¹H NMR techniques have gained extensive acceptance in petrophysics for the evaluation of fluid-saturating reservoir rocks. This thesis presents the development of new NMR methods regarding the reserves (determination of pore length scales and surface relaxivities), productivity (estimates of permeability) and recovery of fluids (resolves of saturation evolution) in rocks.Traditionally, pore lengths are evaluated from the ground relaxation eigenmodes of spin-bearing molecules in pore space. This evaluation is not straightforward since it is affected by surface relaxivity. Here, we use an approach to determine pore length from detecting the high relaxation eigenmodes, in which way the eigenvalue spectrum directly scales to the pore size distribution. Based on this, we extend this approach for the use with low-field NMR spectrometers and 2D NMR eigenmode correlation methods. Surface relaxivity can be further extracted from these 2D correlation maps, which is in agreement with an independent NMR measurement.Permeability is generally estimated from surface relaxation via empirical pore-network models. However, for heterogeneous rocks a single (or averaged) permeability value may not be adequate. Therefore, we measure surface relaxation in conjunction with MRI techniques. Permeability profiles can then be obtained from spatially resolved relaxation maps yielding local connectedness between adjacent slices. The results are confirmed by the comparison of brine-permeability measurements.MRI experiments of fluids in rocks at reservoir-like conditions may yield optimized recovery strategies of reservoir fluids. In this context we combine MRI with diffusion-relaxation correlation measurements during flooding intervals. The results provide substantial information, such as flooding front and saturation profiles of immiscible fluids discriminated by fluid type.
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机译:1 H NMR技术已在岩石物理学中广泛用于评估流体饱和储层岩石。本文介绍了有关岩石储量(确定孔隙度和表面弛豫度),生产率(渗透率的估算)和流体采收率(饱和度演化的解析度)的新NMR方法的发展。自旋轴承分子在孔隙空间的地面弛豫本征模式。该评估不是直接的,因为它受表面弛豫度的影响。在这里,我们使用一种通过检测高弛豫本征模来确定孔长的方法,通过这种方法,本征值谱直接缩放到孔径分布。基于此,我们将此方法扩展为与低场NMR光谱仪和2D NMR本征模式相关方法结合使用。可以从这些2D相关图谱中进一步提取表面弛豫性,这与独立的NMR测量相符。通透性通常是通过经验孔隙网络模型从表面弛豫估计的。但是,对于非均质岩石,单个(或平均)渗透率值可能不够。因此,我们结合MRI技术测量表面松弛。然后可以从空间解析的弛豫图获得渗透率分布图,从而在相邻切片之间产生局部连通性。盐水渗透率测量结果的比较证实了上述结果。在类似油藏的条件下对岩石中的流体进行MRI实验可得出优化的储层采收策略。在这种情况下,我们在洪水期间将MRI与扩散松弛相关性测量结合起来。结果提供了实质性信息,例如通过流体类型区分的不混溶流体的驱替锋和饱和度剖面。
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