Petrophysical
Modelling
Porosity
It sounds simple, but modelling of porosity is perhaps
the most important parameter to estimate during the modelling process.
The best starting point is core plug data as this measurement refers
to the pores that can be occupied by Helium (all pores sizes, but not
bound water, -OH). The Helium porosity can be adjusted to reservoir conditions
by allowing for overburden.
Are the core plugs representative?
Are they on depth with wireline logs?
The wireline logs measure porosity by a variety of techniques,
but all are affected by rock density, bound water and the borehole conditions
to some extent. An environmentally adjusted density - neutron combination
log will provide a good measurement in a clean lithology. The petrophysicist
will attempt to eliminate the bound water (“shale”) from
the readings and calculate an effective porosity that can be calibrated
to core plug data. This is sometimes known as effective porosity, but
the definition varies somewhat from person to person. For purposes of
calculating static volumes and hydrocarbons-in-place, the effective porosity
is a good estimate (See Slideshow, Slide
7).
Are there any wells where the porosity logs look suspect?
A quick model with a few layers may
identify wells where there is a shift that cannot be explained geologically
By what method was the porosity calculated and is
it a consistent for all wells?
The common errors are inconsistent
fluid or rock densities
Has the calculated porosity been adjusted to core
plug data (where present)?
Thus may or may not be required
Are there any thin alternating sand and shale intervals
where the logs are not fully responding to the sand beds?
Core plugs may be biased towards the best sands in interbedded
sequences.
Permeability
Permeability is obtained primarily from core analysis data.
In case there is no core, then analogue field data should be used. Routine
core analysis data is measured as permeability to air at surface conditions.
At some point in the workflow of the petrophysicist, geologist or engineer,
this needs to be adjusted to liquid permeability at reservoir conditions.
Estimation of permeability in the uncored intervals is
always subject to uncertainty. This is where identifying the facies can
have an important influence on the final permeability distribution. The
most useful method is the permeability- porosity cross plot of core plug
data as this is not affected by log-core depth shifts. A porosity – permeability
relationship can often be derived, but in some cases the scatter is so
wide that it is meaningless. Other logs that can be used to estimate
permeability are GR and density-neutron separation or NMR logs. Bear
in mind that when using exponential relationships, a change in porosity
from say 0.22 to 0.24 can result in a large change in the calculated
permeability, so correct porosity estimate is important, with a check
needed for extreme values.
When deriving permeability from porosity a statistical
relationship is recommended as it is often more representative of the
actual heterogeneity and should give better dynamic results. A method
such as co-kriging can be used with a correlation coefficient of 0.7
for instance. This is different to the fixed relationships used traditionally
by reservoir engineers.
Where are the high permeability intervals?
How far laterally are these expected to go?
Does well test data fit the calculated permeability
(perm*height)?
Are high permeability intervals related to geological
facies?
Net Reservoir
Net reservoir is that where a significant proportion of
fluid is expected to flow under the reservoir conditions. That infers
a permeability cut-off, but as permeability cannot be directly measured,
other cut-offs are frequently used, such as porosity < 0.1 or Vshale > 0.4.
The wells can be subdivided into net and non-net intervals
accordingly. A particular zone on a log may have a NTG of say 0.6. Unlike
traditional mapping, it is not essential to map this NTG as a continuous
property and often is causes confusion. It is better to model net and
non-net facies (0/1) or use a cut-off after the modelling has been done,
otherwise the benefits of the 3-D modelling are diluted.
There is another stage in the dynamic realm for the engineers
to consider. Not all the net porosity is occupied by hydrocarbons that
can move. That is where special core analysis parameters can be used
to estimate pore size distribution and capillary pressure. From this
parameters such as irreducible water and residual oil can be estimated
that will help to calculate mobile oil under particular reservoir conditions.
