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    • 4. 发明申请
    • Full Waveform Inversion Using Perfectly Reflectionless Subgridding
    • 全波反射采用完全无反射的子网格
    • US20140372043A1
    • 2014-12-18
    • US14286107
    • 2014-05-23
    • Wenyi HuAnatoly BaumsteinJohn E. AndersonCarey M. Marcinkovich
    • Wenyi HuAnatoly BaumsteinJohn E. AndersonCarey M. Marcinkovich
    • G01V1/34
    • G01V1/303G01V2210/679
    • Method for reconstructing subsurface profiles for seismic velocity or other geophysical properties from recorded seismic data. In one embodiment, a starting model of seismic velocity is assumed (10). The computational domain is divided into two (or more) subdomains by horizontal planes based on an analysis of velocity model (30), and the allowed maximum grid size for each subdomain is determined (50). Auxiliary perfectly matched layers (PML's) are attached to each planar interface between subdomains (80), e.g. two PML's on each side of the interface between the coarse and fine subdomains. Simulated seismic data are computed using the SG-DO technique (100-230). The simulated seismic data are compared to the recorded seismic data, then the residual is calculated (240) and used to update the model (320). The method may be iterated until the model is suitably converged (260).
    • 从记录的地震数据重建地震速度或其他地球物理特性的地下剖面的方法。 在一个实施例中,假定地震速度的起始模型(10)。 基于速度模型(30)的分析,计算域由水平面划分为两个(或多个)子域,并确定每个子域的允许的最大网格大小(50)。 辅助完美匹配层(PML)附接到子域(80)之间的每个平面界面,例如。 两个PML在粗略和精细子域之间的界面的每一边。 使用SG-DO技术(100-230)计算模拟地震数据。 将模拟地震数据与记录的地震数据进行比较,然后计算残差(240)并用于更新模型(320)。 可以重复该方法,直到模型适当地收敛(260)。
    • 9. 发明申请
    • Poynting Vector Minimal Reflection Boundary Conditions
    • 坡印矢量最小反射边界条件
    • US20160223697A1
    • 2016-08-04
    • US14887621
    • 2015-10-20
    • Tetyana VdovinaValeriy BrytikJohn E. AndersonThomas A. DickensWilliam CurryCarey M. Marcinkovich
    • Tetyana VdovinaValeriy BrytikJohn E. AndersonThomas A. DickensWilliam CurryCarey M. Marcinkovich
    • G01V1/28G06F17/16
    • A method for exploring for hydrocarbons, including: simulating a seismic waveform, using a computer, wherein computations are performed on a computational grid representing a subsurface region, said computational grid using perfectly matched layer (PML) boundary conditions that use an energy dissipation operator to minimize non-physical wave reflections at grid boundaries; wherein, in the simulation, the PML boundary conditions are defined to reduce computational instabilities at a boundary by steps including, representing direction of energy propagation by a Poynting vector, and dissipating energy, with the dissipation operator, in a direction of energy propagation instead of in a phase velocity direction; and using the simulated waveform in performing full waveform inversion or reverse time migration of seismic data, and using a physical property model from the inversion or a subsurface image from the migration to explore for hydrocarbons.
    • 一种用于探索碳氢化合物的方法,包括:使用计算机模拟地震波形,其中在表示地下区域的计算网格上执行计算,所述计算网格使用完全匹配层(PML)边界条件,其使用能量耗散算子 最小化网格边界处的非物理波反射; 其中,在模拟中,定义了PML边界条件以减少边界处的计算不稳定性,所述步骤包括表示坡坡廷矢量的能量传播方向,以及耗散算子在能量传播方向上耗散能量,而不是 在相速度方向上; 并使用模拟波形进行地震数据的全波形反演或反向时间偏移,并使用来自反演的物理性质模型或来自迁移的地下图像来探索碳氢化合物。