Christopher J. Landry, Maša Prodanović, Zuleima Karpyn, Peter Eichhubl
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引用次数: 0
Abstract
Natural fractures in subsurface reservoirs are frequently partially cemented with mineral precipitates, and it is unclear if fracture permeability models developed for rough barren fractures are applicable for fractures where roughness originates from cement linings. Here, we use a digital rock physics workflow to quantify the error in fracture permeability predicted by these models for five digitally synthesized rough fractures and four fractures imaged using three-dimensional X-ray computed microtomography. Samples include a rough, artificially-induced barren fracture in sandstone, a cement-lined natural fracture in limestone sampled from outcrop, and two cement-bridged natural fractures in tight-gas sandstones sampled from reservoir core. The images are then processed, segmented, characterized to determine statistical moments of the aperture distribution, and used in lattice Boltzmann model flow simulations. We address complications in measuring aperture distributions from images when the fracture pore space morphology deviates from the typical theoretical description of rough fractures and evaluate three different methods of measuring local aperture. The alternative cubic law using the nominal mean aperture is found to overestimate fracture permeability by upwards of one to two orders of magnitude, while the fracture permeability models using statistical moments of the aperture distribution are far more accurate for both rough barren and partially cemented fractures. We also define an empirical description of the upper and lower bounds of fracture permeability estimates as a function of relative roughness that is applicable to both rough barren and partially cemented fractures.
地下储层中的天然裂缝经常部分被矿物沉淀物胶结,目前还不清楚为粗糙贫瘠裂缝开发的裂缝渗透率模型是否适用于因胶结衬里而产生粗糙的裂缝。在此,我们使用数字岩石物理工作流程,对这些模型预测的五条数字合成粗糙断裂和四条使用三维 X 射线计算机显微层析成像技术成像的断裂渗透率误差进行量化。样本包括砂岩中人工诱导的粗糙贫瘠断裂、从露头取样的石灰岩中的水泥衬砌天然断裂以及从储层岩芯取样的致密气砂岩中的两条水泥桥接天然断裂。然后对图像进行处理、分割、特征描述,以确定孔径分布的统计矩,并用于晶格玻尔兹曼模型流动模拟。我们讨论了当断裂孔隙空间形态偏离粗糙断裂的典型理论描述时,通过图像测量孔径分布的复杂性,并评估了三种不同的局部孔径测量方法。结果发现,使用标称平均孔径的替代立方定律会高估断裂渗透率,高出一到两个数量级,而使用孔径分布统计矩的断裂渗透率模型对于粗糙贫瘠断裂和部分胶结断裂都要精确得多。我们还定义了断裂渗透率估算上下限与相对粗糙度函数关系的经验描述,该描述适用于粗糙贫瘠断裂和部分胶结断裂。
期刊介绍:
-Publishes original research on physical, chemical, and biological aspects of transport in porous media-
Papers on porous media research may originate in various areas of physics, chemistry, biology, natural or materials science, and engineering (chemical, civil, agricultural, petroleum, environmental, electrical, and mechanical engineering)-
Emphasizes theory, (numerical) modelling, laboratory work, and non-routine applications-
Publishes work of a fundamental nature, of interest to a wide readership, that provides novel insight into porous media processes-
Expanded in 2007 from 12 to 15 issues per year.
Transport in Porous Media publishes original research on physical and chemical aspects of transport phenomena in rigid and deformable porous media. These phenomena, occurring in single and multiphase flow in porous domains, can be governed by extensive quantities such as mass of a fluid phase, mass of component of a phase, momentum, or energy. Moreover, porous medium deformations can be induced by the transport phenomena, by chemical and electro-chemical activities such as swelling, or by external loading through forces and displacements. These porous media phenomena may be studied by researchers from various areas of physics, chemistry, biology, natural or materials science, and engineering (chemical, civil, agricultural, petroleum, environmental, electrical, and mechanical engineering).