GEOLOGICAL LOG DATA PROCESSING METHODS AND APPARATUSES

    公开(公告)号:US20170298727A1

    公开(公告)日:2017-10-19

    申请号:US15628911

    申请日:2017-06-21

    摘要: A method and a resistivity image logging tool connected or connectable to one or more processing devices process geological log data to construct missing information from destroyed or occluded parts using cues from observed data. The geological log data signals can be generated through use of the logging tool having one or more electrodes interacting with a formation intersected by a borehole. The processing involves the steps of: in respect of one or more data dimensions associated with missing values in a log data set, decomposing the signal into a plurality of morphological components; and morphologically reconstructing the signal such that missing values are estimated.

    METHOD FOR DETERMINING GEOLOGICAL SURFACE AND SUBSURFACE RESISTIVITY
    63.
    发明申请
    METHOD FOR DETERMINING GEOLOGICAL SURFACE AND SUBSURFACE RESISTIVITY 有权
    用于确定地质表面和表面电阻率的方法

    公开(公告)号:US20160033672A1

    公开(公告)日:2016-02-04

    申请号:US14451074

    申请日:2014-08-04

    IPC分类号: G01V3/38 G01V3/36

    摘要: A method for determining geological subsurface resistivity. The method includes obtaining a set of lightning parameters associated with a lighting strike received by a geological volume of material, the set of lightning parameters including an indicium of the current of the lightning strike at a first initial time and an indicium of the current of the lightning strike at a first decay time subsequent to the first initial time, and inferring the resistance of the volume of geological material, at least in part, from the set of lightning parameters.

    摘要翻译: 确定地质地下电阻率的方法。 该方法包括获得与由材料的地质体积接收的照明打击相关联的一组闪电参数,闪电参数的集合包括在第一初始时间的雷击电流的标记和 在第一次初始时间之后的第一衰减时间雷击,并且至少部分地从闪电参数组推断出地质材料体积的电阻。

    Induction tool for detail evaluation of near borehole zone
    64.
    发明授权
    Induction tool for detail evaluation of near borehole zone 有权
    近井眼区域详细评估感应工具

    公开(公告)号:US07567869B2

    公开(公告)日:2009-07-28

    申请号:US11741575

    申请日:2007-04-27

    CPC分类号: G01V3/28

    摘要: Measurements made with an induction logging tool are processed to provide a resistivity model of fluid invasion of the formation. Up to five zones can be determined over a radial distance of about 0.6 m. It is emphasized that this abstract is provided to comply with the rules requiring an abstract which will allow a searcher or other reader to quickly ascertain the subject matter of the technical disclosure. It is submitted with the understanding that it will not be used to interpret or limit the scope or meaning of the claims.

    摘要翻译: 用感应测井工具进行的测量被处理以提供地层流体侵入的电阻率模型。 可以在约0.6米的径向距离上确定多达五个区域。 要强调的是,该摘要被提供以符合要求摘要的规则,这将允许搜索者或其他读者快速确定技术公开的主题。 提交它的理解是,它不会用于解释或限制权利要求的范围或含义。

    METHOD AND APPARATUS FOR GENERATING A MAGNETIC RESONANCE DATA FILE
    65.
    发明申请
    METHOD AND APPARATUS FOR GENERATING A MAGNETIC RESONANCE DATA FILE 有权
    用于产生磁共振数据文件的方法和装置

    公开(公告)号:US20080116892A1

    公开(公告)日:2008-05-22

    申请号:US11936857

    申请日:2007-11-08

    IPC分类号: G01V3/36 G01V3/14 G01V3/38

    摘要: In a method for operating a magnetic resonance imaging system to generate a magnetic resonance data file, raw magnetic resonance data are acquired, and k-space is established in a computerized storage medium, with k-space being divided into a contiguous central region and a contiguous region surrounding the central region. In a computerized procedure, the raw data are entered into k-space at a constant sampling rate for both of the central and peripheral regions, while sampling the central region with a first density of sampling points, and sampling the peripheral region at a second density of sampling points that is less than the first sampling density. The set of data points thereby representing sampled k-space is made available in a data file as an output from the computerized procedure, in a form allowing an image to be reconstructed from the contents of the data file.

    摘要翻译: 在用于操作磁共振成像系统以产生磁共振数据文件的方法中,获取原始磁共振数据,并且在计算机化存储介质中建立k空间,其中k空间被划分为连续的中心区域和 围绕中心区域的连续区域。 在计算机程序中,以中央和外围区域的恒定采样率将原始数据输入到k空间中,同时以第一密度采样点对中心区域进行采样,并以第二密度采样外围区域 的采样点小于第一采样密度。 由此表示采样的k空间的数据点集合在数据文件中作为来自计算机化过程的输出,以允许从数据文件的内容重建图像的形式提供。

    Using electrical impedance tomography to map subsurface hydraulic
conductivity
    66.
    发明授权
    Using electrical impedance tomography to map subsurface hydraulic conductivity 失效
    使用电阻断层扫描来映射地下水力传导性

    公开(公告)号:US6147497A

    公开(公告)日:2000-11-14

    申请号:US106405

    申请日:1998-06-29

    CPC分类号: G01V3/24

    摘要: The use of Electrical Impedance Tomography (EIT) to map subsurface hydraulic conductivity. EIT can be used to map hydraulic conductivity in the subsurface where measurements of both amplitude and phase are made. Hydraulic conductivity depends on at least two parameters: porosity and a length scale parameter. Electrical Resistance Tomography (ERT) measures and maps electrical conductivity (which can be related to porosity) in three dimensions. By introducing phase measurements along with amplitude, the desired additional measurement of a pertinent length scale can be achieved. Hydraulic conductivity controls the ability to flush unwanted fluid contaminants from the surface. Thus inexpensive maps of hydraulic conductivity would improve planning strategies for subsequent remediation efforts. Fluid permeability is also of importance for oil field exploitation and thus detailed knowledge of fluid permeability distribution in three-dimension (3-D) would be a great boon to petroleum reservoir analysts.

