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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Using a pseudo-steady-state flow equation and 4D seismic traveltime shifts for estimation of pressure and saturation changes
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Using a pseudo-steady-state flow equation and 4D seismic traveltime shifts for estimation of pressure and saturation changes

机译:使用拟稳态流动方程式和4D地震传播时间偏移来估算压力和饱和度变化

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Pressure and saturation changes cause a change in seismic P-wave velocity resulting in a shift in 4D traveltime. A discrimination between both effects is important to enhance reservoir management decisions. We explored the possibility of linking the fields of reservoir engineering and 4D seismic. A simple inversion scheme based on a reservoir engineering flow equation for pore pressure predictions combined with the Hertz-Mindlin and Gassmann rock-physics models to discriminate pressure and saturation effects from 4D time shifts was presented. To account for no-flow reservoir boundaries, the pseudo-steady-state flow equation giving the pressure distribution was extended with a superpositioning method. During the inversion, three parameters were determined by a nonlinear, least-squares fitting method: the thickness of the hydrocarbon column, the pressure at the well position, and its decay rate away from the well. We successfully tested our approach on a synthetic and a field data case, where the CO_2 injection well at the Sn?hvit field, Norway, served as a good example to demonstrate our method. We observed a good correlation between simulation and inversion in our synthetic study. Our theory was limited to homogeneous reservoir conditions and produces spatially low frequent outputs. To apply the model in complex fields, such as at Sn?hvit, we introduced a spatially varying Mindlin-exponent over the field and used the theory as an heuristic model assuming that a variation of the Mindlinexponent takes a change in pressure sensitivity into account. This assumption provided the possibility to indirectly include heterogeneities in grain sorting and porosity variation and improved the model significantly. We see the advantage of our method in its fast and direct implementation to study first-order effects of pressure and saturation behavior on time-lapse seismic data using a simple inversion algorithm instead of computationally intensive simulations.
机译:压力和饱和度的变化会引起地震P波速度的变化,从而导致4D传播时间发生变化。两种效果之间的区别对于增强储层管理决策很重要。我们探索了将油藏工程和4D地震领域联系起来的可能性。提出了一种基于储层工程流方程的孔隙压力预测的简单反演方案,并结合了Hertz-Mindlin和Gassmann岩石物理学模型来区分4D时移中的压力和饱和度效应。为了解决无流动油藏边界问题,采用叠加方法扩展了给出压力分布的拟稳态流动方程。在反演过程中,通过非线性最小二乘拟合法确定了三个参数:烃柱的厚度,井位置处的压力及其远离井的衰减率。我们成功地在合成和现场数据案例中测试了我们的方法,其中在挪威Sn?hvit油田的CO_2注入井是证明我们方法的一个很好的例子。在我们的综合研究中,我们观察到了模拟与反演之间的良好相关性。我们的理论仅限于均质储层条件,并产生空间较低的频繁产出。为了将模型应用到诸如Sn?hvit的复杂领域,我们在该领域引入了空间变化的Mindlin指数,并在假设Mindlinexponent的变化考虑了压力敏感性变化的情况下,将该理论用作启发式模型。该假设提供了在晶粒分类和孔隙度变化中间接包含异质性的可能性,并显着改善了模型。我们看到了我们的方法的优势,该方法可以快速,直接地实现,它使用简单的反演算法而不是计算密集型模拟来研究时移地震数据的压力和饱和行为的一阶效应。

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