Abstract
Development of accurate predictive models and rate expressions that mimic observed transport and biodegradation phenomena occurring in the field and in the laboratory are important tools for assessing the efficacy of bioremediation. Biotransformation rates obtained from microscale laboratory experiments are typically not commensurate with rates obtained from field-scale bioremediation systems. Generally, field scale biotransformation rates are an order of magnitude or more slower than those observed in the laboratory.1,2 The differences observed can be attributed to scale dependent rate processes such as sorption to natural geosorbents, mass transport limitations and macroscale heterogeneities.
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D’Adamo, P.C., Bouwer, E.J., Ball, W.P. (2002). Coal Tar Contamination: Bioremediation and Bioavailability. In: Chadam, J., Cunningham, A., Ewing, R.E., Ortoleva, P., Wheeler, M.F. (eds) Resource Recovery, Confinement, and Remediation of Environmental Hazards. The IMA Volumes in Mathematics and its Applications, vol 131. Springer, New York, NY. https://doi.org/10.1007/978-1-4613-0037-3_12
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DOI: https://doi.org/10.1007/978-1-4613-0037-3_12
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