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Gas Migration in Shear
Zones (GAM) Laboratory Studies |
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The laboratory tests were focused on three main issues.
- Development of new coring techniques to recover undisturbed
shear zone samples
- Porosity and permeability measurements
- Visualisation and structural analysis of pore spaces in
a shear zone sample
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Development of new coring techniques to recover
undisturbed shear zone samples. (Sandia Labs)
Innovative coring techniques have been implemented both in the
field and in the laboratory to minimise damage to the shear zone.
These techniques were used to obtain porosity, permeability, and
pore visualisation specimens from matrix and shear zone materials.
Porosity and permeability measurements.
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Porosities are shown as a function of effective confining
pressure for Core #1. This core sample includes both shear zone
and matrix material. Porosity is less than 1% and decreases
with increasing effective confinement |
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Gas permeabilities were obtained at a constant effective confining
pressure (2.1 MPa for these data), but at different combinations
of pore and absolute confining pressures. The permeabilities
are plotted as a function of reciprocal pressure to obtain Klinkenberg-corrected
permeabilities. |
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Relative permeabilities were measured in September and December
of 1998. The water permeability curves are essentially continuous
for the two measurements; however the gas (N2)
permeabilities are not. As water saturation increases the gas
permeability drops. Intrinsic liquid permeabilities measured
at 100% saturation are also shown. |
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Capillary pressure measurements begin with a liquid-saturated
specimen. Gas (nitrogen) pressure is incremented in steps at
the sample inlet. At each gas pressure, the specimen reaches
equilibrium as the gas pushes some of the liquid out of the
specimen. |
Visualisation and structural analysis of pore
spaces in a shear zone sample.
X Ray Tomography
The image below (diameter 9mm) was record using X-ray tomography
of one of the successfully removed rock cores. X-ray tomography
is a non-destructive technique which allows us to visualise the
inside of the rock cores without actually slicing them up. It is
similar to CAT scans used in medicine and produces 2D slices. Click
on the X-ray tomography picture to see these images linked up into
a virtual trip through the core, the core is the lighter cylindrical
shape in the centre and the darker areas observed in the core are
pore space.

Click on image to view animation
(550 KB mpeg)
Laser Scanning Confocal Microscopy (LSCM)
(Sandia Labs)
3D imaging with was carried out using Laser Scanning Confocal Microscopy
(LSCM):
- Illumination and detection are confined to a single location
in specimen at any time
- Improved resolution to theoretical limit set by Rayleigh diffraction
(~0.2 micron)
- Capability for optical sectioning (distribution of fluorescence
intensity in xyz space)
A schematic of the instrumentation is shown below.

This technique produces images which allow the surface porespace
of the samples to be visualised. The image below is a low magnification
view of region within several mm-wide
macroscopic shear zone
Higher magnification images can also be taken.
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Block-like microcracking in phenocryst within shear zone
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High-resolution image illustrating sharp transition to region
with no porosity
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Higher magnification view of region within macroscopic shear zone
, illustrating bimodal porosity distribution within shear zone
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