首页> 外文会议>EAGE conference & exhibition;SPE EUROPEC 2005;Madrid 2005 >Uncertainty estimation in seismic-basedporosity and saturation inversion: Examplesfrom unconsolidated and hard rockenvironments
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Uncertainty estimation in seismic-basedporosity and saturation inversion: Examplesfrom unconsolidated and hard rockenvironments

机译:基于地震的孔隙度和饱和度反演中的不确定度估计:来自未固结和坚硬岩石环境的示例

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Uncertainties associated with predicting pay, saturation, and porosity in the subsurface are related not only toseismic inversion accuracy, resolution, and confidence in rock-physics relations, but also to diagenetic processesassociated with porosity reduction processes and hydrocarbon migration into the reservoir. In this paper, we usestochastic simulation techniques and formal Bayesian inversion to explore the uncertainty associated withporosity and saturation estimates obtained in two prototypical environments: a consolidated, hard sand reservoirin east Texas and soft, unconsolidated sediments in marine environments offshore Asia. In hard rocks, brinesaturation is often correlated with increased cementation and reduced porosity, and hydrocarbons often migrateinto large-porosity areas. Therefore, porosity and saturation are often correlated. In soft unconsolidatedsediment environments, sands have high porosities, and porosity and saturation have a large degree ofindependence. A Markov chain Monte-Carlo (MCMC) simulation technique is used to exploit this geologicalinformation to simulate expected ranges of porosity and saturation associated with these geological processes.Baysian inversion is used to generate optimal estimates of porosity and saturation with uncertainty. We showthat although in hard matrix the response to changes in fluid saturation may be very small, a reliable saturationestimate can be obtained due to the diagenetic processes. In soft sediments, where matrix is more sensitive tochanges in fluid modulus and saturation, confidence in saturation estimates may be higher than the hardsediments example. These effects can be captured using joint inversion techniques that are based both on rockphysics and diagenetic characterization of the reservoir.
机译:与预测地下开采量,饱和度和孔隙度相关的不确定性不仅与地震反演的准确性,分辨率和对岩石物理关系的信心有关,而且与与孔隙度降低过程和油气运入储层的成岩过程有关。在本文中,我们使用随机模拟技术和形式贝叶斯反演来探讨在两种典型环境中获得的孔隙度和饱和度估算值相关的不确定性:德克萨斯州东部的固结硬砂储层和亚洲近海海洋环境中的软质未固结沉积物。在坚硬的岩石中,盐水饱和度通常与胶结作用的增加和孔隙率的降低有关,并且碳氢化合物通常会迁移到大孔隙度的区域。因此,孔隙率和饱和度通常是相关的。在软的非固结沉积环境中,砂具有高孔隙度,并且孔隙度和饱和度具有很大的独立性。使用马尔可夫链蒙特卡洛(MCMC)模拟技术来利用此地质信息来模拟与这些地质过程相关的孔隙度和饱和度的预期范围,并使用贝叶斯反演来生成具有不确定性的孔隙度和饱和度的最佳估计值。我们表明,尽管在硬质基质中对流体饱和度变化的响应可能非常小,但由于成岩过程,可以获得可靠的饱和度估计。在基质对流体模量和饱和度变化更敏感的软质沉积物中,饱和度估计的可信度可能高于硬质沉积物的示例。可以使用基于岩石物理学和储层成岩特征的联合反演技术来捕获这些影响。

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