Chen S, Yao X, Qiao J, Watson A T
Department of Chemical Engineering, Texas A&M University, College Station 77843, USA.
Magn Reson Imaging. 1995;13(4):599-606. doi: 10.1016/0730-725x(95)00013-7.
The inversion time (TI) weighted inversion-recovery spin-echo (IRSE) imaging technique was used for laboratory characterization of fractures and porous matrix in permeable media. The method is based on the fact that relaxation rates in fractures and those in surrounding porous matrix are substantially different. Thus, by selectively suppressing imaging signals from either fractures or porous matrix, one can highlight fluid distributions in either of these regions so that fractures can be unambiguously identified and surrounding porous structures can be characterized. The advantages over conventional NMR spin-echo imaging are demonstrated with various fractured porous rock types. A technique to speed acquisitions of images of fluid distributions in porous matrix is also demonstrated.
反转时间(TI)加权反转恢复自旋回波(IRSE)成像技术用于对可渗透介质中的裂缝和多孔基质进行实验室表征。该方法基于这样一个事实,即裂缝中的弛豫率与周围多孔基质中的弛豫率有很大差异。因此,通过选择性地抑制来自裂缝或多孔基质的成像信号,可以突出这些区域中任一个区域的流体分布,从而能够明确识别裂缝并表征周围的多孔结构。通过各种裂缝性多孔岩石类型展示了该方法相对于传统核磁共振自旋回波成像的优势。还展示了一种加快获取多孔基质中流体分布图像的技术。