碳酸盐岩储层垂向渗透率及其对CO2提高采收率和储量的影响分析

Bo Ren, J. Jensen, L. Lake, I. Duncan, Frank Male
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引用次数: 0

摘要

本研究的目的是提高对垂直(层向)渗透率(kz)的地质统计学理解,以及它在二氧化碳提高采收率(EOR)和储存过程中对储层性能的影响。在大多数地质和储层建模中,对Kz的研究远远少于对水平渗透率(kx, ky)的研究。然而,我们的工作表明,了解kz特征对于更好地评估其对CO2提高采收率和储存性能预测的影响同样重要。我们对San Andres碳酸盐岩储层42口井的9000个全岩心三轴渗透率(kx, ky, kz)进行了研究。我们分析了kz数据,包括异质性、相关性和样本充分性测量。我们分析了kz > kmax = max(kx, ky)的最大和最小分数点的井,以探索与大kz相吻合的地质因素。我们通过潜在渗透性屏障(如柱面岩)的条件概率来量化这些地质效应。每口井都至少有一些全岩心在kz > kmax。这是一个统计上合理的结果;只有Prob(kz > kmax)在统计上与1/3不同的地方是非各向同性的岩心样本。然而,在传统的岩心数据解释中,建模者通常假设kz小于kmax。对于kz - bb0 - kmax的岩心比例最小(11%)的井,其累积分布函数不同,且与柱头岩的存在一致。我们发现,在许多井中,kz的变量大约是kx的两倍。这使得kz更难解释,因为它曾经(通常是)严重采样不足。为了了解kz非均质性对CO2流动的影响,我们建立了一系列流动模拟模型,在考虑kz实现、流动形式(如浮力流动)、CO2注入策略和储层非均质性的同时,捕捉了这些渗透率的地质统计学特征。CO2流动模拟表明,对于粘性流动,假设变量kx与油藏相似,且kz/kx = 0.1为常数,则累积产油量与kx和kz为不相关变量的模拟情况接近(在0.5%以内)。然而,对于浮力流体,两种情况下的产油量相差10%(当注入二氧化碳的碳氢化合物孔隙体积HCPV为2.0时)。这种流动可能发生在CO2注入速率小、注入时间长、井间区域和/或垂直渗透管道的情况下。我们的地质统计学特征展示了碳酸盐岩储层中kz的控制因素,以及如何改进传统的解释方法。这项研究可以帮助二氧化碳提高采收率和储存运营商改进注入开发方案,特别是对于存在浮力流动的油藏。更广泛地说,这些发现可能适用于其他类似的地下浮力驱动的流体置换,包括储氢、地热生产和含水层二氧化碳封存。
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Analysis of Vertical Permeability and Its Influence on CO2 EOR and Storage in a Carbonate Reservoir
The objective of this study is to improve understanding of the geostatistics of vertical (bed-normal) permeability (kz) and its influence on reservoir performance during CO2 enhanced oil recovery (EOR) and storage. kz is scrutinized far less often than horizontal permeability (kx, ky) in most geological and reservoir modeling. However, our work indicates that it is equally important to understand kz characteristics to better evaluate their influence on CO2 EOR and storage performance prediction. We conducted this study on about 9,000 whole-core triaxial permeability (kx, ky, kz) measurements from 42 wells in a San Andres carbonate reservoir. We analyzed kz data, including heterogeneity, correlation, and sample sufficiency measures. We analyzed wells with the largest and smallest fractions of points with kz > kmax = max(kx, ky), to explore geological factors that coincided with large kz. We quantified these geological effects through conditional probabilities on potential permeability barriers (e.g., stylolites). Every well had at least some whole-cores where kz > kmax. This is a statistically justifiable result; only where Prob(kz > kmax) is statistically different from 1/3 are core samples non-isotropic. In conventional core data interpretation, however, modelers usually assume kz is less than kmax. For the well with the smallest fraction (11%) of cores where kz > kmax, the cumulative distribution functions differ and coincides with the presence of stylolites. We found that kz is about twice as variable as kx in many wells. This makes kz more difficult to interpret because it was (and usually is) heavily undersampled. To understand the influence of kz heterogeneity on CO2 flow, we built a series of flow simulation models that captured these geostatistical characteristics of permeability, while considering kz realizations, flow regimes (e.g., buoyant flow), CO2 injection strategies, and reservoir heterogeneity. CO2 flow simulations showed that, for viscous flow, assuming variable kx similar to the reservoir along with a constant kz/kx = 0.1 yields a close (within 0.5%) cumulative oil production to the simulation case with both kx and kz as uncorrelated variables. However, for buoyant flow, oil production differs by 10% (at 2.0 hydrocarbon pore volume HCPV of CO2 injected) between the two cases. Such flows could occur for small CO2 injection rates and long injection times, in interwell regions, and/or with vertically permeable conduits. Our geostatistical characterization demonstrates the controls on kz in a carbonate reservoir and how to improve conventional interpretation practices. This study can help CO2 EOR and storage operators refine injection development programs, particularly for reservoirs where buoyant flow exists. More broadly, the findings potentially apply to other similar subsurface buoyancy-driven flow displacements, including hydrogen storage, geothermal production, and aquifer CO2 sequestration.
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