Doughty D A, Tomutsa L
BDM-Oklahoma, National Institute for Petroleum and Energy Research (NIPER), Bartlesville 74005, USA.
Magn Reson Imaging. 1996;14(7-8):869-73. doi: 10.1016/s0730-725x(96)00218-4.
The high-field magnetic resonance (MR) characteristics of fluids in porous reservoir rock exhibit short T2 relaxation times and broad natural line widths. These characteristics severely restrict which MR imaging (MRI) methodology can be used to obtain high-resolution porescale images of fluids in porous rock. An MR microscopy protocol based on 3D backprojection using strong imaging gradients was developed to overcome many of these constraints. To improve the image quality of two-phase systems, multinuclear MRI using proton MR to image the brine phase and 19F MR of a fluorinated hydrocarbon to image the oil phase was used. Resolution as high as 25 microns per pixel has been obtained for fluid systems in Bentheim and Fontainebleau sandstones. Separate proton and 19F images of brine and oil phases show good agreement with total saturation images. Software has been developed to perform 3D erosion/dilations and to extract the pore size distribution from binarized 3D images of fluid filled porosity. Results from pore size measurements show significant differences in the nature of the pore network in Fontainebleau and Bentheim sandstones.
多孔储层岩石中流体的高场磁共振(MR)特征表现为T2弛豫时间短且自然线宽宽。这些特征严重限制了可用于获取多孔岩石中流体高分辨率孔隙尺度图像的磁共振成像(MRI)方法。基于使用强成像梯度的三维反投影开发了一种磁共振显微镜协议,以克服其中许多限制。为了提高两相系统的图像质量,采用了多核MRI,利用质子MR对盐水相成像,并利用氟化烃的19F MR对油相成像。对于本特海姆砂岩和枫丹白露砂岩中的流体系统,已获得高达每像素25微米的分辨率。盐水相和油相的单独质子图像和19F图像与总饱和度图像显示出良好的一致性。已开发出软件来执行三维侵蚀/膨胀,并从流体填充孔隙度的二值化三维图像中提取孔径分布。孔径测量结果表明,枫丹白露砂岩和本特海姆砂岩的孔隙网络性质存在显著差异。