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Water flooding of the Oseberg 0st oil field, Norwegian North Sea: Application of formation water chemistry and isotopic composition for production monitoring

机译:挪威北海Oseberg 0st油田的水驱:地层水化学和同位素组成在生产监测中的应用

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This case study demonstrates how natural heterogeneities of formation and injection waters can be applied to a number of production related applications, extending into the mature life of a reservoir. Break-through of injection water, identification and characterisation of production intervals and evaluation of responses to operational events are some of the possible applications during production.The Oseberg 0st oil field in the North Sea represents a complex situation with commingled production from all Brent Group formations. The Sr isotope composition is an excellent parameter for defining the natural baseline of formation water, with a good spatial resolution and vertical stratification. Aquifer water from the Utsira Formation is injected for pressure support, and reinjection of produced water has also been applied since the onset of water production. Utsira Formation water has high Mg, low Ba and low Sr content compared to the reservoir formation waters. Isotopic compositions (5D and ~(87)Sr/~(86)Sr) are also distinct. A non-reactive behaviour of Ba and Sr is verified from binary cross-plots and geochemical modelling. Break-through of injection water could be identified in five production wells based on Ba/Mg ratios. In one of the reservoir compartments (Beta Saddle), water injection points were changed after approximately three years. The Ba/Mg ratio could also identify the second injection water break-through in one of the wells due to an intermediate period of higher formation water content Since the Sr content in the Utsira water is low, the ~(87)Sr/~(86)Sr ratio is a good natural tracer for formation water movements even at high ratios of injected water. In particular, the vertical stratification of ~(87)Sr/~(86)Sr is useful for quantifying production from different intervals in commingled wells. A methodology for using operational events, such as production allocations or shut-ins, for characterisation of production zones is discussed.
机译:该案例研究证明了地层水和注入水的天然非均质性如何可应用于许多与生产相关的应用,并延伸到储层的成熟寿命中。注入水的突破,生产间隔的识别和表征以及对作业事件响应的评估是生产过程中的一些可能应用。北海的Oseberg 0st油田代表着复杂的局面,来自所有Brent Group地层的混合生产。 Sr同位素组成是定义地层水自然基线的极佳参数,具有良好的空间分辨率和垂直分层。从Utsira地层注入的含水层水用于压力支撑,自开始生产水以来,也已进行了回注。与储层地层水相比,Utsira地层水具有高Mg,低Ba和Sr含量。同位素组成(5D和〜(87)Sr /〜(86)Sr)也不同。通过二元交叉图和地球化学模型验证了Ba和Sr的非反应性行为。根据Ba / Mg比例,可以在五个生产井中识别出注入水的突破。在其中一个储水箱(贝塔鞍座)中,注水点在大约三年后发生了变化。由于地层水含量较高的中间时期,Ba / Mg比还可以确定其中一口井的第二次注水突破。由于Utsira水中的Sr含量较低,因此〜(87)Sr /〜( 86)Sr比是即使在注入水比例很高的情况下也能很好地追踪地层水运动的示踪剂。特别地,〜(87)Sr /〜(86)Sr的垂直分层可用于量化混合井中不同间隔的产量。讨论了使用操作事件(例如生产分配或关闭)来表征生产区域的方法。

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