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    • 2. 发明申请
    • Method to determine properties of a sedimentary body from thickness and grain size distribution at a point within the body
    • 确定沉积体的性质的方法,从体内的一个点处的厚度和粒度分布来确定
    • US20060265131A1
    • 2006-11-23
    • US10550172
    • 2004-03-18
    • Max DeffenbaughDavid HoyalNeal AdairChun Huh
    • Max DeffenbaughDavid HoyalNeal AdairChun Huh
    • G01V1/28
    • G01V1/30G01V1/306G01V2210/661
    • A method to determine the properties of a water-lain sediment body from a measurement of grain size distribution and deposit thickness at one location in the body is disclosed. In one embodiment, the method comprises (a) determining the flow properties at the measured location, (b) extrapolating the flow properties back to the inlet through which the depositing flow was emitted, (c) determining at least one property of the water-lain sediment throughout the sediment body by modeling the flow properties using the extrapolated flow properties at the inlet from step (b) as a boundary condition. The flow properties associated with the sediment body include flow velocity, suspended sediment volume fractions, deposition time, and flow height. The properties of the water-lain sediments include, in addition to the flow properties associated with deposition of the sediments, the thickness of the sediment body, the size of the body, the shape of the body, and the grain size distribution at each point within the body.
    • 公开了一种通过测量身体中一个位置的粒度分布和沉积物厚度来确定水体沉积物的性质的方法。 在一个实施方案中,该方法包括(a)确定在测量位置处的流动性质,(b)将流动特性外推回到沉积流被排出的入口,(c)确定水 - 通过使用来自步骤(b)的入口处的外推流动性质作为边界条件来模拟流动性质来沉淀整个沉积物体中的沉积物。 与沉积物相关的流动特性包括流速,悬浮物体积分数,沉积时间和流动高度。 除了与沉积物沉积相关的流动特性之外,水沉积物的性质还包括沉积物的厚度,身体的尺寸,身体的形状以及每个点的粒度分布 在身体内。
    • 6. 发明授权
    • Method to determine properties of a sedimentary body from thickness and grain size distribution at a point within the body
    • 确定沉积体的性质的方法,从体内的一个点处的厚度和粒度分布来确定
    • US07433784B2
    • 2008-10-07
    • US10550172
    • 2004-03-18
    • Max DeffenbaughDavid C. HoyalNeal L. AdairChun Huh
    • Max DeffenbaughDavid C. HoyalNeal L. AdairChun Huh
    • G06F19/00
    • G01V1/30G01V1/306G01V2210/661
    • The properties of a water-lain sediment body are determined from a measurement of grain size distribution and deposit thickness at one location in the body is disclosed. The flow properties at the measured location are determined, the flow properties are extrapolated back to the inlet through which the depositing flow was emitted, at least one property of the water-lain sediment throughout the sediment body is determined by modeling the flow properties using the extrapolated flow properties at the inlet as a boundary condition. The flow properties associated with the sediment body include flow velocity, suspended sediment volume fractions, deposition time, and flow height. The properties of the water-lain sediments include, in addition to the flow properties associated with deposition of the sediments, the thickness of the sediment body, the size of the body, the shape of the body, and the grain size distribution at each point within the body.
    • 水体沉积物的性质是根据​​粒度分布的测量和体内一个位置的沉积厚度来确定的。 确定测量位置处的流动性质,将流动特性外推回到沉积流体通过该入口流入沉积物体的入口,通过使用 入口处的外推流量特性作为边界条件。 与沉积物相关的流动特性包括流速,悬浮物体积分数,沉积时间和流动高度。 除了与沉积物沉积相关的流动特性之外,水沉积物的性质还包括沉积物的厚度,身体的尺寸,身体的形状以及每个点的粒度分布 在身体内。
    • 9. 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。