About ASC
Home
News
Downloads
Quality
Contact Us
Site Map
Services
Overview
Petroleum
Geothermal
Mining
Rad Waste
CO2 Storage
Engineering
Lab Testing
Software
InSite Software
InSite Modules
Licensing and Support
Custom Solutions
Demo Download
Hardware
Monitoring
Systems
OMNIBUS Range
Sensors
Data Acquisition
Research
Publications
Example Studies
External Links
Client Area
News
Releases
Manuals
Licenses
Support
InSite FAQ
Change Password
News
InSite v2.15a
ASC is pleased to announce the release of version 2.15a of InSite seis...
ASC at ARMA Symposium 2010
ASC at Second European Geothermal Review
Employment Opportunities
Workshop on Monitoring Technologies
ISO 9001:2008
Publication Abstract
not signed in
Log In
Title
The assessment of damage around critical engineering structures using induced seismicity
Authors
Pettitt, W.S., C. Baker, R.P.Young, L-O Dahlstrom and G Ramqvist
Publication Reference
2002, Pure and Applied Geophysics,
159
, 179 - 195
Abstract
Two large-diameter boreholes have been excavated vertically from the floor of a tunnel at the Äspö Hard Rock Laboratory, Sweden. The two deposition holes will have simulated high-level radioactive waste canisters installed in them in an experiment undertaken to test the retrievability of waste from a proposed repository. Induced seismicity and other acoustic monitoring techniques have been used to investigate the Excavation Damaged Zone (EDZ) around the two holes. High-frequency acoustic emission (AE) monitoring has been used to delineate regions of stress-induced micro-fracturing on the millimetre scale. This is shown to locate in 'breakout' regions orthogonal to the maximum principal stress and clustered spatially around pre-existing macroscopic fractures. Three-dimensional velocity surveys have been conducted along ray paths that pass through the damaged region and through a stress-disturbed zone around the excavation. Induced micro-fracturing and stress disturbance are observed as sharp decreases in velocity as the excavation proceeds through the rock mass. The combination of the high-resolution velocity measurements and the AE source locations has allowed the linking of the velocity measurements to a volume of excavation damaged rock. This then provides a quantitative estimate of the effect of the EDZ on the rock mass.
Key Figure
Link
http://link.springer.de/link/service/journals/00024/papers/2159001/21590179.pdf
Return to publications list
<
Return to the home page
::
Contact Us
Applied Seismology Consultants
An Itasca International Company