stochastic seismic inversion applied to reservoir characterization
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36 CSEG Recorder January, 2001
FEATURE ARTICLE
Seismic inversion has been used for several decades in thepetroleum industry, both for exploration and production purpos-
es. During this time, seismic inversion methods have progressed
from the initial recursive inversion method to the present pletho-
ra of methods and software packages available to transform
band-limited seismic traces to impedance traces. The application
of seismic impedance data has also progressed from qualitative
assessments of prospects to the quantitative description of reser-
voir properties necessary for reservoir characterization.
Reservoir characterization requires the construction of
detailed 3D petrophysical property models contained within a
geological framework. Structural interpretation of seismic data
has been and continues to be important in the generation of theframework of the reservoir model. Seismic data has been less fre-
quently involved in the generation of the petrophysical parame-
ters that populate the 3D model. There are several reasons for this
lack of application of seismic data to property modeling - lack of
a 3D dataset (only 2D data available), inability to relate seismic
data quantitatively to reservoir properties, and lack of sufficient
vertical resolution to generate detailed property models. The per-
vasive availability and acceptance of 3D data has substantially
overcome the first obstacle. Seismic impedance volumes calculat-
ed from these 3D datasets can, for many reservoirs, provide a
seismic parameter that can be directly related to a reservoir prop-
erty (porosity, for example), thereby addressing the second prob-
lem. The last problem - the lack of sufficient vertical resolutionfor characterization applications, has been a more difficult prob-
lem to solve. Stochastic seismic inversion is one method that can
provide the vertical resolution sufficient to generate detailed 3D
reservoir property models.
Seismic resolution is a function of the frequency of the record-
ed seismic wavefield and the velocity of the medium. Although
some enhanced recovery methods, such as steam floods or fire
floods, can alter the velocity of the medium by elevating the tem-
perature of the reservoir, the velocity of the medium is generally
considered to be fixed. Despite our best efforts to maximize the
frequencies emitted and recorded during seismic acquisition, we
often fall short of the resolution desired by geologists and engi-
neers for use in reservoir modeling - vertical seismic resolution is
typically one to two orders of magnitude less than log resolution
(hundreds to thousands of centimeters versus tens of centimeters
or less).
Reservoir models constructed from log data alone display an
excellent vertical resolution and a poor areal (horizontal) resolu-
tion. This is a direct reflection of the resolution characteristics of
the log data - high vertical resolution and limited depth of inves-tigation. Seismic data possess the opposite resolution characteris
tics: high areal resolution (bin size of the 3D survey) and poor
vertical resolution (function of the seismic frequency content and
velocity of the reservoir). Stochastic seismic inversion provides a
unique framework wherein the advantages of seismic and log
data can be combined. The stochastic impedance volume derive
its areal resolution from the seismic data, but derives the vertica
resolution from the log data used in the inversion procedure. The
resulting high resolution (both vertical and horizontal) 3D vol
ume is well suited for use in building detailed property models.
As outlined in Haas and Dubrule (1994), the log data (sonic
and density) are used in the simulation of pseudo-logs at eachtrace within the seismic survey (figure 1). A synthetic seismo
gram is generated from the pseudo-impedance log and is com
pared with the actual seismic trace at that location. The
simulation that produces the best match between the synthetic
seismogram and the actual seismic trace, as defined by some
quantitative measure of goodness of fit, is retained as the inver-
sion solution at that location. The vertical resolution of the simu
lated log data is determined by the selection of the vertical cel
size (determined by the user), not by the frequency content of the
seismic data (as determined by Mother Nature). The result of the
stochastic seismic inversion is a 3D volume with a seismic-like
areal resolution and a log-like vertical resolution that honors both
the log data and the seismic data.
The enhanced resolution of the stochastic inversion process is
evident from a visual examination of the seismic data cubes dis
played in figures 2-4. Figure 2 displays the input seismic volume
Figure 3 is the result of a sparse spike estimation and recursive
inversion. This inversion result displays a resolution similar to
that of the input data. That is to be expected, as the vertical reso
lution is derived from the seismic data, and is therefore subject to
the inherent limitations of seismic resolution. Figure 4 depicts the
stochastic inversion cube, which displays a much finer vertica
resolution than is observed in the input data or the recursive
inversion result (figures 2 and 3). The overall impedance trends
can be observed in both inversion results (figures 3 and 4)- layer
or regions of high (red color) and low (blue color) impedance
however, the stochastic inversion result (figure 4) has a much bet
ter vertical definition within these general impedance trends.
