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A NEW DUAL-PERMEABILITY MODEL FOR NATURALLY FRACTURED RESERVOIRS

机译:天然裂缝性储层的双重渗透模型

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摘要

Naturally fractured reservoirs (NFRs) are the reservoirs with two distinct types of porous media called the fracture and matrix. The pressure behavior of naturally fractured reservoirs is usually studied by using theWarren and Root model [Warren, J.E. and Root, P.J., The Behavior of Naturally Fractured Reservoirs, SPEJ, Soc. Pet. Eng. J., vol. 3, no. 3, pp. 245-255, 1963]. The Warren and Root model assumes that production from the naturally fractured system goes from the matrix to the fracture and thence to the wellbore. However, this assumption is oversimplified if the contrast between the permeability of the matrix system and that of the fracture system is not significant. In order to estimate the limits of validity of solutions based on the Warren-Root model and to study the pressure behavior of a naturally fractured reservoir when the contrast between the two permeabilities are not significant, it is necessary to solve the original model proposed by Barenblatt and Zheltov [Barenblatt, G.I. and Zheltov, Y.P., Fundamental Equations of Filtration of Homogeneous Liquids in Fissured Rocks, Soviet Phys., vol. 5, p. 522, 1960]. But the analytical solutions to this model which were obtained by numerical analysis or numerical inversion are very complex and inconvenient to use. Assuming that both the matrix system and fracture system produce directly into the wellbore, a new mathematical model for dual-permeability naturally fractured reservoirs is presented in this paper. Based on our proposedmodel, it is concluded that there are four stages for the pressure behavior of NFRs. The dual-permeability system behaves like a reservoir with a constant pressure boundary when the dimensionless time approaches infinite. The solution procedure proposed in this paper is a fast tool to evaluate a vertical well performance in a dual-permeability naturally fractured reservoir.
机译:天然裂缝性储层(NFR)是具有两种不同类型的多孔介质的储层,称为裂缝和基质。通常使用Warren和Root模型研究自然裂缝储层的压力行为[Warren,J.E. and Root,P.J.,自然裂缝储层的行为,SPEJ,Soc。宠物。 。 J.,第3号3,第245-255页,1963年]。 Warren and Root模型假设自然裂缝系统的产量从基质到裂缝,再到井筒。但是,如果基体系统的渗透率与裂缝系统的渗透率之间的对比度不显着,则可以简化此假设。为了评估基于Warren-Root模型的解的有效性极限并研究两种渗透率之间的对比不显着时天然裂缝性储层的压力行为,有必要解决Barenblatt提出的原始模型和Zheltov [Barenblatt,GI和Y.P. Zheltov,《裂隙岩石中均相液体过滤的基本方程》,《苏联物理学》,第1卷。 5,第522,1960年]。但是,通过数值分析或数值反演获得的该模型的解析解非常复杂且使用不便。假设基质系统和裂缝系统都直接进入井眼,本文提出了双渗透天然裂缝储层的新数学模型。根据我们提出的模型,可以得出结论:NFR的压力行为分为四个阶段。当无量纲时间接近无限时,双渗透系统的行为就像具有恒定压力边界的储层。本文提出的求解程序是评估双渗透自然裂缝储层中垂直井性能的快速工具。

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