    摘要翻译: 使用电阻抗层析成像(EIT)来绘制地下水力传导性。 EIT可用于绘制在地下测量幅度和相位的水力传导率。 液压传导性取决于至少两个参数:孔隙度和长度尺度参数。 电阻层析成像(ERT)测量并映射三维导电性(可与孔隙度相关)。 通过引入相位测量以及幅度,可以实现相关长度尺度的期望的附加测量。 液压导电性控制从表面冲洗不需要的流体污染物的能力。 因此,廉价的水力传导图可以改进后续修复工作的规划策略。 流体渗透性对于油田开采也是非常重要的,因此三维(3-D)流体渗透率分布的详细知识将对石油储层分析师是一个很大的好处。

    Electromagnetic induction spectroscopy for identifying hidden objects
    67.
    发明授权
    Electromagnetic induction spectroscopy for identifying hidden objects 失效
    用于识别隐藏物体的电磁感应光谱

    公开(公告)号:US5963035A

    公开(公告)日:1999-10-05

    申请号:US915656

    申请日:1997-08-21

    申请人: I. J. Won

    发明人: I. J. Won

    CPC分类号: G01V3/12

    摘要: A spectrogram of secondary magnetic field strength as a function of frequency and spatial relationship is used to identify hidden objects. A time-varying multi-frequency primary electromagnetic field is generated, preferably over the range 100 Hz to 300 kHz, which induces a time-varying multi-frequency secondary electromagnetic field about the hidden object. The strength of the secondary field, typically inphase and quadrature, is plotted as a spectrogram over a low frequency broadband spectrum as a function of frequency and spatial relationship between the hidden object and the secondary field strength detector. From this spectrogram, indications may be had of the hidden object's characteristics such as location, size and shape, and material composition. Preferably, the measured spectrogram is compared against a library of reference spectrograms by a computer to identify the hidden object.

    摘要翻译: 使用作为频率和空间关系的函数的次级磁场强度的光谱图来识别隐藏物体。 产生时变多频初级电磁场,优选地在100Hz至300kHz的范围内,这引起了关于隐藏对象的时变多频次级电磁场。 二次场的强度,通常为相位和正交,作为与低频宽带频谱之间的谱图作为隐藏对象和次级场强检测器之间的频率和空间关系的函数进行绘制。 从这个光谱图可以看出隐藏物体的特征,如位置,大小和形状,以及材料组成。 优选地,通过计算机将测量的光谱图与参考光谱图的文库进行比较以识别隐藏的对象。

    Method for identifying non-magnetic minerals in earth formations
utilizing magnetic susceptibility measurements
    68.
    发明授权
    Method for identifying non-magnetic minerals in earth formations utilizing magnetic susceptibility measurements 失效
    利用磁化率测量法识别地层中的非磁性矿物的方法

    公开(公告)号:US4507613A

    公开(公告)日:1985-03-26

    申请号:US434443

    申请日:1982-10-15

    申请人: Eric P. Dion

    发明人: Eric P. Dion

    CPC分类号: G01V3/28

    摘要: A magnetic susceptibility log is run through an earth formation to identify the presence of any select non-magnetic minerals in association with magnetic minerals. The select non-magnetic mineral is identified as being present when the magnetic susceptibility measurement exceeds a level at which a measurable concentration of the select non-magnetic mineral is expected to be present.

    摘要翻译: 磁化率对数通过地层运行,以识别与磁性矿物相关的任何选择的非磁性矿物的存在。 当磁化率测量超过期望可选择的非磁性矿物的可测量浓度的水平时,选择的非磁性矿物被鉴定为存在。

    ESTIMATING MAGNETIC FIELD USING A NETWORK OF SATELLITES

    公开(公告)号:US20240012171A1

    公开(公告)日:2024-01-11

    申请号:US18023911

    申请日:2021-09-02

    IPC分类号: G01V3/40 G01V3/38 G01V3/36

    CPC分类号: G01V3/40 G01V3/38 G01V3/36

    摘要: A computer-implemented method includes: receipt and accession of magnetic field data from a constellation of satellites providing global coverage over the Earth in a time span less than one day; inter-calibrating the magnetic field data from all satellites to a common standard; quantifying the global magnetic disturbance and selecting quiescent intervals at least as short as one day for evaluation of Earth's internally-generated field; calculating global maps of the mean vector magnetic field for each quiet interval from the average of all satellite measurements in angular bins; converting the time sequence of global maps of the mean fields to time series of angular harmonic coefficients via direct convolution; applying spectral and regression analysis to the harmonic coefficient time series to identify and remove artifacts in the signals; reconstructing a continuous time and spatial representation of the magnetic field continuous in time and angular position globally.