Characterization of Tight Carbonate Reservoir by Using Nuclear Magnetic Resonance Log Analysis in the Bahrain Field

Rabab Al Saffar, Michael Dowen
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Abstract

The Bahrain Field (the "Field"), discovered in 1932, is an asymmetric anticline trending in a North-South direction of the Kingdom of Bahrain. It is a geologically complex field with 16 multi-stack carbonate and sandstone reservoirs, most of them oil bearing. The fluids varying from shallow tarry oil in Aruma to dry gas in the Khuff and pre-Khuff reservoirs. The Field has more than 2000 wells of which 90% have good quality log data. The Ostracod and Magwa reservoirs are heterogeneous, layered tight reservoirs and have been on production since 1964. The Ostracod reservoir consists of very heterogeneous with limestone intervals intercalated between shale layers, with a total thickness of around 200 ft. The Magwa reservoir conformably underlies the Ostracod reservoir. The Ostracod averages 120 ft in thickness and is dominated by limestone with high porosity, low permeability, and variable water saturations. Core derived permeability measurements are usually less than 5 mD and porosities average 22%. Production performance of individual wells is extremely variable and in many cases appears to be at odds with log-calculated saturations. Wells having good oil saturation often produce water and wells with low oil saturation produce high volumes of oil. Several studies have been conducted in an attempt to understand and resolve this. The variability of oil saturation which has been mapped both laterally across the Field and vertically within wells, led to the question of what caused the variation in oil saturation. The variation is not a function of depth, which one might expect. Causes might include oil failure to migrate into certain reservoir compartments, a loss of the original charge to shallower reservoir or the oil charge been restricted by rock quality. This paper attempts to address the variability in saturations seen across the Field and link known productivity to the Petrophysical interpretations. Nuclear Magnetic Resonance (NMR) logs had been employed in a targeted area of the Field in order to investigate rock quality in an attempt to explain the oil saturation distribution. A small NMR core study was undertaken in order to calibrate the NMR log response. The NMR data had been initially processed with what was considered a representative cut-off for Middle East Carbaonte rocks. This core study resulted in a surprisingly low series of T2 cut-off. The NMR logs were reprocessed with the more representative T2 cut-off. The resulting bound and free fluid fractions seemed to explain the observed well production.
巴林油田致密碳酸盐岩储层核磁共振测井特征研究
巴林油田(“油田”)发现于1932年,是巴林王国南北走向的不对称背斜。这是一个地质复杂的油田,有16个多叠位的碳酸盐岩和砂岩油藏,其中大部分为含油油藏。流体从Aruma的浅层焦油油到Khuff和前Khuff储层中的干气不等。该油田有2000多口井,其中90%的井测井资料质量较好。介形虫和Magwa储层为非均质层状致密储层,自1964年开始投产。介形虫储层由非常不均匀的灰岩层间或于页岩层之间组成,总厚度约为200英尺。Magwa储层整合在介形虫储层下方。介形虫层的平均厚度为120英尺,主要由高孔隙度、低渗透率和可变含水饱和度的石灰石组成。岩心渗透率测量值通常小于5md,孔隙度平均为22%。单口井的生产动态变化很大,在许多情况下与测井计算的饱和度不一致。含油饱和度好的井通常产水,含油饱和度低的井产油量大。为了理解和解决这个问题,已经进行了几项研究。含油饱和度的变化已经在整个油田的横向和井内的垂直方向上进行了绘制,这导致了含油饱和度变化的问题。这种变化并不是人们所期望的深度的函数。原因可能包括油运移到某些储层隔室失败,原始装药流失到较浅的储层,或者油装药受到岩石质量的限制。本文试图解决整个油田饱和度的可变性,并将已知的生产力与岩石物理解释联系起来。利用核磁共振测井技术对该油田的目标区域进行了岩石质量调查,试图解释含油饱和度分布。为了校准核磁共振测井响应,进行了一项小型核磁共振岩心研究。核磁共振数据最初被认为是中东碳酸盐岩的代表性截止点。这项核心研究得出了令人惊讶的低T2临界值。核磁共振测井用更具代表性的T2截止值重新处理。由此产生的束缚流体和自由流体馏分似乎解释了观察到的井产量。
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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