Abstract

Steam treatment of contaminated soil and aquifer sediment is a promising method of cleaning soil. The treatment is based on steam injection into a water saturated porous aquifer (Gudbjerg et al. 2004), by which the heat transfers the contaminants into the vapour phase, allowing entrapment in an active carbon filter connected to a large vacuum suction device. The treatment is effective against several important groundwater contaminants, including pentachlorophenole and perchloroethylene, typically found in association with industrial processes or dry cleaning facilities. Furthermore, as an example of removal of non-aqueous phase liquids (NAPLs) large amounts of creosote have been recovered after steam injection in a deep aquifer (Kuhlmann 2002; Tse & Lo 2002). Steam treatment is dependent on the complete heating of the soil volume under treatment. The steam has a strongly adverse impact on trees and other plants with deep root systems within the soil, but no other visible effects have been reported. The aim of the activities undertaken during collaborative projects carried out by the Geological Survey of Denmark and Greenland (GEUS) and the Danish Institute of Agricultural Sciences (DJF) for the Danish Environmental Protection Agency and the local authorities in Copenhagen (Københavns Amt) was to establish to what extent the microbial community was affected by the steam treatment of the soil. A few results from the literature indicate that the microbial activity increases in steam treated soil (Richardson et al. 2002), probably due to microbial degradation of the soil contaminants in combination with microbial utilisation of heatkilled organisms. It is, however, not known whether this increased microbial activity is associated with the development of pathogenic micro-organisms; these are typically able to grow at higher temperatures than the general microbial community in soil.

Highlights

  • Steam treatment of contaminated soil and aquifer sediment is a promising method of cleaning soil

  • Steam treatment is dependent on the complete heating of the soil volume under treatment

  • The aim of the activities undertaken during collaborative projects carried out by the Geological Survey of Denmark and Greenland (GEUS) and the Danish Institute of Agricultural Sciences (DJF) for the Danish Environmental Protection Agency and the local authorities in Copenhagen (Københavns Amt) was to establish to what extent the microbial community was affected by the steam treatment of the soil

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Summary

Hedehusene ground surface collection well

Pumping, treating and recycling water at the site over many years had controlled the distribution of the contamination, but the main contamination was still present at very high levels and has become a long-term threat to continued groundwater extraction. The steam treatment in Hedehusene was carried out during the winter 2001–2002. Wells delivering steam were buried nine metres below the land surface, allowing the transfer of steam below the contamination plume (Fig. 1). The steam was pumped continuously for a period of five months, until the temperature reached 90°C. Heating of the soil allowed the transfer of the contaminant to the vapour phase which was trapped in an active carbon filter

The steam treatment in Hedehusene
General microbial community adaptation to growth at high temperature
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