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Subterranean ecosystems - Universidade de Évora

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IAH 2007 XXXV Congress - Groundwater and Ecosystems Lisbon, Portugal<br />

Microbial ecology and geochemistry of bio<strong>de</strong>gradation in porous aquifers –<br />

new concepts for limitations and stimulations<br />

[1] Christian GRIEBLER, [1] Robert, BAUER, [1] Bettina ANNESER, [1] Christian WINDERL,<br />

[1] Tillmann LUEDERS, [1] Piotr MALOSZEWSKI, [1] Florian EINSIEDL, [1] Willibald STICHLER,<br />

[2] Massimo ROLLE, [2] Sebastian BAUER, [2] Christina EBERHARDT, [2] Peter GRATHWOHL,<br />

[3] Lars RICHTERS, [1] Rainer U. MECKENSTOCK<br />

[1] GSF – National Research Center for Environment and Health, Institute of Groundwater Ecology, Ingolstädter<br />

Landstrasse 1, 85764 Neuherberg, Germany, e-mail: christian.griebler@gsf.<strong>de</strong><br />

[2] ZAG – Center of Applied Geosciences, University of Tuebingen, Sigwartstrasse 10, 72076<br />

Tuebingen, Germany.<br />

[3] Stadtwerke Düsseldorf AG, Höherweg 200, 40233 Düsseldorf, Germany.<br />

ABSTRACT<br />

The bio<strong>de</strong>gradation of organic pollutants in groundwater systems may be limited by the <strong>de</strong>pletion of essential<br />

nutrients, the low number of <strong>de</strong>gra<strong>de</strong>rs and specific biokinetics. However, the main problem seems to be the<br />

insufficient mixing of e-donors and e-acceptors. Main <strong>de</strong>gradation activities in contaminant plumes should<br />

therefore be located at their fringes. We call this working hypothesis the ‘plume fringe concept’. In or<strong>de</strong>r to<br />

investigate if bio<strong>de</strong>gradation in porous media is mixing-controlled and to elucidate the ecological role of<br />

pollutant <strong>de</strong>grading microbes, lab and field investigations were performed. These comprised (1) experiments in<br />

2-D aquifer mo<strong>de</strong>l systems, (2) retrieving of intact sediment cores at a former gasworks site and (3) installation<br />

of a novel high-resolution multi-level well.<br />

1) To assess the importance of individual abiotic (e.g. mixing, toxicity, nutrients) and biotic (e.g. cell<br />

distribution and activity, redox tolerance) parameters for bio<strong>de</strong>gradation un<strong>de</strong>r well controlled lab<br />

conditions, contaminant plumes were generated in 2-D aquifer mo<strong>de</strong>l systems, and subsequently inoculated<br />

with aerobic and/or anaerobic bacterial strains to investigate bio<strong>de</strong>gradation at high spatial resolution. The<br />

collection of empirical data was accompanied by state of the art reactive transport mo<strong>de</strong>lling.<br />

2) For the linkage of processes involved in bio<strong>de</strong>gradation and the respective microorganisms, fresh sediment<br />

samples were collected repeatedly from a sandy tar oil-contaminated aquifer. The total microbial<br />

community structure as well as the distribution of functional marker genes were correlated to prevailing<br />

physical-chemical sediment characteristics.<br />

3) To elucidate the importance of scale in relation to bio<strong>de</strong>gradation activities in porous media, a highresolution<br />

multilevel well was installed. This well allows the simultaneous withdrawal of groundwater<br />

samples from the contaminated zone with a vertical spatial resolution of up to 3 centimetres.<br />

The 2-D microcosms and the investigated aquifer bio<strong>de</strong>gradation of contaminants was followed by vertically<br />

resolved concentration measurements, compound-specific stable isotope ( 13<br />

C/ 12<br />

C, 34<br />

S/ 32<br />

S and 18<br />

O/ 16<br />

O) analysis, the<br />

i<strong>de</strong>ntification of signature metabolites, the spatial distribution of microbial biomass, and specific <strong>de</strong>gra<strong>de</strong>rs via<br />

marker genes indicating potential <strong>de</strong>gradation activities.<br />

Major outcomes so far may be summarized as follows:<br />

▪ Dispersion in porous aquifers controls contaminant transformation to a high <strong>de</strong>gree, but in anoxic<br />

environments further processes (most probably coupled to biokinetics) limit anaerobic bio<strong>de</strong>gradation.<br />

▪ Sediment heterogeneity and transient hydraulic conditions exhibit a significant positive effect on the overall<br />

bio<strong>de</strong>gradation.<br />

▪ The fringes of contaminant plumes display small scale and steep physical-chemical gradients in the range of<br />

centimeters to <strong>de</strong>cimeters. These gradients are the hot spots of bio<strong>de</strong>gradation.<br />

▪ At these hot spots the relative abundance of specific <strong>de</strong>gra<strong>de</strong>rs was highest. Up to 50% of the cells present<br />

in sediment samples from the fringe zone could be shown to carry <strong>de</strong>gradation-specific functional genes.<br />

Keywords: bio<strong>de</strong>gradation ecology, plume fringe concept, small-scale gradients, high-resolution sampling,<br />

mixing-controlled bio<strong>de</strong>gradation, spatial and temporal dynamics<br />

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