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The interpretation of amplitude changes in 4D seismic data arising from gas exsolution and dissolution

机译:解释4D地震数据中由于气体溶解和溶解引起的振幅变化

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摘要

This study examines the four-dimensional (4D) seismic signatures from multiple seismic surveys shot during gas exsolution and dissolution in a producing hydrocarbon reservoir, and focuses in particular on what reservoir information may be extracted from their analysis. To aid in this process, hydrocarbon gas properties and behaviour are studied, and their relationship to the fluid-flow physics is understood using numerical simulation. This knowledge is then applied to interpret the seismic response of a turbiditc field in the UK Continental Shelf (UKCS). It is concluded that for a repeat seismic survey shot 6 months or more after a pressure change above or below bubble point (as in our field case), the gas-saturation distribution during either exsolution or dissolution exists in two fixed saturation conditions defined by the critical and the maximum possible gas saturation. Awareness of this condition facilitates an interpretation of the data from our field example, which has surveys repeated at intervals of 12-24months, to obtain an estimate of the critical gas saturation of between 0.6 and 4.0%. These low values are consistent with a range of measurements from laboratory and numerical studies in the open literature. Our critical gas-saturation estimate is also in qualitative agreement with the solution gas-oil ratios estimated in a material balance exercise using our data. It is not found possible to quantify the maximum gas saturation using the 4D seismic data alone, despite the advantage of having multiple surveys, owing to the insensitivity of the seismic amplitudes to the magnitude of this gas saturation. Assessment of the residual gas saturation left behind after secondary gas-cap contraction during the dissolution phase suggests that small values of less than a few per cent may be appropriate. The results are masked to some extent by an underlying water flood. It is believed that the methodology and approach used in this study may be readily generalized to other moderate- to high-permeability oil reservoirs, and used as input in simulation model updating.
机译:这项研究检查了在油气开采和开采过程中气体抽散和溶解过程中进行的多次地震勘测中的四维(4D)地震特征,并特别关注了可以从其分析中提取哪些储层信息。为了帮助这一过程,研究了烃类气体的性质和行为,并通过数值模拟了解了它们与流体物理的关系。然后,将这些知识应用于解释英国大陆架(UKCS)中浊度场的地震响应。结论是,对于在高于或低于气泡点的压力变化后6个月或更长时间进行的重复地震勘测(如在我们的现场案例中),在溶解或溶解过程中,气体饱和度分布存在两种固定的饱和度条件,即临界和最大可能的气体饱和度。意识到这种情况有助于从我们的现场示例中解释数据,该示例以12-24个月的间隔重复进行调查,以获得临界气体饱和度的估计值介于0.6%和4.0%之间。这些低值与公开文献中来自实验室和数值研究的一系列测量值一致。我们的临界气体饱和度估计值也与使用我们的数据进行的物料平衡练习中估计的溶液气油比在质量上一致。尽管地震波幅值对该气体饱和度的大小不敏感,但尽管具有多次勘测的优势,但仍无法仅使用4D地震数据来量化最大气体饱和度。对溶解阶段二次气顶收缩后留下的残余气体饱和度的评估表明,小于几个百分点的较小值可能是合适的。结果在一定程度上被潜在的洪水淹没了。可以相信,本研究中使用的方法和方法可以很容易地推广到其他中等至高渗透率的油藏,并用作模拟模型更新的输入。

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