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    • 1. 发明授权
    • Process for predicting behavior of a subterranean formation
    • 预测地下地层行为的过程
    • US6052520A
    • 2000-04-18
    • US245983
    • 1999-02-05
    • James W. Watts, III
    • James W. Watts, III
    • E21B49/00G01V11/00G06F17/50G06F19/00G01V1/00G06T17/50
    • G06F17/5018E21B49/00G01V11/00G06F2217/16
    • A method is disclosed of predicting a characteristic of a fluid-containing physical system such as a reservoir. The physical system is discretized to a plurality of gridcells. For each gridcell, nonlinear governing equations are constructed that are representative of fluid properties for each fluid. The nonlinear terms are linearized to derive linear equations at a current timestep. The linear equations are then solved to determine estimates of the solution. The estimated solution is then improved by a gridcell-by-gridcell computation wherein flows into and out of a particular gridcell are determined using linearized values of nonlinear terms in gridcells adjacent that particular gridcell. The improved solution is used to predict a property of a fluid in the physical system at end of the timestep. These calculation steps are repeated for a plurality of timesteps and the results are used to predict a property of the physical system and the fluids it contains as a function of time.
    • 公开了一种预测诸如储存器的含液体物理系统的特性的方法。 物理系统离散化为多个网格单元。 对于每个网格单元,构造了表示每个流体的流体特性的非线性控制方程。 线性化的非线性项目以在当前时间步长上导出线性方程。 然后求解线性方程式以确定解的估计。 然后通过网格逐网格计算来改进估计的解决方案,其中流入和流出特定网格单元的流量是使用与特定网格单元相邻的网格单元中的非线性项的线性化值来确定的。 改进的解决方案用于在时间步骤结束时预测物理系统中的流体的属性。 对于多个时间步骤重复这些计算步骤,并且结果用于预测物理系统及其包含的流体的属性作为时间的函数。
    • 2. 发明授权
    • Method for determining seismic velocities
    • 确定地震速度的方法
    • US5978314A
    • 1999-11-02
    • US821551
    • 1997-03-21
    • Long Don Pham
    • Long Don Pham
    • G01V1/30G01V1/36
    • G01V1/303
    • A method for determining a substantially optimal NMO velocity function for use in stacking a CMP gather of seismic data traces. The method begins with an initial estimate of the NMO velocity function for the CMP gather. This initial estimate is typically determined through conventional seismic velocity analysis. The method then picks a first velocity-traveltime pair falling on the initial estimate of the NMO velocity function and conducts a two-dimensional interpolative search of trial velocity-traveltime pairs in the neighborhood of the pick to find a substantially optimal velocity-traveltime pair. This substantially optimal velocity-traveltime pair is the trial velocity-traveltime pair having the highest stack response and is substituted for the pick in the NMO velocity function. The method then proceeds to find substantially optimal velocity-traveltime pairs to replace each of the other picks on the initial estimate of the NMO velocity function. Preferably, the two-dimensional interpolative search consists of a one-dimensional parabolic interpolative search to identify the optimal velocity for each computational time within a specified time window, followed by a one-dimensional search to select one of these optimal velocities which, together with its corresponding computational time, becomes the substantially optimal velocity-traveltime pair for the pick in question.
