会员体验
专利管家(专利管理)
工作空间(专利管理)
风险监控(情报监控)
数据分析(专利分析)
侵权分析(诉讼无效)
联系我们
交流群
官方交流:
QQ群: 891211   
微信请扫码    >>>
现在联系顾问~
热词
    • 1. 发明申请
    • Method of Stratigraphic Modeling of Faults
    • 断层地层建模方法
    • US20160077237A1
    • 2016-03-17
    • US14483371
    • 2014-09-11
    • Tao SunMartin PerlmutterMichael James PyrczMorgan SullivanAshley Harris
    • Tao SunMartin PerlmutterMichael James PyrczMorgan SullivanAshley Harris
    • G01V99/00
    • G01V99/005G01V2210/642G06F17/5009
    • A new gridding method is disclosed for forward stratigraphic modeling that allows for syndepositional and/or postdepositional fault movement. The new gridding algorithm may represent both the lateral move of structure block, and provide efficiency that is comparable to the structured grid for forward stratigraphy model accessing previous deposited sediments stored in the grid. Embodiments of the disclosed methods allow for structural moves by performing a set of simple operations on the grid. The operations are generally simple, and do not change the overall topology of the grid. Therefore the operation can be easily repeated and the overall topological structure of the grid remains largely unchanged for simple access by the forward stratigraphic model. Further details and advantages of various embodiments of the method are described in more herein.
    • 公开了一种新的网格化方法,用于前向地层建模,允许综合沉积和/或后沉积故障运动。 新的网格算法可以代表结构块的横向移动,并且提供与用于前向地层学模型访问先前沉积在网格中的沉积物的结构化网格相当的效率。 所公开的方法的实施例允许通过在网格上执行一组简单的操作来进行结构移动。 操作通常很简单,不要改变网格的整体拓扑。 因此,通过前向地层模型的简单访问,可以容易地重复操作并且电网的整体拓扑结构基本上保持不变。 该方法的各种实施例的更多细节和优点在本文中更详细地描述。
    • 2. 发明申请
    • SEDIMENT TRANSPORT SIMULATION WITH PARAMETERIZED TEMPLATES FOR DEPTH PROFILING
    • 用于深度分布的参数化模式的SEDIMENT运输模拟
    • US20160070829A1
    • 2016-03-10
    • US14478805
    • 2014-09-05
    • Tao SunMorgan SullivanMichael James PyrczMartin PerlmutterJacob Covault
    • Tao SunMorgan SullivanMichael James PyrczMartin PerlmutterJacob Covault
    • G06F17/50G06F17/10
    • G06F17/5009G01V99/005G06F17/10
    • Depth-averaged flow simulation systems and methods provided herein employ parameterized templates for dynamical depth profiling for at least one step of a simulation. In one illustrative computer-based embodiment, the simulation method includes, for each map point at one given time step: determining a flow template and a sediment concentration template based on depth-averaged flow velocity and depth-averaged sediment concentrations of different classes of grain size for that map point; employing the templates to construct a vertically-distributed flow velocity profile and vertically-distributed sediment concentration profiles for associated classes of grain size for that map point, thereby obtaining 3D flow velocity and 3D sediment concentration fields; using the 3D fields to calculate fluid and sediment fluxes; updating the flow velocity and sediment concentration profiles based on the divergence of the fluxes; integrating the profiles to compute updated depth-averaged flow velocity and sediment concentrations and center of gravity; and solving the depth-averaged flow equations for the next time step.
    • 本文提供的深度平均流动模拟系统和方法使用用于动态深度分析的参数化模板用于至少一个模拟步骤。 在一个说明性的基于计算机的实施例中,对于在给定时间步骤的每个地图点,模拟方法包括:基于深度平均流速和不同种类的粒子的深度平均沉积物浓度确定流模板和沉降物浓度模板 该地图点的大小; 采用模板构建垂直分布的流速分布图和垂直分布的沉积物浓度分布,用于该地图点的相关类型的粒度,从而获得3D流速和3D泥沙浓度场; 使用3D场来计算流体和泥沙流量; 基于通量的发散度来更新流速和沉积物浓度分布; 整合轮廓以计算更新的深度平均流速和沉积物浓度和重心; 并解决下一个时间步长的深度平均流量方程。