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Laboratory NMR Studies Of Unconventional Rocks Of 'LUKOIL-Western Siberia' Oil Fields

机译:“卢布西西伯利亚”油田非传统岩石的实验室NMR研究

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This paper presents the results of NMR studies of structure of void space of rock of complicated fields with hard reserves. Objects of study - "fritillary", "weathering crust", "bazhenite". These rocks are difficult for studying by conventional methods due to their high heterogeneity, low porosity and permeability, due to presence of large amounts of clays. Therefore we have used NMR relaxometer for study the structure of void space of such rocks. Total by NMR relaxometer were studied more than 200 samples of the three types of rocks, were made more than 500 NMR measurements 100% saturated and of dry samples. For a detailed study of the structure of the pore space was used the method of nuclear magnetic resonance (NMR), because the standard capillary methods (method of semipermeable membranes and of centrifugation) do not reveals the characteristic features of the structure of the void space which are inherent for these rocks. By using standard researches in principle not possible to determine the pore size and pore channels of less than 0.1 microns, and by these methods is impossible to study the so called "clay bound water" as a component in the distribution of fluids in the rock. In addition, the NMR method is more accurate and non-destructive method for studying the structure of the pore space of rocks. For the same samples, parallel of the NMR studies, were carried out routine investigations of reservoir properties, and more detailed lithological studies using a scanning electron microscope and gas chromatograph.
机译:本文介绍了硬储备复杂领域空隙空间结构的NMR研究结果。研究对象 - “贝母”,“风化外壳”,“挥之齐”。由于其具有大量粘土的存在,这些岩石难以通过常规方法进行研究,因为它们的存在高,孔隙率低和渗透率。因此,我们已经使用了NMR辐射仪来研究这种岩石的空隙空间的结构。通过NMR松弛仪进行总计三种类型的岩石的200多个样本,使100%饱和和干燥样品的100%以上。对于对孔隙结构的结构进行了详细研究,使用了核磁共振(NMR)的方法,因为标准毛细管方法(半透明膜和离心的方法)不透露空隙空间结构的特征特征这是这些岩石所固有的。通过原则上使用标准研究,不可能确定小于0.1微米的孔径和孔径,并且通过这些方法是不可能研究所谓的“粘土水”作为岩石中流体分布的组分。此外,NMR方法是研究岩石孔隙空间结构的更准确和非破坏性的方法。对于相同的样品,对NMR研究的并行进行,进行了储层性能的常规研究,以及使用扫描电子显微镜和气相色谱仪的更详细的岩性研究。

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