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An Integrated Approach To Obtain Reliable Permeability Profiles From Logs in a Carbonate Reservoir

机译:一种从碳酸盐岩储层中的测井曲线获得可靠渗透率剖面的综合方法

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Permeability is one of the key petrophysical parameters in reservoir evaluation. Information about permeability is commonly derived from cores and test data, which generally cover only part of the reservoir section, but can also be derived from logs and then extrapolated to uncored intervals and wells. Two logs provide such information: acoustic and nuclear magnetic resonance (NMR). In the Karachaganak field, an approach based on the acoustic tool was preferred because of the textural characteristics of the vuggy carbonate reservoir. The approach relies also on the use of image logs to obtain a detailed description of the reservoir-rocks texture and to discriminate between rocks with primary interparticle porosity or very small vugs and lithotypes with multimodal distribution of pores, enlarged vugs, and touching vugs. More than 900 m of core have been used to validate the permeability log derived from the analysis of Stoneley waves in 25 wells from this field. A correlation between the validated log-derived permeability and the textural facies from image logs has allowed the relationship between permeability variations and the geological framework to be established. The results have been compared with dynamic data from production logging through the definition of flow units from Stoneley-wave-derived permeability and porosity-log data and the use of a stratigraphic-modified Lorenz plot (SMLP) to identify possible fluid-entry points. Three main permeability trends have been identified: 1. For undolomitized or patchily dolomitized biohermal deposits 2. for pervasively dolomitized lithologies characterized by lower mean permeability values 3. for facies characterized by well-developed vuggy porosity with enhanced dissolution phenomena (i.e., touching vugs and microfracturing) Also, well-test results have highlighted the occurrence, in some wells, of very high k values in the biohermal deposits, which are clearly unmatchable by log-derived matrix permeability. Open fractures have been observed in these wells on the image logs, thus suggesting that the enhanced permeability and the improved well performances have to be related to their presence. The comparison of log-derived permeability and well-test results has given a new perspective in the interpretation of well-test results with respect to the geological framework and a well-defined sequence-stratigraphic model. The extension of this methodology to new wells could improve knowledge of the petrophysical characteristics of the reservoir and allow better prediction of reservoir productivity.
机译:渗透率是储层评价中关键的岩石物理参数之一。关于渗透率的信息通常来自岩心和测试数据,这些数据通常仅覆盖部分储层,但也可以从测井中获得,然后外推到无岩心的层段和井中。两个日志提供了这样的信息:声波和核磁共振(NMR)。在卡拉恰格纳克油田,由于碳酸盐岩孔隙结构的特征,首选基于声学工具的方法。该方法还依赖于使用图像测井来获得对储层岩石质地的详细描述,并区分具有主要颗粒间孔隙度的岩石或非常小的孔洞和岩石型的岩石,这些孔洞具有多峰分布的孔洞,扩大的孔洞和接触孔洞。超过900 m的岩心已用于验证从该油田25口井的斯通利波分析得出的渗透率测井曲线。验证的测井资料渗透率与图像测井的纹理相之间的相关性允许建立渗透率变化与地质框架之间的关系。将结果与生产测井中的动态数据进行了比较,方法是根据斯通利波推导的渗透率和孔隙度测井数据定义流动单元,并使用地层修正的洛伦兹图(SMLP)来识别可能的流体进入点。已经确定了三种主要的渗透率趋势:1.对于未透云石化或部分白云石化的生物体沉积物2.对于具有较低平均渗透率值特征的普遍白云石化岩性3.对于以发达的松散孔隙度和增强的溶解现象为特征的相(即,接触孔洞和此外,良好的测试结果突出表明,在某些井中,生物herm沉积物中的k值非常高,这显然与对数衍生的基质渗透率无法匹配。在图像测井的这些井中已观察到裸眼裂缝,因此表明渗透率的提高和井眼性能的提高必须与其存在有关。对数导出的渗透率和试井结果的比较为地质结构和定义明确的层序-地层模型的试井结果的解释提供了新的视角。将该方法扩展到新井可以提高对储层岩石物理特性的了解,并可以更好地预测储层产能。

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