Range of RACOS® services,
advantages and unique features
RACOS® is a comprehensive procedure for determining from core samples
3D values of important in situ parameters such as stresses, elasticity
and deformability, as well as the effects of pore pressure change on
these values1.
The basic laboratory measurements are made on samples taken from core
from the zone of interest. These measurements determine the spatial
seismic anisotropy and the 3D dynamic elastic parameters. From the measured
data the 3D effective in situ stresses are derived directly. They are
essential for stability analysis and sanding evaluations2.
The determination of the pore
pressure effectiveness (3D Biot coefficient) is necessary for the calculation
of the total in situ stresses. The 3D in situ total stresses3
are required for frac planning. The 3D pore pressure effectiveness (also
derived from the laboratory measurements) can be used to evaluate preferred
in situ flow directions.
Supplementary investigations
can be made to determine in situ stress conditions after the pore pressure
has changed and/or under paleo conditions, to evaluate recent tectonic
stress components and (if not already available) for the geographic
reorientation.
On the basis of
the laboratory measurements, without additional stress-strain tests,
3D elastic and total deformation parameters can be determined for relevant
loadings. The measured propagation velocities of elastic waves can be
used to correlate sonic log data with in situ parameters. The orientations
of the 3D parameters can also be used to define principal directions
for plug preparation for further investigations of 3D properties (permeability,
strength).
The determination
of the complete 3D magnitudes of in situ stresses and important rock
parameters is offered on the basis of RACOS® core analyses. No work
is required at the drilling site, and the analyses can be carried out
at any convenient time. No assumptions are necessary about parameter
values or constituitive laws for the rock.
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1
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3D strength parameters
can be determined with on additional laboratory testing.
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2
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The total
stress is the external loading against which the internal loading (the
pore pressure) acts. Its vertical component corresponds to the total
overburden pressure and the minimum total stress component corresponds
to the closure pressure of a hydraulic frac.
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3
|
The total
stress is the external loading against which the internal loading (the
pore pressure) acts. Its vertical component corresponds to the total
overburden pressure and the minimum total stress component corresponds
to the closure pressure of a hydraulic frac.
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