Orleans, France




Bioreactors for deep environments

The BIOREP facility is a high pressure set up to perform percolation and transfer experiments on fluid-rock interactions under a large range of pressure and temperature conditions, while continuously monitoring geochemical and bio-geochemical evolution. The facility is particularly adapted to monitor biological system evolution during the experiment.

The range of pressure and temperature of BIOREP allows simulating conditions that are typical for CO2 storage or for CO2 leakage, along a deep well or in the overburden. It could be also employed to simulate other subsurface storage conditions (e.g. other gas, water, oils) and systems of exploitation (e.g. geothermal, in-situ biolixiviation).

The facility could be used to do classical batch experiments, equilibration or transfer experiment between compartments through columns and also microfluidic percolations in highly pressurized micro-chips.

Brief technical description with picture and/or diagram


The percolation is performed between 2 or 3 high pressurized batch cells, with a high pressure syringes or a pump and can be applied to fluids (gas or liquids, supercritical fluids). Different setup can be realized in order to answer specific questions (i.e. with different types of regulating modules between these cells). For instance: Batch A can be set up with a predefined geochemical equilibrium and a gas phase can be introduced. A chosen reaction matrix (being crushed rock, sediments, pellets or synthetic material) inoculated with microorganisms can be tested in different percolation systems (column, Hassler cell or microcells). The B batch allows collecting fluids after percolation for sampling purpose. At the end of experiment, the column can be analysed.

Experimental conditions: Temperature from -10 to 120°C. Pressure up to 200 bar.

Materials in contact with fluids: PTFE, PEEK, C276 (Hastelloy) and silica and borosilicate for the microfluidic cells.


Advantages (technical, economic…)


Thanks to its modular and compartmentalized conception, BIOREP allows a wide range of experiment to study microbiological and geochemical processes with in situ conditions – typical for CO2 storage or related to (well, overburden condition).


All the gases and liquids can be collected under pressure or progressively degassed to avoid the risk and biases linked to decompression.


Besides those basic principal characteristics and adaptation, the BIOREP facility is divided in three different modules that allow specific approaches:  


Three reactors platform with transfer patterns that can be designed according to the desired experiment


Microfluidic and analytical lines that allow the transfer of pressurized fluids into microchips and captors/ electrodes with low consumption of experimental fluids. The microfluidic approach also allows to perform spectral (IR/RAMAN) characterization.


Closed loop build to recirculate fluids into an Hassler cell. This design is particularly suitable to experiment and assess the stabilization phases of an injected fluid through rock percolation. The module also allows to measure any loss or collapsing effect of the rock plug. It is particularly suitable to study injectivity.



Three Hassler like reactors that allow to handle different types of sample and conditions at the same time.




Areas of research




State of the Art, uniqueness & specific advantages

BIOREP allows the monitoring of microbiological systems in high pressure and dynamic conditions, which is unique. In specific, BIOREP differs from other facilities on the following properties:


  • Respect of the biologic neutrality of the containment and limit the risk of bio-corrosion associated. Most material in contact with the studied medium and biological system is Téflon or Hastelloy.

  • Sampling procedure and process adapted to micro biological material to ensure a slow decompression and avoid cell lethality related to decompression.

  • Possibility of managing independently the batch’s geochemistry and therefore to create gradients through the column between the two batches (for instance between oxic and anoxic areas).

  • Possibility to use geological laboratories on chips as well as transfer cells (Hassler cell, columns).

  • Pressure, temperature, gas consumption and regulation, flow rate, pH and redox can be monitored on line depending the designed setup and with the highest standard of precision.

Scientific Environment

The facility situated in BRGM research centre in Orléans, France, benefits from the support of the different laboratory and technicians from BRGM. The team managing BIOREP will provide support in designing and setting up experiments. In addition, chemical, biological and mineral characterization of samples can be provided by BRGM (including Raman). Modelling of the experiments and reactive transport processes is also possible and can be provided.


Operating by


Bureau de Recherches Géologiques et Minières
STORAGE technologies:
Pressure/injection, Migration, Caprock/well integrity, Leakage mitigation/remediation, Reactivity/mineralisation, Leakage, Static modelling, Dynamic modelling
UTILISATION technologies:
CO2 Conversion to Solid Carbonates, Biogeochemical Conversion and Hydrogenation of CO2
Research Fields:
Fluid dynamics, Chemistry/Geochemistry, Microbiology, Material science, Modelling, Engineering, Thermodynamics

Location & Contacts

Orleans, France
Sylvain Stephant
RICC Contacts - Secondary contact
Sébastien Dupraz

Facility Availability

Availability per year (in UA)
BIOREP Facility is typically available 8
Duration of a typical access (average) and number of external users expected for that access
The typical duration for an access is 2 UA

Quality Control / Quality Assurance (QA)

Activities / tests / data are:
Acredited To Standard: ISO9001; ISO14001 and NF-EN-ISO/CEI 17025 (solely for the analysis in the laboratory and not for the platform itself)

Operational or other constraints

Specific risks:
Handling pressurized vessels and chemicals. However, if the users are not entitled or do not want to perform the experiments themselves, we will provide assistance or replacement to perform the duty.
Legal issues:

CCUS Projects

EU-Funded CCUS Projects
FEDER funding
Other CCUS Projects
ANR CGS µlab
Private Project
IPGP Island.



Selected Publications

Chemical Geology 265, 54-62. (2009)
Experimental approach of CO2 biomineralization in deep saline aquifers.
Dupraz, S., Ménez, B., Gouze, P., Leprovost, R., Bénézeth, P., Pokrovsky, O.S., Guyot, F.
Chemical Geology 265, 44-53. (2009)
Experimental and numerical modeling of bacterially induced pH increase and calcite precipitation in saline aquifers.
Dupraz, S., Parmentier, M., Ménez, B., Guyot, F.
Comptes Rendus Geoscience 343, 246-259. (2011)
CO2 geological storage: The environmental mineralogy perspective.
Guyot, F., Daval, D., Dupraz, S., Martinez, I., Ménez, B., Sissmann, O.
10.6084/m9.figshare.7871507 (2007)
Impact of the deep biosphere on CO 2 storage performance
Ménez, B., Dupraz, S., Gérard, E., Guyot, F., Rommevaux-Jestin, C., Libert, M., Jullien, M., Michel, C., Delorme, F., Battaglia-Brunet, F., Ignatiadis, I., Garcia, B., Blanchet, D., Huc, A.Y., Haeseler, F., Oger, P., Dromart, G., Ollivier, B., Magot, M