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Rock physics modelling of the carbonate reservoirs: A log-based algorithm to determine the pore aspect ratio

机译:碳酸盐储层的岩石物理建模:一种基于孔径宽高比的基于逻辑算法

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Rock physics models play an important role in understanding the elastic behavior of saturated rocks, and in the quantitative interpretation of seismic data in the areas between well controls. Most of the rock physics models were developed for clastic reservoirs. However, estimation of elastic properties in the carbonate reservoirs have been criticized recently. The major challenge on these reservoirs are primarily due to the pore type variation and the presence of fractures across the rock matrix. To overcome this issue, an aspect ratio (the ratio between the minor and major axes of an ellipsoidal pore) of the pore space was defined to consider the geometry of pores. Aspect ratio has a significant impact on the velocity of the saturated rock, however its quantification on the reservoir scale remains a challenging subject. Aspect ratio is commonly estimated from thin section analysis, however, thin sections are not commonly available for the entire logged reservoir interval. Hence, a constant aspect ratio is typically allocated for each pore type within the target layer. Considering the variation of depositional setting with depth, as well as including the role of diagenetic processes on the carbonate rocks, allocating a single constant aspect ratio across the reservoir interval could introduce uncertainties. In this paper, we introduce a log-based algorithm to estimate a variable aspect ratio that can be applied over the entire length of the logged interval. This method is based on the diverse influence of different pore types on the velocity and density logs. In addition, we include the impact of pressure variation on Xu and Payne (2009) model. Utilizing our methodology, the velocity log is estimated in a carbonate reservoir. The estimated velocity log shows better match with the measured velocity log compared with Lee (2005) (improved Gassmann) and Xu and Payne (2009) models. There are however some disparities left in the reconstruction of the velocity profile that encourages to understand the carbonate reservoirs further. (C) 2020 Elsevier B.V. All rights reserved.
机译:岩石物理模型在理解饱和岩石的弹性行为以及良好控制之间的地区地震数据的定量解释方面发挥着重要作用。大多数岩石物理模型是为碎屑藏开发的。然而,最近批评了碳酸盐储层中弹性性质的估计。这些水库的主要挑战主要是由于孔型变异和岩石基质上的骨折存在。为了克服这个问题,定义了孔隙空间的纵横比(椭圆形孔的次要轴之间的比率和大轴之间的比率)以考虑孔的几何形状。宽高比对饱和岩石的速度产生了重大影响,但其对储层规模的定量仍然是一个具有挑战性的主题。纵横比通常从薄截面分析中估计,然而,薄部分通常不可用于整个记录的储层间隔。因此,通常为靶层内的每个孔类型分配恒定纵横比。考虑到深度的沉积设置的变化,以及包括在碳酸盐岩上的作用作用,分配储层间隔的单一恒定宽度比可以引入不确定性。在本文中,我们介绍了一种基于日志的算法来估计可以在记录间隔的整个长度上施加的可变宽度比。该方法基于不同孔隙类型对速度和密度日志的不同影响。此外,我们还包括压力变化对徐和薪通(2009)模型的影响。利用我们的方法,速度日志估计在碳酸盐储层中。与LEE(2005)(改进的Gassmann)和Xu和Payne(2009)模型相比,估计的速度日志与测量的速度日志显示出更好的匹配。然而,有些差异留在速度概况的重建中,鼓励进一步了解碳酸盐储层。 (c)2020 Elsevier B.V.保留所有权利。

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