The Grimsel Test Site website operates the same data protection policy as Nagra https://www.nagra.ch/
Full details can be found here : Nagra's data protection policy
For a fully detailed technical overview of the Grimsel geology please view : Geology of the Grimsel Test Site (GTS)
Around 300 million years ago, granitic melts solidified at a depth of around 10 - 13 km. The volume of the rock decreased due to cooling and deep fracture systems formed. Residual magma rose through these to form dyke rocks (lamprophyres and aplites).
The rocks of the Aar Massif remained virtually undisturbed for more than 200 million years. Extensive deformation of the rock body then began during the course of the alpine orogeny, around 40 million years ago. The Aar Massif subsided and was overlain by the alpine nappes moving towards the north.
At the time of maximum overburden (approximately 12 km), the rock was exposed to high temperatures (around 450°C) and pressures (around 300 MPa). The main schistosity and shear zones were formed during this period.
The crystalline rock in the Grimsel area has long been thought of as a "Massif", a large block of crystalline basement pushed up through the overlying sediments. However, recent observations in the new Lötschberg railway tunnel indicate that it is, in fact, a massive thrust sheet, overlying sediments in some areas.
In the uplift phase - still continuing with a rate of around 0.5 to 0.8 mm per year today - the tension joints with their beautiful crystals (see The Crystal Cave) were formed around 16 million years ago.
Full-Scale Emplacement (FE) Experiment, Nagra participation in the EU project
Large Underground Concept Experiments (LUCOEX)
Invitation
to the presentation of the FE backfilling machine
on Monday 19th of May 2014 starting at 3pm and
to dinner in the evening, followed
by a one-day workshop on
bentonite material production & emplacement
on Tuesday 20th of May 2014
from 9am until approx. 4pm.
Location
The presentation and workshop will be
held in the facilities of Belloli SA
in Grono GR, Switzerland
(https://goo.gl/maps/jeU9K).
Please don't hesitate to contact Ms. Fankhauser (+41 56 4371 339
We would be pleased to welcome you in Grono!
Herwig R. Müller (Nagra), PM of the FE experiment
Hanspeter Weber (Nagra), LUCOEX work-package leader
The FE Experiment is a 1:1-scale heater experiment investigating the THM-coupled effects on the engineered barrier system and on the host rock (Opalinus Clay), which will be installed and run in the Mont Terri underground research laboratory.
Mont Terri Webpage : http://www.mont-terri.ch
Bentonite Block Pedestal Load Tests carried out at the Grimsel Test Site
A multi-barrier approach ensures the long-term isolation of radioactive waste and is the adopted solution of preference for radioactive waste management. The Engineered Barrier System (EBS) is one part of this passive multi-barrier system approach and it refers to all barriers introduced through technological (engineered) activities. It is complemented by the natural barrier, also referred to as the geological barrier or geosphere.
Most of the experiments running at Grimsel are focusing on using in-situ tests to analyse and characterise the near field of a nuclear waste repository. The near field includes the Engineered Barrier System (EBS) and the immediate rock surrounding a repository. In Nagra's concept, the disposal tunnels and caverns are placed deep underground (from around 600m) and in stable rock formations. Slightly different disposal methods are envisaged for the high level waste (HLW - spent fuel rods from reactors or vitrified waste) and the intermediate to low level waste (I/LLW - industrial waste). These two concepts are explained below.
Nagra's concept for an underground nuclear waste repository
The high level waste is contained within large steel disposal canisters.
These canister are placed on bentonite pedestals within the disposal tunnel at regular intervals, and the tunnel backfilled with bentonite.
Nagra's high level waste (HLW) disposal concept - cutaway
Video overview of disposal concept for High Level Waste (HLW)
Grimsel experiments which are relevant to the high level waste (HLW) concept are :
Low level waste is contained within steel drums, and these steel drums are placed into concrete disposal casks, and filled with mortar.
The disposal casks are stacked into the low level waste disposal caverns which are lined with concrete. When full, the caverns are backfilled with mortar.
Nagra's low level waste disposal cavern concept - cutaway
Nagra's low level waste disposal cavern concept - cutaway - close-up
The low level waste (LLW) disposal cavern is shown below during the operational phase, and when it has been backfilled with mortar and sealed.
