首页> 外文会议>SPWLA Annual Logging Symposium;Society of Petrophysicists and Well Log Analysts, inc >ADVANCED FORMATION LOGGING: A CASE STUDY OF REVEALING THE TRUE POTENTIAL OF A GAS RESERVOIR
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ADVANCED FORMATION LOGGING: A CASE STUDY OF REVEALING THE TRUE POTENTIAL OF A GAS RESERVOIR

机译:先进的地层测井:揭示天然气储层真实潜力的案例研究

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The economic decision to develop a new field depends heavily on the reservoir quality which, in turn, is based on two factors: the storage capacity and the flow capacity of the reservoir. The former is controlled by the porosity and hydrocarbon saturation and the latter is control by the permeability. This crucial information are computed using sets of logging measurement which is often supported by routine and advanced core analysis data. The process of comparing the log based interpretation with the core results can be time consuming and costly. New developments in logging technology especially in geochemical and dielectric logging are aiming to improve the log derived interpretation and reduce the uncertainties of the evaluation. This paper presents a case study where the integration of the advanced and standard logging tool is used to reveal the true potential of a gas reservoir.For Chevron in Western Australia the standard formation evaluation is usually based on spectral gamma ray, resistivity, density, neutron, sonic and magnetic resonance logs. This logging suite has been proven successful in determining the reservoir quality in clean gas sand reservoirs. However in new frontier fields the uncertainty becomes larger due to complex mineralogy, the choice of saturation equation, unknown formation salinity and the paucity of SCAL data. In this case study, the standard logging suites does provide a reasonable result, however, the introduction of the geochemical log reveals the existence of iron-rich heavy minerals, which suggests a higher calculated porosity after mineralogy correction. The dielectric log being sensitivity to water permittivity was used to measure the irreducible water volume independent of the inputs needed by a typical conventional water saturation method. In oil base mud environments, the dielectric log can measure the irreducible water in the reservoir as it is not displaced by the oil base filtrate. This advanced formation evaluation shows an increase of 22% gas in place in a particular compartment.A continuous permeability measurement can usually be inferred by the magnetic resonance log based on the free fluid and bound fluid ratio using the Timur-Coates equation. The bound fluid volume is determined by using a typical T2, 33 ms cutoff. However, the paramagnetic minerals in the formation are known to cause alteration in magnetic resonance relaxation time. In this example, the paramagnetic minerals caused a faster transverse relaxation time, hence a higher bound fluid will be computed if the T2 cutoff is not adjusted. This phenomenon has been a difficult challenge to solve in our industry. A new approach to compute the permeability was tried in this study where the irreducible water computed from the dielectric log was used as the bound fluid. The free fluid was computed by subtracting the total porosity with the dielectric irreducible water. The Timur-Coates permeability using these inputs is more consistent with offset data and confirmed by the mobilities from the formation pressure testing tool. The new approach reveals an almost 300% increase of flow capacity compared to conventional methods in the studied section.
机译:开发新油田的经济决策在很大程度上取决于储层质量,而储层质量又取决于两个因素:储层的储水量和储水量。前者受孔隙度和烃饱和度控制,后者受渗透率控制。这些关键信息是使用测井数据集计算得出的,而这些数据通常会得到常规和高级岩心分析数据的支持。将基于日志的解释与核心结果进行比较的过程可能既耗时又昂贵。测井技术特别是地球化学和介电测井技术的新发展旨在改善测井推导的解释并减少评估的不确定性。本文介绍了一个案例研究,其中使用了高级和标准测井工具的集成来揭示气藏的真正潜力。 对于西澳大利亚的雪佛龙公司,标准地层评估通常基于谱伽马射线,电阻率,密度,中子,声波和磁共振测井曲线。已证明该测井套件可成功确定清洁气砂储层的储层质量。但是,在新的前沿领域,由于复杂的矿物学,饱和度方程的选择,未知的地层盐度和SCAL数据的匮乏,不确定性变得更大。在本案例研究中,标准测井套件确实提供了合理的结果,但是,地球化学测井的引入揭示了富铁重矿物的存在,这表明在进行矿物学校正后,计算出的孔隙度更高。对介电常数敏感的介电测井曲线用于测量不可减少的水量,而与典型的常规水饱和法所需的输入量无关。在油基泥浆环境中,电介质测井可以测量储层中不可还原的水,因为水不会被油基滤液取代。这项先进的地层评估表明,在特定隔层中,到位的天然气增加了22%。 通常可以使用Timur-Coates方程根据自由流体和束缚流体的比率通过磁共振测井推断出连续磁导率的测量值。通过使用典型的T2(33毫秒截止)来确定束缚流体体积。但是,已知地层中的顺磁性矿物会引起磁共振弛豫时间的改变。在此示例中,顺磁性矿物导致了更快的横向弛豫时间,因此,如果不调整T2截止值,则将计算出更高的束缚流体。在我们的行业中,这种现象一直是难以解决的挑战。在这项研究中尝试了一种计算渗透率的新方法,该方法将从介电测井中计算出的不可还原水用作约束流体。通过用电介质不可还原水减去总孔隙率来计算自由流体。使用这些输入的Timur-Coates渗透率与偏移数据更加一致,并由地层压力测试工具的运动性证实。与研究部分中的常规方法相比,新方法显示出流量增加了近300%。

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