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    • 21. 发明申请
    • METHOD FOR ESTIMATING FORMATION HYDROCARBON SATURATION USING NUCLEAR MAGNETIC RESONANCE MEASUREMENTS
    • 使用核磁共振测量估算形成碳氢化合物的方法
    • US20090206834A1
    • 2009-08-20
    • US12364104
    • 2009-02-02
    • Chanh Cao Minh
    • Chanh Cao Minh
    • G01V3/32
    • G01V3/32G01N24/081G01R33/50Y02A90/344
    • A method for estimating fluid saturation in a formation penetrated by a wellbore from nuclear magnetic resonance measurements made at a plurality of lateral depths into the formation from the wellbore includes estimating a bound water volume, a total porosity and a free water volume at each of the lateral depths from the nuclear magnetic resonance measurements. A minimum water saturation is estimated at each lateral depth from the total porosity, the free water volume and the bound water volume at each lateral depth. A value of water saturation is estimated at each lateral depth from the minimum water saturation at each lateral depth. A relationship between lateral depth and water saturation is determined. Water saturation is estimated at a selected lateral depth greater than the greatest lateral depth of the nuclear magnetic resonance measurements.
    • 通过从井眼在多个横向深度处进行的核磁共振测量来估计由井眼穿透的地层中的流体饱和度的方法包括估计每个井下的结合水体积,总孔隙率和自由水体积 横向深度从核磁共振测量。 从每个横向深度处的总孔隙率,自由水体积和结合水体积的每个横向深度估计最小水饱和度。 在每个横向深度处的最小水饱和度的每个横向深度估计水饱和度的值。 确定横向深度和水饱和度之间的关系。 在选择的横向深度估计水饱和度大于核磁共振测量的最大横向深度。
    • 22. 发明授权
    • Methods for formation evaluation based on multi-dimensional representation of nuclear magnetic resonance data
    • 基于核磁共振数据多维表示的形成评估方法
    • US07034528B2
    • 2006-04-25
    • US10604869
    • 2003-08-22
    • Chanh Cao MinhNicholas J. Heaton
    • Chanh Cao MinhNicholas J. Heaton
    • G01V3/00
    • G01N24/081G01V3/32
    • A method is disclosed for interpretation of multi-dimensional nuclear magnetic resonance data taken on a sample of an earth formation. Specifically, a set of NMR data is acquired for a fluid sample located either in a borehole or in a laboratory environment. From the set of NMR data, a multi-dimensional distribution is calculated using a mathematical inversion that is independent of prior knowledge of fluid sample properties. The multi-dimensional distribution is graphically displayed on a multi-dimensional map. Each fluid instance or artifact visible on the graph is identified as representing a probable existence of a detected fluid. One or more quantitative formation evaluation answers for one or more fluid instances is computed based on the multi-dimensional distribution associated with the respective fluid instance.
    • 公开了一种用于解释在地层样品上采集的多维核磁共振数据的方法。 具体地,对于位于钻孔或实验室环境中的流体样品,获取一组NMR数据。 从一组NMR数据,使用独立于流体样品性质的现有知识的数学反演来计算多维分布。 多维分布图形显示在多维地图上。 图上可见的每个流体实例或伪影被识别为表示检测到的流体的可能存在。 基于与相应流体实例相关联的多维分布来计算一个或多个流体实例的一个或多个定量形成评估答案。
    • 25. 发明授权
    • Estimating porosity and fluid volume
    • 估算孔隙度和流体体积
    • US08614573B2
    • 2013-12-24
    • US12886962
    • 2010-09-21
    • Chanh Cao Minh
    • Chanh Cao Minh
    • G01V3/00
    • G01V3/18Y02A90/344
    • The present disclosure relates to a method to estimate a subsurface formation property. A downhole logging tool is provided and disposed in a wellbore. Multiple measurements of various measurement types are obtained at various depths of investigation using the downhole logging tool. The multiple measurements may include natural gamma ray measurements, density measurements, resistivity measurements, nuclear measurements, and nuclear magnetic resonance measurements. The signal-to-noise ratio of the measured signals is increased using, for example, lateral stacking and multi-shell inversion. The subsurface formation property is estimated using the increased signal-to-noise ratio signals. The subsurface formation property may include porosity, adsorbed gas volume, free gas volume, bound water volume, free water volume, oil volume, and kerogen volume. A fluid analysis may be performed using a multi-dimensional nuclear magnetic resonance technique. Fluids such as water, oil, gas, and oil-based mud in the wellbore may be identified and/or evaluated.
