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    • 3. 发明授权
    • Method and tool for producing a formation velocity image data set
    • 用于生成地层速度图像数据集的方法和工具
    • US06678616B1
    • 2004-01-13
    • US09434694
    • 1999-11-05
    • Kenneth W. WinklerRalph M. D'Angelo
    • Kenneth W. WinklerRalph M. D'Angelo
    • G01V100
    • G01V1/52G01V1/44
    • Methods and tools are provided for real time velocity imaging of a borehole wall with sufficiently high resolution to identify vugs, worm holes, thin beds, dip angles, fractures and breakouts, for both open hole logging and logging while drilling in the presence of OBM's. A method is provided which includes transmitting an ultrasonic pulse through the borehole wall, receiving at first and second spaced-apart receivers an ultrasonic pulse refracted from the borehole wall, and producing a velocity image data value indicative of difference of arrival times at first and second spaced-apart receivers. This is repeated at a plurality of azimuths and depths to produce a velocity image data set. The method uses compressional pulses and/or pseudo-Raleigh pulses. A tool is provided for wireline use having an ultrasonic transmitter for transmitting ultrasonic pulses into the borehole wall, and a plurality of ultrasonic receivers. A processor in the tool produces real time velocity image data values indicative of time of flight of an ultrasonic pulse in the borehole wall. A similar tool is provided for logging while drilling (LWD).
    • 提供了方法和工具,用于在具有足够高分辨率的井壁实时速度成像,以便在存在OBM的同时进行钻孔时识别出孔,蜗杆孔,薄床,倾角,断裂和断裂。 提供了一种方法,其包括:通过所述钻孔壁传输超声波脉冲;在所述第一和第二间隔开的接收器处接收从所述钻孔壁折射的超声波脉冲,以及产生指示第一和第二时间到达时间差的速度图像数据值 间隔开的接收器。 这在多个方位角和深度处重复以产生速度图像数据集。 该方法使用压缩脉冲和/或伪罗利脉冲。提供了一种用于电缆使用的​​工具,其具有用于将超声波脉冲发射到井壁中的超声波发射器和多个超声波接收器。 工具中的处理器产生指示井眼壁中的超声波脉冲的飞行时间的实时速度图像数据值。 提供了一种类似的工具,用于钻井记录(LWD)。
    • 4. 发明授权
    • Method of predicting mechanical failure in formation utilizing stress
derivatives which measure formation nonlinearity
    • 使用测量地层非线性的应力衍生物预测地层机械故障的方法
    • US5619475A
    • 1997-04-08
    • US555796
    • 1995-11-09
    • Kenneth W. Winkler
    • Kenneth W. Winkler
    • G01H5/00G01V1/50G01V1/40
    • G01H5/00G01V1/50G01N2291/02491G01N2291/0421G01N2291/0422
    • A method for determining whether a formation is subject to incipient failure are disclosed. The method comprises determining in situ a nonlinear parameter of a formation, and determining whether the nonlinear parameter and/or a derivative of that nonlinear parameter as a function of stress has a relatively large negative value in order to determine whether the formation is subject to incipient failure. In a preferred embodiment, the nonlinear parameter of the formation is a derivative of the square of the shear or compressional velocity with respect to formation stress. The nonlinear parameter of the derivative of the square of the shear velocity with respect to stress is considered to have a large negative value when it is .ltoreq.-0.1 (km/sec).sup.2/ MPa, while the nonlinear parameter of the derivative of the square of the compressional velocity with respect to stress is considered to have a large negative value when it is .ltoreq.-0.2 (km/sec).sup.2 /MPa. The derivative of the derivative of the square of the shear or compressional velocity with respect to stress is considered to have a large negative value when the derivative is .ltoreq.-0.06 (km/sec).sup.2 /(MPa).sup.2. Typically, rocks will fail if uniaxially stressed between 11-5 MPa beyond any of those points.
    • 公开了一种确定地层是否遭受初期故障的方法。 该方法包括原位确定地层的非线性参数,并且确定作为应力的函数的该非线性参数的非线性参数和/或导数是否具有相对较大的负值,以便确定地层是否受到初始 失败。 在优选实施例中,地层的非线性参数是相对于地层应力的剪切或压缩速度的平方的导数。 当剪切速度相对于应力的平方的导数的非线性参数在≤0.1(km / sec)2 / MPa时被认为具有大的负值,而导数的非线性参数 相对于应力的压缩速度的平方被认为具有大的负值,当它为
    • 6. 发明授权
    • Borehole apparatus and methods for measuring formation velocities as a
function of azimuth, and interpretation thereof
    • 钻孔装置和用于测量作为方位角的函数的地层速度的方法及其解释
    • US5544127A
    • 1996-08-06
    • US220717
    • 1994-03-30
    • Kenneth W. Winkler
    • Kenneth W. Winkler
    • E21B47/12G01C21/00G01V1/02G01V1/16G01V1/20G01V1/30G01V1/40G01V1/52G01V1/00
    • G01V1/303G01V1/52G01N2291/02491G01N2291/0421G01N2291/0422
    • Borehole tools are provided with at least one transmitter which generates acoustic waves at a plurality of azimuthal locations about the borehole, and at least one receiver which receives and measures a characteristic (e.g., velocity) of the acoustic waves at related azimuthal locations. The direction of minimum velocity around the borehole is considered the direction of maximum uniaxial stress in the formation. From the velocity as a function of azimuth information, determinations of formation properties, and logs of the same can be made. The azimuthal direction of minimum velocity around the borehole predicts the propagation direction of artifically induced hydrofractures. The velocity variation around the borehole at a particular depth of the borehole is taken as an indication of susceptibility to failure, with higher velocity variations indicative of a more poorly consolidated formation or a formation with a large uniaxial stress. The curvature of the velocity versus stress curve in the formation is also indicated by how poorly a sine wave fits to the velocity data. Other parameters of the formation are obtained by fitting a best fit curve to the azimuth versus velocity data, where adjustable parameters of the best fit curve constitute the formation parameters.
    • 钻孔工具设置有至少一个发射器,其在围绕钻孔的多个方位位置处产生声波,以及至少一个接收器,其接收并测量相关方位角处的声波的特性(例如速度)。 井眼周围最小速度的方向被认为是地层最大单轴应力的方向。 根据作为方位角信息的函数的速度,可以确定其形成性质和其原木。 井眼周围最小速度的方位方向预测了人为引起的水力裂缝的传播方向。 在井眼特定深度处的钻孔周围的速度变化被认为是对破坏敏感性的指示,较高的速度变化表示更不均匀的地层或具有大的单轴应力的地层。 地层中速度与应力曲线的曲率也由正弦波与速度数据拟合程度的差异表示。 通过将最佳拟合曲线拟合到方位角对速度数据,其中最佳拟合曲线的可调参数构成地层参数,可获得其他参数。