首页> 外文会议>SPWLA Annual Logging Symposium;Society of Petrophysicists and Well Log Analysts, inc >CORE PLUG NUCLEAR MAGNETIC RESONANCE (NMR) ANALYSIS AS A METHOD TO ESTIMATE PERMEABILITY ANISOTROPY
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CORE PLUG NUCLEAR MAGNETIC RESONANCE (NMR) ANALYSIS AS A METHOD TO ESTIMATE PERMEABILITY ANISOTROPY

机译:核芯核磁共振(NMR)分析作为估算渗透率各向异性的一种方法

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Porosity and permeability data are two of the most important petrophysical properties typically measured from core plugs taken from cored wells for reservoir characterization. Laminated reservoir facies can impart permeability anisotropy within reservoir intervals. Permeability anisotropy is commonly characterized by permeability measurements collected from horizontal (parallel to bedding) and vertical (perpendicular to bedding) core plugs taken adjacent or close to each other along the cored section. However, more horizontal core plugs are typically collected than paired horizontal and vertical core plugs. As a result of this, any k_v/k_h data derived may not be representative of the entire cored interval. In addition, it is often not possible to retrospectively collect vertical plugs from cored sections of older wells. This study examined whether nuclear magnetic resonance (NMR) could be utilized to determine core plug permeability anisotropy (k_v/k_h) from a single horizontal (or vertical) plug. The potential advantages of NMR are that: it is non-destructive, so the core plug is still available for further analysis; it would be possible to retrospectively collect permeability anisotropy data from existing horizontal core plugs; and a more representative k_v/k_h can be derived from a single plug than by deriving k_v and k_h from adjacent horizontal and vertical plugs. The approach investigated focused on using an NMR tomographic core measurement on the scale of individual lamina within cores. We simultaneously probe two size scales to estimate permeability at the pore scale and the layering at the laminar scale using spatially resolved T_2 relaxation measurements. By digitally slicing the rock down to 1 mm using advanced pulsed gradient NMR methods, porosity and pore size distributions can be quantified at the laminar scale in strongly laminated sediments. This information is used to estimate slice permeability via the T_2 log mean (k_(SDR)) model, which can then be used to estimate the permeability anisotropy by evaluating the sliced permeability values in either parallel or series. The ratio of these estimates is the k_v/k_h permeability anisotropy. In addition, perpendicular permeability can be predicted from k_v/k_h, if standard core analysis permeability data exists for the measured core plug. To enable calibration of NMR results with ‘hard data’, suitable oil well core plug samples from a number of stratigraphic intervals have been used. Core plugs were selected with a range of existing analyses such as, mineralogical and textural measurements, along with porosity and permeability, determined by standard core plug analysis techniques. Core plugs were selected in pairs with one plugged horizontal and one vertical. The traditional core plug data and our new NMR method were used to assess the application. Initial results showed that comparable permeability anisotropy data could be collected from single plugs by NMR when compared to k_v/k_h from horizontal and vertical core plug data. In some cases where there were differences between the NMR technique and the traditional core k_v/k_h data, the vertical and horizontal core plugs sampled slightly different intervals or degrees of lamination varied between the plugs. Hence, the NMR permeability anisotropy data may be more representative than the paired vertical and horizontal core plug data.
机译:孔隙度和渗透率数据是最重要的两个岩石物理性质,通常从取自岩心井的岩心塞进行测量以表征储层。层状储层相可在储层层段内赋予渗透率各向异性。渗透率各向异性通常的特征是沿水平方向(平行于顺层)和垂直方向(垂直于顺层)岩心塞沿岩心段相邻或接近地采集渗透率测量值。但是,通常收集的水平芯塞比成对的水平芯塞和垂直芯塞要多。结果,导出的任何k_v / k_h数据可能都无法代表整个核心间隔。另外,通常不可能从旧井的岩心段追溯收集竖向塞子。这项研究检查了是否可以利用核磁共振(NMR)来确定单个水平(或垂直)塞子的岩心塞渗透率各向异性(k_v / k_h)。 NMR的潜在优点是:它是非破坏性的,因此芯塞仍可用于进一步分析;有可能回顾性地从现有的水平岩心塞收集渗透率各向异性数据;与通过从相邻的水平和垂直插头导出k_v和k_h相比,可以从单个插头导出更具代表性的k_v / k_h。研究的方法侧重于在核芯内部单个薄片的尺度上使用NMR断层成像核芯测量。我们同时探测两个尺寸尺度,以使用空间分辨的T_2弛豫测量来估计孔隙尺度的渗透率和层尺度的分层。通过使用先进的脉冲梯度NMR方法将岩石数字化切片至1 mm,可以在层状尺度上定量测定强烈层压的沉积物中的孔隙度和孔径分布。该信息用于通过T_2对数均值(k_(SDR))模型估计切片渗透率,然后可以通过评估平行或串联切片的渗透率值将其用于评估渗透率各向异性。这些估计的比率为k_v / k_h磁导率各向异性。此外,如果存在用于测得的岩心塞的标准岩心分析渗透率数据,则可以根据k_v / k_h预测垂直渗透率。为了能够使用“硬数据”校准NMR结果,已使用了来自多个地层间隔的合适油井岩心塞样品。通过标准的岩心塞分析技术确定岩心塞,并进行一系列现有分析,例如矿物学和质地测量以及孔隙率和渗透率。成对选择芯插头,水平插头一对,垂直插头一对。使用传统的岩心塞数据和我们的新NMR方法来评估应用。初步结果表明,与水平和垂直岩心塞数据的k_v / k_h相比,可通过NMR从单个塞子收集可比较的渗透率各向异性数据。在某些情况下,核磁共振技术与传统的核芯k_v / k_h数据之间存在差异,垂直和水平核芯棒的采样间隔或层压程度略有不同。因此,NMR渗透率各向异性数据可能比成对的垂直和水平岩心塞数据更具代表性。

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