    • 本公开涉及一种估计地下地层特性的方法。 井下测井工具被提供并设置在井眼中。 使用井下测井工具在不同深度的测量中获得各种测量类型的多次测量。 多个测量可以包括自然伽马射线测量,密度测量,电阻率测量,核测量和核磁共振测量。 测量信号的信噪比例如使用横向堆叠和多壳反演来增加。 使用增加的信噪比信号估计地下地层形成特性。 地下形成特性可以包括孔隙率,吸附气体体积,游离气体体积,结合水体积,游离水体积,油体积和干酪根体积。 可以使用多维核磁共振技术进行流体分析。 可以鉴定和/或评估井眼中的液体,例如水,油,气体和油基泥浆。
    • 26. 发明授权
    • Method for determining fluid type in reservoir
    • 确定储层流体类型的方法
    • US08378684B2
    • 2013-02-19
    • US12423073
    • 2009-04-14
    • Chanh Cao MinhMichel Claverie
    • Chanh Cao MinhMichel Claverie
    • G01V3/10
    • G01V3/28
    • A method for determining a formation type within a wellbore includes forming the wellbore such that the wellbore intersects fractures within a formation. Hydrocarbons are produced from the formation. An induction tool is disposed into the wellbore after producing the hydrocarbons. A resistivity of a portion of the formation is measured with the induction tool. The resistivity of the portion of the formation is compared with a known formation type. The formation type of the portion of the formation is determined based on the resistivity. A characteristic of the formation type is output.
    • 用于确定井筒内的地层类型的方法包括形成井筒,使得井筒与地层内的裂缝相交。 烃从地层中产生。 在制造碳氢化合物之后,将感应工具设置在井眼中。 用感应工具测量地层的一部分的电阻率。 将地层部分的电阻率与已知的地层类型进行比较。 基于电阻率确定地层部分的形成类型。 输出形成类型的特征。
    • 28. 发明申请
    • ESTIMATING POROSITY AND FLUID VOLUME
    • 估计孔隙度和流体体积
    • US20110068788A1
    • 2011-03-24
    • US12886962
    • 2010-09-21
    • CHANH CAO MINH
    • CHANH CAO MINH
    • G01V3/175
    • G01V3/18Y02A90/344
    • The present disclosure relates to a method to estimate a subsurface formation property. A downhole logging tool is provided and disposed in a wellbore. Multiple measurements of various measurement types are obtained at various depths of investigation using the downhole logging tool. The multiple measurements may include natural gamma ray measurements, density measurements, resistivity measurements, nuclear measurements, and nuclear magnetic resonance measurements. The signal-to-noise ratio of the measured signals is increased using, for example, lateral stacking and multi-shell inversion. The subsurface formation property is estimated using the increased signal-to-noise ratio signals. The subsurface formation property may include porosity, adsorbed gas volume, free gas volume, bound water volume, free water volume, oil volume, and kerogen volume. A fluid analysis may be performed using a multi-dimensional nuclear magnetic resonance technique. Fluids such as water, oil, gas, and oil-based mud in the wellbore may be identified and/or evaluated.
    • 本公开涉及一种估计地下地层特性的方法。 井下测井工具被提供并设置在井眼中。 使用井下测井工具在不同深度的测量中获得各种测量类型的多次测量。 多个测量可以包括自然伽马射线测量,密度测量,电阻率测量,核测量和核磁共振测量。 测量信号的信噪比例如使用横向堆叠和多壳反演来增加。 使用增加的信噪比信号估计地下地层形成特性。 地下形成特性可以包括孔隙率,吸附气体体积,游离气体体积,结合水体积,游离水体积,油体积和干酪根体积。 可以使用多维核磁共振技术进行流体分析。 可以鉴定和/或评估井眼中的液体,例如水,油,气体和油基泥浆。
    • 29. 发明授权
    • Method for estimating formation hydrocarbon saturation using nuclear magnetic resonance measurements
    • 使用核磁共振测量估算地层烃饱和度的方法
    • US07888933B2
    • 2011-02-15
    • US12364104
    • 2009-02-02
    • Chanh Cao Minh
    • Chanh Cao Minh
    • G01V3/00
    • G01V3/32G01N24/081G01R33/50Y02A90/344
    • A method for estimating fluid saturation in a formation penetrated by a wellbore from nuclear magnetic resonance measurements made at a plurality of lateral depths into the formation from the wellbore includes estimating a bound water volume, a total porosity and a free water volume at each of the lateral depths from the nuclear magnetic resonance measurements. A minimum water saturation is estimated at each lateral depth from the total porosity, the free water volume and the bound water volume at each lateral depth. A value of water saturation is estimated at each lateral depth from the minimum water saturation at each lateral depth. A relationship between lateral depth and water saturation is determined. Water saturation is estimated at a selected lateral depth greater than the greatest lateral depth of the nuclear magnetic resonance measurements.
    • 通过从井眼在多个横向深度处进行的核磁共振测量来估计由井眼穿透的地层中的流体饱和度的方法包括估计每个井下的结合水体积,总孔隙率和自由水体积 横向深度从核磁共振测量。 从每个横向深度处的总孔隙率,自由水体积和结合水体积的每个横向深度估计最小水饱和度。 在每个横向深度处的最小水饱和度的每个横向深度估计水饱和度的值。 确定横向深度和水饱和度之间的关系。 在选择的横向深度估计水饱和度大于核磁共振测量的最大横向深度。