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首页> 外文期刊>Journal of Applied Geophysics >Effects of CO2 on P-wave attenuation in porous media with micro-cracks: A synthetic modelling study
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Effects of CO2 on P-wave attenuation in porous media with micro-cracks: A synthetic modelling study

机译:二氧化碳对微裂纹多孔介质中P波衰减的影响:综合模拟研究

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摘要

The presence of CO2 in hydrocarbon reservoirs can cause significant changes in seismic wave properties. In turn these properties can be used to map CO2 saturation in hydrocarbon reservoirs or aquifers - either from natural sources or by injection from the surface. We present the results of a synthetic modelling study of the effects of supercritical CO2 saturation on P-wave attenuation in a medium consisting of four horizontal layers, including a target aquifer. The target aquifer is modelled fully by an effective medium containing pores saturated with brine and/or CO2 and randomly-aligned microcracks at different densities. The other layers are modelled solely by their bulk seismic velocities and densities. We first compute synthetic seismograms for a reference case where the third layer is completely isotropic with no cracks, no pores and no fluid saturation. We then calculate synthetic seismograms for finite crack densities of 0.01, 0.02 and 0.03 at varying degrees of CO2 saturation in the third layer. The results of our analysis indicate that attenuation is sensitive both to CO2 saturation and the crack density. For a given crack density, attenuation increases gradually with decreasing percentage of CO2 saturation and reaches a maximum at around 10% saturation. The induced attenuation increases with crack density and with offset. These observations hold out the potential of using seismic attenuation as an additional diagnostic in the characterisation of rock formations for a variety of applications, including hydrocarbon exploration and production, subsurface storage of CO2 or geothermal energy extraction. (C) 2016 Elsevier B.V. All rights reserved.
机译:碳氢化合物储层中CO2的存在会导致地震波特性发生重大变化。反过来,这些属性可以用于绘制烃源或含水层中的CO2饱和度图-来自自然资源或通过地表注入。我们介绍了在包括目标含水层在内的四个水平层组成的介质中,超临界CO2饱和度对P波衰减的影响的综合建模研究的结果。目标含水层可以通过有效介质完全建模,该介质包含充满盐水和/或CO2的孔隙以及不同密度的随机排列的微裂缝。其他层仅通过其整体地震速度和密度建模。我们首先为参考情况计算合成地震图,其中第三层是完全各向同性的,没有裂缝,没有孔隙并且没有流体饱和。然后,我们在第三层中不同程度的CO2饱和度下针对0.01、0.02和0.03的有限裂纹密度计算合成地震图。我们的分析结果表明,衰减对CO2饱和度和裂纹密度均敏感。对于给定的裂纹密度,衰减随着CO2饱和度百分比的降低而逐渐增加,并在大约10%饱和度时达到最大值。感应衰减随裂纹密度和偏移而增加。这些观察结果表明,在多种应用中,包括碳氢化合物勘探和生产,CO2地下存储或地热能提取,都可以将地震衰减作为岩层表征中的附加诊断手段。 (C)2016 Elsevier B.V.保留所有权利。

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