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Assessing Relative Permeabilities of Two Phase Flows of Water and Steam in Geothermal Reservoirs: State of the Art Relations

机译:评估地热储层中水和蒸汽两相流的相对渗透率:最新技术关系

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A basic understanding of two phase flow of water and steam in geothermal reservoirs is essential to predict the performance of high temperature geothermal wells and reservoirs. Current simulation tools for liquid dominated reservoirs base flow calculations on the traditional Darcy equation, where flow is a function of fluid parameters such as density and viscosity, as well as the intrinsic permeability of the surrounding media to transmit fluid. For two phase flow of water and steam, this approach is based on the relative permeability of each phase, which is the effective portion of the intrinsic permeability for the phase.The traditional flow relation neglects interfacial shear forces and buoyancy effects acting between the two phases, introducing errors unless the two phases are flowing in completely separated channels. Thus, this formulation predicts that relative permeability is linearly dependant on the water saturation, since it should only account for the portion occupied by that phase in the cross sectional area of the flow channel. Experiments, generally with one dimensional flow, have shown this not to be the case, indicating that the relative permeability scales with the water saturation with an exponent greater than one (Eliasson et al. 1980, Verma 1986, Piquemal 1994, Satik 1998,Mahiya 1999).In this paper a literature review is presented together with a theoretical analysis of one dimensional two phase flow, using the concept of relative permeabilities as variable functions of water saturation. It is shown that relative permeabilities cannot be material constants but must also depend on flow configuration, thus relationship between water saturation and relative permeabilities must be developed in order to generate predictions more in accordance with observed experimental results. This paper states the theoretical groundwork for a large scale experimental study of the relative permeabilities of two phase flow of water and steam. The goal of the experimental work is to develop empirical relationshipsfor two phase flow, using relative permeabilities, that describe the flow more accurately than existing formulations do.
机译:对地热储层中水和蒸汽的两相流的基本了解对于预测高温地热井和储层的性能至关重要。当前用于以液体为主的储层的仿真工具基于传统的达西方程式进行流量计算,其中流量是流体参数(例如密度和粘度)以及周围介质传输流体的固有渗透率的函数。对于水和蒸汽的两相流,此方法基于每个相的相对磁导率,这是该相的固有磁导率的有效部分。 传统的流动关系忽略了两相之间作用的界面剪切力和浮力效应,除非两相在完全分开的通道中流动,否则会引入误差。因此,该公式预测相对渗透率与水饱和度呈线性关系,因为它只应考虑该相在流动通道横截面中所占的部分。通常在一维流中进行的实验表明情况并非如此,这表明相对渗透率随水饱和度的变化而增大,且指数大于一(Eliasson等,1980; Verma,1986; Piquemal,1994; Satik,1998,Mahiya)。 1999)。 本文使用相对渗透率作为水饱和度的变量函数,对一维两相流进行了理论综述,并对一维两相流进行了理论分析。结果表明,相对渗透率不能是材料常数,而必须取决于流动形态,因此必须建立水饱和度与相对渗透率之间的关系,以便根据观察到的实验结果产生更多的预测。本文为水和蒸汽两相流的相对渗透率的大规模实验研究奠定了理论基础。实验工作的目的是发展经验关系 对于两相流,使用相对渗透率,可以比现有配方更准确地描述流。

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