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Advanced Spectrometry and NMR Based Porosity Partitioning Integrated Technique in Evaluating Cretaceous Pinda Formation, Offshore Angola

机译:高级光谱法和NMR基孔隙率分区综合技术评价白垩纪Pinda形成,海上安哥拉

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Characterization of complex Cretaceous reservoirs of offshore Angola, Lower Congo basin, poses similar uncertainties of evaluating carbonates in other parts of the world. The formation is a mixture of clastics, with carbonates at varying fraction that changes with depositional environment. With horizons of complete carbonates and fraction of dolomite and anhydrite, it poses a real challenge to any Petrophysicist engaged in evaluation of these oil bearing formations. The primary evaluation problem becomes even more complicated with porosity related issues since the primary oil reservoirs in general fall in the carbonate sections with moderate porosity and with varying secondary porosity like vugs and occurrences of fractures at different intervals. There is often a significant difference in permeability between testing results and those estimated from formation evaluation results or computed from formation tester data. These observations have also been verified with core results. A need for integrated evaluation could therefore be easily reckoned, with proper matrix evaluation to generate a better estimation of intergranular porosity and a complementary method for accurate estimation of secondary porosity from vugs, and then incorporating the results to generate a more realistic permeability. Apart from evaluation challenges with conventional logs, the drilling mud system and logging dynamics generates some environment effect on the acquired data which impedes the efficient use of the data. Photoelectric factor is an important measurement in complex lithology, but its accuracy is very sensitive to mud systems and to borehole rugosity. The method of estimation of carbonates based on elemental yields from the new generation elemental logging devices has evolved significantly and in recent years magnesium can be separated out of the concentrations to provide a major input for estimating dolomitic fraction out of total carbonate in the formation. The remaining issue of porosity partitioning has been developed since 1995 with the incorporation of nuclear magnetic resonance (NMR) data. For carbonates, the porosity systems were assumed in a completely different way to accommodate the larger vugular fraction in the evaluation schemes. This new approach has been generated based on the knowledge and experience acquired in evaluating carbonates throughout the world. The approach in estimating permeability therefore takes advantage of the computation of vugular pore fraction from NMR. The recent technique provides significant accuracy while correlating with other answers from testing and core results. Improvement of the results depends on the data acquisition and uncertainty can be reduced by proper planning. The acquisition for the current case was forced to a limit since the drilling was carried out with very saline mud. Although, higher salinity for mud and formation water is always environmentally challenging to logging, a proper approach in cancelling the effect of borehole chlorine can generate very reasonable log quality. In the current analysis for Pinda carbonates, the authors utilize the carbonate-dedicated workflow comprising of elemental spectroscopy and nuclear magnetic resonance data acquired in an offshore well. Integrating all data and information with a proper workflow, realistic estimation of permeability was possible with a rock typing framework based on calibrated porosity partitioning.
机译:近海安哥拉复合白垩纪储层的特征在于刚果盆地,在世界其他地区评估碳酸盐的类似不确定性。该形成是疏土性的混合物,其具有随沉积环境变化的不同馏分的碳酸盐。随着完全碳酸盐和白云石和空中物的级数的视野,它对任何从事这些油轴承结构评估的岩石物理学家构成了真正的挑战。主要评估问题变得更加复杂,因为孔隙率相关的问题,因为一般的初级油储存器落入具有中等孔隙率的碳酸盐部分,并且具有不同的次要孔隙率,如不同的间隔的裂缝和骨折发生。测试结果之间通常存在显着差异,并且从地层评估结果估计或从地层测试仪数据计算的那些。这些观察结果也通过核心结果进行了验证。因此,可以容易地估计对综合评估,具有适当的基质评估,以产生晶间孔隙率的更好估计和用于从Vugs精确估计次级孔隙率的互补方法,然后结合结果以产生更现实的渗透率。除了使用传统日志的评估挑战之外,钻井泥浆系统和记录动态还会对所获取的数据产生一些环境影响,阻碍了数据的有效使用。光电因子是复杂岩性的重要测量,但其精度对泥浆系统非常敏感,并钻孔粗糙。基于新一代元素测井装置的元素产量的碳酸酯估计方法显着发展,近年来,镁可以分离出浓度的浓度,以提供用于在形成中的总碳酸盐中估算白云岩部分的主要输入。自1995年自1995年以来,已经开发了孔隙度分区的其余问题,并入核磁共振(NMR)数据。对于碳酸盐,以完全不同的方式假设孔隙率系统以适应评估方案中的较大的纵向级分。这一新方法是基于在全世界评估碳酸盐中获得的知识和经验而产生的。因此,估计渗透性的方法利用了来自NMR的尾骨孔径的计算。最近的技术提供了显着的准确性,同时与测试和核心结果的其他答案相关。结果的改进取决于数据采集和不确定性,可以通过适当的规划来减少。由于钻井用盐水泥进行了钻孔,所以当前情况的收购被迫限制。虽然泥浆和地层水的良长度始终对测井始终挑战,但是取消钻孔氯效果的适当方法可以产生非常合理的日志质量。在目前对Pinda碳酸盐的分析中,作者利用了包括在近海井中获取的元素光谱和核磁共振数据的碳酸盐专用工作流程。将所有数据和信息与适当的工作流程集成,基于校准孔隙率分区的岩石键入框架,可以实现渗透性的现实估计。

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