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STUDY ON THE RELATIONSHIP BETWEEN ROCK PROPERTIES AND NMR MEASUREMENT OF THE LOW PERMEABILITY, DUCTILE, SHALY SANDSTONES

机译:低渗透率,韧性,泥质砂岩的岩石性质与NMR测量关系的研究

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摘要

Assessments of shaly and low permeability hydrocarbon reservoir sandstones are always problematic. Traditional log-based techniques provide rock porosity but at best can only estimate permeability. Recent advances in the nuclear magnetic resonance (NMR) log technology provide additional benefits through a more direct permeability estimation based on computed volumes of movable and immovable fluids. However, the presence of clay, in reservoir rocks proves to be problematic not only for the traditional log measurements but also for NMR log interpretation. Many shaly sandstones that have good porosity appear to have highly variable permeability. In the presence of clays the most commonly used T_2 cutoff values seem to eventually yield inaccurate permeability estimates. This paper presents results of a study that focuses on NMR measurements on shaly sand samples taken from various oilfields in Australia. The study suggests that the T_2 cutoff values for the samples appear to be significantly different from the 'standard' values, in order for NMR-derived irreducible water to match core-derived irreducible water. This is also shown by the samples' resulting NMR-derived permeability estimates that are in more satisfactory agreement with the directly measured permeability values. The overall results underline the need to study T_2 cutoff values more closely for specific reservoir rocks before their practical uses in the field.
机译:谢利和低渗透性碳氢化合物储层砂岩的评估总是有问题的。基于传统的基于日志的技术提供岩石孔隙,但最佳只能估算渗透率。核磁共振(NMR)日志技术的最新进展通过基于计算的可移动和不可移动的流体的渗透率估计提供额外的益处。然而,在储层岩石中存在粘土,证明不仅是传统的日志测量而且对于NMR对数解释而言。许多具有良好孔隙率的Shaly砂岩似乎具有高度可变的渗透性。在粘土存在下,最常用的T_2截止值似乎最终产生不准确的渗透率估计。本文介绍了一项研究的结果,专注于从澳大利亚各种油田采取的谢利砂样上的NMR测量。该研究表明,样品的T_2截止值似乎与“标准”值显着不同,以便NMR衍生的不可缩续的水与核心衍生的不可缩续的水相匹配。这也通过样本显示的样品,从而导致与直接测量的渗透率值更令人满意的渗透率估计。整体结果强调了在实地实际用途之前更紧密地研究T_2截止值。

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