Rock-Fluid
Interaction
The
previous
two
chapters described
the
data needed
to
model
the
solid
structure
of the
reservoir
and the
behavior
of
fluids
contained within
the
solid
structure. Small-scale laboratory measurements
of fluid flow in
porous media
show that
fluid
behavior
depends
on the
properties
of the
solid
material.
The
interaction between rock
and fluid is
modeled using
a
variety
of
physical
parameters that include relative permeability
and
capillary pressure
[Collins,
1961;
Dake,
1978;
Koederitz,
et
al.,
1989].
Laboratory measurements provide
information
at the
core scale (Macro Scale) and,
in
some cases,
at the
micro-
scopic
scale (Micro Scale). They
are the
subject
of the
present chapter.
14.1 Porosity, Permeability,
Saturation,
and
Darcy's
Law
Porosity, permeability,
and
saturation
can be
obtained
from
Mega Scale
measurements such
as
well logs
and
well tests,
and by
direct measurement
in
the
laboratory. Comparing values
of
properties obtained using methods
at two
different
scales demonstrates
the
sensitivity
of
important physical parameters
to
the
scale
at
which they were measured. Ideally there will
be
good agreement
between
the two
scales; that
is,
well
log
porosity
or
well test permeability
will
agree with corresponding values measured
in
the
laboratory.
In
many cases,
however,
there
are
disagreements. Assuming measurement error
is
not
the
source
of
disagreement, differences
in
values show that
differences
in
scale
can
impact
the
measured value
of the
physical parameter.
A
well test permeability,
for
example,
represents
an
average over
an
area
of
investigation that
is
very large
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