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Permeability prediction in tight carbonate rocks using capillary pressure measurements

机译:利用毛细压力测量预测致密碳酸盐岩的渗透率

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摘要

The prediction of permeability in tight carbonate reservoirs presents ever more of a challenge in the hydrocarbon industry today. It is the aim of this paper to ascertain which models have the capacity to predict permeability reliably in tight carbonates, and to develop a new one, if required. This paper presents (i) the results of laboratory Klinkenberg-corrected pulse decay measurements of carbonates with permeabilities in the range 65 nD to 0.7 mD, (ii) use of the data to assess the performance of 16 permeability prediction models, (iii) the development of an improved prediction model for tight carbonate rocks, and (iv) its validation using an independent data set. Initial measurements including porosity, permeability and mercury injection capillary pressure measurements (MICP) were carried out on a suite of samples of Kometan limestone from the Kurdistan region of Iraq. The prediction performance of sixteen different percolation-type and Poiseuille-type permeability prediction models were analysed with the measured data. Analysis of the eight best models is included in this paper and the analysis of the remainder is provided in supplementary material. Some of the models were developed especially for tight gas sands, while many were not. Critically, none were developed for tight gas carbonates. Predictably then, the best prediction was obtained from the generic model and the RGPZ models (R-2 = 0.923, 0.920 and 0.915, respectively), with other models performing extremely badly. In an attempt to provide a better model for use with tight carbonates, we have developed a new model based on the RGPZ theoretical model by adding an empirical scaling parameter to account for the relationship between grain size and pore throat size in carbonates. The generic model, the new RGPZ Carbonate model and the two original RGPZ models have been tested against independent data from a suite of 42 samples of tight Solnhofen carbonates. All four models performed very creditably with the generic and the new RGPZ Carbonate models performing well (R-2 = 0.840 and 0.799, respectively). It is clear from this study that the blind application of conventional permeability prediction techniques to carbonates, and particularly to tight carbonates, will lead to gross errors and that the development of new methods that are specific to tight carbonates is unavoidable. (C) 2015 Elsevier Ltd. All rights reserved.
机译:致密碳酸盐岩储层渗透率的预测在当今的烃工业中提出了越来越多的挑战。本文的目的是确定哪些模型能够可靠地预测致密碳酸盐岩的渗透率,并在需要时开发新的模型。本文介绍了(i)实验室Klinkenberg校正的渗透率在65 nD至0.7 mD范围内的碳酸盐的脉冲衰减测量结果,(ii)使用这些数据评估16种渗透率预测模型的性能,(iii)开发改进的致密碳酸盐岩预测模型,以及(iv)使用独立数据集进行验证。最初的测量包括孔隙度,渗透率和汞注入毛细管压力测量(MICP),是对一组来自伊拉克库尔德斯坦地区的Kometan石灰石样品进行的。利用测得的数据分析了十六种不同的渗流型和泊瓦依型渗透率预测模型的预测性能。本文包括对八个最佳模型的分析,并在补充材料中提供了对其余模型的分析。有些模型是专门为致密气砂开发的,而有些则不是。至关重要的是,都没有开发出致密的气态碳酸盐。然后可以预见,从通用模型和RGPZ模型(分别为R-2 = 0.923、0.920和0.915)获得最佳预测,而其他模型的表现则非常差。为了提供一种适用于致密碳酸盐的更好模型,我们基于RGPZ理论模型开发了一个新模型,方法是添加经验比例参数以说明碳酸盐中晶粒尺寸与孔喉尺寸之间的关系。通用模型,新的RGPZ碳酸盐模型和两个原始的RGPZ模型已针对来自42个致密索恩霍芬碳酸盐样品的独立数据进行了测试。这四个模型的表现都非常出色,其中通用模型和新的RGPZ Carbonate模型表现良好(分别为R-2 = 0.840和0.799)。从这项研究中可以清楚地看到,将常规渗透率预测技术盲目应用到碳酸盐,特别是致密碳酸盐中,将导致严重误差,并且不可避免地会开发出专门针对致密碳酸盐的新方法。 (C)2015 Elsevier Ltd.保留所有权利。

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