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Methodology to Estimate the Optimal Production Rate and OWC Advance in Naturally Fractured Reservoirs in the South of Mexico

机译:估算墨西哥南部自然骨折水库的最优生产率和OWC进展的方法

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A great problem of naturally fractured reservoirs is the abrupt irruption of water in wells. To predict this behavior, a methodology that uses numerical sector models and discrete fracture Network (DFN) was designed; so-called Pseudoradial models (PRM). These models were calibrated to match the water invaded wells production history and subsequently it was applied to proposed or new wells. This methodology was used successfully in Pijije field, Mexico. The first pseudoradial models were generated in the Pijije field due to the abrupt water irruption problem it presented. Three well models were built based on the calibration of the model built for the Pijije-101 well. The DFN was generated from average characterization of fractures obtained from FMI logs and general input from the field pressure and production behavior. Once the variables of uncertainty were analyzed, a conventional radial model was initially built and calibrated with the historical production and pressure profiles. To achieve this match, the values of porosity in both systems (matrix and fracture) were changed drastically and the water front advance resulting was homogeneous and only present a coning phenomenon when the OWC reaches a minimum distance of 200 meters from the well. The second part of the analysis was carried out with the pseudoradial model; in this case, the parameters with greater impact were the characteristics of discrete fracture network. The pseudoradial model managed to reproduce the well production and pressure history. Analyzing the results, it was concluded that both scenarios were acceptable. Reviewing the water advance fronts in both cases, the pseudoradial model did not have a uniform front of OWC advance and showed areas not drained (corresponding to present or absence of fractures) and the water moves through the preferential fracture channels represented by the DFN in the model. Two methods for determining critical rates or optimal production rates (OPR) and the OWC advance were evaluated: conventional radial models and pseudoradial models. The study was carried out to the Pijije-101 and Terra JSK field wells that presented abrupt water irruption possibly associated with water conning in the producing formation. Later the methodology was applied to new wells in the same field for calculating their optimal production rates. Although conventional radial model does not consider features and phenomena present in NFR, the movement of fluids and conning effect was correctly model. The pseudoradial model, in the same way, reproduced the dynamic behavior observed in this conventional case but presenting irregular advance of the OWC and areas not drained or partially drained which according to literature is more realistic. The main difference between the two models is the distribution of permeability and how the fluids move within the reservoir. Conventional radial model presents only a vertical variation, while a tensor of permeability (i, j, k) was included in the pseudoradial models. Due to the complexity of the NFR, it is recommended to perform analysis of water conning using pseudoradial models since it manages to represent the fractured medium with a more realistic and physical sense of the dynamic involved.
机译:一种自然裂缝储层的一个很大问题是井中的水突然突然。为了预测这种行为,设计了一种使用数值扇区模型和离散裂缝网络(DFN)的方法;所谓的伪影型模型(PRM)。这些模型被校准以匹配水入侵的井生产历史,随后将其应用于提议或新井。该方法在墨西哥Pijije Field成功使用。由于它呈现的突然的水侵扰问题,在Pijije领域中产生了第一伪模型。基于为Pijije-101的模型的校准构建了三种井模型。从FMI日志获得的裂缝和来自现场压力和生产行为的一般输入的平均表征产生DFN。一旦分析了不确定性的变量,就历史生产和压力轮廓初始构建和校准了传统的径向模型。为了实现这一匹配,两个系统(矩阵和骨折)中的孔隙度值大幅变化,并产生的水前部前进是均匀的,并且当OWC距离井中的最小距离为200米时,才呈现锥形现象。分析的第二部分是用伪组模型进行的;在这种情况下,具有更大影响的参数是离散裂缝网络的特性。伪影型模型成功再现了井生产和压力历史。分析结果,得​​出结论,这两种情况都是可接受的。在两种情况下审查水预先前线,伪影型模型没有均匀的OWC进展前面,并且显示未排出的区域(对应于骨折的情况或不存在),水通过DFN中所示的优先裂缝通道移动模型。评估了两种确定临界率或最佳生产率(OPR)和OWC进展的方法:传统的径向模型和伪影像模型。该研究是对Pijije-101和Terra JSK领域井进行的,该井呈现出可能与生产形成中的水刺痛有关的突然的水侵扰。后来,该方法应用于同一领域的新井,以计算其最佳生产率。虽然常规径向模型不考虑NFR中存在的特征和现象,但流体和凝固效果的运动是正确的模型。伪影大模型以相同的方式再现在该传统情况下观察到的动态行为,而是呈现OWC的不规则进展,并且根据文献的不排水或部分排出的区域是更现实的。两种模型之间的主要区别是渗透性分布以及流体如何在储层内移动。常规径向模型仅呈现垂直变化,而伪物模型中包括渗透率(I,J,K)的张量。由于NFR的复杂性,建议使用伪影型模型进行分析,因为它可以管理具有更现实和涉及的动态感应的骨折介质。

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