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Gas Migration in Shear
Zones (GAM)
In-situ Tests |
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The initial phase included a series of hydraulic cross hole tests
to characterise the water flow through the shear zone.
A series of dipole tracer tests were carried out using different
tracers:
- Solute tracers (non-reactive tracers e.g. fluorescent
dyes).
- Particle tracers (microspheres / nanospheres and pharges).
- Gas tracers (helium, xenon, argon and SF6
(sulphur hexafluoride
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Solute and Particle Tracer Tests
Five successful tracer tests were carried out with non reactive
solute tracers.
Tracer recovery was high, but particle tracer tests showed a strong
dependency of tracer recovery on the orientation of dipole field.
A series of Radar Reflection surveys were also carried out during
gas injection tests. Radar surveys were conducted before the start
of the gas injection and then 1, 5 and 22 hours after the start
of the injection. The reflectograms obtained from these survey indicate
that the gas propagated through the shear zone by displacing the
pore water.

The difference in the reflectograms is shown after 1hour, 5 hours
and 22 hours of gas injection. This technique allows the visualisation
of the gas flow path.
After 5 hours significant changes in the reflectograms could be
seen, and after 22 hours the flow field seemed to stabilise. The
gas distribution agreed with the results of the hydraulic tests
which suggested these were the most likely flow paths in the shear
zone.
Gas Tracer Tests.
11 gas injection tests in total took place at the GTS. The dipole
distances were between 1 and 2 meters and a wide range of gas injection
rates were applied.
The retardation of the more soluble gases was surprisingly low
and the breakthrough times were short (breakthrough time refers
to the time elapsed between addition of tracer and its first arrival
at the extraction end).

The diagram above represents the experimental set
up for the gas tracer tests of the in situ test. A controlled flow
of gas is injected into the injection interval. The shear zone is
isolated via hydraulic packers at both the injection and extraction
boreholes. The extracted water/gas mixture is separated and the
gaseous portion is sent to a mass spectrometer for analysis of the
gas fraction (see photo below).

For each experimental run graphs were produced of
the gas concentrations measured at the extraction side of the experiment.
The graph below shows that the injected gas He, Ar, SF6
and Xe behave similarly in the shear zone and recovery is around
100 % for each of these gases. H2S had a
low recovery rate and this is thought to be due to the reactivity
of the H2S within the injection and extraction
equipment of the test (H2S gas was in a N2
carrier gas).

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