Phase I of the LTD project runs from 2005 until 2008. During this
time,four main experiments are being carried out in situ at the
GTS.
The monopole experiment
Aims:
To study matrix diffusion in undisturbed rock
matrix and compare results of in situ, laboratory and modelling
studies.
Overview:
To
circulate a radionuclide cocktail around an interval deep in undisturbed
rock matrix for one year to simulate radionuclide transport processes
in the matrix. After circulation, the rock matrix will be removed
by large diameter overcores and the radionuclide profiles will
be analysed in detail to determine the extent of diffusion.
Outcomes:
Computer models for matrix diffusion will be verified
via in situ testing.
The in situ porosity experiment
Aims:
To study changes in porosity around a fracture
system, to determine the extent of connected pore space in the
matrix and to compare in situ and lab derived porosity values.
See also the PSG experiment.
Overview:
To
inject specialised resins (including radionuclide doped resins)
into a shear zone, and the matrix rock surrounding a shear
zone. New techniques for field characterisation will also
be investigated.
Investigate links between hydraulic testing, lab-derived
diffusion co-efficients and porosity changes at increasing
depths from a shear zone.
Outcomes:
Development of field characterisation techniques,
derive correction factors for lab-based porosity determinations.
Natural Tracer Study
Aims:
To find evidence of long term diffusion to support
the in situ derived data.
Overview:
Use
natural tracers (natural radionuclides, stable isotopes and
chemical signals) in the rock to provide evidence for long term
(on a repository time scale) matrix diffusion (see example on
the right from sedimentary rock in Northern Switzerland).
Outcomes:
Techniques and understanding will be developed
and evaluated to provide high quality data for PA calculations
on the extend of matrix diffusion.
Diffusion Process Study
Aims:
Locate and quantify Cs-137 concentrations in the
rock matrix and examine structural and mineralogical associations.
Overview:
Samples
from the former Excavation Project will be re-examined for evidence
of radionuclide matrix diffusion from the earlier Migration
experiment (see CRR - Radionuclide
Migration Programme - RMP ) using beta autoradiography and
gamma spectrometry techniques.