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    • 1. 发明申请
    • [METHODS AND SYSTEMS FOR RESISTIVITY ANISOTROPY FORMATION ANALYSIS]
    • [电阻率成像分析方法与系统]
    • US20050114030A1
    • 2005-05-26
    • US10604492
    • 2003-07-25
    • Cheng LiuQiming LiFrank ShrayJacques Tabanou
    • Cheng LiuQiming LiFrank ShrayJacques Tabanou
    • G01V3/20G06F19/00
    • G01V3/20
    • Techniques for determining a formation property by simplifying various two-geological-layer or multi-geological-layer models into a multi-electrical-layer model. A volume fraction of a layer in a multi-electrical-layer model is determined for an anisotropic region (sliding window) of the formation. The multi-electrical-layer electrical model includes a relative-lower-resistivity layer and a relative-higher-resistivity layer. A high-resolution resistivity measurement is used in the determination and resistivities for the relative-lower-resistivity layer and for the relative-higher-resistivity layer based on the volume fraction and bulk resistivity measurements of the anisotropic region are determined. The formation property is based on the volume fraction, the resistivity of the relative-lower-resistivity layer, the resistivity of the relative-higher-resistivity layer, a total porosity of the anisotropic region, and bulk resistivity measurements of the region.
    • 通过将各种地质层或多地质层模型简化为多电层模型来确定地层特性的技术。 针对地层的各向异性区域(滑动窗口)确定多电层模型中的层的体积分数。 多电层电气模型包括相对低电阻率层和相对较高电阻率的层。 在相对低电阻率层的测定和电阻率中使用高分辨率电阻率测量,并且基于各向异性区域的体积分数和体电阻率测量确定相对较高电阻率层。 形成性质基于体积分数,相对低电阻率层的电阻率,相对高电阻率层的电阻率,各向异性区域的总孔隙率和该区域的体电阻率测量值。
    • 2. 发明授权
    • Methods and systems for resistivity anisotropy formation analysis
    • 电阻率各向异性形成分析的方法和系统
    • US06950748B2
    • 2005-09-27
    • US10604492
    • 2003-07-25
    • Cheng Bing LiuQiming LiFrank P. ShrayJacques Tabanou
    • Cheng Bing LiuQiming LiFrank P. ShrayJacques Tabanou
    • G01V3/20G01V3/38
    • G01V3/20
    • Techniques for determining a formation property by simplifying various two-geological-layer or multi-geological-layer models into a multi-electrical-layer model. A volume fraction of a layer in a multi-electrical-layer model is determined for an anisotropic region (sliding window) of the formation. The multi-electrical-layer electrical model includes a relative-lower-resistivity layer and a relative-higher-resistivity layer. A high-resolution resistivity measurement is used in the determination and resistivities for the relative-lower-resistivity layer and for the relative-higher-resistivity layer based on the volume fraction and bulk resistivity measure ments of the anisotropic region are determined. The formation property is based on the volume fraction, the resistivity of the relative-lower-resistivity layer, the resistivity of the relative-higher-resistivity layer, a total porosity of the anisotropic region, and bulk resistivity measurements of the region.
    • 通过将各种地质层或多地质层模型简化为多电层模型来确定地层特性的技术。 针对地层的各向异性区域(滑动窗口)确定多电层模型中的层的体积分数。 多电层电气模型包括相对低电阻率层和相对较高电阻率的层。 在相对较低电阻率层的确定和电阻率中使用高分辨率电阻率测量,并且基于各向异性区域的体积分数和体电阻率测量确定相对较高电阻率层。 形成性质基于体积分数,相对低电阻率层的电阻率,相对高电阻率层的电阻率,各向异性区域的总孔隙率和该区域的体电阻率测量值。
    • 3. 发明授权
    • Deep and/or shallow electrical resistivity investigation suitable for
dual resistivity-induction logging
    • 深和/或浅电阻率测量适用于双电阻率测井
    • US4319192A
    • 1982-03-09
    • US4621
    • 1979-01-18
    • Roland ChemaliJacques Tabanou
    • Roland ChemaliJacques Tabanou
    • G01V3/24G01V3/26
    • G01V3/265G01V3/24
    • A dual resistivity and induction apparatus for the investigation of earth formations traversed by a borehole, comprises an electrode system, supported on a support member, comprising a central electrode and five pairs of electrodes respectively short-circuited and aligned symmetrically about the central electrode at increasing distances therefrom; the central electrode and the electrodes of the fourth and fifth pairs are called current electrodes, the electrodes of the first, second and third pairs are called voltage electrodes; a source of alternating current at a first frequency, f.sub.1, is coupled between the electrodes of the fifth and fourth pairs; a source of alternating current at a second frequency, f.sub.2, is coupled between the electrodes of the fifth pair and an electrode at electrical infinity with respect to the electrode system; a circuit arrangement coupled to the electrodes of the fourth pair for generating current at f.sub.1 from the central electrode for maintaining the potential difference between the first and second pairs of electrodes at substantially zero and for generating current at f.sub.2 from the central electrode for maintaining the potential difference between the first and third pairs of electrodes at substantially zero; first and second impedances, respectively interposed between each of the source of alternating current and the current generating circuit and the fourth pair of current electrodes; and transmitter and receiver coils supported on the support member, for inducing at a third frequency, f.sub.3, electromagnetic energy; the length, along the axis of the support member, of each of the electrodes of the fifth pair is several orders of magnitude smaller than the relative spacing along the support member of that fifth pair of electrodes to reduce the interference between the electrode system and the coil system.
