Biodegradation of Organic Chemicals in Soil/Water Microcosms System: Model Development
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The chemical interactions of hydrophobic organic contaminants with soils and sediments may result in strong binding and slow subsequent release rates that significantly affect remediation rates and endpoints. In order to illustrate the recalcitrance of chemical to degradation on sites, a sorption mechanism of intraparticle sequestration was postulated to operate on chemical remediation sites. Pseudo-first order sequestration kinetics is used in the study with the hypothesis that sequestration is an irreversibly surface-mediated process. A mathematical model based on mass balance equations was developed to describe the fate of chemical degradation in soil/water microcosm systems. In the model, diffusion was represented by Fick’s second law, local sorption-desorption by a linear isotherm, irreversible sequestration by a pseudo-first order kinetics and biodegradation by Monod kinetics. Solutions were obtained to provide estimates of chemical concentrations. The mathematical model was applied to a benzene biodegradation batch test and simulated model responses correlated well compared to measurements of biodegradation of benzene in the batch soil/water microcosm system. A sensitivity analysis was performed to assess the effects of several parameters on model behavior. Overall chemical removal rate decreased and sequestration increased quickly with an increase in the sorption partition coefficient. When soil particle radius, a, was greater than 1 mm, an increase in radius produced a significant decrease in overall chemical removal rate as well as an increase in sequestration. However, when soil particle radius was less than 0.1 mm, an increase in radius resulted in small changes in the removal rate and sequestration. As pseudo-first order sequestration rate increased, both chemical removal rate and sequestration increased slightly. Model simulation results showed that desorption resistance played an important role in the bioavailability of organic chemicals in porous media. Complete biostabilization of chemicals on remediation sites can be achieved when the concentration of the reversibly sorbed chemical reduces to zero (i.e., undetectable), with a certain amount of irreversibly sequestrated chemical left inside the soil particle solid phase.
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- Biodegradation of Organic Chemicals in Soil/Water Microcosms System: Model Development
Water, Air, and Soil Pollution
Volume 178, Issue 1-4 , pp 131-143
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- organic chemicals
- soil/water microcosms system
- mathematical model
- Industry Sectors
- Author Affiliations
- 1. State Key Laboratory of Hydrology, Water Resources and Hydraulic Engineering, Hohai University, Nanjing, 210098, People’s Republic of China
- 2. National Research Program, U.S. Geological Survey, M.S. 413, Box 25046, Federal Center, Denver, CO, 80225-0046, USA
- 3. Geologic Division, U.S. Geological Survey, M.S. 964, Box 25046, Federal Center, Denver, CO, 80225-0046, USA
- 4. Department of Civil and Environmental Engineering, Lehigh University, Bethlehem, PA, 18015, USA