基于概率地层评价和地质力学分析的Najmah非常规页岩储层水力压裂潜力综合研究

Tingyin He, J. Hornbrook, B. Dharanidharan, M. Al-Bahar, A. Al-Sane, Vandana Suresh, J. Hickey
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引用次数: 0

摘要

Najmah页岩是一种富含有机物的泥灰岩,通常被认为是科威特侏罗纪和白垩纪储层的主要烃源岩。本研究的目的是评估Najmah储层的原始油气储量(OHIP)和地质力学特性,以帮助设计科威特西部的水力压裂增产方案。综合岩石物理评价采用常规岩心和侧壁岩心测量,采用标准和先进的裸眼测井来估计净产层、孔隙度、含油饱和度和地质力学性质。Najmah页岩作为一种潜在的非常规储层,其储层评价面临诸多挑战。这些挑战包括高总有机碳(TOC)对常规孔隙度测井和电阻率测井以及相关页岩体积估算的模糊影响。在这项研究中,开发了一个概率多矿物模型,以更准确地评估岩石的TOC以及相关的孔隙度、饱和度和粘土体积。利用伽马能谱测井和元素能谱测井等先进测井技术,改进了复杂地层的矿物学模型。常规岩心分析、程序热解和x射线衍射(XRD)分析用于验证和校准多矿物模型结果。由于地层中存在双重孔隙系统,因此使用Simandoux饱和度方程来评估流体饱和度。基于偶极子声波测井分析,开发了特定井的各向异性水平应力剖面,从而对目标层段有了更深入的了解。根据多矿物建模的结果,在整个西科威特,Najmah页岩的平均TOC随井而异,最高可达14.8%。Najmah页岩的有效孔隙度为1% ~ 8%。这些富含有机物的地层含水饱和度很低。根据地点的不同,水区可能出现在富有机质区间的上方或下方。Najmah页岩的地质力学性质有利于水力压裂增产,与已探明的页岩生产区类似。Najmah页岩下方的Sargelu段表现出明显较高的最小水平应力梯度,而Najmah页岩上方的石灰岩则表现出较弱的应力屏障。Najmah页岩的概率地层评价结果表明,该地层中存在大量的油气。Najmah及邻近单元的地质力学特性有利于水力压裂增产。目标地层附近含水带的评价对于研究该地层的增产潜力至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
An Integrated Study of Probabilistic Formation Evaluation and Geomechanical Analysis to Investigate the Potential of Hydraulic Fracture Stimulation in Najmah Unconventional Shale Reservoirs
The Najmah Shale, an organic-rich marl, is generally considered the primary source rock for hydrocarbons in Kuwait’s Jurassic and Cretaceous reservoirs. The purpose of this study was to estimate the original hydrocarbons in place (OHIP) and the geomechanical properties of the Najmah reservoir to aid in the design of a hydraulic fracture stimulation program in West Kuwait. An integrated petrophysical evaluation utilized conventional and sidewall core measurements, and standard and advanced open-hole logs were used to estimate net pay, porosity, oil saturation, and geomechanical properties. Formation evaluation of the Najmah Shale as a potential unconventional reservoir posed numerous challenges. These challenges included the ambiguous effects that high total organic carbon (TOC) has on conventional porosity logs and resistivity logs and the associated shale volume estimations. In this study, a probabilistic multi-mineral model was developed to more accurately assess the TOC of the rock and the associated porosity, saturation, and clay volume. Advanced well logs, including spectral gamma ray and elemental spectroscopy logs, were used to improve the mineralogical model of the complex formation. Routine core analysis, programmed pyrolysis, and X-ray diffraction (XRD) analyses were used to verify and calibrate the multi-mineral model results. Since a dual-porosity system was present in the formation, the Simandoux saturation equation was used to evaluate the fluid saturations. Anisotropic horizontal stress profiles were developed for specific wells based on analysis of dipole sonic logs, resulting in a greater regional understanding of the target interval. Based on the results of the multi-mineral modeling, the average TOC of the Najmah Shale varies from well to well throughout West Kuwait, with values as high as 14.8%. The effective porosity of the Najmah Shale ranges from 1 to 8%. Water saturation is low for these organic-rich formations. Water zones may occur above or below the organic-rich interval depending on the location. The geomechanical properties of the Najmah Shale are conducive to hydraulic fracture stimulation, by analogy to proven productive shale plays. The Sargelu interval, below the Najmah Shale, exhibits distinctly higher minimum horizontal stress gradients while the limestone above the Najmah Shale presents a weaker stress barrier. The results of the probabilistic formation evaluation of the Najmah Shale indicated that a significant volume of hydrocarbons is present in the formation. The geomechanical properties of the Najmah and adjacent units are conducive to successful hydraulic fracture stimulation. The evaluation of water-bearing zones adjacent to the target formation is critical to the investigation of the formation’s stimulation potential.
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