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Naturally fractured reservoirs
Nuclear waste disposal
Salt related deformation
Basin structure evolution
CO
2
and gas storage in salt caverns
R&D
JIP
Contact
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Home
About
Services
Naturally fractured reservoirs
Nuclear waste disposal
Salt related deformation
Basin structure evolution
CO
2
and gas storage in salt caverns
R&D
JIP
Contact
You
Wol
Geoscience Services
CO
2
and gas storage in salt caverns
CONTACT US
Case study: Nothern Europe
Context
Client
: Some data used are collected from existing scientific publications on the Epe repository site.
Location
: Germany, Europe
Main goal
:
Man-made caverns to store CO
2
and other gas. Model stability and related surface subsidence.
Geology
: Zechstein salt
Tectonic
: Permian European Basin
Methodology
Data analysis and interpretation
3D model of exisiting or planned caverns
3D present-day stress models around interacting caverns (ARCH)
Subsidence modeling based on existing and/or planned caverns (ARCH)
Other applications using similar methodology
This workflow for modeling man-made salt caverns can also be applied to:
Mining
Tunneling
Nuclear waste disposal
Main outcomes
Cavern network data
The main data on salt cavern are:
• Location and depth of salt cavern network at repository site
• Shape of each salt cavern measured from sonar survey
• Subsidence caused by salt cavern network over time and measured withe GPS stations and/or satellite data (InSAR)
Cavern shape reconstruction
The main data on salt cavern are:
(a) Example of cavern shape data obtained by sonar survey
(b) Reconstructed cavern shape from sonar survey data;
(c) Meshed cavern with triangular elements suitable for 3D geomechanical simulations (ARCH)
Cavern mechanical interaction
• 3D stress field is computed (Arch) around two mechanically interacting salt caverns.
• The caverns can be modeled as empty or pressurized cavities.
• Rock mechanical properties are set in Arch as well as the 3D far field stresses (magnitudes and orientations).
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Subsidence caused by cavern network
Measured (2006) and geomechanically modeled (Arch) subsidence caused by salt cavern network.
The observed subsidence has been taken from Sroka et al. (2018) on the Epe salt repository site (Germany).
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