Michael J. McFarland is an Assistant Professor in the Division of Environmental Engineering at Utah State University and has a joint appointment with the Utah Water Research Laboratory, Logan, Utah. He conducts research and teaches courses in chemical thermodynamics and advanced biological waste treatment processes. McFarland is currently conducting research on biological cometabolism of aromatic and chlorinated aliphatic hydrocarbons.
Thermodynamic Framework for Evaluating PAH Degradation in the Subsurface
Article first published online: 4 AUG 2005
Volume 29, Issue 6, pages 885–896, November 1991
How to Cite
McFarland, M. J. and Sims, R. C. (1991), Thermodynamic Framework for Evaluating PAH Degradation in the Subsurface. Groundwater, 29: 885–896. doi: 10.1111/j.1745-6584.1991.tb00576.x
Discussion open until May 1, 1992.
- Issue published online: 4 AUG 2005
- Article first published online: 4 AUG 2005
- Received May 1990, revised December 1990, accepted March 1991.
A method is presented to evaluate the influence of redox conditions and pH on mineralization of polycyclic aromatic hydrocarbons (PAH) in subsurface environments. Microbial yields based on the free energy liberated from heterotrophic PAH metabolism are estimated under various environmental conditions using a simple bioenergetic growth model. The types and chemical forms of electron acceptors addressed in this paper include oxygen, nitrate, sulfate, carbon dioxide, iron (Fe+3and FeOOH), and manganese (Mn+4 and MnO2). PAHs addressed include naphthalene (2-fused aromatic rings), anthracene (3-fused aromatic rings), phenanthrene (3-fused aromatic rings), and pyrene (4-fused aromatic rings).
Calculated free energy changes demonstrated that sequential utilization of electron acceptors will follow the order Mn+4, O2, NO3−1, Fe+3, MnO2, FeOOH, SO4−2, and CO2. The behavior in microbial growth yield predictions were found to mimic the change in free energy liberated with the use of different electron acceptors. Despite release of free energy under all conditions evaluated, the small energy liberated during PAH mineralization under sulfate-reducing and methanogenic conditions suggests that heterotrophic degradation of PAH compounds under these conditions is unlikely to occur.
The large microbial growth yields associated with reduction of free metal species (Mn+4, Fe+3) during PAH oxidation suggest a selective advantage for microbes that can tolerate acid conditions and/or participate in metal chelation processes.