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    • 21. 发明授权
    • Method for predicting fluid flow
    • 预测流体流动的方法
    • US09128212B2
    • 2015-09-08
    • US13201395
    • 2010-01-21
    • Tao SunDachang Li
    • Tao SunDachang Li
    • E21B43/00E21B47/00G06F17/10G06F7/57G01V99/00
    • G01V99/00G01V99/005G06F17/10G06F17/5009
    • A method of enhancing a geologic model of a subsurface region is provided. A bed topography of the subsurface region is obtained. The bed topography is defined by a plurality of cells with an elevation associated with each cell center. The bed topography is represented as a cell-centered piecewise constant representation based on the elevations associated with the cells. The bed topography is reconstructed to produce a spatially continuous surface. Flux and gravitation al force-related source terms are calculated based on the reconstructed bed topography. Fluxes are calculated between at least two of the cells. Fluid flow, deposition of sediments onto the bed, and/or erosion of sediments from the bed are predicted using the fluxes and gravitational force-related source terms. The predictions are inputted into the geologic model to predict characteristics of the subsurface region, and the predicted characteristics are outputted.
    • 提供了一种增强地下区域地质模型的方法。 获得地下区域的床形地貌。 床形状由具有与每个细胞中心相关联的高度的多个细胞定义。 基于与细胞相关联的高度,床形状表示为以细胞为中心的分段常数表示。 床形状被重建以产生空间连续的表面。 基于重构床形貌计算通量和重力与力相关源项。 在至少两个细胞之间计算通量。 流体流动,沉积物沉积到床上,和/或从床上沉积物的侵蚀是使用流量和重力相关的源项预测的。 将预测输入到地质模型中,以预测地下区域的特征,并输出预测特征。
    • 24. 发明授权
    • Method for geologic modeling through hydrodynamics-based gridding (Hydro-Grids)
    • 通过基于流体动力学网格(Hydro-Grids)进行地质建模的方法
    • US07742875B2
    • 2010-06-22
    • US11629822
    • 2005-06-24
    • Dachang LiTao SunChun HuhChris J. DonofrioJohn C. Van WagonerMax Deffenbaugh
    • Dachang LiTao SunChun HuhChris J. DonofrioJohn C. Van WagonerMax Deffenbaugh
    • G01V1/28G06F19/00
    • G01V1/306G01V1/282G01V2210/661
    • The present invention is a method of hydrodynamics-based gridding (Hydro-Grids) for creating geologic models of subsurface volumes, such as reservoirs. Vertical grid surfaces may be chosen in an unstructured fashion to provide lateral resolution where needed. Lateral grid surfaces are created to represent surfaces of constant geologic time based on simulation of the depositional processes that created the subsurface volume. The values of geologic properties are then specified within each cell created by the intersections of the vertical and lateral surfaces. The geologic data may include, for example, seismic data, outcrop studies, well log data, core data, numerical modeling data, and interpreted stratigraphic surfaces based on seismic data. The modeled geologic properties of the subsurface volume may include, for example, grain size distribution, connectivity, net-to-gross, porosity, permeability and pore pressure.
    • 本发明是一种基于流体动力学网格(Hydro-Grids)的方法,用于创建诸如水库的地下体积的地质模型。 可以以非结构化的方式选择垂直网格表面以在需要时提供横向分辨率。 创建横向网格表面以基于产生地下体积的沉积过程的模拟来表示恒定地质时间的表面。 然后在由垂直和侧面的交点创建的每个单元格中指定地质属性的值。 地质数据可以包括例如基于地震数据的地震数据,露头研究,测井数据,核心数据,数值模拟数据和解释地层表面。 地下体积的模拟地质特征可以包括例如粒度分布,连通性,净对毛孔,孔隙度,渗透性和孔隙压力。
    • 26. 发明申请
    • Method for Predicting Fluid Flow
    • 流体流动预测方法
    • US20150227655A1
    • 2015-08-13
    • US14692474
    • 2015-04-21
    • Tao SunDachang Li
    • Tao SunDachang Li
    • G06F17/50G01V99/00G06F17/10
    • G01V99/00G01V99/005G06F17/10G06F17/5009
    • A method of enhancing a geologic model of a subsurface region is provided. A bed topography of the subsurface region is obtained. The bed topography is defined by a plurality of cells with an elevation associated with each cell center. The bed topography is represented as a cell-centered piecewise constant representation based on the elevations associated with the cells. The bed topography is reconstructed to produce a spatially continuous surface. Flux and gravitational force-related source terms are calculated based on the reconstructed bed topography. Fluxes are calculated between at least two of the cells. Fluid flow, deposition of sediments onto the bed, and/or erosion of sediments from the bed are predicted using the fluxes and gravitational force-related source terms. The predictions are inputted into the geologic model to predict characteristics of the subsurface region, and the predicted characteristics are outputted.