Blocking of Well Logs into the Modelling Grid
The first property modelling step is to sample the well
logs into the modelling grid at the well positions. If the layering is
fine enough, then this is straightforward. It is best to make the non-net
intervals in the well log curves indeterminate so that they are not included
in the net cell values, i.e. for porosity and permeability. Avoid using
special averaging methods, for a first pass at least, unless there is
a particular strong reason. The key step is to compare the well log curves
with the blocked well logs and check distribution histograms for net,
porosity and permeability.
If thicker cells are required, often due to the number
of cells that can be handled in the dynamic realm, then care must be
taken that the log readings are not averaged out too much, resulting
in lack of clear cut property layers and often leading to an underestimate
of overall permeability in the reservoir.
Don’t forget, the reservoir engineering model behaves
according to porosity and permeability, facies are not used. Extensive
facies modelling is useless for dynamic work unless it reflects changes
in permeability.
3-D Petrophysical Modelling Methods and Algorithms.
The method selected will depend on the number of wells
and their spacing. It is common for the wells to target the best reservoir
and they will not always represent the whole hydrocarbon volume being
modelled. The geological model or facies model will influence how the
properties are extrapolated away from well data points. Note that changing
the correlation will change the interval being extrapolated.
It is best to start with a simple method such as moving
average to see if any trends are apparent. Kridging is a good method
for identifying trends across the whole field and works well for thin
beds that are believed to cover a large area such as shorefaces.
Beware of unwanted abrupt changes in properties at the
boundary of facies. This can occur if the facies are modelled independently.
It is possible to use the facies as a guide rather than modelling the
properties separately (See Slideshow, Slide
8).
Sequential Gaussian Simulation uses the statistical distribution
of the well data and this can be used to generate lateral heterogeneity
or indeed smoother patterns. A secondary property can be used to influence
the result, such as a seismic attribute or a previously generated property.
The main task in petrophysical modelling is to generate
areal variations in properties that attempt to reflect the geology and
honour the well data. At the same time, it is usually required for the
non-net facies, porosity and permeability to have similar trends, but
with an element of heterogeneity. Vastly differing trends in the various
properties will cause problems dynamically (e.g. high porosity, very
low permeability).
It is useful to compare the statistical distribution of
the data for original well logs, blocked well logs and the 3-D model.
There would normally be a close match between the original logs and blocked
logs for each zone. However the 3-D model is designed to be dependant
on well spacing, facies modelling, depth trends and it is NOT normally
required for the statistics to be the same as the well data. It is possible
to make comparisons within a particular area where properties are expected
to match, such as within the channel belts of a reservoir, ignoring the
poorer quality interchannel areas.
-
Are the properties expected to be smooth are have
a lot of variation between wells?
-
How much dependence is there between net, porosity
and permeability?
Hydrocarbon Saturation
In most reservoirs the hydrocarbon saturation can be readily
calculated from the well logs and a hydrocarbon-water contact can be
established from exploration wells with formation pressure tests (RFTs).
Extending these observations to calculate the saturations in the rest
of the reservoir requires further steps. Initial wells will obviously
show original saturations, but as soon as production has started, subsequent
wells will have higher contacts and flushed intervals so cannot be used
for OOIP calculations. The hydrocarbon saturation is usually at a maximum
in the crest of the structure and decreases significantly near the original
oil-water contact. The oil saturation is also higher in good quality
reservoir than poor quality reservoir. Therefore it is common practice
to use a function that relates water saturation to height above the free
water level to reservoir quality. Each cell in the model can then be
evaluated in 3-D and water saturation calculated. Methods that should
be considered are:
- Bulk Volume Water – Height (FOIL) does not need
permeability
- Permeability – Height (e.g. J-function) relies
on permeability calculation and special core analysis
In both these method a geometrical property of height above
the FWL needs to be generated in the model.
While most methods rely on establishing a contact and this
is important for static hydrocarbon volumes, it should also be recognised
that the interval near the contact will not contribute very much to the
reserves. It is not a good idea to artificially deepen the contact, based
on very low oil saturations, unless there are special circumstances.
Core fluorescence data may assist in defining the oil-water contact,
but in some reservoirs there may be good fluorescence below the current
free water level based on RFT measurements.
|