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y silica gel column chromatography, weight determination, glass<br />

capillary gas chromatography and mass spectrometry.<br />

Enumeration of Microbial Populations<br />

Total numbers of microorganisms per gram dry weight of sediment<br />

were determined by direct count procedures. Portions of collected<br />

sediment samples were preserved with formalin. Microorgansims in the<br />

preserved samples were collected on a 0.2 mm pore size Nuclepore filter<br />

which had been stained with irgalan black. The microorganisms were<br />

stained with acridine orange and viewed using an Olympus epif luorescence<br />

microscope. Cells staining orange or green were counted<br />

selected fields and the mean concentration determined.<br />

in 20 randomly<br />

Hydrocarbon utilizing microorganisms were enumerated using a three<br />

tube Most Probable Number (MPN) procedure. Serial dilutions of sediment<br />

samples, prepared using Rila marine salts solutions, were inoculated<br />

into sealed serum vials containing 10 ml BushnjeAl Haas broth (Difco) and<br />

50 ml of Arabian crude oil spiked with C hexadecane (sp. act.<br />

1 mCi/ml) . After 14 days incubation at 15°C, the C0 2 (if any) in the<br />

head space was collected by flushing and trapping in oxifluor CO .and<br />

quantitated by liquid scintillation counting. Vials showing CO<br />

production (counts significantly above background) were scored as<br />

positive and the Most Probable Number of hydrocarbon utilizers per gram<br />

dry weight calculated from standard MPN tables.<br />

Biodegradation Potentials<br />

Portions of sediment samples were placed into serum vials<br />

containing 10 ml Bushnell Haas broth. and 50 ml light Arabian crude oil<br />

spiked with either., C hexadecane, C pristane, C naphthalene, C<br />

benzanthracene or C 9-methylanthracene. After 14 days incubation,<br />

microbial hydrocarbon degrading activities were stopped by addition of<br />

KOH. The<br />

"<br />

C0„ produced from mineralization of the radiolabelled<br />

hydrocarbon was determined by acidifying the solution, flushing the<br />

headspace, trapping the CO in oxifluor C0„ and quantitating the C<br />

by liquid scintillation counting. The residual undegraded hydrocarbons<br />

and biodegradation products were recovered by extraction with hexane.<br />

The<br />

L<br />

C in each solvent extract was determined and fractionated, using<br />

silica gel column chromatography, into undegraded hydrocarbon fractions<br />

(hexane + benzene eluates) and degradation product fractions (methanol<br />

eluate + residual non-eluted counts). A 0.75 cm diameter X 10 cm column<br />

packed with 70-230 mesh silca gel 60 was used. Radiolabelled material<br />

in each fraction was quantitated by liquid scintillation counting.<br />

Sterile controls were used to correct for efficiency of recovery and<br />

fractionation. Triplicate determinations were made for each sample and<br />

radiolabelled hydrocarbon substrate <strong>com</strong>bination. The percent<br />

hydrocarbon mineralization was calculated as C0 2 produced (above<br />

sterile control)/ C hydrocarbon, added. The .percent hydrocarbon<br />

biodegradation was calculated as<br />

'<br />

C0„ produced +, C methanol fraction<br />

+ C residual (all above sterile control)/ C hydrocarbon added.<br />

Carbon balances generally accounted for approximately 90% of the<br />

radiolabelled carbon added to the sediment (except for naphthalene where<br />

volatility losses prevented efficient recovery).

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