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  4. Engineered and subsequent intrinsic in situ bioremediation of a diesel fuel contaminated aquifer
 
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Engineered and subsequent intrinsic in situ bioremediation of a diesel fuel contaminated aquifer

Auteur(s)
Hunkeler, Daniel 
Centre d'hydrogéologie et de géothermie 
Höhener, P
Zeyer, J
Date de parution
2002
In
Journal of Contaminant Hydrology, Elsevier, 2002/59//231-245
Mots-clés
  • Bioremediation
  • Petroleum hydrocarbons
  • Groundwater
  • Redox processes
  • Bioremediation

  • Petroleum hydrocarbon...

  • Groundwater

  • Redox processes

Résumé
A diesel fuel contaminated aquifer in Menziken, Switzerland was treated for 4.5 years by injecting aerated groundwater, supplemented with KNO<sub>3</sub> and NH<sub>4</sub>H<sub>2</sub>PO<sub>4</sub> to stimulate indigenous populations of petroleum hydrocarbon (PHC) degrading microorganisms. After dissolved PHC concentrations had stabilized at a low level, engineered in situ bioremediation was terminated. The main objective of this study was to evaluate the efficacy of intrinsic in situ bioremediation as a follow-up measure to remove PHC remaining in the aquifer after terminating engineered in situ bioremediation. In the first 7 months of intrinsic in situ bioremediation, redox conditions in the source area became more reducing as indicated by lower concentrations of SO<sup>2</sup><sub>4</sub>‾ and higher concentrations of Fe(II) and CH<sub>4</sub>. In the core of the source area, strongly reducing conditions prevailed during the remaining study period (3 years) and dissolved PHC concentrations were higher than during engineered in situ bioremediation. This suggests that biodegradation in the core zone was limited by the availability of oxidants. In lateral zones of the source area, however, gradually more oxidized conditions were reestablished again, suggesting that PHC availability increasingly limited biodegradation. The total DIC production rate in the aquifer decreased within 2 years to about 25% of that during engineered in situ bioremediation and remained at that level. Stable carbon isotope analysis confirmed that the produced DIC mainly originated from PHC mineralization. The total rate of DIC and CH<sub>4</sub> production in the source area was more than 300 times larger than the rate of PHC elution. This indicates that biodegradation coupled to consumption of naturally occurring oxidants was an important process for removal of PHC which remained in the aquifer after terminating engineered measures.
Identifiants
https://libra.unine.ch/handle/123456789/4133
_
10.1016/S0169-7722(02)00059-1
Type de publication
journal article
Dossier(s) à télécharger
 main article: Hunkeler_D-Engineered_and_subsequent-20171127.pdf (827.99 KB)
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