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Nuclear-Magnetic-Resonance Petrophysics in Thin Sand/Shale Laminations

机译:薄砂/页岩层合中的核磁共振岩石物理

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We discuss the use of nuclear-magnetic-resonance (NMR) logging in the petrophysical evaluation of thin sand/shale laminations. NMR helps detect thin beds, determine fluid type, establish the hydrocarbon type and volume if hydrocarbon is present, and, finally, determine the permeability of the sand layers (as opposed to that of the sand/shale system). Experiments were conducted on samples of 100% sand, 100% clay, and sand/clay layers with an NMR-logging tool at surface to verify the characteristic T2 bimodal relaxation distribution often observed in NMR logs that are acquired in thin beds. From the bimodal distribution, it is often possible to determine a cutoff to separate the productive sand layers from the shale layers and, with it, the porosity fraction of each component. Subsequently, the sand fraction, or net/gross ratio, can be estimated assuming that the 100%-sand porosity is known. Because gas, oil, and water have different NMR properties, fluid-typing techniques such as 2D NMR offer useful insights into the fluid type and properties in thin-layer sands. Because the laminations thickness is often less than the antenna aperture, the estimated permeability of the sand/ shale system will undercall the true permeability of the sand layers only. In this case, their permeability can be estimated quickly from Darcy's fluid-flow model. We show examples of thin sand/shale laminations that are oil-bearing and gas-bearing. In each case, the NMR detection was verified against borehole-imaging logs, and the fluid type in the sands was determined from multidimensional NMR analysis. The derived hydrocarbon volume was then compared with the results estimated from a triaxial induction tool. Permeability of the sand layers was also computed and compared to that of nearby thick sands. Core data in one well was used to validate NMR detection, porosity, permeability, and net sand thickness.
机译:我们讨论在薄砂岩/页岩层的岩石物理评价中使用核磁共振(NMR)测井。 NMR帮助检测薄层,确定流体类型,确定是否存在碳氢化合物(如果存在碳氢化合物)和体积,最后确定砂层的渗透率(与砂/页岩系统的渗透率相反)。在表面使用NMR测井仪对100%砂,100%粘土和砂/粘土层的样品进行了实验,以验证经常在薄床中采集的NMR测井中观察到的特征性T2双峰弛豫分布。根据双峰分布,通常可以确定一个分界值,以将生产性砂层与页岩层以及每个组分的孔隙率分开。随后,假设已知100%的砂岩孔隙度,就可以估算出砂石含量或净/毛比。由于天然气,石油和水具有不同的NMR特性,因此诸如2D NMR这样的流体分型技术可为深入了解薄层砂岩中的流体类型和特性提供有用的见识。因为叠片的厚度通常小于天线孔径,所以估计的砂岩/页岩系统的渗透率只会影响砂层的真实渗透率。在这种情况下,可以从达西的流体流动模型快速估算其渗透率。我们显示了含油和含气的薄砂/页岩薄板的例子。在每种情况下,都针对井下成像测井记录核实NMR,并根据多维NMR分析确定砂中的流体类型。然后将导出的碳氢化合物体积与从三轴感应工具估算的结果进行比较。还计算了沙层的渗透率,并将其与附近的厚沙的渗透率进行了比较。使用一口井中的岩心数据来验证NMR检测,孔隙率,渗透率和净砂厚度。

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