    • 用于研究由钻孔穿过的地层的双电阻率和感应装置包括支撑在支撑构件上的电极系统,其包括中心电极和五对电极,其分别在增加的情况下围绕中心电极对称地短路和对齐 距离; 中心电极和第四对和第五对的电极称为电流电极,第一,第二和第三对的电极称为电压电极; 以第一频率f1的交流电源耦合在第五和第四对的电极之间; 以第二频率f2的交流电源耦合在第五对的电极和相对于电极系统的无限远的电极之间; 耦合到第四对的电极的电路装置,用于从中心电极在f1处产生电流,用于将第一和第二对电极之间的电位差保持在基本上为零,并且用于从中心电极产生电流,以保持电位 第一对和第三对电极之间的差异基本为零; 第一和第二阻抗,分别插入在每个交流电源和电流产生电路和第四对电流电极之间; 以及支撑在所述支撑构件上的发射器和接收器线圈,用于以第三频率f3感应电磁能; 沿着支撑构件的轴线的第五对的每个电极的长度比沿着该第五对电极对的支撑构件的相对间隔小几个数量级,以减少电极系统和 线圈系统
    • 5. 发明授权
    • Wellbore antennae system and method
    • US06691779B1
    • 2004-02-17
    • US09428936
    • 1999-10-28
    • Abdurrahman SezginerJacques TabanouReinhart Ciglenec
    • Abdurrahman SezginerJacques TabanouReinhart Ciglenec
    • E21B4700
    • E21B7/06E21B23/00E21B47/01E21B47/011E21B47/12E21B47/122E21B49/00E21B49/10
    • An apparatus and a method for controlling oilfield production to improve efficiency includes a remote sensing unit that is placed within a subsurface formation, an antenna structure for communicating with the remote sensing unit, a casing joint having nonconductive “windows” for allowing a internally located antenna to communicate with the remote sensing unit, and a system for obtaining subsurface formation data and for producing the formation data to a central location for subsequent analysis. The remote sensing unit is placed sufficiently far from the wellbore to reduce or eliminate effects that the wellbore might have on formation data samples taken by the remote sensing unit. The remote sensing unit is an active device with the capability of responding to control commands by determining certain subsurface formation characteristics such as pressure or temperature, and transmitting corresponding data values to a wellbore tool. The inventive system includes an antenna structure that is for delivering power and communication signals to the remote sensing unit. In one embodiment, the antenna structure is formed on an external surface of a wellbore casing. In another embodiment, the antenna structure is formed on a downhole tool such as a drilling collar or a cased hole wireline tool. For those embodiments in which the antenna structure is formed on a cased holed wireline tool, a casing joint is provided that includes nonconductive windows for allowing RF signals to be transmitted from within the casing to the remote sensing unit and from the remote sensing unit to the wireline tool. An inventive method therefore includes providing RF power through the inventive antenna system to the remote sensing unit to wake it up and to place it into an operational mode. The method further includes receiving modulated data values from the remote sensing unit through the antenna system that are then transmitted to the surface where operational decisions for the well may be made.
