T. Bruel et al., Relationship between hydrodynamics and open fractures in a fractured system compartmentalised by faults and confirmation of a double fracture porosity, B SOC GEOL, 170(3), 1999, pp. 401-412
Hydrodynamic characterisation of real fracture systems is necessary to impr
ove modelling of fracture reservoirs as well as nuclear waste disposal site
s. This characterisation is usually considered globally and theoretically b
ut very few studies have aimed to identify the real physical environment of
flow (matrix, faults, joints etc.) before establishing hydrodynamical mode
ls.
We present a case study in a fractured reservoir aiming to give an example
of how and why fluids actually flow within a given fracture at the various
scales of fracturation of a fracture network.
This study demonstrates that the determination of type and orientation of f
ractures actually supporting flow is necessary for accurate interpretation
of the pumping tests within a fractured reservoir. It also shows that there
is no simple relationship between the fault offset and the importance of f
low, probably due to the influence of in situ stress. It is shown that the
combination of various methods can be used to determine the fracture-flow r
elationship and behaviour at subseismic scale in subsurface conditions.