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    • 1. 发明申请
    • Telemetry Method and System for Subsurface Well and Reservoir and Logging Data
    • 地下水库和测井资料遥测方法与系统
    • US20100073190A1
    • 2010-03-25
    • US12237559
    • 2008-09-25
    • Otto N. FaniniRaman ViswanathanJorge Omar MaxitHarold Andrade
    • Otto N. FaniniRaman ViswanathanJorge Omar MaxitHarold Andrade
    • G01V3/00
    • G01V11/002E21B47/12G06F17/14
    • A method and system for transmitting data through a transmission medium between surface and subsurface transceivers. A surface transceiver and a subsurface transceiver are each configured to selectively transmit over a plurality of transmission channels, each transmission channel having a range of frequencies within the total frequency bandwidth. The surface transceiver is adapted to initialize a channel to determine at least one parameter affecting the current maximum data rate for transmission of information through the channel using a given transmission methodology. At least one of the channels uses carrierless phase/amplitude (CAP) modulation for its transmission methodology. The surface transceiver and the subsurface transceiver adapt to cooperatively periodically test a channel by transmission of a calibration signal from the subsurface transceiver to the surface transceiver. Control circuitry compares the received calibration signal with the calibration signal, responding to the result of the comparison to adjust at least one parameter as necessary to achieve an optimum rate of data transmission through said channel.
    • 一种用于通过传输介质在表面和地下收发器之间传输数据的方法和系统。 表面收发器和次表面收发器各自被配置为选择性地在多个传输信道上传输,每个传输信道具有在总频带宽内的频率范围。 表面收发器适于初始化信道以确定影响当前最大数据速率的至少一个参数,以便使用给定的传输方法通过信道传输信息。 至少一个信道对其传输方法使用无载相位/幅度(CAP)调制。 表面收发器和地下收发器适应于通过从地下收发器向地面收发器的校准信号的传输来协调地周期性地测试信道。 控制电路将接收到的校准信号与校准信号进行比较,响应于比较结果,根据需要调整至少一个参数以实现通过所述通道的最佳数据传输速率。
    • 4. 发明申请
    • COMMUNICATION BETWEEN DOWNHOLE TOOLS AND A SURFACE PROCESSOR USING A NETWORK
    • 使用网络的井下工具与表面处理器之间的通信
    • US20160084076A1
    • 2016-03-24
    • US14490298
    • 2014-09-18
    • Otto N. FaniniHarold Andrade
    • Otto N. FaniniHarold Andrade
    • E21B47/12
    • E21B47/12H04L67/12H04L69/08
    • A system for communicating with subsurface components includes: a surface host connected to a subsurface location; a subsurface host connected to the surface host by a communication link, the subsurface host configured to communicate with the surface host using a communication protocol; and a plurality of tools configured to be disposed in a borehole, the plurality of downhole tools communicatively coupled to the subsurface host via a communication network. The communication network is divided into a plurality of network subsets, each network subset of the plurality of network subsets including one or more downhole tools, all of the one or more downhole tools configured to communicate using a common protocol, each network subset including a network device configured to receive data and translate the data to the common protocol, the common protocol of one network subset being different than the common protocol of at least one other network subset.
    • 用于与地下部件通信的系统包括:连接到地下位置的表面主机; 通过通信链路连接到所述表面主机的地下主机,所述地下主机被配置为使用通信协议与所述表面主机进行通信; 以及被配置为设置在钻孔中的多个工具,所述多个井下工具通过通信网络通信地耦合到地下主机。 通信网络被分成多个网络子集,多个网络子集的每个网络子集包括一个或多个井下工具,所有一个或多个井下工具被配置为使用公共协议进行通信,每个网络子集包括网络 被配置为接收数据并将数据转换为公共协议的设备,一个网络子集的公共协议与至少一个其他网络子集的公共协议不同。
    • 9. 发明授权
    • Conductivity anisotropy estimation method for inversion processing of
measurements made by a transverse electromagnetic induction logging
instrument
    • 横向电磁感应测井仪测量电导率各向异性估算方法
    • US5999883A
    • 1999-12-07
    • US42982
    • 1998-03-17
    • Pravin GuptaBerthold F. KriegshauserOtto N. Fanini
    • Pravin GuptaBerthold F. KriegshauserOtto N. Fanini
    • E21B41/00G01V3/28G06F19/00G01V3/38
    • G01V3/28E21B2041/0028
    • A method for determining an initial estimate of the horizontal conductivity and the vertical conductivity of an anisotropic earth formation. Electromagnetic induction signals induced by induction transmitters oriented along three mutually orthogonal axes are measured. One of the mutually orthogonal axes is substantially parallel to a logging instrument axis. The electromagnetic induction signals are measured using first receivers each having a magnetic moment parallel to one of the orthogonal axes and using second receivers each having a magnetic moment perpendicular to a one of the orthogonal axes which is also perpendicular to the instrument axis. A relative angle of rotation of the perpendicular one of the orthogonal axes is calculated from the receiver signals measured perpendicular to the instrument axis. An intermediate measurement tensor is calculated by rotating magnitudes of the receiver signals through a negative of the angle of rotation. A relative angle of inclination of one of the orthogonal axes which is parallel to the axis of the instrument is calculated, from the rotated magnitudes, with respect to a direction of the vertical conductivity. The rotated magnitudes are rotated through a negative of the angle of inclination. Horizontal conductivity is calculated from the magnitudes of the receiver signals after the second step of rotation. An anisotropy parameter is calculated from the receiver signal magnitudes after the second step of rotation. Vertical conductivity is calculated from the horizontal conductivity and the anisotropy parameter.
