Andra
Centre de Meuse/Haute-Marne BP9 55290 Bure, France

STORAGE

URL-Andra (FR2.1)

Underground research laboratory - Andra

 

Since 1999, Andra has been investigating and characterizing the Callovo-Oxfordian clay layer which could host a reversible deep geological disposal for High-level and Intermediate-Level Long-Lived radioactive Waste (Cigéo project). The site selected is located on the eastern boundary of the Paris Basin (Meuse/Haute Marne region). Claystone formations, due to in particular a very low permeability and high confining properties, are indeed candidates to host a radioactive waste disposal. In this region, the Callovo-Oxfordian formation lies between around 420 m to 600 m deep, and its thickness is at least about 130 m. The Callovo-Oxfordian formation is surrounded by two main calcareous formations (Dogger and Oxfordian). The characterization studies are carried out thoroughly in a specific site where is implemented an Underground Research Laboratory within the Callovo-Oxfordian formation, called “Meuse/Haute Marne URL” (MHM URL).

    More than 15 years of research and development works have been carrying out in this URL to support the main milestones and reports of the Cigéo project. The MHM URL will continue to play a key role for the next steps of the Cigéo project. Due to an important network of drifts available (Figure 1), the MHM URL could be open for experiments not focused on radioactive waste management such as CO2 studies in the framework of ECCSEL. The MHM URL has been granted to operate until 2030 allowing to envisage long term experiment if required.

 

Brief technical description with picture and/or diagram

 

The MHM URL consists in (Figure 1):

 

  • 2 shafts of 500 m (one of 4 m and the other of 5 m of diameter);

  • 1 drift 40 m long at –445m (upper part of Callovo-Oxfordian clay formation, more rich in calcite) from the ground surface;

  • A current network of more 1.8 km of drifts located at – 490m (corresponding to the middle of the clay layer with the highest clay minerals content). The sections of drift vary between 18 and 60 m2

  •  according to scientific and technological objectives. About 850 boreholes been drilled in all directions (vertical up and down, horizontal, oblique) up to 100 m long, in a wide range of diameter between 22 mm and 350 mm. The purposes of these boreholes are very large (Figure 2):

  • R&D objectives: geological survey, hydrogeological, geochemical, microbiological and rock mechanical studies;

  • Characterisation of anthropic impacts: temperature, excavation and ventilation, alkaline plume etc.

  • Technical aims: excavation and support (lining) techniques.

 More than 12 000 sensors have been installed in the rock, inside boreholes, in the drifts, in the shafts, allowing a continuous monitoring at distance. The type of sensors tested is very large according to concerned Thermal, Hydraulic, Mechanical, Chemical and Radiological domains: from very classical sensors (ex. pressure/temperature) to the development of innovative optic fiber with distributed measurements and sensors for thermal and mechanical long term monitoring.

Specifically for fluids, experiences in continuous pH and redox measurements are online. Direct analyses (by chromatography or spectrometry) underground are also possible.

Hydro-mechanical and geochemical characterisations of clay (deep) formations are commonly assessed in the context of nuclear waste geological repository and could be easily adapted to CO2 storage experiments where clay plays the role of cap-rock in this case. Hydro-mechanical responses of clay solicited by gas injection have been conducted in the MHM URL in order to assess hydro-fracturing characteristics of the Callovo Oxfordian clay formation. This in situ large scale gas injection test called PGZ experiment, started in 2009 (and with a new experiment in preparation in 2020), allows us to investigate gas migration mechanisms in clay materials and to define in particular:

  • Gas entry pressure

  • Gas pathway dilation

  • Gas migration parameters at large scale

  • Fracturing pressure

 

Thus, N2 was injected at various pressure steps up to 98 bars and the data collected might be used for CO2 injection experiments. The MHM URL has also a good experience in the field of microbiological and geochemical experiments (cleaning procedures for drilling tools and borehole equipment, use of argon as drilling fluid to avoid oxygen impact, download equipment made exclusively of inert material, sampling protocols) and to study these processes with in situ conditions (PAC, BAC, POX experiments).  

