Improving the Permeability Derivation from NMR Data for Reservoir Rocks with Complicated Pore Connectivity

H. Kwak, Jun Gao, A. Harbi
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引用次数: 2

Abstract

The formation permeability is one of the most important Petrophysical information acquired by low field Nuclear Magnetic Resonance (NMR) data. The absolute permeability of reservoir rocks can be accurately calculated by porosity measured by NMR if permeability is well correlated with porosity [1, 2]. This is true for the rocks with all pores are well connected, such as conventional sandstone reservoir. The correlation between permeability and porosity, however, does not always established well for carbonate reservoir rocks, which are known to have heterogeneous pore-to-pore connectivity. Thus, without accurate pore connectivity information, the permeability derived from NMR data for rocks with poor connection among pores is not quite accurate. The current study proposes a new method to measure an accurate pore-to-pore connectivity from the total volume of a fluid displacement through miscible single phase fluid mixing process. The pore connectivity factor is calculated from the fluid connectivity through different pore systems which can be derived by the volume comparison of NMR invisible D2O replacement with NMR visible H2O in each pore systems. Once the pore connectivity is measured, it is applied to the modified permeability model, such as modified free-fluid model (Timur-Coates model) [3], to calculate accurate permeability. Another benefit of the proposed method is the flexibility of D2O injection condition. Carbonate reservoir rocks with various degrees of connectivity have been studied in the current study. For the verification purpose, the permeabilities calculated by the proposed method have been compared to those measured by other conventional laboratory techniques. The proposed method can also be applied to NMR logging technique for accurate NMR driven permeability derivation which currently accepted as references for reservoirs with complicated connectivity, such as carbonates.
利用核磁共振数据改进孔隙连通性复杂储层渗透率推导方法
地层渗透率是低场核磁共振资料获取的最重要的岩石物性信息之一。如果渗透率与孔隙度关系良好,通过核磁共振测量孔隙度可以准确计算出储层岩石的绝对渗透率[1,2]。对于孔隙连通良好的岩石,如常规砂岩储层,也是如此。然而,对于碳酸盐岩储集层来说,渗透率和孔隙度之间的相关性并不总是建立得很好,因为碳酸盐岩储集层具有非均质孔间连通性。因此,如果没有准确的孔隙连通性信息,对于孔隙连通性差的岩石,通过核磁共振数据获得的渗透率不是很准确。本研究提出了一种新的方法,通过混相单相流体混合过程,从流体驱替的总体积来精确测量孔间连通性。孔隙连通性系数由流体通过不同孔隙体系的连通性来计算,通过对各孔隙体系中核磁共振不可见D2O置换量与核磁共振可见H2O置换量的比较得出。一旦测量到孔隙连通性,将其应用于修正的渗透率模型,如修正的自由流体模型(Timur-Coates模型)[3],以计算出准确的渗透率。该方法的另一个优点是D2O注入条件的灵活性。目前研究的碳酸盐岩储集层具有不同程度的连通性。为了验证目的,用该方法计算的渗透率与其他常规实验室技术测量的渗透率进行了比较。该方法还可应用于核磁共振测井技术,对碳酸盐岩等连通性复杂的储层进行精确的核磁共振渗透率推导。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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