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Physics-Based Initialization Captures Post-Migration Structural Deformationin Mixed-Wet Carbonates:An Integrated Workflow for Tilted Oil-WaterContact Reservoirs

机译:基于物理的初始化捕获迁移后结构变形蛋白混合湿碳酸盐:用于倾斜的油水储层的综合工作流程

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This study attempts to describe and model the process leading to the genesis of the tilted oil-water contact(OWC)observed in the lower part of the Thamama Group in an offshore Abu Dhabi field.Post-oil-migration deformation is thought to be the mechanism that produced a tilted OWC dippingtowards the Northeast.Deciphering the tectonic evolution from Jurassic to Paleocene times confirms along and complex structural history combining burial,halokinesis,uplift and tilting.Diapiric activity wasprobably established in the eastern accumulation by pre-Jurassic times,followed by localized salt-relateddoming in both parts of the field.During the mid-Eocene occurred a late tilting of the northeastern part ofthe field,enhancing the curvature of the area.This late tilting caused oil saturation redistribution.In uplifted areas of the field,watersaturationdecreased along the drainage curve whereas in areas brought structurally closer to the Free WaterLevel(FWL),water saturation increased along a scanned imbibition curve.The objective of this study is to retrace the saturation history of the field using lab-measured boundingcapillary pressures.This workflow ensures the correct initialization of the dynamic reservoir model andreproduces the observed field behavior.Drainage and imbibition capillary pressures are available for different rock types(RT),measuredunder various experimental set-ups(mercury injection,porous plate,centrifuge).This study reconciles labmeasurements with wireline logs and Dean-Stark data to produce a representative capillary pressure curvefor each RT.Next,the structural deformation history is representedas a series of elementary geometric transformations(localized subsidence and global translation)to restore the reservoir in its pre-deformation state.Wirelinelog saturationsare matched to capillary-based water saturations by adjusting the present day free water level(FWL)and the change of FWL due to seepage.The dynamic model is then initialized by enumeration with the original water saturation and let toequilibrate for 40,000 years.The fluid redistribution and pressures are then monitored to confirm that equilibrium has been attained.This equilibration step ensures that the fluids are at their correctstate ofrelative permeability and capillary pressure at the start of simulation,something that is not garanteed inthe case of direct enumeration of the final saturations.The implications of such procedure on the dynamicbehaviorare explored by simulating 50 years of production history and compa.This study greatly improved the saturation modelling by moving from synthetic porosity-bin functions tophysics and texture based capillary pressures.The proposed workflow enhanced the history-match qualityand reproduced observed field behaviors such as the high water-cut development in the Northeast.A tilted OWC might increase the in-place however extracting those resources might prove morechallenging in the face of the low oil mobility.The oil below OWC might not be recovered underconventional waterflood methods and would warrant an EOR implementation.In the future,an appraisalwell is planned in the Northeast to assess the volume and mobility of the oil below OWC.It is the first time an integrated workflow,combining SCAL and structural geology,is proposed tocorrectly initialize the dynamic model for reservoirs that experienced a post-migration deformation,hencemaking the present study unique.
机译:本研究试图描述和模拟导致在近海阿布扎比领域的山顶集团下部观察到倾斜的油水接触(OWC)的成因的过程。普罗斯 - 迁移变形被认为是制作倾斜的OWC的机制是东北部的倾斜。修改侏罗纪的构造演进到古典时代,以及复杂的结构史,组合埋葬,卤代碱,隆起和倾斜和倾斜的侏罗纪逐步建立的透镜活性,其次是在东部积累中,其次是局部盐相关的盐在田间的两个部分。中期地发生了东北部门的晚期倾斜,增强了该地区的曲率。这次倾斜导致油饱和再分布。在田地的升高的区域,水域升起了沿着排水曲线,而在结构上靠近自由水利(FWL)的区域,水饱和度沿着扫描ED IMBIBITITION曲线。本研究的目的是使用实验室测量的绑定群压力来察觉该领域的饱和历史。该工作流程确保了动态储存模型的正确初始化,并且可以使观察到的现场行为。可用于不同的岩石类型(RT),各种实验组(汞注射,多孔板,离心机)。本研究与有线日志和Dean-STARK数据调和了LabmeSurement,以产生各种RT.Next的代表性毛细管压力曲线,结构变形历史是代表了一系列基本的几何变换(本地化沉降和全局翻译),以通过调整现今的自由水位(FWL)和变化,将储存器恢复到其预变形状态。用与毛细管基水饱和度匹配由于渗漏引起的FWL。然后通过枚举机智初始化动态模型H原始水饱和度并允许足够的40,000年。然后监测流体再分配和压力以确认已经获得了平衡。该平衡步骤确保流体在模拟开始时液体渗透性渗透性和毛细管压力的校正渗透性和毛细管压力。不是GarAnteed的案例直接枚举最终饱和的情况。这些程序对通过模拟50年的生产历史和Compa探索的动态行为的影响。本研究大大改善了通过从合成孔隙函数托管中移动了饱和度建模基于纹理的毛细管压力。该拟议的工作流程增强了历史匹配Quality,再现的观察到的现场行为,如东北的高水路开发。倾斜的OWC可能会增加就地,然而提取这些资源可能会在脸上证明MoreChallenging低油流动性。OWC MIG下面的油HT不恢复不变性的水机械方法,并将保证EOR实施。在未来,在东北方案计划在东北方案评估OWC下面的油的体积和移动性。它是第一次综合工作流程,结合SCAL和结构地质学,建议ToCorretely初始化储存器的动态模型,经历了迁移后变形,造成了本研究独特。

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