 

Areas of research

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Installations

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State of the Art, uniqueness & specific advantages

In France, the MHM URL is the only facility accessible for in situ experiments in a deep clay formation at 500 m depth, with a hydraulic pressure of 46 bars and a vertical stress of 12MPa, allowing to perform different tests from small scale to large scale and in representative conditions of these ones of a cap-rock for capture and storage CO2 concept.

Andra has collected a large number of data concerning the properties of the Callovo-oxfordian clays at different scales (I.e. from the pore scale up to the scale of the geological formation) which will be available to support new projects. Surrounding calcareous formation were also investigated. Thus, the geological environment is already well defined and it would not be required to plan a lot of analyses to be characterised. The overall operating and maintenance works of the MHM URL is operated by Andra. This high cost will not be charged on ECCSEL projects.

Scientific Environment

The MHM URL benefits from the support of Andra’s technicians and engineers: 40 scientists of Andra specialized in geology, rock mechanic, hydrogeology, chemistry, fluid transfer, biology, corrosion, sensors and data acquisition system, work on site. A specific team provides support in designing and setting up experiments. Several contractors used to work in the MHM URL can give support in specific domains (drilling, geological survey and sampling, chemical, biological and mineral characterizations). It’s also possible to perform in situ gas and fluid analyses (by ionic chromatography, or Raman spectrometry…). Andra has also a hall for technological demonstrators on MHM centre that could be accessible to people involved in ECCSEL projects.

 

To achieve all objectives, Andra has developed an important network of collaboration with others scientific partners as experts in their domains

EU funded projects: Lucoex (large scale heating of Callovo-Oxfordian formation); Modern2020 (development of in situ monitoring for survey of repository); Cebama (properties and long term in situ evolution of cementitious material/component)

Operating by

Andra

Andra
France
STORAGE technologies:
Pressure/injection, Migration, Reactivity/mineralisation, Microseismicity, Monitoring
Research Fields:
Chemistry/Geochemistry, Geology/Geophysics, Mechanics/Geomechanics, Monitoring, Physical processes, Engineering

Location & Contacts

Location
Centre de Meuse/Haute-Marne BP9 55290 Bure, France
Contacts
Gilles Armand
RICC Contacts - Secondary contact
Aliouka Chabiron

Facility Availability

Availability per year (in UA)
The experiment may be available all year round and the data are remotely accessible.
Duration of a typical access (average) and number of external users expected for that access
Depend on the experiment, but a few years is a common duration.

Quality Control / Quality Assurance (QA)

Activities / tests / data are:
Controlled: ISO9001 et ISO14001

Operational or other constraints

Specific risks:
-Respect of safety rules defined by Andra, wear safety equipment, French medical ability for underground works; -In case of need to use supercritical CO2, a meeting with safety engineer will be necessary to define this possibility -The concept of the experimental set-up should be validated by Andra for safety reasons and co-activity management.
Legal issues:
n/a

CCUS Projects

Selected Publications

Journal of Hydrology, 521, 141-156 (2015)
Gas and water flow in an excavation-induced fracture network around an underground drift: A case study for a radioactive waste repository in clay rock
De La Vaissière R., Armand G., Talandier J.
Analytical methods, 3, 877-887 (2011)
FT-IR metrology aspects for on-line monitoring of CO2 and CH4 in underground laboratory conditions
ailteau C., Pironon J., De Donato P., Vinsot A., Fierz T., Garnier C., Berreso O.
Applied Geochemistry, 49- 168-177 (2014)
Hydrogen uptake and diffusion in Callovo-Oxfordian clay rock for nuclear waste disposal technology
Bardelli F., Mondelli C., Didier M., Vitillo J., Cavicchia D., Robinet J-C., Leone L., Charlet L.
Applied Clay Science, 88–89, 1-9 (2014)
Impact of high-pH fluid circulation on long term hydromechanical behaviour and microstructure of compacted clay from the laboratory of Meuse-Haute Marne (France)
Cuisinier O., Deneele D., Masrouri F., Abdallah A., Conil N.
Analytical methods, 3, 877-887 (2011)
FT-IR metrology aspects for on-line monitoring of CO2 and CH4 in underground laboratory conditions
Cailteau C., Pironon J., De Donato P., Vinsot A., Fierz T., Garnier C., Berreso O.

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