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Integration of Time-Lapse Seismic Data Using the Onset Time Approach:The Impact of Seismic Survey Frequency

机译:使用起始时间方法的时间流逝地震数据集成:地震测量频率的影响

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The seismic inversion method using the seismic onset times has shown great promise for integrating real-continuous seismic surveys for updating geologic models.However,due to the high cost of seismic surveys,such frequent seismic surveys are not commonly available.In this study,we focus on analyzing the impactof seismic survey frequency on the onset time approach,aiming to extend the advantages of onset timeapproach when infrequent seismic surveys are available.To analyze the impact of seismic survey frequency on the onset time approach,first,we conduct asensitivity analysis based on the frequent seismic survey data(over 175 surveys)of steam injection in aheavy oil reservoir(Peace River Unit)in Canada.The calculated onset time maps based on seismic surveydata sampled at various time intervals from the frequent data sets are compared to examine the need andeffectiveness of interpolation between surveys.Additionally,we compare the onset time inversion with thetraditional seismic amplitude inversion and quantitatively investigate the nonlinearity and robustness forthese two inversion methods.The sensitivity analysis shows that using interpolation between seismic surveys to calculate the onsettime an adequate onset time map can be extracted from the infrequent seismic surveys.This holds goodas long as there are no changes in the underlying physical mechanisms during the interpolation period.A 2D waterflooding case demonstrates the necessity of interpolation for large time span between theseismic surveys and obtaining more accurate model update and efficient data misfit reduction during theinversion.The SPE Brugge benchmark case shows that the onset time inversion method obtains comparablepermeability update as the traditional seismic amplitude inversion method while being much more efficient.This results from the significant data reduction achieved by integrating a single onset time map rather thanmultiple sets of amplitude maps.The onset time approach also achieves superior convergence performanceresulting from its quasi-linear properties.It is found that the nonlinearity of the onset time method can besmaller than that of the amplitude inversion method by several orders of magnitude.
机译:使用地震发作时间的地震反演方法对整合实际的地震调查来说,用于更新地质模型的抗震反演方法。然而,由于地震调查的高成本,这种常见的地震调查通常不可用。在这项研究中,我们专注于分析地震调查频率对起始时间方法的影响,旨在扩展出现尖锐的地震调查时发病的优势。要分析地震测量频率对发病时间方法的影响,首先,我们进行了基于渐敏分析在加拿大的蒸汽喷射蒸汽喷射蒸汽注射液(超过175次调查)上。比较了基于频繁数据集的各种时间间隔采样的地震勘探数据的计算发行时映射,以检查在调查之间的插值需要和效率。加法,我们将起始时间倒置与椎体震荡振荡进行比较e反转并定量地研究了两种反转方法的非线性和鲁棒性。敏感性分析表明,使用地震调查之间的插值可以从不频繁的地震调查中提取足够的发起时间地图。如果没有,则可以提取足够的出现时间映射。如果没有插值期间的底层物理机制的变化。2D水上案例表明了在替代的大型时间跨度之间的插值的必要性,并在经过者期间获得更准确的模型更新和有效的数据不足减少.PE坚定不移的基准情况表明发病时间反转方法获得比较的人可折射率更新作为传统地震幅度反转方法,同时更有效。这是通过集成单个起始时间图而不是多样的幅度图来实现的显着的数据减少。起始时间方法也实现了SUP从其准线性属性的ERIOR融合性能。发现开始时间方法的非线性可以通过几个级比幅度反转方法的非线性。

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