Continued on Page 38
STOCHASTIC SEISMIC INVERSION APPLIED TORESERVOIR CHARACTERIZATION
By Gary Robinson, (RC)2, Englewood, Colorado, USA
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FEATURE ARTICLE Contd
A typical stochastic inversion exhibits a vertical resolution of
approximately 1-2 meters. This is generally the same order ofmagnitude of resolution used in constructing the petrophysical
reservoir property models, and the impedance data may be used
along with the well log data to generate models of reservoir prop-
erties such as porosity. Figures 5 and 6 present porosity models of
the interval depicted in the previous figures. The model of figure
5 was calculated using only the log data, whereas the model of
figure 6 incorporated both the impedance and porosity informa-
tion. Again, although overall trends are generally similar, specif-
ic details can be significantly different. The influence of the
stochastic inversion impedance model (figure 4) on the porosity
model shown in figure 6 is clearly discernible, as features
observed in the impedance model (figure 4) that are not present
in the log-only porosity model (figure 5) are again present in the
porosity model derived from both the seismic and the log data
(figure 6).
In carbonate reservoirs, impedance and porosity typically
exhibit an inverse relationship (Rafavich, Kendall, and Todd,
1984); in clastic reservoirs, the relationship of porosity and
impedance may be complicated by additional factors, such as a
lack of impedance contrast between reservoir and non-reservoir
rocks or fluid effects. In the case of a clear relationship between Continued on Page 40
STOCHASTIC SEISMIC INVERSION APPLIED TO RESERVOIR CHARACTERIZATION
Continued from Page 36
Figure 1. Schematic depiction of the stochastic inversion process.
porosity and impedance, the seismic impedance volume may be
incorporated directly with well data, via geostatistics, neural net-
works, or other methods, to populate the cells of the petrophysi
cal model, as was done in constructing the porosity model o
figure 6. Where the relationship between impedance and porosi-
ty is murky, the impedance data may be combined with facies
data to derive a facies volume. Petrophysical properties can then
be distributed by facies within the overall model framework.
In summary, the impedance cube resulting from a stochasticinversion provides sufficient vertical resolution, as well as area
resolution, for use in reservoir characterization. This stochastic
inversion impedance volume can be combined with log and engi
neering data, utilizing deterministic or statistical methods, to
arrive at a reservoir model which has incorporated various data
types from different disciplines (geology, geophysics, engineer-
ing) to arrive at a final, consistent 3D property model for use in
reservoir characterization.
Figure 2. Input seismic data volume.
Figure 3. Recursive inversion result. Note that vertical resolution is similar to that of thinput data.
Figure 4. Stochastic inversion result. Note that the vertical resolution is significantlyimproved from that of the input data.
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FEATURE ARTICLE Contd
STOCHASTIC SEISMIC INVERSION APPLIED TO RESERVOIR CHARACTERIZATION
Continued from Page 38
Figure 5. Porosity model derived from kriging porosity log data.
Figure 6. Porosity model derived from collocated co-kriging of stochastic inversion andporosity log data. Compare with porosity model of figure 5 and the stochastic inversion offigure 4.
References:
Haas, A., and Dubrule, O., 1994, Geostatistical inversion - a
sequential method of stochastic reservoir modeling constrained by
seismic data: First Break, 12, 561-569.
Rafavich, F., Kendall, C. H. St. C., and Todd, T. P., 1984, The
relationship between acoustic properties and the petrographic character
of carbonate rocks: Geophysics, 49, 1622-1636.
GARY ROBINSON
Gary Robinson received a
B.S. degree in Geology from
Stanford University, and an M.S.
degree in Geophysics from the
University of Houston. He
began his career with Mobil in
1978, and has worked for CGG,
Elf Aquitaine, Eastern American
Energy, and Saudi Aramco priorto joining RC Squared in 1998.
His current interest is in the application of seismic data to
reservoir characterization and modeling.
First Canadian Open Business Forumon
Building Corporate Social and Environmental Responsibility3rd Federico Garca Lorca seminar
Calgary, Alberta Thursday 8 March 2001
Hon. David Kilgour, MP, PC, Secretary of State for Latin America and Africa *
Eric P. Newell, Chairman and Chief Executive Officer, Syncrude Canada Limited *
Tim W. Faithfull, President and CEO, Shell Canada Limited *
David Pollock, Executive Director, Pembina Institute *
Phil Prince, Phd, President and CEO, Canadian Energy Research Institute *
Henry Day, Vice-President, Peru 2021, President, Solgas, (Repsol-YPF S.A)*
Heather Scoffield,Journalist, The Globe and Mail *
Rosemarie Kuptana, Director, International Institute for Sustainable Development
Including keynote luncheon speaker:
Charles O. Holliday, Jr., Chairman and Chief Executive Officer and
Chief Safety, Health and Environmental Officer, E.I. du Pont de Nemours & Co.
Chairman, World Business Council on Sustainable Development
* confirmed
For more information, and sponsorship opportunities, please contact event organiser, David Mitrovica, P. Geoph.:
Email: [email protected] Telephone: 403-230-9031