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Rock Physics of Reservoir Rocks with Varying Pore Water Saturation and Pore Water Salinity

机译:不同孔隙水饱和度和孔隙水盐度的储层岩石物理研究

摘要

Advanced waterflooding (injection of water with selective ions in reservoirs) is amethod of enhanced oil recovery (EOR) that has attracted the interest of oil and gas companies that exploit the Danish oil and gas reservoirs. This method has been applied successfully in oil reservoirs and in the Smart Water project performed in a laboratory scale in order to evaluate the EOR processes in selected core plugs. A major step towards this evaluation is to identify the composition of the injected water that leads to increased oil recovery in reservoirs and to define changes in the petrophysical properties of the rock due to the water injection. During advanced waterflooding of reservoirs, or in the Smart Water project, during core flooding experiments, several chemical and petrophysical processes occur in the grains and pore space due to rock, brine and oil interactions. These processes may affect the rate and amount of oil recovered.Advanced waterflooding experiments of reservoir rocks are performed on laboratory scale, but the mechanisms that describe the effects of water injection on the rock minerals are poorly understood. After many decades, a methodology on how this technique should be performed on specific geological structures and why it is sometimes successful; has yet to be established. The presence of both oil and water in the pore space, several different ions present in the injected water that contact the pore walls, possible changes in the fluid wetting the surface of the grains and high stress applied on the minerals, comprise the complex system of waterflooding. These parameters affect the fluid/fluid, solid/fluid and solid/solid interfaces. The changes of the petrophysical and mechanical properties of the core affected from waterflooding are the main topic of research in the present study. In an effort to simplify the complex system of waterflooding, the parameters that affect the solid/fluid interfaces simultaneously, during the experiments, are studied individually. Many chemical and petrophysical phenomena have been documented in previous studies that may affect either the mechanical or physical properties of the rock during waterflooding experiments. The phenomena include decreased pore stiffness and subsequent compaction and can be related to a variety of parameters; including precipitation and dissolution reactions, as well as adsorption reactions and changes in wettability. In order to understand the potential mechanisms under the action of water injection, the present study investigates the effect of the selected ions on the solid/fluid interface of the porous medium under reservoir conditions by studying the following conditions separately: 1) during coreflooding experiments, the rock is subjected to high external stresses that resemble the reservoir stresses; 2) the fluid distribution within the pore space changes during the flow through experiments and wettability alterations may occur; 3) different ions, present in the salt water injected in the core, interact with the surface of the mineral.This study aims to improve the theoretical understanding of the detailed mechanisms involved in waterflooding, using advanced and sensitive tools on a laboratory scale to illustrate the potential mechanisms behind the action of water injection on oil and brine bearing rocks. In order to investigate the action of pore water with selective ions on the solid/fluid interface, low field nuclear magnetic resonance (NMR) spectrometry, ultrasonic velocities, electrical resistivity and mineralogical characterization are performed on quarry and reservoirs cores. The rocks are saturated with fluids similar to the ones used in the core flooding experiments. Ultrasonic velocities and electrical resistivity data are collected to detect changes with respect to strength and pore geometry of the rock. Low field NMR spectrometry is used to detect changes in texture, wettability