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    • 32. 发明授权
    • Method for constructing a geologic model of a subsurface reservoir
    • 构建地下储层地质模型的方法
    • US07369980B2
    • 2008-05-06
    • US10586373
    • 2005-02-22
    • Max DeffenbaughPaul A. Dunn
    • Max DeffenbaughPaul A. Dunn
    • G06G7/48
    • E21B49/00G01V1/301
    • The present invention is a method for constructing a geologic model of a subsurface reservoir which is a composite sedimentary body (30) composed of many smaller fundamental sedimentary bodies (32). In one embodiment, the fundamental sedimentary bodies (32) within the composite body (30) are specified by the properties of the flow which built them, including the flow properties that existed at the local inlet (36) of each fundamental body (32). The statistical distribution of these local inlet properties is characterized throughout the composite sedimentary body (30) using either outline forms of some of the fundamental sedimentary bodies (32) or a well penetration which samples the composite sedimentary body (30). The geologic model is constructed by placing an appropriate statistical distribution of the fundamental sedimentary bodies (32) into the outline form of the composite sedimentary body (30) so that the grain size distribution and/or other geologic properties are specified at each point within the composite sedimentary body (30).
    • 本发明是一种构造地下储层的地质模型的方法,该地下储层是由许多较小的基底沉积体组成的复合沉积体(30)(32)。 在一个实施例中,复合体(30)内的基础沉积体(32)由构成它们的流动特性来确定,包括存在于每个基体(32)的局部入口(36)处的流动性质, 。 这些局部入口性质的统计分布在整个复合沉积体(30)中的特征是使用一些基本沉积体(32)的轮廓形式或对复合沉积体(30)进行取样的井渗透。 地质模型是通过将基础沉积体(32)的适当统计分布放置在复合沉积体(30)的轮廓形式中构成的,以使得粒度分布和/或其他地质特性在 复合沉积体(30)。
    • 37. 发明授权
    • Systems and methods for in situ resistive heating of organic matter in a subterranean formation
    • 地层中有机物原位电阻加热的系统和方法
    • US09394772B2
    • 2016-07-19
    • US14489113
    • 2014-09-17
    • William P. MeurerChen FangFederico G. GalloNazish HodaMichael W. Lin
    • William P. MeurerChen FangFederico G. GalloNazish HodaMichael W. Lin
    • E21B43/24E21B36/04
    • E21B43/2401E21B36/04
    • A method for pyrolyzing organic matter in a subterranean formation includes powering a first generation in situ resistive heating element within an aggregate electrically conductive zone at least partially in a first region of the subterranean formation by transmitting an electrical current between a first electrode pair in electrical contact with the first generation in situ resistive heating element to pyrolyze a second region of the subterranean formation, adjacent the first region, to expand the aggregate electrically conductive zone into the second region, wherein the expanding creates a second generation in situ resistive heating element within the second region and powering the second generation in situ resistive heating element by transmitting an electrical current between a second electrode pair in electrical contact with the second generation in situ resistive heating element to generate heat with the second generation in situ resistive heating element within the second region.
    • 用于在地下地层中热解有机物质的方法包括通过在电接触中的第一电极对之间传输电流来在地下地层的第一区域中至少部分地在集束导电区内为第一代原位电阻加热元件供电 利用第一代原位电阻加热元件来热解邻近第一区域的地层的第二区域,以将聚集导电区域扩展到第二区域,其中扩展在第二区域内产生第二代原位电阻加热元件 通过在与第二代原位电阻加热元件电接触的第二电极对之间传输电流来向第二代原位电阻加热元件供电,以在第二区域内的第二代原位电阻加热元件产生热量 n。