    • 提供了一种增强地下区域地质模型的方法。 获得地下区域的床形地貌。 床形状由具有与每个细胞中心相关联的高度的多个细胞定义。 基于与细胞相关联的高度,床形状表示为以细胞为中心的分段常数表示。 床形状被重建以产生空间连续的表面。 基于重构床形貌计算通量和重力相关源项。 在至少两个细胞之间计算通量。 流体流动,沉积物沉积到床上,和/或从床上沉积物的侵蚀是使用流量和重力相关的源项预测的。 将预测输入到地质模型中,以预测地下区域的特征,并输出预测特征。
    • 27. 发明授权
    • Sediment transport by fully developed turbulent flows
    • 充分发展的湍流的沉积物运输
    • US08370121B2
    • 2013-02-05
    • US13131800
    • 2009-11-16
    • Tao SunDachang LiDavid Hoyal
    • Tao SunDachang LiDavid Hoyal
    • G06G7/48
    • G01V11/00
    • The invention is a method of modeling a hydrocarbon reservoir. A parameter value in a set of equations is adjusted so that the output of the equations accurately matches observed sediment erosion and deposition behavior for sediment sizes throughout a range of about 10 microns to about 10 centimeters. An initial condition of a sediment bed in the hydrocarbon reservoir is defined. The equations are applied to the initial condition, wherein outputs of the equations express how a fluid flow affects erosion and deposition of sediments at the initial condition. The initial condition is adjusted based on the equation outputs to create a subsequent sediment bed condition. The equations are re-applied to the subsequent sediment bed condition a pre-determined number of times. The subsequent sediment bed condition is re-adjusted after each re-application of the equations. The model of the hydrocarbon reservoir is created and outputted.
    • 本发明是一种对油气藏进行建模的方法。 调整一组方程式中的参数值,使得方程式的输出与约10微米至约10厘米范围内的沉积物大小的观察到的沉积物侵蚀和沉积行为精确匹配。 定义烃储层中沉积床的初始条件。 方程应用于初始条件,其中方程式的输出表示流体流如何影响初始条件下沉积物的侵蚀和沉积。 初始条件根据方程输出进行调整,以产生随后的沉积床状况。 方程式重新应用于随后的沉积床状态预定次数。 随后的沉积床条件在每次重新应用方程之后重新调整。 创建并输出了油气藏的模型。
    • 28. 发明申请
    • Sediment Transport By Fully Developed Turbulent Flows
    • 充分发展湍流的沉积物运输
    • US20110232913A1
    • 2011-09-29
    • US13131800
    • 2009-11-16
    • Tao SunDachang LiDavid Royal
    • Tao SunDachang LiDavid Royal
    • E21B43/00G06G7/57G06F17/10
    • G01V11/00
    • The invention is a method of modeling a hydrocarbon reservoir. A parameter value in a set of equations is adjusted so that the output of the equations accurately matches observed sediment erosion and deposition behavior for sediment sizes throughout a range of about 10 microns to about 10 centimeters. An initial condition of a sediment bed in the hydrocarbon reservoir is defined. The equations are applied to the initial condition, wherein outputs of the equations express how a fluid flow affects erosion and deposition of sediments at the initial condition. The initial condition is adjusted based on the equation outputs to create a subsequent sediment bed condition. The equations are re-applied to the subsequent sediment bed condition a pre-determined number of times. The subsequent sediment bed condition is re-adjusted after each re-application of the equations. The model of the hydrocarbon reservoir is created and outputted.
    • 本发明是一种对油气藏进行建模的方法。 调整一组方程式中的参数值,使得方程式的输出与约10微米至约10厘米范围内的沉积物大小的观察到的沉积物侵蚀和沉积行为精确匹配。 定义烃储层中沉积床的初始条件。 方程应用于初始条件,其中方程式的输出表示流体流如何影响初始条件下沉积物的侵蚀和沉积。 初始条件根据方程输出进行调整,以产生随后的沉积床状况。 方程式重新应用于随后的沉积床状态预定次数。 随后的沉积床条件在每次重新应用方程之后重新调整。 创建并输出了油气藏的模型。