and pore‐fluid distribution. While investigating the petrophysical properties of reservoir rocks, information concerning the mineralogy is an important factor for the establishment of a rock physical model. Therefore, additional experiments are performed; X-ray diffraction (XRD), backscatter electron microscopy images (BSEM), mercury injection capillary pressure (MICP) curves and specific surface analysis (BET) illustrate the mineralogy and texture of the rock samples.Chalk from Stevns Klint near Copenhagen, Denmark, (a rock analogue to reservoir chalk from the North Sea) was used for rock mechanical testing in order to understand the potential mechanisms behind the action of ions in high concentration on the chalk surface; such as precipitation and dissolution. The effect of the divalent ions on the elasticity and pore collapse of this rock was observed and validated from the ultrasonic velocity data. Low field NMR was used to detect any precipitation that may occur in the pore space of chalk saturated with divalent ions. Precipitation occurred only in single cases; therefore, it is doubtful whether it is the responsible mechanism for the water weakening of chalk. The same rock material was used to illustrate the use of low field NMR to detect differences in the texture of chalk; in our case a carbonate mudstone and a carbonate wackestone as previously observed by electron microscopy.The solid-fluid affinity of chalk from the Gorm field, Berea sandstone and chlorite bearing greensand from the Solsort field was defined from low field NMR data. Longitudinal relaxation time (T1), transverse relaxation time (T2) and self-diffusion coefficient of the fluids within the core plugs were measured at different saturation states; water, reservoir oil and oil and water at irreducible water saturation. T1/T2 ratio proved a non-destructive and fast way to determine the solid-fluid affinity and fluid distribution within the pore space of the selected rocks.Finally, supplementary experimental work includes the determination of small amounts of oil in water samples from the NMR T2 distribution. Low field NMR spectrometry was able to accurately determine the oil and water volume in effluents. This is found very useful, because when the oil reaches residual saturation during core flooding experiments, the produced oil is very small and the quantification of these fluids is often difficult.iv
机译:先进的注水技术(向储层中注入选择性离子水)是提高采收率(EOR)的一种方法,引起了开发丹麦油气藏的油气公司的兴趣。该方法已成功应用于油藏和实验室规模的Smart Water项目中,以评估所选岩心塞中的EOR过程。进行此评估的主要步骤是确定注入的水的成分,该成分可提高储层中的油采收率,并确定由于注入水而导致岩石的岩石物理性质发生变化。在水库的高级注水过程中,或在Smart Water项目中,在岩心驱替实验期间,由于岩石,盐水和石油的相互作用,谷物和孔隙中发生了几种化学和岩石物理过程。这些过程可能会影响油的采收率和数量。在实验室规模上进行了储层岩石的高级注水实验,但对于描述注水对岩石矿物影响的机理了解甚少。几十年后,出现了一种方法,该方法应如何在特定的地质结构上执行该技术,以及为何有时会成功;尚未建立。孔隙空间中同时存在油和水,注入的水中与孔隙壁接触的几种不同离子,润湿谷物表面的流体可能发生变化以及施加在矿物上的高应力,构成了复杂的注水。这些参数影响流体/流体,固体/流体和固体/固体界面。受注水影响的岩心的岩石物理力学特性的变化是本研究的主要课题。为了简化复杂的注水系统,在实验过程中同时研究了同时影响固/液界面的参数。在以前的研究中已经记录了许多化学和岩石物理现象,这些现象可能会在注水实验中影响岩石的机械或物理性质。这种现象包括孔隙刚度降低和随后的压实,并且可能与多种参数有关;包括沉淀和溶解反应,以及吸附反应和润湿性变化。为了了解注水作用下的潜在机理,本研究通过分别研究以下条件,研究了选定离子对储层条件下多孔介质固/液界面的影响:1)在岩心驱替实验中,岩石受到类似于储层应力的高外部应力; 2)在实验过程中,孔隙空间中的流体分布会发生变化,并且可能会发生润湿性变化; 3)注入岩心的盐水中存在的不同离子与矿物质表面相互作用。本研究旨在通过在实验室规模上使用先进且灵敏的工具来说明对驱水机理的详细理论理解注水作用在含油和含盐水岩石上的潜在机理。为了研究含选择性离子的孔隙水对固/液界面的作用,对采石场和储层岩心进行了低场核磁共振(NMR)光谱,超声波速度,电阻率和矿物学表征。岩石被岩心驱油实验中所用的流体浸透。收集超声波速度和电阻率数据,以检测岩石强度和孔隙几何形状的变化。低场NMR光谱法用于检测质地,润湿性和孔隙流体分布的变化。在研究储层岩石的岩石物理特性时,有关矿物学的信息是建立岩石物理模型的重要因素。因此,需要执行其他实验; X射线衍射(XRD),背向散射电子显微镜图像(BSEM),汞注入毛细管压力(MICP)曲线和比表面分析(BET)说明了岩石样品的矿物学和质地。来自丹麦哥本哈根附近Stevns Klint的粉笔为了了解岩石中高浓度离子在白垩表面上作用的潜在机理,使用了(类似于北海储层白垩的岩石类似物)进行岩石力学测试;例如沉淀和溶解。观察到二价离子对该岩石的弹性和孔隙塌陷的影响,并根据超声速度数据进行了验证。低场NMR用于检测在被二价离子饱和的白垩的孔隙中可能发生的任何沉淀。仅在单例中发生降水;因此,这是否是导致粉笔水弱化的负责机制值得怀疑。使用相同的岩石材料来说明使用低场NMR检测白垩质地的差异。在我们的案例中是碳酸盐泥岩和碳酸盐瓦克石,以前通过电子显微镜观察到。来自低场NMR数据定义了来自Gorm油田的白垩,来自Solsort油田的Berea砂岩和带有绿泥石的绿泥的固液亲合力。测量了在不同饱和状态下岩心塞内流体的纵向弛豫时间(T1),横向弛豫时间(T2)和自扩散系数。水,储层中的油以及油和水处于无法还原的饱和状态。 T1 / T2比被证明是确定所选岩石孔隙内固液亲和力和流体分布的一种非破坏性快速方法。最后,补充实验工作包括通过NMR测定水中的少量油T2分布。低场NMR光谱法能够准确测定废水中的油和水量。这被发现非常有用,因为当油在岩心驱油实验中达到残余饱和度时,产出的油非常小,并且通常很难对这些流体进行定量.iv

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