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Reservoir Baffling Seen by Disequilibrium of DFA Fluid Gradients and by Wireline Pressure Transients and DSTs

机译:通过DFA流体梯度的不平衡以及电缆压力瞬变和DST看到的储层挡板

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In this reservoir study, three adjacent structures have been subject to largely the same fluid charge withrnan original oil charge and a very recent light hydrocarbon charge (all indicated by petreolum systemsrnmodeling and organic geochemical analyses). In addition, all wells have an oil-water contact (OWC) andrntwo have a gas-oil contact (GOC), while the GOC in the third well is not far away. Thus, allrndepth-dependent in-reservoir fluid geodynamic processes are visible within each well; no extrapolationrnaway from the wells is required. Moreover, the ~30 meter oil columns in evidently connected sands arernamenable to simple dynamic modeling thereby aiding in understanding. All three structures are found tornhave very different reservoir realizations, particualry regarding the dispositions of asphaltenes in spite ofrnnominally similar initiation conditions after the secondary charge. That is, different reservoir fluidrngeodynamic processes took place producing different constraints on production in each of the structures.rnOne well showed a light oil underlain by a tar mat. A second well showed large, disequilibrium gradientsrnof gas-oil ratio (GOR) and asphaltene content without phase separated asphaltenes in core. The third wellrnshowed a tar mat on a shale break in the oil column not far form the GOC. There were no asphaltenes inrncore above the shale break and tar mat. However, below the shale break there was asphaltene throughoutrnthe core while retaining permeability, but no tar mat on the OWC. These differences were not ascribedrnto any paleo-OWC nor are they related to differing biodegradation. In addition, these differences are notrnconsistent with any depressurization expalanation.rnTo resolve the differences, a variety of data streams were used including downhole fluid analysisrncoupled with thermodynamic analysis from the Flory-Huggins-Zuo Equation of State (FHZ EoS) and itsrnreliance on the Yen-Mullins model of asphaltenes. In addition, well test results provide key productionrninformation and are corroborated by vertical intereference testing on wireline. Petroleum system modelingrnand organic geochemical analysis of oil and core extract samples have also been very useful. Therndifferences seen in the different wells relate to several important parameters such as the different extentrnof baffling which impacts both production rates as well as equilibration rates of reservoir fluids. Anotherrnkey parameter is the extent of density stacking versus a lateral fluid front for the secondary lightrnhydrocarbon charge. Proximity to the charge point enhances the lateral nature of the charge yielding rapid asphaltene instability precluding tar mat formation in sections of the well. This information is very usefulrnwhen projecting reservoir properties away form wellbore.
机译:在该储层研究中,三个相邻的构造物在很大程度上与原来的石油装料和最近的轻质烃装料(相同的石油系统建模和有机地球化学分析表明)具有相同的流体装料。此外,所有油井都具有油水接触(OWC),两个油井都具有气油接触(GOC),而第三井中的GOC距离也不远。因此,在每个井中都可以看到与深度有关的所有储层流体地球动力学过程。不需要从井中推断。此外,在明显相连的砂岩中约30米的油柱可简化动态建模,从而有助于理解。发现这三种结构都具有非常不同的储层实现方式,尽管在二次装料后引发条件基本相似,但是关于沥青质的布置却存在一些特殊性。就是说,不同的储层流体动力学过程发生了,对每个结构的生产产生了不同的约束。一口井的焦油垫层显示了轻油。第二口井表现出较大的不平衡梯度,气油比(GOR)和沥青质含量,岩心中没有相分离的沥青质。第三口井在离GOC不远的油柱的页岩裂缝处显示了一块焦油垫。在页岩断裂和焦油垫上方没有沥青质内核。但是,在页岩断裂之下,整个岩心中都有沥青质,同时保持了渗透性,但OWC上没有焦油垫。这些差异不归因于任何古有机碳,也不与不同的生物降解有关。此外,这些差异与任何降压解释都不一致。为解决差异,使用了多种数据流,包括井下流体分析,Flory-Huggins-Zuo状态方程(FHZ EoS)的热力学分析及其对日元的依赖-沥青质的马林斯模型。此外,油井测试结果提供了关键的生产信息,并通过电缆的垂直内部测试得到了证实。石油系统建模以及石油和岩心提取物样品的有机地球化学分析也非常有用。在不同的井中看到的温度差异与几个重要参数有关,例如影响油藏流体生产率和平衡率的不同范围挡板。另一个关键参数是次级轻质烃装料的密度堆积程度与侧向流体前沿的关系。靠近装料点会增强装料的侧向特性,从而导致沥青质快速不稳定,从而排除了井段中焦油垫的形成。当将储层特性从井眼投射出去时,此信息非常有用。

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