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AN MICP-BASED PORE TYPING WORKFLOW – CORE SCALE TO LOG SCALE

机译:基于MICP的孔分型工作流程-核对数刻度

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Carbonate reservoirs are inherently complex in their nature. This complexity is due to a combination of depositional rock fabric textures and diagenetic modification of the rocks. Post-depositional processes can modify the original petrophysical properties (e.g. permeability, irreducible water saturation and relative permeability) and result in a disconnection between original depositional rock fabric and current reservoir properties.Pore types are a critical element of rock types since they exert a dominant control over petrophysical properties and fluid flow. Their proper definition is especially important in complex carbonates with multiple pore systems. Several papers, however, restrict pore typing to MICP groups without transferring to log domain necessary for reliable earth modeling.A procedure has been developed to describe the dominant pore types occurring within a carbonate reservoir based on the interpretation of standard core data, mercury injection capillary pressure data and wireline log data. This procedure incorporates the following components: sample selection methodology, data acquisition, data quality control and corrections, parameterization of the MICP curves using Gaussian decomposition, clustering, extrapolation of MICP derived pore types groups (PTGs) to all core plug samples, and lastly prediction in the log-domain.The workflow described here is unique in that it describes the process from sample selection through log-scale prediction, PTGs are defined independently of the original depositional geology, parameters which describe the whole MICP curve shape are utilized, and objective clustering is used to remove subjective decisions.In this paper, we will describe the proposed workflow and present a case study from a carbonate field where characterizing PTGs in this way provided a better understanding of controls on rock properties and fluid flow than was achieved by looking at the depositional facies alone.
机译:碳酸盐岩储层本质上是复杂的。这种复杂性是由于沉积岩石织物质地和岩石的成岩作用的结合所致。沉积后的过程可能会改变原始的岩石物理性质(例如渗透率,不可减少的水饱和度和相对渗透率),并导致原始沉积岩层与当前储层性质之间的脱节。 孔隙类型是岩石类型的关键元素,因为它们主要控制岩石物理特性和流体流动。在具有多个孔隙系统的复杂碳酸盐中,它们的正确定义尤为重要。但是,有几篇论文将孔类型限制为MICP组,而没有转移到可靠的地球建模所必需的对数域。 根据标准岩心数据,注汞毛细管压力数据和电缆测井数据的解释,已经开发出一种方法来描述碳酸盐岩储层中主要的孔隙类型。该程序包含以下组成部分:样品选择方法,数据采集,数据质量控制和校正,使用高斯分解对MICP曲线进行参数化,聚类,将MICP衍生的孔类型组(PTG)外推到所有岩心塞样品,最后进行预测在日志域中。 这里描述的工作流程是独特的,它描述了从样品选择到对数尺度预测的过程,独立于原始沉积地质学定义了PTG,利用了描述整个MICP曲线形状的参数,并且使用了客观聚类来消除主观决定。 在本文中,我们将描述拟议的工作流程,并从碳酸盐岩领域进行案例研究,与仅查看沉积相相比,以这种方式表征PTG可以更好地理解对岩石特性和流体流动的控制。

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