Part
I:
Reservoir Engineering Primer
71
successful
commercial
microbial
EOR
projects.
The
projects
reflected
a
diversity
of
locations, lithologies, depths,
porosities,
permeabilities,
and
temperatures.
Two of the
projects were
in the
U.S.,
two in
China,
and one in
Argentina,
and
included
sandstone, fractured dolomite, siltstone/sandstone,
and
fractured
sandstone
reservoirs.
Reservoir depths ranged
from
4450
to
6900 feet, tempera-
tures
from
110°
to
180°
F,
porosity
from
0.079
to
0.232,
and
effective
permeabil-
ity
from
1.7
to
300
md.
Evidence
from
laboratory research
and
case/field studies
shows
that microbial
EOR
processes
can
result
in the
incremental recovery
of
oil
and
also reduce water production
from
high permeability zones. However,
more
research needs
to be
done
to
maximize
the
potential
for
microbial EOR.
Some
effort
in
this direction
has
been conducted.
A
microbial transport simulator
was
developed under
the
auspices
of the
U.S. Department
of
Energy
as
a
modification
to the
black
oil
simulator BOAST.
8.3
Nonconventional
Fossil
Fuels
Clean
energy refers
to
energy that
is
generated with little environmental
pollution. Natural
gas is a
source
of
clean energy.
Oil and gas fields are
considered conventional sources
of
natural
gas.
In
the
following,
we
discuss
two
nonconventional
sources
of
natural gas:
coalbed
methane,
and gas
hydrates.
(oalbed
Methane
Coalbeds
are
an
abundant source
of
methane
[Selley,
1998;
Rogers,
1994].
The
presence
of
methane
gas in
coal
has
been well known
to
coal miners
as a
safety
hazard,
but is now
being viewed
as a
source
of
natural gas.
The gas is
bound
in the
micropore
structure
of the
coalbed.
It is
able
to
diffuse
into
the
natural
fracture
network when
a
pressure gradient exists between
the
matrix
and
the fracture
network.
The
fracture
network
in
coalbeds consists
of
microfractures.
The
microfractures allow Darcy
flow and are
called
"cleats."
Gas
recovery
from
coalbeds depends
on
three
processes
[Kuuskraa
and
Brandenburg,
1989].
Coalbed methane exists
as a
monomolecular
layer
on the
internal surface
of the
coal matrix.
Its
composition
is
predominately methane,
but
can
also include other constituents, such
as
ethane, carbon dioxide, nitrogen
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