Fate and Stability of Nonextractable Residues of [14C]PAH in Contaminated Soils under Environmental Stress Conditions

• Published in: Environmental science & technology Vol. 32; no. 17; pp. 2585 - 2590
• Main Authors: Eschenbach, Annette, Wienberg, Reinhard, Mahro, Bernd
• Format: Journal Article
• Language: English
• Published: Washington, DC American Chemical Society 01-09-1998
• Subjects: Applied sciences; AROMATIC HYDROCARBONS; BIODECONTAMINACION; Biodegradation; Biological and physicochemical properties of pollutants. Interaction in the soil; BIOREMEDIATION; Contamination; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Environmental impact; Environmental protection; Exact sciences and technology; HIDROCARBUROS AROMATICOS; Hydrocarbons; HYDROCARBURE AROMATIQUE; POLLUTED SOIL; Pollution; Pollution, environment geology; POLYCYCLIC AROMATIC HYDROCARBONS; RESIDU; RESIDUES; RESIDUOS; Soil and sediments pollution; Soils; SOL POLLUE; SUELO CONTAMINADO; Anthracene; Stability; Hydrocarbon; Physical dressing; Pollutant behavior; Carbon Isotopes; Thawing; Polycyclic aromatic compound; EDTA; Soil pollution; Freezing; Pyrene; Naphthalene; Decontamination; Chemical treatment; Biological treatment; Carbon 14
• ISSN: 0013-936X; 1520-5851
• DOI: 10.1021/es9708272

It has been recognized during recent years that polycyclic aromatic hydrocarbons (PAH) may form nonextractable residues in soil and that this process may be stimulated by microbial activities. To use that process intentionally for soil bioremediation, one must ensure that the formed nonextractable PAH residues will not be released from the soil on the long run. The long-term stability of four different nonextractable [14C]PAH residues ([14C]naphthalene, [14C]anthracene, [14C]pyrene, and [14C]benzo[a]pyrene) was therefore monitored under different ecological stress conditions. It was found that a considerable fraction of the total [14C]PAH residues could be released as 14CO2 from the soil being partly due to a biogenic reduction of the nonextractable 14C residue fraction. The turnover of this fraction was comparable to the natural turnover rate for humic substances. Neither the addition of humus-degrading microorganisms nor a mechanical stress treatment of the soil structure by freezing and thawing led to a mobilization of the nonextractable [14C]PAH residues. However, a significant mobilization of the nonextractable 14C activity occurred when EDTA was added to the soil. The metal−organic soil complexes were destabilized by this complexing agent and released 14C activity that was attached to colloidal or dissolved organic matter.