Long-term simulation of in situ biostimulation of polycyclic aromatic hydrocarbon-contaminated soil
| Autor: | Maiysha D. Jones, Stephen D. Richardson, Michael D. Aitken, David R. Singleton |
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| Rok vydání: | 2011 |
| Předmět: |
Environmental Engineering
Polycyclic aromatic hydrocarbon Bioengineering Microbiology Article Biostimulation chemistry.chemical_compound Soil Environmental Chemistry Soil Pollutants Polycyclic Aromatic Hydrocarbons Groundwater Soil Microbiology chemistry.chemical_classification Bacteria Chemical oxygen demand Biodegradation Pollution Anoxic waters Soil contamination Oxygen Biodegradation Environmental chemistry Environmental chemistry Pyrene Soil microbiology |
| Zdroj: | Biodegradation. 23(4) |
| ISSN: | 1572-9729 |
| Popis: | A continuous-flow column study was conducted to evaluate the long-term effects of in situ biostimulation on the biodegradation of polycyclic aromatic hydrocarbons (PAHs) in soil from a manufactured gas plant site. Simulated groundwater amended with oxygen and inorganic nutrients was introduced into one column, while a second column receiving unamended groundwater served as a control. PAH and dissolved oxygen (DO) concentrations, as well as microbial community profiles, were monitored along the column length immediately before and at selected intervals up to 534 days after biostimulation commenced. Biostimulation resulted in significantly greater PAH removal than in the control condition (73% of total measured PAHs vs. 34%, respectively), with dissolution accounting for a minor amount of the total mass loss (~6%) in both columns. Dissolution was most significant for naphthalene, acenaphthene, and fluorene, accounting for >20% of the total mass removed for each. A known group of PAH-degrading bacteria, ‘Pyrene Group 2’ (PG2), was identified as a dominant member of the microbial community and responded favorably to biostimulation. Spatial and temporal variations in soil PAH concentration and PG2 abundance were strongly correlated to DO advancement, although there appeared to be transport of PG2 organisms ahead of the oxygen front. At an estimated oxygen demand of 6.2 mg O2/g dry soil and a porewater velocity of 0.8 m/day, it took between 374 and 466 days for oxygen breakthrough from the 1-m soil bed in the biostimulated column. This study demonstrated that the presence of oxygen was the limiting factor in PAH removal, as opposed to the abundance and/or activity of PAH-degrading bacteria once oxygen reached a previously anoxic zone. |
| Databáze: | OpenAIRE |
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