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首页> 外文期刊>AAPG Bulletin >Carbonate rock characterization and modeling: Capillary pressure and permeability in multimodal rocks—A look beyond sample specific heterogeneity
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Carbonate rock characterization and modeling: Capillary pressure and permeability in multimodal rocks—A look beyond sample specific heterogeneity

机译:碳酸盐岩的表征和建模:多峰岩石中的毛细压力和渗透率-超越样品比异质性的外观

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摘要

Carbonate rocks are known for their heterogeneity and petro-physical complexity. This commonly leads to large uncertainties in reservoir models that are intended to predict fluid storage and fluid flow. In this article, focus is given to the characterization of pore systems at core-plug scale to provide improved models for permeability and saturation prediction. These methods fall under a wider rock-typing workflow. We examine the use of mercury-air capillary pressure data for rock-type definition and for predicting saturation and permeability. We present new methods for modeling saturation in rocks with multimodal pore-throat size distributions. The methods bear similarity to those previously published but with some key differences, mainly by relating the capillary pressure data to the pore systems representative for a rock type. We also present a new method for relating permeability to pore-throat sizes that is more versatile, in that it can be employed for all types of pore-throat size distributions—unimodal or multimodal. We demonstrate that a normalized pore-throat radius parameter forms a straight line relationship with permeability over six orders of magnitude. It appears to be a fundamental property for all pore systems so far examined. The wider implication of the workflows presented is that they offer better integration between the methods used for saturation prediction and the methods used for permeability prediction, something that is desirable for all subsurface studies.
机译:碳酸盐岩以其非均质性和岩石物理复杂性而闻名。这通常导致旨在预测流体存储和流体流量的储层模型存在很大的不确定性。在本文中,重点是岩心塞尺度上的孔隙系统表征,以提供用于渗透率和饱和度预测的改进模型。这些方法属于更广泛的摇滚工作流程。我们研究了使用汞-空气毛细管压力数据进行岩石类型定义以及预测饱和度和渗透率。我们提出了用于模拟具有多峰孔喉尺寸分布的岩石中饱和度的新方法。该方法与以前发表的方法相似,但有一些主要区别,主要是通过将毛细管压力数据与代表岩石类型的孔隙系统相关联。我们还提出了一种将渗透率与孔喉尺寸相关联的新方法,该方法更加通用,因为它可用于所有类型的孔喉尺寸分布(单峰或多峰)。我们证明归一化的孔喉半径参数与渗透率超过六个数量级形成一条直线关系。到目前为止,它似乎是所有孔隙系统的基本特性。所提出的工作流程的广泛含义是,它们在用于饱和度预测的方法和用于渗透率预测的方法之间提供了更好的集成,这是所有地下研究所希望的。

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