    • 6. 发明申请
    • Downhole measurement of formation characteristics while drilling
    • 钻井时地层特征的井下测量
    • US20070137293A1
    • 2007-06-21
    • US11312683
    • 2005-12-19
    • Julian PopReza TaherianMartin PoitzschJacques Tabanou
    • Julian PopReza TaherianMartin PoitzschJacques Tabanou
    • E21B49/08
    • E21B49/005E21B49/081
    • A method for determining a property of formations surrounding an earth borehole being drilled with a drill bit at the end of a drill string, using drilling fluid that flows downward through the drill string, exits through the drill bit, and returns toward the earth's surface in the annulus between the drill string and the periphery of the borehole, including the following steps: obtaining, downhole near the drill bit, a pre-bit sample of the mud in the drill string as it approaches the drill bit; obtaining, downhole near the drill bit, a post-bit sample of the mud in the annulus, entrained with drilled earth formation, after its egression from the drill bit; implementing pre-bit measurements on the pre-bit sample; implementing post-bit measurements on the post-bit sample; and determining a property of the formations from the post-bit measurements and the pre-bit measurements.
    • 一种用于确定围绕钻井的地层钻孔的性质的方法,其使用在钻柱上向下流动的钻井流体在钻柱的端部钻出,通过钻头离开,并朝向地球表面返回 钻柱与钻孔周边之间的环形空间,包括以下步骤:在钻柱附近获得钻头附近的井下钻头样品,当钻柱接近钻头时; 在钻头附近获得钻孔附近的井下钻孔后的钻头样品,在钻头从其钻出之后夹带钻井泥土; 对前置位采样执行预位测量; 对后位采样进行后位测量; 以及从后位测量和前位测量确定地层的属性。
    • 10. 发明申请
    • [SYSTEM AND METHOD FOR ANALYZING A THIN BED FORMATION]
    • [用于分析薄床形成的系统和方法]
    • US20050171697A1
    • 2005-08-04
    • US10708012
    • 2004-02-02
    • Denis HeliotJacques TabanouJaideva Goswami
    • Denis HeliotJacques TabanouJaideva Goswami
    • G01V3/38G06F19/00G06G7/48
    • G01V3/38
    • A system and method is disclosed for determining a physical characteristic or property associated with each of a plurality of layers of laminated formation traversed by a wellbore, wherein the laminated formation includes thin beds. The method includes providing one or more high resolution logs of a formation property for the laminated formation. From this log, the bed boundaries are detected and more particularly, the individual beds disposed between the boundaries. Then, the facies for each of the plurality of the beds detected is identified, using one or more high resolution logs of the laminated formation. Each of the identified facies is then defined. This includes importing volumetric descriptions for each of the facies and assigning one of the volumetric descriptions to each of a plurality of the beds detected, wherein each of the volumetric descriptions assigned to a bed is derived from a bed having the same facies. One or more squared logs for formation property is then generated by using the imported volumetric descriptions of the facies for plurality to generate a value of the formation property for each of the beds. This squared log is then convolved to generate a reconstructed log. The reconstructed log is compared with a low resolution log of the formation property for laminated formation. By adjusting the values of the squared log the difference between the reconstructed log and the squared log may be minimized. In this way, and by repeating the adjusting compared steps, and adjusted squared log may be suggested as an optimized squared log of the formation property. The optimized squared logs may then be the subject of a volumetric analyses to generate an output medium having the square log and the volumetric analyses thereon.
    • 公开了一种系统和方法,用于确定与由井筒穿过的层叠地层的多个层中的每一层相关联的物理特性或性质,其中所述层压结构包括薄床。 该方法包括提供一层或多层用于叠层地层的地层性能的高分辨率测井。 从该日志中检测床边界,更具体地说,设置在边界之间的各个床。 然后,使用层叠地层的一个或多个高分辨率原木来识别检测到的多个床中的每一个的相。 然后定义每个识别的相。 这包括导入每个相的体积描述,并将一个体积描述分配给检测到的多个床中的每一个,其中分配给床的每个体积描述源自具有相同相的床。 然后通过使用对于多个相的相的进口体积描述来生成每个床的形成性质的值来生成用于形成性质的一个或多个平方的原木。 然后将该平方日志进行卷积以生成重建的日志。 将重建的对数与层压成形的形成性质的低分辨率对数进行比较。 通过调整平方日志的值,重建日志和平方日志之间的差异可能被最小化。 以这种方式,并通过重复调整比较步骤,并且调整的平方日志可以被建议为形成特性的优化平方对数。 然后,优化的平方日志可以是体积分析的对象,以产生具有平方对数的输出介质和其上的体积分析。