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Improved characterisation and modelling of heterolithic tidal sandstone reservoirs

机译:改善了异质性潮汐砂岩储层的表征和模拟

摘要

Tidal heterolithic sandstone reservoirs comprise millimetre- to centimetre-scale intercalations of mudstone and sandstone. Their effective flow properties are poorly predicted by data that do not sample a representative elementary volume (REV), or models that fail to capture the complex 3D architecture of sandstone and mudstone layers. The aim of this dissertation is to develop improved predictions of effective single and multiphase permeabilities in heterolithic tidal sandstones. A surface-based modelling approach has been developed, which honours the geometry of geologic heterogeneity surfaces, integrating easily measurable outcrop derived dataset as input parameters. The workflow uses template surfaces to represent heterogeneities classifiedudby geometry rather than length-scale. The surface-based methodology has been applied to generate generic, 3D mini-models of trough and planar cross-bedded tidal sandstones with differing proportions of sandstone and mudstone. The models closely capture the bedform architectures observed at outcrop and are suitable for flow simulation. Quantitative geometrical input data to construct the models was extracted from an outcrop analogue which records deposition in a tide-dominated deltaic and estuarine setting. The model results demonstrate that effective single-phase permeability of tidal crossbedded sandstones varies with sample volume. A REV of 1 m3 was identified, confirming that the model volume of 9 m3 (> REV) yields representative values. The impact on effective permeability of seven geometric parameters controlling the density of mudstone drapes was determined: mudstone drape coverage, foreset thickness, toeset dip angle, dune climb angle, foreset to toeset ratio, style of cross-bedding (trough or tabular), size of the mudstone drape patches. The impact of seven geometric parameters on effective permeability was determined. Effective permeability decreases as the mudstone fraction increases, and is highly anisotropic. Each parameter investigated can significantly impact on effective permeability, depending upon the flow direction and sandstone fraction, causing considerable spread of the values. During oil/water flow, relative permeabilities are not affected by mudstone drapes, but the irreducible oil saturation varies depending on flow direction and mudstone content. Theudworkflow presented here can be used with subsurface data, supplemented by outcrop analog observations, to generate effective single and multi-phase permeability values to be derived for use in larger-scale reservoir models.
机译:潮汐异质砂岩储层包括毫米至厘米级的泥岩和砂岩插层。没有对代表性基本体积(REV)进行采样的数据或无法捕获砂岩和泥岩层的复杂3D体系结构的模型,很难有效预测其有效流动特性。本文的目的是开发改进的预测异质潮汐砂岩中单相和多相渗透率的方法。已经开发了一种基于表面的建模方法,该方法尊重地质异质性表面的几何形状,将易于测量的露头导出数据集集成为输入参数。工作流使用模板表面来表示按几何类型分类的非均质性,而不是长度尺度。基于表面的方法已被用于生成槽和平面的跨层潮汐砂岩的通用3D微型模型,其中砂岩和泥岩的比例不同。这些模型紧密地记录了在露头观测到的岩床构造,并且适用于流动模拟。从露头类似物提取用于构建模型的定量几何输入数据,该露头类似物记录潮汐为主的三角洲和河口环境中的沉积。模型结果表明,潮汐交错层砂岩的有效单相渗透率随样品量的变化而变化。确定了1 m3的REV,从而确认9 m3(> REV)的模型体积产生了代表值。确定了七个控制泥岩盖布密度的几何参数对有效渗透率的影响:泥岩盖布覆盖率,前兆厚度,前倾倾角,沙丘爬升角,前倾与前倾比,横卧样式(谷状或板状),大小的泥岩悬垂补丁。确定了七个几何参数对有效渗透率的影响。有效渗透率随泥岩分数的增加而降低,并且是高度各向异性的。所研究的每个参数都可能对有效渗透率产生重大影响,具体取决于流动方向和砂岩分数,从而导致该值的显着分散。在油/水流动过程中,相对渗透率不受泥岩悬垂性的影响,但不可减少的油饱和度会根据流向和泥岩含量而变化。这里介绍的 udworkflow可以与地下数据一起使用,并通过露头模拟观测进行补充,以生成有效的单相和多相渗透率值,以推导用于大型储层模型。

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