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In-Depth Investigation of the Validity of the Archie Equation in Carbonate Rocks

机译:碳酸盐岩中阿奇方程有效性的深入研究

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Archie found an empirical equation for consolidatedsandstones relating several formation parameters, such as,porosity and water saturation. Despite its common use bypetroleum engineers, Archie equation is not easy to apply tocarbonate rocks because formation parameters (a, m, n) arefunctions of changes in the pore geometry, clay content,tortuosity of the pores, as well as formation pressure. Theother important issue that Archie equation fails to address isthe fluid critical point for the multi-component state in whichdifferent phases co-exist. This being the case for light oil andcondensate reservoirs, the straightforward application of theArchie equation in carbonate rocks has severe limitations.The Archie equation is valid only when the rock is stronglywater wet and clay free, which is not the case in carbonaterocks. There is no linear or direct correlation betweenresistivity index (IR) and formation water saturation in thecarbonate rocks. Therefore, the Archie equation cannot begeneralized over the entire carbonate reservoir.In this paper, a series of experiments is performed inorder to derive the correct form of the Archie Equation thatcan be applied to carbonate rocks. The parameter a is furthersplit to account for the composition, pore geometry andformation pressure. By separating these parameters, it ispossible to find more precise correlation with formationresistivity and formation water saturation for carbonatereservoirs. Also derived are the correlations betweenresistivity and the composition of the carbonate rock as well asformation pressure. Finally, an equation is proposed fortaking into account changes due to the presence of criticalfluids. The generalized equation can then be applied to anyfluid in a carbonate formation with varied geometry and claycontent.
机译:阿奇发现了一个整合的经验方程 与几个地层参数有关的砂岩,例如, 孔隙度和水饱和度。尽管它被 石油工程师,阿奇方程式不容易应用 碳酸盐岩,因为地层参数(a,m,n)为 孔隙几何形状,粘土含量, 孔隙的曲折性以及地层压力。这 阿奇方程式无法解决的另一个重要问题是 多组分状态的流体临界点,其中 不同阶段共存。轻油就是这种情况, 冷凝水储层的直接应用 碳酸盐岩中的阿奇方程具有严重的局限性。 仅当岩石坚硬时,阿奇方程才有效 湿润且不含粘土,在碳酸盐中则不是这种情况 岩石。两者之间没有线性或直接的相关性 储层中的电阻率指数(IR)和地层水饱和度 碳酸盐岩。因此,阿尔奇方程不能为 概括了整个碳酸盐岩储层。 在本文中,我们进行了一系列实验 为了得出阿奇方程的正确形式, 可以应用于碳酸盐岩。参数a更远 分开考虑组成,孔的几何形状和 地层压力。通过分离这些参数,它是 可能找到与地层更精确的相关性 碳酸盐岩的电阻率和地层水饱和度 水库。还推导了 电阻率和碳酸盐岩的组成以及 地层压力。最后,提出了一个方程 考虑到由于关键因素而导致的变化 液体。然后可以将广义方程式应用于任何 碳酸盐岩层中具有不同几何形状和黏土的流体 内容。

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