    • 一种用于确定用于堆叠地震数据轨迹的CMP集合的基本上最佳的NMO速度函数的方法。 该方法从CMP聚集的NMO速度函数的初始估计开始。 这个初步估计通常是通过传统的地震速度分析来确定的。 然后,该方法选择落在NMO速度函数的初始估计上的第一速度 - 旅行时间对,并且对拾取附近的试验速度 - 行进时间对进行二维内插搜索,以找到基本上最佳的速度 - 行进时间对。 这个基本上最佳的速度 - 旅行时间对是具有最高堆栈响应的试验速度 - 旅行时间对,并且代替NMO速度函数中的选取。 然后,该方法继续找到基本上最佳的速度 - 旅行时间对来替代NMO速度函数的初始估计上的其他选择中的每一个。 优选地,二维内插搜索由一维抛物线内插搜索组成,以在指定时间窗内为每个计算时间识别最佳速度,随后进行一维搜索以选择这些最佳速度中的一个,其连同 其对应的计算时间成为所讨论的拾取器的基本上最佳的速度 - 行进时间对。
    • 5. 发明授权
    • Method for attenuating surface wavetrains in seismic data
    • 地震数据衰减表面瓦斯的方法
    • US5781503A
    • 1998-07-14
    • US790947
    • 1997-01-29
    • Young C. Kim
    • Young C. Kim
    • G01V1/36G01V1/28
    • G01V1/36G01V2210/32
    • A method for attenuating source-generated surface wavetrains in a set of seismic data traces. According to the method, the seismic data traces are Fourier transformed with respect to time to determine the frequency components of the surface wavetrain. A phase matching operation is then performed using estimates of the wavenumbers for each of the frequency components to approximately align the surface wavetrain in the seismic data traces. Next, a spatial low-pass filter is used to remove the approximately aligned surface wavetrain. Finally, the phase matching is removed and an inverse Fourier transformation is performed to return the seismic data traces to the time domain.
    • 一种用于在一组地震数据轨迹中衰减源生成的表面波长的方法。 根据该方法,地震数据轨迹相对于时间进行傅里叶变换,以确定表面波纹的频率分量。 然后使用每个频率分量的波数的估计来执行相位匹配操作,以近似地对准地震数据迹线中的表面波形。 接下来,使用空间低通滤波器去除大致对准的表面波纹。 最后,去除相位匹配,并执行逆傅里叶变换以将地震数据轨迹返回到时域。
    • 8. 发明授权
    • Method of datuming seismic data and method of processing seismic data
    • 地震资料数据化方法及地震数据处理方法
    • US5629905A
    • 1997-05-13
    • US127297
    • 1993-09-24
    • Yiu-Wa A. Lau
    • Yiu-Wa A. Lau
    • G01V1/36
    • G01V1/36
    • Disclosed is a method of datuming seismic trace data from a first horizon to a lower second subsurface horizon, both located above a target horizon. A seismic source and receiver are positioned along the first horizon and each assigned a coordinate representing a position along the first horizon. The seismic trace data includes both header information and seismic data. The header information includes the coordinates assigned to the source and receiver. The seismic data is a record of reflection amplitude versus travel time of a seismic signal traveling from the source, downward through and intersecting the second horizon at a downward intersection point, reflecting upward from the target horizon, upward through and intersecting the second horizon at an upward intersection point, and upward to the receiver. The method generally includes determining for both the downward upward intersection points, coordinates along the second horizon corresponding to positions along the second horizon. The header information will now include these coordinates along the second horizon. Additionally, disclosed is a method of processing seismic trace data, in which datumed seismic trace data, datumed by any method or as described above, is now processed utilizing surface consistent algorithms to remove the effect of the subsurface between the first and second horizon.
    • 公开了一种将地震迹线数据从位于目标水平线上方的第一水平线到下部第二地下水平线的数据的方法。 地震源和接收器沿着第一水平线定位,并且每个地震源和接收器分配表示沿着第一水平线的位置的坐标。 地震迹线数据包括报头信息和地震数据。 标题信息包括分配给源和接收器的坐标。 地震数据是地震信号从源头向下穿过并与第二水平线相交的反射幅度与行进时间的记录,向下交叉点,从目标水平线向上反射,向上穿过并与第二水平线相交, 向上交叉点,并向上接收。 该方法通常包括确定向下的向上交叉点,沿着与沿着第二水平线的位置相对应的沿着第二水平线的坐标。 标题信息现在将包括沿着第二层的这些坐标。 此外,公开了一种处理地震迹线数据的方法,其中使用表面一致算法来处理由任何方法或如上所述的数据化地震迹线数据,以消除第一和第二地平线之间的地下影响。