Forward Integration of Dynamic Data into 3-D Static Modeling Significantly Improves Reservoir Characterization

B. Kayode, O. Meza, Nerio Quintero, Shaikha J Aldossary
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Abstract

Geo-modelling is usually done to honor static data such as core, well logs and seismic acoustic impedance (AI) map where available. Once the static geo-model is complete, history matching is carried out by tuning the static model properties until the model reproduces observed dynamic behavior. The objective of this paper is to showcase how a systematic a priori integration of dynamic elements into geo-modelling eliminated the need for history matching. These dynamic elements are; connected reservoir regions CRR (Kayode et.al 2018) and permeability-thickness (kh) interpretation from Pressure Transient Analysis PTA. This paper also introduces the concept of CRR based permeability modeling. CRRs were defined based on time-lapse shut-in pressure trend groups. Core and log data were grouped on the basis of the identified CRR and used to build CRR-based Neural Network models for predicting permeability logs of non-cored wells within each CRR. The geo-modeler then created two geo-realizations by using the permeability logs within each CRR to distribute permeability within the CRR using two assumptions of variogram lengths (i) variogram range obtained from analysis of limited core data, (ii) variogram range required to ensure intra-CRR connectivity. Pressure transient was simulated for wells with observed PTA data using the two realizations, and a comparison of the log-log plots of simulated pressure transient derivative and observed pressure transient derivative were used to determine the quality of each realization for each well. The realization that provided the least squares of error across all the wells was selected as base-case geo-model. Permeability correction coefficients were applied on the base-case geo-model until PTA kh were acceptably matched. The resulting permeability log at the PTA well is referred to as PTA-corrected permeability log. Some cored wells were originally exempted from the neural-network permeability modelling because they didn't have logs (sonic, density and neutron logs). Hybrid permeability logs were derived from a combination of the predicted permeability logs and core permeability at these well locations. All permeability correction logs (i) PTA-corrected permeability logs and (ii) Hybrid permeability logs were then fed back into the geo-modeling workflow to generate an improved permeability distribution which respects core data, PTA kh, and CRRs. The do-nothing simulation run has more than 80% of wells’ pressure data acceptably history matched. This application demonstrates that a priori integration of dynamic elements like CRR, PTA kh, and the use of CCR-based permeability modeling results in a better characterized geo-model with potential for eliminating the need for history matching.
将动态数据前向集成到三维静态建模中可以显著改善储层表征
地质建模通常是为了获取静态数据,如岩心、测井曲线和地震声阻抗(AI)图。一旦静态地理模型完成,就通过调整静态模型属性来执行历史匹配,直到模型再现观察到的动态行为。本文的目的是展示如何将动态元素系统地先验地集成到地理建模中,从而消除了对历史匹配的需要。这些动态元素是;连接储层区域CRR (Kayode等,2018)和压力瞬态分析PTA的渗透率-厚度(kh)解释。本文还介绍了基于CRR的渗透率建模的概念。crr是根据随时间推移关井压力趋势组来定义的。将岩心和测井数据根据确定的CRR进行分组,并用于建立基于CRR的神经网络模型,以预测每个CRR内非取心井的渗透率测井曲线。然后,地质建模师利用每个CRR内的渗透率测井曲线,通过两个变异函数长度假设(i)从有限岩心数据分析中获得的变异函数范围,(ii)确保CRR内连通性所需的变异函数范围,创建了两个地理实现。利用这两种实现对实测PTA数据井的压力瞬变进行了模拟,并将模拟压力瞬变导数与实测压力瞬变导数的对数-对数图进行了比较,以确定每口井的每种实现的质量。选择提供所有井误差最小二乘的实现作为基本情况地质模型。渗透率校正系数应用于基本情况地质模型,直到PTA kh可接受匹配。由此得到的PTA井渗透率测井称为PTA校正渗透率测井。一些取心井最初不需要神经网络渗透率建模,因为它们没有测井数据(声波测井、密度测井和中子测井)。混合渗透率测井是由这些井位的预测渗透率测井和岩心渗透率相结合得出的。所有渗透率校正测井(i) PTA校正的渗透率测井和(ii)混合渗透率测井然后被反馈到地质建模工作流程中,以生成考虑岩心数据、PTA kh和crr的改进渗透率分布。不做任何事情的模拟运行使超过80%的井压力数据可接受的历史匹配。该应用表明,将动态元素(如CRR、PTA kh)先验整合,并使用基于ccr的渗透率建模,可以获得更好的特征地质模型,并有可能消除对历史匹配的需求。
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