Osmosis and Clay Swelling Effects in Gas Shale Formations under Stress

Vena F. Eveline, I. Akkutlu
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引用次数: 6

Abstract

Water-shale interactions are traditionally perceived as complex phenomena due to reactive nature of shale with water. However, the current trends in shale gas industry requires an advanced-level of understanding of these interactions and their impact on gas production. In this paper we investigate the invasion of fracturing water into the formation and the subsequent water-shale interactions. Objective of this work is to study osmosis and clay swelling effects of the invasion on the formation permeability. For this purpose, a new geomechanically-coupled reservoir flow simulator is developed, which accounts for water imbibition, osmosis and clay swelling effects on the formation permeability under stress. The simulation model considers the formation has a multi-scale pores consisting of microcracks, clay pores and organic pores. Water imbibition occurs in the water-wet inorganic part of the matrix in the microcracks. Osmosis and clay swelling effects develop in the clay pores acting as semi-permeable membrane to the imbibed water and changing the local stress in the formation. The simulation model includes aqueous and gaseous phases with three components: water, gas and salt. The simulation results show that the formation permeability is dynamically affected during the shut-in period by a combination of mechanisms including imbibition, capillarity, diffusion/osmosis, and total stress. Notably, a permeability impairment zone, rather a fracture skin, develops near the fracture. The permeability alteration is due to osmosis-related clay swelling and changing stresses in the formation. The magnitude of the permeability alteration is controlled mainly by the salt concentration difference between the fracturing fluid and the clay-bound water, the clay-membrane efficiency, the clay cation exchange capacity (CEC), the clay porosity, the stress and the duration of the shut-in time. We develop a fracture skin factor that can be used with the single-phase (gas) shale reservoir flow simulators that are typically run in the absence of water invasion at the scale of the stimulated reservoir volume (SRV) and in multidimensional geometries. Currently there is a clear need in the unconventional industry to better-understand and control the hydraulic fracturing fluid-shale interactions. This work is an important milestone considering the complexity of the problem and suggesting that the water chemistry and the formation lithology plays a significant role after the fracturing operations.
应力作用下页岩气层渗透与粘土溶胀效应
由于页岩与水的反应性质,水-页岩相互作用传统上被认为是一种复杂的现象。然而,目前页岩气行业的发展趋势需要对这些相互作用及其对天然气生产的影响有更深入的了解。本文研究了压裂水侵入地层以及随后的水-页岩相互作用。本文的目的是研究渗透和粘土溶胀对地层渗透率的影响。为此,开发了一种新型的地质力学耦合油藏流动模拟器,该模拟器考虑了应力作用下的吸水、渗透和粘土膨胀对地层渗透率的影响。该模拟模型认为地层具有由微裂缝、粘土孔隙和有机孔隙组成的多尺度孔隙。渗吸作用发生在微裂纹中基体的水湿无机部分。渗透作用和粘土溶胀作用在粘土孔隙中产生,粘土孔隙作为半透膜作用于水的吸收,改变了地层中的局部应力。模拟模型包括水相和气相,由水、气和盐三种组分组成。模拟结果表明,在关井期间,地层渗透率受渗吸、毛细作用、扩散/渗透作用和总应力等多种机制的动态影响。值得注意的是,裂缝附近形成了一个渗透性损伤区,而不是裂缝表皮。渗透率的改变是由于与渗透有关的粘土膨胀和地层中应力的变化。渗透率蚀变的幅度主要受压裂液与粘土结合水的盐浓度差、粘土膜效率、粘土阳离子交换容量(CEC)、粘土孔隙度、应力和关井时间等因素的控制。我们开发了一种裂缝表皮因子,可用于单相(气)页岩储层流动模拟器,该模拟器通常在模拟储层体积(SRV)的规模和多维几何形状下,在没有水侵的情况下运行。目前,非常规油气行业显然需要更好地了解和控制水力压裂液与页岩的相互作用。考虑到问题的复杂性,这项工作是一个重要的里程碑,表明水化学和地层岩性在压裂作业后发挥着重要作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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