strong> the flanks of foreland basins in Canada and<br />

Venezuela. A significant fracti<strong>on</strong> of the c<strong>on</strong>venti<strong>on</strong>al<br />

oil reserves are also biodegraded and major future oil<br />

discoveries are likely to be mainly biodegraded, too<br />

as they are expected in deep-water areas with low<br />

thermal gradients and shallow explorati<strong>on</strong> targets.<br />

These petroleum reservoirs are cooler than 80ºC and<br />

therefore ideal envir<strong>on</strong>ments for microbial<br />

degradati<strong>on</strong>. As it became accepted <strong>on</strong>ly recently that<br />

biodegradati<strong>on</strong> of petroleum in reservoirs proceeds<br />

anaerobically little is known about the processes and<br />

the c<strong>on</strong>trolling factors involved in subsurface<br />

hydrocarb<strong>on</strong> and n<strong>on</strong>-hydrocarb<strong>on</strong> degradati<strong>on</strong>.<br />

A laboratory microcosm study of anaerobic<br />

petroleum degradati<strong>on</strong> under sulphate-reducing and<br />

methanogenic c<strong>on</strong>diti<strong>on</strong>s was undertaken over a<br />

period of two years. The microbial communities and<br />

hydrocarb<strong>on</strong> distributi<strong>on</strong> patterns were analysed<br />

parallel to the detailed analysis of the distributi<strong>on</strong> of<br />

polar compounds using an ultra-high resoluti<strong>on</strong> 12T<br />

Fourier Transform I<strong>on</strong> Cyclotr<strong>on</strong> Res<strong>on</strong>ance Mass<br />

Spectrometer (FTICRMS). The whole degraded oil<br />

samples were analysed for acidic comp<strong>on</strong>ents (using<br />

electrospray i<strong>on</strong>isati<strong>on</strong> (ESI) in negative mode), basic<br />

compounds (ESI positive mode) as well as for low<br />

A<br />

original 302 days metha. 686 days metha.<br />

polar and highly aromatic comp<strong>on</strong>ents such as<br />

sulphur and aromatic hydrocarb<strong>on</strong> compounds using<br />

Atmospheric Pressure Photoi<strong>on</strong>isati<strong>on</strong> (APPI)<br />

techniques.<br />

The forming or destructi<strong>on</strong> of some polar compound<br />

classes indicates the c<strong>on</strong>diti<strong>on</strong>s under which oil<br />

B<br />

biodegradati<strong>on</strong> occurs. Whereas many hydroxy and<br />

carboxylic acid compounds are formed (Fig 1A-C) the<br />

occurrence of e.g. some NOx classes are related to<br />

biodegradati<strong>on</strong> mechanism. This novel knowledge<br />

received from laboratory experiments will be used to<br />

predict the biodegradati<strong>on</strong> history of natural<br />

biodegraded oil reservoirs.<br />

C<br />

163

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