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Improved Permeability Prediction Relations for Low-Permeability Sands

机译:改进的低渗透性砂岩渗透率预测关系

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This work addresses the problem of estimating Klinkenbergcorrected permeability from single-point, steady-state measurements on samples from low permeability sands. The "original" problem of predicting the corrected or "liquid equivalent" permeability (i.e., referred to as the Klinkenbergcorrected permeability) has been under investigation since the early 1940s — in particular, using the application of "gas slippage" theory to petrophysics by Klinkenberg.1 In the first part of our work, the applicability of the Jones- Owens4 and Sampath-Keighin5 correlations for estimating the Klinkenberg-corrected (absolute) permeability from singlepoint, steady-state measurements is investigated. We also provide an update to these correlations using modern petrophysical data. In the second part of our work, we propose and validate a new "microflow" model for the evaluation of an equivalent liquid permeability from gas flow measurements. This work is based on a more detailed application of similar concepts employed by Klinkenberg. In fact, we can obtain the Klinkenberg result as an approximate form of our result. Our theoretical "microflow" result is given as a rational polynomial in terms of the Knudsen number (the ratio of the mean free path of the gas molecules to the characteristic flow length (typically the radius of the capillary)). The following contributions are derived from this work: ● Validation and extension of the correlations proposed by Jones- Owens and Sampath-Keighin for low permeability samples. ● Development and validation of a new "microflow" model which correctly represents gas flow in low permeability core samples. This model is also applied as a correlation for prediction of the equivalent liquid permeability in much the same fashion as the Klinkenberg model, although our new model is substantially more theoretical (and robust) as compared to the Klinkenberg correction model.
机译:这项工作解决了通过对低渗透性砂岩样品进行单点稳态测量来估算经过克林肯贝格校正的渗透率的问题。自1940年代初以来,就一直在研究预测校正的或“等效液体的”渗透率(即称为Klinkenberg校正的渗透率)的“原始”问题,特别是将“气体滑移”理论应用于Klinkenberg的岩石物理学中.1在我们工作的第一部分中,研究了Jones-Owens4和Sampath-Keighin5相关性从单点稳态测量值估算Klinkenberg校正(绝对)渗透率的适用性。我们还使用现代岩石物理数据提供了这些相关性的更新。在我们工作的第二部分中,我们提出并验证了一种新的“微流”模型,用于从气流测量中评估等效液体渗透率。这项工作基于Klinkenberg所采用的类似概念的更详细的应用。实际上,我们可以获得克林根贝格结果作为我们结果的近似形式。我们的理论“微流”结果以Knudsen数(气体分子的平均自由程与特征流长度(通常为毛细管的半径)之比)的形式作为有理多项式给出。这项工作得出以下贡献:●验证并扩展了Jones-Owens和Sampath-Keighin针对低渗透性样品提出的相关性。 ●开发和验证新的“微流”模型,该模型可以正确表示低渗透性岩心样品中的气流。尽管我们的新模型与Klinkenberg修正模型相比在理论上(和鲁棒性)高得多,但该模型也以与Klinkenberg模型几乎相同的方式用作相关等效液体渗透率的预测。

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