Nagra's low level waste (LLW) disposal concept - operational
Nagra's low level waste (LLW) disposal concept - backfilled
Video overview of disposal concept for High Level Waste (HLW)
Grimsel experiments which are relevant to the low level waste (LLW) concept are :
Since 1984 the Grimsel Test Site has been carrying out a wide range of investigations in many fields, including geology, geophysics, hydrogeology, rock mechanics and radionuclide transport. The scientific work performed has been already shown to over 50,000 visitors and has been presented in many papers at conferences or published in scientific journals. Presently the existing projects are running under Phase VI (See here for full history of experiements ).
Three Phase V projects, FEBEX, HPF and GMT were officially extended into 2005. This allowed a greater volume of high quality data to be collected from these projects where long term monitoring is a fundemental part of the investigation.
In general, the Phase VI projects are focusing on :
The following projects are presently running at the Grisel Test Site. Full details are available following the links.
The CFM experiment looks at the role played by colloid () generation rates and mechanisms at the Engineered Barrier System (EBS) – host rock boundary under in-situ conditions. The formation and transport of colloids and colloid-associated radionuclides is monitored under repository relevant flow conditions and over relevant distances.
CFM concept layout - click for a larger image
The initial aim of the FEBEX experiment, back in 1997, was to study the behaviour of the nearfield components (Engineered Barrier System, host rock) for a high-level radioactive waste repository in crystalline rock. Detailed understanding of early time coupled processes is needed to predict the nearfield evolution in terms of evolution of thermal conductivity of partially saturated buffer, the role of thermal convection, the on-set of corrosion/gas production, gas transport capacity of the nearfield (saturation history) and the geochemical evolution of the nearfield (e.g. iron/bentonite interactions).
FEBEXe - during construction, and computer model of the HLW disposal concept
The FORGE experiment aims, under realistic boundary conditions, to obtain larger scale (decimetre scale) 2-phase flow properties for host rock and EBS materials, to assess and visualise gas and water flow in sand/bentonite mixtures and to demonstrate the functioning of gas permeable plugs and seals on a decimetre scale.
Figure 1: Drawing of the mock-up experiment with the steel cylinder confining the experiment, mortar discs at moth ends (grey/brown), the S/B seal (brown/yellow), the pure bentonite (yellow) and the ring-TDRs (black). Instruments are schematically indicated to show the locations of the monitoring levels.
The overall aim of the LCS project is to increase the understanding of high-pH cement interaction effects in the repository near field and the geosphere in order to make confident, robust and safety-relevant predictions of future system behaviour, irrespective of repository host rock, engineered barrier system (EBS) and waste type. This requires an improved thermodynamic database and a refinement of existing modelling tools
Long Term Cement Studies (LCS) Concept
This is a long-term, large-scale experiment which aims to further examine in-situ matrix diffusion and pore space visualisation at the Grimsel Test Site
long Term Diffusion concept
A vital aspect of Nagra's involvement is, beside the further monitoring of water content changes in the bentonite buffer, the refinement of the TDR technique as a method for water content measurements in low porosity rock formations. Since 1996, the TDR probes are monitoring the evolution of the EBS system. The laboratory experiment will feed into the ongoing FEBEX long-term monitoring programme at the GTS by providing new calibration functions for the granite probes. Post-processing of the entire TDR data base will provide an updated TDR data set for the FEBEX master data base
Experimental Setup
This is an in-situ resin impregnation experiment which aims to visualise connective porosity and open pore spaces available for matrix diffusion in intact rock matrices.
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The production of gas will occur during the life of the Engineered Barrier System (EBS). The GAST test looks at the effective functioning of gas permeable seals at realistic scale and with realistic boundary conditions, the validation and, if necessary, improvement of current conceptual models for the re saturation and gas invasion processes into S/B seals.
Schematic picture of the GAST experiment layout with the 8-10m long sand/bentonite plug in between two gravel packs.
The full-scale low-pH shotcrete plug was constructed in 2007 in the context of ESDRED and the TEM project has been part of the experiment set-up right from the start. While the overall goals are to demonstrate the construction feasibility and to test the support capacity of the plug, the objectives of the TEM project are to investigate the efficiency of an existing wireless magneto-inductive (MI) transmission technique and to evaluate seismic tomography as a non-intrusive monitoring technique.
Perspective view of the experimental layout and monitoring installations
The aim of CRIEPI’s in-situ experiments at the GTS is to demonstrate the performance of newly developed technologies for fracture characterisation and tracer testing. The relevant parameters of the investigations are fracture aperture and geometry.
Japanese research teams and GTS staff at the C-FRS site. Photo: comet.
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