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Open AccessJournal ArticleDOI

余目油田におけるレザバー•キャラクタライゼイション (その2)

仙石 雄三, +2 more
- 01 Jan 1993 - 
- Vol. 58, Iss: 1, pp 78-91
TLDR
In this paper, the relationship between acoustic impedance (velocity) and rock properties such as porosity and clay content was analyzed in the reservoir interval based on the results of well log data analysis.
Abstract
Predicting the reservoir rock properties such as porosity and clay content is essential for estimating reserves and planning the optimum development of oil and gas fields. Modern seismic data, especially 3-D seismic data, has played an important role in reservoir characterization. A study has been performed to predict the reservoir disrtibution and the rock properties using 3-D seismic data in the Amarume oil field. The reservoirs are mainly in Kitamata Formation of Miocene which is considered to be deep-sea sediment gravity flow deposits. Several sandstone layers, which are discontinuous in horizontal direction, bear hydrocarbons. Productive sandstone reservoirs lie approximately 900m below the surface and vary from 5m to 20m in thickness. 3-D seismic survey area is about 2km in East-West direction and 1km in North-South direction. Acoustic impedance was derived from the 3-D data volume by seismic inversion method. Such impedance data can be related to rock properties and physical conditions in the reservoirs. The relationship between acoustic impedance (velocity) and rock properties such as porosity and clay content was analyzed in the reservoir interval based on the results of well log data analysis. An empirical equation was obtained by linear regression analysis to effective porosity versus acoustic impedance with a correlation coefficient of 0.87. The correlation was improved by addition of a clay, shale or tuff content term in the linear regression analysis. These relationships indicate that an increase in clay or shale content rises P-wave velocity. This observation differs from that quoted by several other investigators. Seismically derived acoustic impedance (I) was converted to effective porosity (φ) using the equation [I=5.72-8.15φ]. Depth structures, effective porosity and effective porosity-thickness of the reservoirs were mapped based on the converted effective porosity. The results were consistent with well data. 3-D seismic data can be a powerful tool for predicting the areal distribution of reservoir rock properties.

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References
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Journal ArticleDOI

Effects of porosity and clay content on wave velocities in sandstones

TL;DR: In this paper, the ultrasonic compressional (Vp) and shear (Vs) velocities and first-arrival peak amplitude (Ap) were measured as functions of differential pressure to 50 MPa and to a state of saturation on 75 different sandstone samples, with porosities ϕ ranging from 2 to 30 percent and volume clay content C ranging from 0 to 50 percent.
Journal ArticleDOI

Empirical relationships among seismic velocity, effective pressure, porosity, and clay content in sandstone

TL;DR: In this paper, the influence of effective pressure Pe, porosity ϕ, and clay content C on the compressional velocity Vp and shear velocity Vs of sandstones was investigated.
Journal ArticleDOI

Porosity from seismic data: A geostatistical approach

TL;DR: Using a geostatistical technique called cokriging, the areal distribution of porosity is estimated first in a numerically simulated reservoir model, then in an oilbearing channel-sand of Alberta, Canada as mentioned in this paper.
Journal ArticleDOI

Estimates of velocity dispersion between seismic and ultrasonic frequencies

Kenneth W. Winkler
- 01 Jan 1986 - 
TL;DR: In this article, the authors developed a simple analysis technique that gives estimates of total velocity dispersion between zero frequency and any measurement frequency, assuming that the dry velocities are independent of frequency.

Effects of lithology, porosity and shaliness on p and swave velocities from sonic logs

TL;DR: In this article, the authors analyzed the relationship between P-wave velocity (V,). S-wave velocities (KS), VP/V, and lihology, shaliness and porosity.