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Befriko Saparindra Murdianto
"ABSTRACT
Subsurface models of lithology are often poorly constrained due to the lack of
dense well control. Although limited in vertical resolution, high-quality threedimensional
(3-D) seismic data usually provide valuable information regarding
the lateral variations of lithology. In this thesis, I will show how Bayesian
approach can be used to generate seismically constrained models of
lithology. Unlike cokriging-based simulation methods, this method does not
rely on a generalized linear regression model, which is inadequate when
combining discrete variables, such as lithology indicator; and continuous
variables, such as seismic attributes. This method uses a Bayesian updating
rule to construct a posterior probability distribution function of lithoclasses by
using a priori information from well data and the seismic likelihood to constrain
the 3-D geological scenarios produced by geostatistical technique, which is
then sampled sequentially at all points in space to generate a set of
realizations. The realizations define alternative, equiprobable lithologic
models. The methodology was applied to delineate productive reservoir zone
in Boonsville, Texas. To achieve better result in the Bayesian Sequential
Indicator Simulation, I used acoustic impedance obtained from a seismic
inversion process as the attribute to constrain the simulation. It is expected
that by using this attribute, the separation of the litho-class conditional
distribution will be well defined and at the same time minimizing the overlaps
between the two distributions. The lithology classification obtained from BSIS
is then integrated with the result of the seismic inversion to clearly delineate
the productive zone in the field."
2007
T21196
UI - Tesis Membership  Universitas Indonesia Library
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Dyah Tribuanawati
"Metode litologi seismik bertumpu pada amplitudo gelombang-gelombang seismik yang dipantulkan oleh bidang batas antar lapisan. Litologi seismik menghasilkan penampang pseudosonic log, pseudo velocity atau impedansi akustik yang merepresentasikan litologi lebih baik dari pada seismik struktur.
Amplitudo dari sinyal seismik terpantul tergantung pada variasi impedansi akustik yang merupakan hasil kali kecepatan dan densitas. Sehingga perubahan pada salah satu parameter tersebut, kecepatan atau densitas batuan akan berkontribusi pada variasi respon seismik dari reservoar.
Litologi dan ketebalan reservoar serta sejumlah sifat petrofisika batuan seperti porositas dan saturasi fluida dipengaruhi kedua parameter tersebut. Oleh karena itu untuk mengestimasi sifat-sifat petrofisika batuan dengan menggunakan data seismik harus mengkuantisasi kontribusi masing-masing parameter petrofisika pada pengukuran akustik.
Metoda ini digunakan untuk mengestimasi parameter petrofisika reservoar migas dari data seismik sehingga disebut sebagai 'Seismically guided reservoir characterization di luar sumur pengeboran.
Geostatistik merupakan framework yang mengkombinasikan sample yang terdistribusi secara spatial, berdasarkan atas data log sumur dan data seismik. Yang berguna untuk estimasi yang akurat dari reservoar properties dari ketidakpastian dari model reservoar.
Dalam geostatistik mapping teknik ini berdasarkan atas Kriging, Regresi Linear dan Cokriging untuk memberikan kontribusi berdasarkan informasi petrofisika batuan yang diperoleh dari log sumur dan arah spatial dari seismik attribute. Secara garis besar teknik geostatistik untuk mengkombinasikan informasi petrofisika dan data seismik.
Dengan geostatistik pada situasi dengan minimal kontrol data, dapat memprediksi karakteristik reservoar dengan lebih baik dibandingkan dengan mapping standard.

Seismic Lithology method was introduced in the 1970's was based on amplitude of the seismic waves reflected by the subsurface interfaces. Seismic lithology generates pseudo sonic log, pseudo velocity log or acoustic impedance time section which represents the lithology better than the seismic structure. By using this method it is possible to estimate the petrophysical properties of the reservoir rocks from seismic data. Furthermore it is possible to estimate the reservoir parameters from seismic data. This approach enables to implement a new method which referred to as seismically guided reservoir characterization in the zones outside the borehole.
The amplitudes of reflected seismics signals depend primarily on variations in acoustic impedance. Changes in either rock velocity or density will contribute to variations in the seismic response of the reservoir. A number of petrophysical properties, such as porosity, fluid saturation affect both rock velocity and density. To estimate reservoir properties using seismic data it is necessary to quantify the respective contribution of each petrophysical parameter to the acoustic measurements.
A series of laboratory P wave and S wave measurement has been conducted on limestone core samples from Baturaja limestone reservoir. By using the laboratory acoustic measurement data to support seismic derived porosity and fluid saturation determination in the reservoir. Several parameters have been derived from transit time data such as P and S wave velocities, Poisson ratio. To provide relationship between fluid saturation, porosity, P wave velocity and Poisson ratio, and modify acoustic impedance, crossplots between the parameters have been generated using a combination of laboratory acoustic measurement on core samples and mathematic modelling.
A geostatistical technique integrating well and seismic data has been studied for mapping porosity in hydrocarbon reservoirs. The most important feature of the cokriging method is that it uses spatial correlation functions to model the lateral variability of seismic and porosity measurements in the reservoir interval.
Cokriging was tested on a numerically simulated reservoir model and compared first with kriging, then with a conventional least squares procedure relying only on local correlation between porosity and acoustic impedance. As compared to kriging, the seismically assisted geostatistical method detects subtle porosity lateral variations that cannot be mapped from sparse well data alone.
As compared to the standard least squares approach, cokriging provides not only more accurate porosity estimates that are consistent with the well data. Using seismically derived acoustic impedances, cokrigging also was applied to estimate the distribution of porosity in limestone reservoir.
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1999
T-Pdf
UI - Tesis Membership  Universitas Indonesia Library
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Dina Zaenab
"Extended Elastic Impedance method is one of the methods in reservoir characterization, which is used to identify lithology and fluids content. This method is an extension of Elastic Impedance method by changing SinĀ²θ in Zoeppritz equation with tan χ to get scaled reflectivity equation. χ is angle range between -90° up to 90°. By using proper angle (χ), we can calculate the reflectivity that associates with the log parameter (Gamma Ray, Porosity, Lamda-Rho and Mhu-Rho). To proceeds this scheme we need to derive gradient and intercept from AVO analysis, which is used in Zoeppritz equation to calculate reflectivity volume. The proper angle (χ), which is derived from Whitcombe equation, is 30° for Gamma Ray. While the proper angle (χ) for porosity, mhu-rho, and lambda-rho is 60°, -90° and 15° respectively.
The result of mhu-rho and lamda-rho inversion in the target area contain of sandstone and oil in the time depth range of 1545 ? 1573 ms for horizon 1 and horizon 2. Based on seismic inversion, lamda-rho and mhu-rho crossplot analysis we can see that the distribution of reservoir in target area has lamda-rho value between 9050 ? 9300 m/s*g/cc or 25 ? 37 GPa*g/cc and mhu-rho value between 7500 ? 11200 m/s*g/cc or 25 ? 35 GPa*g/cc."
Depok: Fakultas Matematika Ilmu Pengetahuan Alam Universitas Indonesia, 2009
T 26241
UI - Tesis Open  Universitas Indonesia Library