    • 一种用于确定各向异性地层的水平导电率和垂直导电率的初始估计的方法。 测量由三个相互正交的轴取向的感应发射器引起的电磁感应信号。 相互正交的轴之一基本上平行于测井仪器轴线。 使用第一接收器测量电磁感应信号,每个接收机具有平行于正交轴之一的磁矩,并且使用第二接收器,每个接收器具有垂直于垂直于仪器轴的正交轴之一的磁矩。 从垂直于仪器轴测量的接收机信号计算垂直轴之一的相对旋转角度。 通过将接收机信号的大小旋转通过旋转角度的负值来计算中间测量张量。 相对于垂直导电率的方向,从旋转的大小计算平行于仪器的轴线的正交轴之一的相对倾斜角。 旋转的大小通过倾斜角度的负值旋转。 在第二个旋转步骤之后,根据接收机信号的幅度计算水平电导率。 从第二步旋转后的接收机信号幅度计算各向异性参数。 垂直电导率由水平电导率和各向异性参数计算。
    • 10. 发明授权
    • Method and apparatus for transverse electromagnetic induction well
logging
    • 横向电磁感应测井方法和装置
    • US5781436A
    • 1998-07-14
    • US686848
    • 1996-07-26
    • Stanislav ForgangOtto N. FaniniLeonty A. Tabarovsky
    • Stanislav ForgangOtto N. FaniniLeonty A. Tabarovsky
    • E21B41/00G01V3/28G06F19/00
    • G01V3/28E21B2041/0028
    • A method of measuring the conductivity of earth formations penetrated by a wellbore. The method comprises selectively passing an alternating current through transmitter coils inserted into the wellbore. Each of the transmitter coils has a magnetic moment direction different from the magnetic moment direction of the other ones of the transmitter coils. The alternating current includes a first and a second frequency. The amplitude at the first frequency has a predetermined relationship to the amplitude at the second frequency. The relationship corresponds to the first and the second frequencies. The method includes selectively receiving voltages induced in a receiver coil having a sensitive direction substantially parallel to the axis of the corresponding transmitter coil through which the alternating current is passed. A difference in magnitudes between a component of the received voltage at the first frequency and a component of the voltage at the second frequency is measured, and conductivity is calculated from the difference in magnitudes of the components of the received voltage at the two frequencies. In a preferred embodiment, the step of measuring the difference in magnitudes between the voltage components at the two frequencies includes extracting digital signal samples of the received voltage at predetermined times with respect to a cycle of the transmitter current at the first frequency.
    • 测量井眼穿透的地层导电性的方法。 所述方法包括选择性地使交流电流通过插入到井筒中的发射器线圈。 每个发射器线圈具有与其他发射器线圈的磁矩方向不同的磁矩方向。 交流电流包括第一和第二频率。 第一频率处的振幅与第二频率处的振幅具有预定的关系。 该关系对应于第一和第二频率。 该方法包括有选择地接收在接收器线圈中感应的电压,该接收器线圈具有基本上平行于相应发射器线圈的轴线的敏感方向,交流电通过该轴线。 测量第一频率的接收电压的分量与第二频率处的电压分量之间的幅度差,并根据两个频率处的接收电压的分量的大小差来计算导电率。 在优选实施例中,测量两个频率的电压分量之间的幅度差的步骤包括相对于第一频率处的发射机电流的周期,以预定的时间提取接收电压的数字信号样本。