Stone-II三相渗透率模型的问题,以及一种新的稳健的基于基本面的替代方案

S. Gupta
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摘要

本文的目的是提出一种基于基本原理的、与观测相一致的三相流模型,以避免Stone-II或Baker三相渗透率模型等传统模型的缺陷。Gupta等人(2020)通过将模型生成的结果与现场数据进行比较,研究了SAGD中残余油饱和度的迷团,并强调了将蒸汽油藏中观察到的残余油饱和度与Stone-II和Baker的线性模型相匹配的困难。尽管Stone-II模型在整个行业中非常流行,但重力排水的一个问题是,当水接近不可还原的饱和度时,它似乎会反直觉地限制油的流动。目前的工作首先是用现有的组合方法(如Stone-II)描述问题,该方法将水-油和气-油相对渗透率曲线结合起来,得到存在水和气时的油相对渗透率曲线。然后,从毛细血管层流的基本原理开始,通过连续的类比公式,推导出直接产生所有三相相对渗透率的表达式。在这种情况下,它假定孔径分布近似于先前文献中用于推导两相相对渗透率曲线的函数。概述的方法绕过了具有组合函数的需要,如Stone或Baker所规定的。这样开发的模型使用起来很简单,并且它避免了由于上述Stone-II背景中描述的数学人工制品而导致的非自然现象或差异。该模型还解释了为什么过去一些研究人员发现相对渗透率是温度的函数。新模型也可以通过实验来确定,而不是基于假设的孔径分布。在这种情况下,它作为一组已知依赖于各种饱和度的骨架函数,留下常数由实验确定。这项工作的新颖之处在于开发了一个基于细通道流动基本原理的三相相对渗透率模型,该模型更好地解释了多孔介质流动背景下的观察结果。这项工作的意义在于,除了预测结果更符合预期和解释油的温度相关相对渗透率外,还包括在基于重力的采油方法中更可靠的时间相关残余油相饱和度。
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Issue with Stone-II Three Phase Permeability Model, and A Novel Robust Fundamentals-Based Alternative to It
The objective of this paper is to present a fundamentals-based, consistent with observation, three-phase flow model that avoids the pitfalls of conventional models such as Stone-II or Baker's three-phase permeability models. While investigating the myth of residual oil saturation in SAGD with comparing model generated results against field data, Gupta et al. (2020) highlighted the difficulty in matching observed residual oil saturation in steamed reservoir with Stone-II and Baker's linear models. Though the use of Stone-II model is very popular for three-phase flow across the industry, one issue in the context of gravity drainage is how it appears to counter-intuitively limit the flow of oil when water is present near its irreducible saturation. The current work begins with describing the problem with existing combinatorial methods such as Stone-II, which in turn combine the water-oil, and gas-oil relative permeability curves to yield the oil relative permeability curve in presence of water and gas. Then starting with the fundamentals of laminar flow in capillaries and with successive analogical formulations, it develops expressions that directly yield the relative permeabilities for all three phases. In this it assumes a pore size distribution approximated by functions used earlier in the literature for deriving two-phase relative permeability curves. The outlined approach by-passes the need for having combinatorial functions such as prescribed by Stone or Baker. The model so developed is simple to use, and it avoids the unnatural phenomenon or discrepancy due to a mathematical artefact described in the context of Stone-II above. The model also explains why in the past some researchers have found relative permeability to be a function of temperature. The new model is also amenable to be determined experimentally, instead of being based on an assumed pore-size distribution. In that context it serves as a set of skeletal functions of known dependencies on various saturations, leaving constants to be determined experimentally. The novelty of the work is in development of a three-phase relative permeability model that is based on fundamentals of flow in fine channels and which explains the observed results in the context of flow in porous media better. The significance of the work includes, aside from predicting results more in line with expectations and an explanation of temperature dependent relative permeabilities of oil, a more reliable time dependent residual oleic-phase saturation in the context of gravity-based oil recovery methods.
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