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Magnetic resonance relaxation-tomography to assess fractures induced in Vugular Carbonate Cores

机译:磁共振弛豫断层扫描技术评估在碳酸盐岩心中诱发的裂缝

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A method is presented to study fractures induced in full-size carbonate cores by means of Relaxation-Tomography (RT). This method combines nuclear magnetic resonance (NMR) relaxation and imaging techniques, and consists of obtaining, in addition to the usual H nuclei density (porosity) maps, images as relaxation time maps. By combining voxel-by-voxel signal intensity from the porosity map and relaxation time from the relaxation time map, one get the distribution of the signal intensity as a function of the relaxation time for selected internal regions of interest (ROI). The distribution of the signal intensity vs relaxation time gives information on the distribution of water in different structures inside the sample and therefore on the structure itself. One can compute the fraction of water in the ROI, relative to the total amount of water in the ROI, having relaxation time in a selected range. Also, average relaxation time, as the geometric mean, can be computed. In a previous paper (SPE 49294), we applied the method to quantify (following an operational NMR definition) matrix and vugular porosity in carbonate cores. In this paper we improve the computation of the relaxation time by introducing non-linear fitting of the data and extending the application to the study of fractures induced in carbonates. Sveral internal images from undisturbed vugular and microporous full-size carbonate cores saturated with water were obtained as porosity and longitudianl relaxation time (T sub 1) maps. The T sub 1 histograms from selected ROI's were obtained. Then, fractures were induced in the cores by repeated cycles of freezing and heating. The RT investigation was repeated on the treated cores after each step and the distributions of the relaxation times compared. The changes in the distributions suggest a twofold effect: the forming of new microfractures (increase of local surface-to-volume-ratio) and the expansion of pre-existing fractures (decrease of surface-to-volume ratio).
机译:提出了一种通过松弛层析成像(RT)研究全尺寸碳酸盐岩芯中引起的裂缝的方法。该方法结合了核磁共振(NMR)弛豫和成像技术,并且除了获得通常的H核密度(孔隙度)图之外,还包含图像作为弛豫时间图。通过结合来自孔隙率图的逐个体素信号强度和来自弛豫时间图的弛豫时间,可以得到选定的内部感兴趣区域(ROI)信号强度随弛豫时间的函数分布。信号强度与弛豫时间的分布给出了有关样品内部不同结构中水的分布的信息,因此也给出了结构本身的信息。一个人可以计算出ROI中水的比例,相对于ROI中水的总量,其弛豫时间在选定的范围内。同样,可以计算出平均弛豫时间,作为几何平均值。在以前的论文(SPE 49294)中,我们应用了该方法来量化(遵循可操作的NMR定义)碳酸盐岩心中的基质和孔隙孔隙度。在本文中,我们通过引入数据的非线性拟合并扩展其应用范围以研究碳酸盐岩引起的裂缝,来改善弛豫时间的计算。从孔隙饱和度和纵向弛豫时间(T sub 1)图获得了未受干扰的微孔和微孔全尺寸碳酸盐岩心的几个内部图像。从选定的ROI获得了T sub 1直方图。然后,通过反复的冷冻和加热循环在芯部中引起破裂。在每个步骤之后,对处理过的岩心重复进行RT研究,并比较弛豫时间的分布。分布的变化表明具有双重效应:新的微裂缝的形成(局部表面体积比的增加)和原有裂缝的扩展(表面体积比的减少)。

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