Franšais      print      e-mail    


Atteia, O. and M. Franceschi (2001). Chemical conditions controlling natural attenuation of BTEX and chlorinated solvents : a review. Rev. Sci. Eau 14 (4) : 419-444. [article in French]

Original title: Conditions chimiques contrôlant l'atténuation naturelle des BTEX et solvants chlorés : un état des connaissances.

Full text (PDF)


The increasing reliance on natural attenuation in dealing with contaminated sites in North America is the consequence of:

  1. the extremely long duration and high cost of aquifer rehabilitation by classical methods, and
  2. the discovery of natural biodegradation in many different situations.

However, the use of this management technique is questionable, as intrinsic biodegradation is highly dependent on chemical conditions and particularly on redox equilibria. This paper describes the role of these chemical conditions on BTEX and chlorinated solvent attenuation and, by analyzing the current research, we try to define current limits of the predictability of natural attenuation in field conditions.

Natural attenuation is defined as the sum of processes able to decrease the pollutant concentration at a sampling point in an aquifer. Several physical processes such as dispersion, retardation and solubility play a role in natural attenuation. However, only biodegradation can significantly reduce the overall amount of pollutants in an aquifer, thereby allowing the pollutant concentration to reach the low levels that are required by regulations. The physical processes cited above can be modelled at a site to account for their effect, but the main focus is on biodegradation.

A detailed analysis of the basic thermodynamics of redox reactions involved in biodegradation is necessary to describe the reactions that can potentially occur. A rough analysis shows that BTEX is mainly degraded by oxidation and therefore is degraded more efficiently in aerobic media. However, toluene (and sometime ethylbenzene and xylene) can be degraded by fermentation and thus degradation occurs even in methanogenic conditions. In contrast, chlorinated solvents are degraded mainly by reduction, with the exception of c-DCE (cis-dichloroethylene) and VC (vinyl chloride), which are degraded by reduction and oxidation, thus having two degradative pathways. An overall comparison of reaction rates obtained from laboratory and field experiments clearly demonstrates that under field conditions the supply of redox reactants is a limiting factor in the reaction kinetics.

Degradation of BTEX under field conditions has been widely documented, and toluene ethylbenzene and xylene degradation occurred in almost all chemical environments. The most persistent product observed in almost all the studies was benzene. Due to its persistence, and also its carcinogenic and toxic properties, we focussed on the results obtained for benzene. The kinetic constant for degradation of benzene under most field conditions ranged from almost no degradation in the reduced parts of the plume to fast degradation at the oxygenated border. Degradation under nitrate, methane or iron reducing conditions was almost insignificant, but degradation did occur under sulphate reducing conditions. A detailed analysis of the data on benzene degradation under sulphate reducing conditions showed that there is a competition between bacterial populations for electron acceptors. Benzene is degraded only if electron acceptors are in excess and if no other easily degradable carbon source is present.

The analysis of experimental data on chlorinated solvents is more difficult because fewer studies exist and the degradation processes are slower and more complex. Significant intrinsic biodegradation occurs mainly by reductive dechlorination, with co-metabolism being important only under modified conditions. In the field, PCE (perchloroethylene) and TCE degradation occurred only under methanogenic and sulphate reducing conditions, while c-DCE was degraded in oxygenated media and finally VC degradation occurred under almost all redox potentials. The kinetics of degradation were slow, with half-lives in the order of 1 to several years. It was shown that the variability of such constants was quite high within the same site. This variability could be explained by the availability of reducing species, particularly hydrogen. By comparing the estimated and real length of solvent plumes it was shown that biodegradation was more important than transport for the sites with the most reducing conditions. At other sites, the necessity of both methanogenic conditions and a sufficient pool of electron donors in the aquifer was demonstrated. The high toxicity of VC, when compared to TCE, was of lower concern since it was shown that the plume size was equal to or smaller than that of TCE. This was due to a fast degradation kinetics for VC observed under aerobic conditions.

In conclusion, the controversy surrounding the use of models based on first-order degradation constants arose because of the strong dependence of this constant on prevailing chemical conditions. If the target at risk is far away, use of the statistics on plume length existing for BTEX seems to be sufficient. However, when the benzene content is high and the target at risk is close, there is a need to predict the size of the reduced plume. The approach is the same for more substituted chlorinated solvents. The most important data, which are often missing, are the amount of total 'easily' degradable carbon (i.e. BTEX, short chain acids or alcohols) delivered by the source that will generate the reduced plume. In order to achieve a more precise prediction, models incorporating the whole redox chain need to be developed and tested against existing field data.

Corresponding author

Olivier Atteia, Environnement, Géo-Ingénierie, Imagerie et Développement (EGID), Université Michel de Montaigne Bordeaux 3, 1 Allée Daguin 33607 Pessac Cedex, FRANCE

Email : Olivier.ATTEIA@egid.u-bordeaux.fr
Telephone : (33). / Fax : (33).

Franšais      print      e-mail    

Update: 2006-12-19
© INRS Eau, Terre et Environnement