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RESEARCH INTERESTS

  • Colloids,
  • Environmental geology,
  • Environmental geochemistry,
  • Geomicrobiology,
  • Mineralogy,
  • Soil science,
  • Mineral-bacteria interactions,
  • Bioremediation,
  • Archaeogeology.

 

  • Sampling colloids and nanoparticles in-situ

                                                     

We designed a new technique for in situ sampling of fine particulate matter (PM) including colloids in natural environments. The technique is based on a microlysimeter which is easy to move between field and laboratory and can be routinely used for in situ monitoring. The design of the device aims at limiting bias and artefacts encountered with current sampling methods based on successive field collection of liquid samples, transport, storage and filtration in the laboratory. Samples are directly collected on transmission electron microscopy (TEM) grids, thus totally eliminating the modifications classically due to handling of samples from collection to analysis. Detailed physical and chemical microscopic studies of individual particles can then be performed in order to fully characterize PM in natural media such as soil solutions, atmospheric fallout, rainfall and any aquatic system. This technique can be applied in a number of research fields, such as the characterization and determination of pollution vectors, the tracing of sources of emissions, or investigations on particle interactions.

 

  • Physical & chemical characterization of colloids

 

      Example of clay particles sampled in soil infitration water. Scale bar: 1µm

Physical and chemical characteristics of clay particles. a) Particle size distribution of 1919 clay particles, 81% have a diameter below 0.45 µm. b) Ternary plot representation of the chemical analyses performed on clay particles. The number of cations is based on the calculation of the structural formula; Crosses are representing the analyses from this study and circles are representing reference clay material. c) Normalized elementary concentrations of clay particles expressed in number of cations based on the structural formula. Normalization is done relative to reference material.ay particles. have a diameter below 0.45µm

 

  • Microaggregates in soils

Selected TEM microphotographs of organo-mineral microaggregates and corresponding individual particles analyses.

 

  • Factors affecting the distribution of colloids and nanoparticles in soil porosity and atmospheric fallout


Interpretative sketch of the evolution of the distribution of soil particles with depth.

 

Evolution of the distribution of the particles with time at each depth

 

  • As-bacteria interaction

Herminiimonas arsenicoxydans and Acinetobater calcoaceticus are natural bacteria isolated from As-contaminated environments. One noteworthy characteristic of the bacteria is their ability to oxidize arsenic. In order to investigate the interactions between those bacteria and arsenic we used transmission electron microscopy (TEM) and energy dispersive spectroscopy (EDX) to observe the behavior of the bacteria treated with As[III]. Results showed that a substantial amount of the anion is fixed to the cell wall and into the extracellular polymeric substance (EPS). This sequestration appeared as a dense fibrillar net surrounding the cells. As a comparison, observation of a non As-oxidizing mutant of H. arsenicoxydans showed the same behavior meaning that the precipitation of As is not reliable to the As-oxidizing capacity of the bacteria. Moreover, we propose that such a precipitation into the EPS is due to a passive binding with protonated groups and possibly to a substitution between P and As. Finally, it appears that the tested bacteria are good candidates for As remediation whatever is the oxidation of As in the precipitate.

  • Pb-bacteria interaction

We monitored near-surface atmospheric fallout (15-cm above ground) and soil solution (at 15, 35 and 55 cm below ground) derived nanoparticles over an 8-month period by collecting the particles directly onto TEM grids in anthropogenically-influenced (vineyard) and pristine (native forest) sites in France. Particle clusters trapped on the grid were selected randomly and individual particles were binned into eight different groups (euhedral clays, weathered clays, salts, oxi-hydroxides, bacteria, non-living organic matter, aggregates and undetermined). Bacteria represent 9 – 23% of the collected nanoparticle area (ave. 9.4% and 18% for two atmospheric collection sites and ave. 23% for soil infiltration samples). Bacteria were most often associated with non-living organic matter and comprised a variety of morpho-types. Interestingly, 45% of all the bacteria analyzed by transmission electron microscopy and electron dispersive spectroscopy (TEM-EDX) showed the presence of intracellular grains significantly enriched in lead and phosphorus. Intracellular sequestration of Pb into polyphosphate bodies has been observed in the laboratory, but this is the first observation of this phenomenon in a natural environment. Furthermore, this suggests that microbial-bound Pb may be an important transport mechanism in subsurface environments.

Research
© 2009