首页> 外文会议>SPWLA annual logging symposium;Society of Petrophysicists and Well Log Analysts, inc >A NEW DIRECTIONAL PERMEABILITY MODEL COMBINING NMR AND DIRECTIONAL RESISTIVITY MEASUREMENTS FOR COMPLEX FORMATIONS
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A NEW DIRECTIONAL PERMEABILITY MODEL COMBINING NMR AND DIRECTIONAL RESISTIVITY MEASUREMENTS FOR COMPLEX FORMATIONS

机译:NMR与方向电阻率测量相结合的新方向性渗透率模型

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Conventional permeability models based on MercuryInjection Capillary Pressure (MICP) curves, such as theKatz-Thompson model, require estimation ofmicroscopic length parameters from core MICPexperiments. In wells lacking core data, these modelscannot be applied to estimate permeability. On the otherhand, conventional Nuclear Magnetic Resonance(NMR) permeability models can provide consecutivepermeability assessment along the wellbore, but theyare often unreliable in complex formations. We hereinpropose a new model for depth-by-depth directionalpermeability assessment in complex formations, bycombining borehole NMR and directional electricalresistivity measurements.The objectives of this paper are (a) to introduce a newNMR characteristic T_2 value to represent thecharacteristic length in real pore size distribution thatcontrols rock permeability, (b) to establish a newdirectional permeability model combining NMR anddirectional resistivity measurements, and (c) to test thereliability of the new model for permeabilityassessment in formations with multi-modal porosity(e.g. carbonate and tight sandstone formations).We numerically simulate the directional permeability,directional formation resistivity factor (FRF), and NMRT_2 relaxation curves, in 202 digital rock samples usingour state-of-the-art pore-scale simulation software. Thedigital rock samples are obtained by multi-scaleimaging on real rock samples, including dolostone,limestone, chalk, (tight) carbonate, (tight) sandstone,and sandpack samples. The simulated directionalpermeability is treated as the target reference for eachdigital rock sample.Next, we define a new NMR characteristic T_2 value torepresent the microscopic length parameter in real poresize distribution. The new NMR characteristic T_2 valueis minimally influenced by diffusional coupling effectthat distorts NMR T_2 distribution in multi-modal poresystems, and we numerically and theoreticallydemonstrate this property. Then we develop a newNMR-Resistivity model to estimate directionalpermeability by combining NMR characteristic T_2 anddirectional FRF. The new permeability model iscalibrated on 32 digital rock samples and successfullytested on the other 170 samples, with permeabilityranging from 8.4×10~(-5) mD to 48000 mD, spanning tenorders of magnitude. Results show that the modelestimatedpermeability is in good agreement with thetarget permeability for all rock types.Furthermore, we compare the model-predictedpermeability with lab permeability on 16 carbonate coresamples. We upscale the NMR characteristic T_2 andFRF from pore-scale to core-scale, and then estimatethe core-scale permeability by the proposed NMRResistivitymodel. Excellent agreement between themodel-estimated and lab permeability demonstrates thereliability of the new model on the core scale.Our proposed permeability model can be applied towells with NMR and directional resistivity logs,overcoming the requirement for core measurements. Itprovides accurate and consecutive directionalpermeability assessment along the wellbore. It alsoshows a potential in estimating relative permeability inhydrocarbon-bearing formations. The outcomes of thisresearch can significantly improve permeabilityassessment in complex reservoirs with multi-modalporosity, including carbonate, tight sandstone, andorganic-rich source rocks.
机译:基于汞的常规渗透性模型 注射毛细管压力(MICP)曲线,如 katz-thompson模型,需要估算 来自核心MICP的显微长度参数 实验。在缺乏核心数据的井中,这些模型 不能申请估计渗透率。在另一 手,常规核磁共振 (NMR)渗透性模型可以连续提供 沿着井筒的渗透性评估,但它们 在复杂的地层通常不可靠。我们在本文 提出一个深度深度方向的新模型 复杂地层的渗透性评估,通过 结合钻孔NMR和方向电气 电阻率测量。 本文的目标是(a)介绍一个新的 NMR特征T_2值表示 实际孔径分布的特征长度 控制岩石渗透率,(b)建立一个新的 核磁共振和态联渗透率模型 定向电阻率测量,(c)测试 新型渗透性模型的可靠性 具有多模态孔隙度的地层评估 (例如碳酸盐和紧密砂岩形成)。 我们在数值上模拟定向渗透性, 方向形成电阻率因子(FRF)和NMR T_2放松曲线,在202个数字岩石样品中使用 我们最先进的孔径仿真软件。这 数字岩石样本是通过多尺度获得的 在真正的岩石样本上成像,包括Dolostone, 石灰石,粉笔,(紧密)碳酸盐,(紧)砂岩, 和砂包样品。模拟方向 渗透率被视为每个目标参考 数字岩石样本。 接下来,我们将新的NMR特征T_2值定义为 代表真实孔中的微观长度参数 尺寸分布。新的NMR特征T_2值 通过扩散耦合效应来微小地影响 在多模态孔中扭曲NMR T_2分布 系统,我们在数值和理论上 展示这个属性。然后我们开发一个新的 NMR电阻率模型估计定向 通过组合NMR特征T_2和渗透性 定向FRF。新的渗透性模型是 在32个数字岩石样本上校准并成功校准 在其他170个样本上进行测试,具有渗透性 从8.4×10〜(-5)md到48000 md,跨越十个 数量级。结果表明,模特般的 渗透率与之吻合良好 所有岩石类型的目标渗透性。 此外,我们比较模型预测的 具有16个碳酸核心的实验室渗透性的渗透性 样品。我们高档NMR特征T_2和 FRF从孔鳞到核心级,然后估计 所提出的nmrresistivity的核心透露性渗透率 模型。之间的良好协议 型号估计和实验室渗透性展示了 新模型对核心规模的可靠性。 我们所提出的渗透性模型可以应用于 具有NMR和方向电阻率的孔, 克服核心测量要求。它 提供准确和连续的方向 沿井筒的渗透性评估。它也是 显示估计相对渗透性的潜力 含烃地层。这个结果 研究可以显着提高渗透性 复杂储层的评估多莫代尔 孔隙率,包括碳酸盐,砂岩,和 有机富有的源岩。

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