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Static Stability of Liquid Bridges Between Matrix Blocks of a Gas Invaded Zone of Naturally Fractured Reservoirs

机译:天然裂缝性储层瓦斯侵袭带基质块之间液桥的静态稳定性

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摘要

A large portion of oil and gas reservoirs in the world are located in naturally fractured reservoirs. Despite such importunity, the production mechanisms of these reservoirs are not completely well defined. Gas-oil gravity drainage that takes place in the gas-invaded zone of this type of reservoirs is one instance of such a weakness. The density difference between gas-filled fractures in contact with oil-saturated matrix blocks brings the oil out of the matrix blocks into the fracture. The drained oil can reach the production well through two different paths: continues fracture network and block-to-block path. These two different paths require different approaches to modeling of gravity drainage. Single-block approaches are used when drained oil only travels through the fracture network, which totally formulated before. But when oil prefers to travel through the matrix blocks, continuum approaches such as Darcy's law may not work in their basic forms any more. Liquid bridges and film that form in the horizontal fracture between matrix blocks usually transfer the wetting phase across the fracture. Stability condition and duration of stability can help better understanding of gravity drainage in stacks of blocks. In this article, the stability of liquid bridges between the matrix blocks studied and a minimum length of stability is predicated. The results show that this stable length of liquid bridges formed between adjacent matrix blocks is 2r(0)pi, which is a function of the pore throat. This critical length can be used in modeling of capillary continuity and wetting phase transfer across matrix blocks.
机译:世界上大部分的油气储层都位于天然裂缝储层中。尽管有这样的重要性,但是这些储层的生产机理还没有完全明确。在这种类型的储层的气体侵入区中发生的瓦斯重力引流就是这种弱点的一个实例。与含油饱和的基质块接触的充气裂缝之间的密度差将油从基质块中带出到裂缝中。排出的油可以通过两种不同的途径到达生产井:连续的裂缝网络和逐块途径。这两种不同的路径需要采用不同的方法对重力排水进行建模。当排出的油仅流过裂缝网络时,可以使用单块方法,该裂缝网络之前已完全配制。但是,当石油更喜欢穿越矩阵块时,诸如达西定律之类的连续方法可能不再以其基本形式起作用。在基体块之间的水平裂缝中形成的液桥和薄膜通常将润湿相转移穿过裂缝。稳定性条件和稳定性持续时间有助于更好地理解成堆的重力排水情况。在本文中,确定了所研究的基质块之间的液桥的稳定性以及最小的稳定性长度。结果表明,在相邻矩阵块之间形成的液桥的稳定长度为2r(0)pi,这是孔喉的函数。该临界长度可用于毛细管连续性建模和跨基质块的润湿相转移建模。

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