首页> 外文会议>SPWLA Annual Logging Symposium >PERMEABILITY CONTROLS ON MOLDIC GRAINSTONES: CT BASED PORE NETWORK MODELING OF CARBONATE RESERVOIR ROCK FROM WEST TEXAS AND A NEW NMR-BASED PERMEABILITY TRANSFORM
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PERMEABILITY CONTROLS ON MOLDIC GRAINSTONES: CT BASED PORE NETWORK MODELING OF CARBONATE RESERVOIR ROCK FROM WEST TEXAS AND A NEW NMR-BASED PERMEABILITY TRANSFORM

机译:镁粒的渗透性控制:来自德克萨斯州西部的碳酸盐岩储层岩石的基于CT的孔隙网络建模和基于NMR的新的渗透率转换

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We present a study aimed at understanding the main controls on permeability in carbonate grainstones dominated by moldic porosity in an effort to obtain more accurate permeability transforms from NMR logs in such formations. Computed x-ray microtomography (CT) images of the 3-D pore structure of seven core samples from a well in a West Texas oil reservoir revealed that the connectivity of neighboring molds was influenced heavily by flow paths that traverse a microporous matrix of cements in between the molds. A new process to build a pore network model from the CT images was developed. This process involved identification of individual molds and assignment of hydraulic resistivity for each pore-pore connection based on the porosity and thickness of the intervening microporous cement. The resulting models were successful in matching measured permeabilities of the core samples. Subsequent analysis of the pore network model indicated that the average thickness of the walls separating adjacent molds is a good predictor for the permeability. Specifically, the logarithm of the permeability was observed to vary linearly with the average wall thickness. Based on these findings, a new permeability transform was developed to convert NMR T2-distributions to permeability by estimating the average wall thickness from grain size and moldic porosity. The method was validated with 22 further core samples from the same formation, with significantly lower mean-square error than the traditional NMR-based permeability transforms derived for rocks dominated by primary, intergranular porosity.
机译:我们目前进行的一项研究旨在了解在以模孔为主导的碳酸盐岩中渗透率的主要控制因素,以便从此类地层的NMR测井中获得更准确的渗透率转换。西德克萨斯油藏中一口井的七个岩心样品的3-D孔结构的计算机X射线显微断层扫描(CT)图像显示,横穿水泥微孔基质的流动路径严重影响了相邻模具的连通性。在模具之间。开发了一种从CT图像建立孔隙网络模型的新方法。该过程涉及识别单个模具,并根据插入的微孔水泥的孔隙率和厚度为每个孔-孔连接分配水力电阻率。所得模型成功地匹配了岩心样品的测得的渗透率。孔隙网络模型的后续分析表明,将相邻模具分开的壁的平均厚度是渗透率的良好预测指标。具体而言,观察到渗透率的对数随平均壁厚线性变化。基于这些发现,开发了一种新的磁导率转换,可以通过从晶粒尺寸和铸型孔隙率估算平均壁厚来将NMR T2分布转换为磁导率。该方法用来自同一地层的另外22个岩心样品进行了验证,其均方差明显低于对主要为晶间孔隙度的岩石进行的基于NMR的传统渗透率变换。

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