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6 - Analytical methods for petroleum in cold region soils

Published online by Cambridge University Press:  22 August 2009

Daniel M. White
Affiliation:
Institute of Northern Engineering, PO Box 755910, University of Alaska Fairbanks, Fairbanks AK 99775–5910, USA
D. Sarah Garland
Affiliation:
Dept. of Civil and Environmental Engineering, University of Alaska Fairbanks, PO Box 755900, Fairbanks AK 99775, USA
Craig R. Woolard
Affiliation:
Anchorage Water and Wastewater Utility, 3000 Arctic Boulevard, Anchorage AK 99503–3898, USA
Dennis M. Filler
Affiliation:
University of Alaska, Fairbanks
Ian Snape
Affiliation:
Australian Antarctic Division, Tasmania
David L. Barnes
Affiliation:
University of Alaska, Fairbanks
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Summary

Introduction

In order to demonstrate the effectiveness of a bioremediation project, one must have an accurate measure of the contaminants, both at the start of the project and throughout the treatment process. The measurement of the contaminants throughout the process is important to demonstrate that the treatment is successful and to identify advances or set-backs quickly and effectively.

Proving the disappearance of hydrocarbons is important to the success of a bioremediation project. An accurate measurement of hydrocarbons and their biodegradation products is needed to confirm that petroleum was actually consumed by bacteria (discussed in Chapter 7, Section 7.3). One method of confirming biodegradation of petroleum is the coupled measurement of biodegradation rates by proxy methods and the disappearance of the contaminant. Biodegradation rates do not, in and of themselves, prove the decomposition of contaminants. Measurement of biodegradation rates, however, can be an easy way to demonstrate that the potential exists for contaminant removal. While measures of biodegradation rates are often used to estimate time to closure for a site, or proof of technology, biodegradation rates can be unreliable. Common measures of aerobic biodegradation are loss of contaminants, oxygen (O2) consumption, and carbon dioxide (CO2) evolution. Unfortunately, the CO2 can result from non-biological sources (see Chapter 7, Section 7.2.2.2 for additional discussion). Particularly in low pH groundwater, pH adjustment made during bioremediation could result in CO2 off-gassing from groundwater. Oxygen depletion in the subsurface is also not proof of biodegradation.

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Publisher: Cambridge University Press
Print publication year: 2008

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