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Reservoir Rock Typing of a Giant Carbonate Field

机译:水库岩石打字巨型碳酸盐田地

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Reservoir Rock Types of Kharaib reservoirs have been defined as an interval of rock within which the geological and petrophysical properties that effect fluid flow are consistent and predictable. Lithofacies classifications are a purely geological grouping of reservoir rocks, which have similar lithology, texture, grain size, sorting etc. Each lithofacies indicates a certain depositional environment with a distribution trend and dimension. Petrophysical groups are classified by Porosity, Permeability, Capillary Pressure and Pore throat size distribution. A Rock Type combines both these classifications by linking petrophysical properties and lithofacies as part of the reservoir ock type definition. It has been previously shown that the static rock types are not always representative of multi-phase flow behavior in the reservoir. In this paper, we will present evolution of the rock type scheme within ZADCO. We discuss criteria used to define reservoir rock types in the current unified scheme. The objective of the proposed rock type scheme is to address shortcomings identified with the previous one in use and is based on the following criteria: a) each Rock Type can be characterized by similar depositional environment and diagenetic process; b) Porosity/Permeability overlap is minimal between different rock types; c) each rock type has a typical and unique set of Pore Throat Size Distribution; and d) each rock type has similar set of Capillary Pressure/ Relative Permeability curves at a given wettability. The recognized Reservoir Rock Types have been assigned to reservoir layers were built within a framework based on sequence stratigraphic concepts to ensure that the spatial 3D distribution of each rock types is predictable within a well- defined geological framework and finally to be used in history matching simulation models.
机译:Kharaib储层的储层岩石类型被定义为岩石的间隔,其中影响流体流动的地质和岩石物理性质是一致的和可预测的。 Lithofacies分类是水库岩石的纯地质分组,具有相似的岩性,质地,粒度,分选等。每种锂缺陷表明具有分布趋势和尺寸的一定的沉积环境。通过孔隙,渗透性,毛细管压力和孔喉部尺寸分布来分类岩石物理学组。通过将岩石物理性质和岩石缩放为储层型定义的一部分将岩石型与岩石型相结合这些分类。先前已经表明,静态岩石类型并不总是代表储存器中的多相流动行为。在本文中,我们将在Zadco内展示岩石型方案的演变。我们讨论用于定义当前统一方案中的储层岩石类型的标准。拟议的岩石型方案的目的是解决使用前一个使用中鉴定的缺点,并且基于以下标准:a)每种岩石类型可以通过类似的沉积环境和成岩工艺来表征; b)不同岩石类型之间的孔隙率/渗透性重叠是最小的; c)每种岩石类型具有典型而独特的孔喉尺寸分布;并且D)每种岩石类型在给定润湿性上具有类似的一组毛细管压力/相对渗透曲线。已识别的储存器岩石类型已被分配给储库层内置于基于序列地层概念的框架内,以确保每个岩石类型的空间3D分布在明确定义的地质框架内是可预测的,并且最终将用于历史匹配模拟中的历史匹配仿真楷模。

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