Core Effective and Relative Permeability Measurements for Conventional and Unconventional Reservoirs by Saturation Monitoring in High Frequency 3d Gradient NMR

Brian Chin, Safdar Ali, A. Mathur, C. Barnes, W. V. Gonten
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Abstract

A big challenge in tight conventional and unconventional rock systems is the lack of representative reservoir deliverability models for movement of water, oil and gas through micro-pore and nano-pore networks. Relative permeability is a key input in modelling these rocks; but due to limitations in core analysis techniques, permeability has become a knob or tuning parameter in reservoir simulation. Current relative permeability measurements on conventional core samples rely on density contrast between oil/water or gas/water on CT (Computed Tomography) scans and recording of effluent volumes to determine relative fluid saturations during the core flooding process. However, tight rocks are characterized by low porosities (< 10 %) and ultra-low permeabilities (< 1 micro-Darcy), that make effective and relative permeability measurements very difficult, time-consuming, and prone to high errors associated with low pore volumes and flow rates. Nuclear Magnetic Resonance (NMR) measurements have been used extensively in the industry to measure fluid porosities, pore size characterization, wettability evaluation, etc. Core NMR scans can provide accurate quantification of pore fluids (oil, gas, water) even in very small quantities, using T2, T1T2 and D-T2 activation sequences. We have developed a novel process to perform experiments that measure effective and relative permeability values on both conventional and tight reservoirs at reservoir conditions while accurately monitoring fluid saturations and fluid fronts in a 12 MHz 3D gradient NMR spectrometer. The experimental process starts by acquiring Micro-CT scans of the cylindrical rock plugs to screen the samples for artifacts or microcracks that may affect permeability measurements. Once the samples are chosen, NMR T2 and T1T2 scans are performed to establish residual fluid saturations in the as-received state. If a liquid effective permeability test is required, the samples are then saturated with the given liquid through a combination of humidification, vacuum-assisted spontaneous imbibition, and saturation under pressure and temperature. After saturation, NMR scans are obtained to verify the volumes of the liquids and determine if the samples have achieved complete saturation. The sample is then loaded into a special core-flooding vessel that is invisible to the NMR spectrometer to minimize interference with the NMR signals from the fluids in the sample. The sample is brought up to reservoir stress and temperature, and the main flowing fluid is injected from one side of the sample while controlling the pressures on the other side of the sample with a back pressure regulator. The saturation front of the injected fluid is continuously monitored using 2D and 3D gradient NMR scans and the volumes of different fluids in the sample are measured using NMR T2 and T1T2 scans. The use of a 12 MHz NMR spectrometer provides very high SNR (signal-to-noise ratio); and clear distinction of water and hydrocarbon signals in the core plug during the entire process. The scanning times are also reduced by orders of magnitude, thereby allowing for more scans to properly capture the saturation front and changes in saturation. Simultaneously, the fluid flowrates and pressures are recorded in order to compute permeability values. The setup is rated to 10,000 psi confining pressures, 9000 psi of pore pressure and a working temperature of up to 100 C. Flowrates as low as 0.00001 cc/min can be recorded. These tests have been done with brine, dead and live crudes, and hydrocarbon gases. The measured relative permeability values have been used successfully in both simulation and production modelling studies in various reservoirs worldwide.
基于高频三维梯度核磁共振饱和度监测的常规和非常规储层岩心有效渗透率和相对渗透率测量
对于致密的常规和非常规岩石系统来说,一个巨大的挑战是缺乏具有代表性的储层产能模型来描述水、油气通过微孔和纳米孔网络的运移。相对渗透率是模拟这些岩石的关键输入;但由于岩心分析技术的限制,渗透率已成为储层模拟中的一个旋钮或调整参数。目前,常规岩心样品的相对渗透率测量依赖于CT(计算机断层扫描)扫描油/水或气/水的密度对比,并记录流出量,以确定岩心驱油过程中的相对流体饱和度。然而,致密岩石的特点是低孔隙度(< 10%)和超低渗透率(< 1微达西),这使得有效和相对渗透率的测量非常困难、耗时,并且容易出现与低孔隙体积和低流量相关的高误差。核磁共振(NMR)测量在工业中被广泛用于测量流体孔隙度、孔径表征、润湿性评估等。核心核磁共振扫描可以提供准确的定量孔隙流体(油,气,水),即使在非常小的数量,使用T2, T1T2和D-T2激活序列。我们开发了一种新的实验方法,在储层条件下测量常规和致密储层的有效渗透率和相对渗透率值,同时在12 MHz 3D梯度核磁共振光谱仪上精确监测流体饱和度和流体前缘。实验过程首先获取圆柱形岩石塞的Micro-CT扫描,以筛选可能影响渗透率测量的人工制品或微裂缝。一旦选择了样品,进行核磁共振T2和T1T2扫描,以在接收状态下建立剩余流体饱和度。如果需要进行液体有效渗透性测试,则通过加湿、真空辅助自发渗吸和压力和温度下的饱和相结合,将样品与给定的液体饱和。饱和后,获得核磁共振扫描来验证液体的体积,并确定样品是否达到完全饱和。然后将样品装入一个特殊的核磁共振波谱仪看不见的核心驱油容器中,以尽量减少样品中流体对核磁共振信号的干扰。将样品提升至储层应力和温度,主流动流体从样品一侧注入,同时用背压调节器控制样品另一侧的压力。使用2D和3D梯度核磁共振扫描连续监测注入流体的饱和前沿,使用核磁共振T2和T1T2扫描测量样品中不同流体的体积。使用12 MHz核磁共振光谱仪提供非常高的信噪比(信噪比);在整个过程中,岩心塞内的水、烃信号区分明显。扫描时间也减少了数量级,从而允许更多的扫描,以适当地捕捉饱和前沿和饱和度的变化。同时,记录流体流速和压力,以计算渗透率值。该装置的额定围压为10,000 psi,孔隙压力为9000 psi,工作温度为100℃,流量可低至0.00001 cc/min。这些测试是用盐水、死原油和活原油以及碳氢化合物气体进行的。测量的相对渗透率值已成功地用于世界各地各种油藏的模拟和生产建模研究。
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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