评价注水开发过程中储层变质风险的定量预测方法

H. Salimi, Maryam Namdar Zanganeh, Sven McCarthy, Lucian Pirlea, Jurriaan Nortier, D. Frigo, Haitham Balushi, M. Lawati, M. Yarabi
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引用次数: 0

摘要

在计划/正在进行的注水开发过程中,需要对油田的注水潜力进行调查,以便选择注入水源和设施设计方案。本文介绍了一种新的储层酸化方法的应用,以评估两个中东油田(S和T)的酸化潜力,推荐防止和/或减少H2S产生的方法,并确定最佳的注水方案。新方法包括流体取样和分析、桌面研究、动态油藏模拟和地面设施评估。在桌面研究中,对注入水源(采出水和/或含水层水)、储层特征以及限制未来H2S浓度的缓解策略进行了定性评估。随后,开发了一个包括3个相、18个组分和18个反应的组成非等温动态模型,以定量预测油田生命周期内最可能和最坏情况下的H2S水平。为了评估关键不确定参数对H2S水平的影响,进行了几次敏感性测试。桌面研究得出结论,S油田产出的H2S具有非微生物外部来源,可能来自深部有机硫化合物的热裂解,并从Huqf烃源岩迁移到储层中。在模拟中,这种热生成的H2S与地层水中的初始背景H2S水平一起呈现。Base-Case-Scenario结果表明,在背景H2S水平(350 ppmv)的S油田,由于添加了水致微生物酸化,注入水突破后H2S水平增加到1000 ppmv。在没有背景H2S水平的T油田,微生物H2S水平在2044年达到195 ppmv,含水率为95%。最坏情景的结果表明,如果在基本情景中VFA含量被严重低估,抽提能力被高估,那么在S区和T区注入低矿化度含水层水时,微生物酸化的风险将会很高。在最坏情况下,S田和T田的气相H2S浓度分别达到最大值3400和1200 ppmv。对微生物酸化缓解方案的分析表明,在该站注入高矿化度采出水回注(PWRI)是目前最有效的微生物酸化预防方法,是T和S油田的最佳缓解方案,其效果和效率远远优于注入硝酸盐。在最坏的情况下,PWRI有效地阻碍了微生物H2S的生成,并使产气中的H2S浓度保持在背景H2S水平附近。虽然PWRI不是S和T油田的选择,并且没有将PWRI转移到S和T油田的基础设施,但进一步的分析可能会证明这一计划的改变是合理的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Quantitative and Predictive Reservoir-Souring Approach to Assess Reservoir-Souring Risk During Waterflood Development
Souring potentials of fields during planned-/ongoing-waterflood development need to be investigated to enable the selection of the injection-water source and facility-design options. This paper presents the application of a novel reservoir-souring approach to assess the souring potential of two Middle-East fields (S and T), to recommend ways to prevent and/or reduce H2S production, and to determine the optimum solution for injection water. The novel approach includes fluid sampling and analysis, a desktop study, a dynamic-reservoir simulation, and a surface-facility evaluation. In the desktop study, a qualitative assessment of souring associated with injection-water sources (produced water and/or aquifer water) and reservoir characteristics and mitigation strategies to limit future H2S concentrations were carried out. Subsequently, a compositional non-isothermal dynamic model that includes 3 phases, 18 components, and 18 reactions was developed to quantitatively predict the most-likely and the worst-case H2S levels over the fields’ life. Several sensitivity runs were performed to assess the impact of the key uncertain parameters on the H2S level. The desktop study concluded that the produced H2S from field S has a non-microbial external source, which is likely to be derived from thermal cracking of organosulfur compounds at depth and migrated into the reservoir from the Huqf source rocks. This thermally-generated H2S is presented with an initial background H2S level in the formation water in the simulations. The Base-Case-Scenario results reveal that in the S field with the background H2S level (350 ppmv), the level of H2S increases to 1000 ppmv after injection-water breakthrough because of the addition water-induced microbial souring. In the T field without background H2S levels, the level of microbial H2S reaches 195 ppmv in year 2044 at a water cut of 95%. The results of the Worst-Case Scenarios indicate that if the VFA content is significantly underestimated and the abstraction capacity is overestimated in the Base-Case Scenarios, the risk of microbial souring would be high in the S and T fields when injecting low-salinity Fars-aquifer water. In the Worst-Case Scenarios, the gas-phase H2S concentration attains max values of 3,400 and 1,200 ppmv, respectively, for the S and T fields. Analysis of the microbial-souring mitigation options suggest that injecting the high-salinity produced-water re-injection (PWRI) at the station—being the most robust microbial-souring-prevention method available—is the best mitigation option in the T and S fields and its effectivity and efficiency are far superior to nitrate injection. In the Worst-Case Scenario, PWRI effectively hampers the generation and production of microbial H2S and maintains the H2S concentration in the produced gas around the background H2S level. Although PWRI is not an option for the S and T fields and there is no infrastructure in place for transferring the station-PWRI to the S and T fields, further analysis might justify this change of plans.
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