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Estimating the fracture density of small-scale vertical fractures when large-scale vertical fractures are present

机译:存在大型垂直裂缝时估算小型垂直裂缝的裂缝密度

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Fractures in reservoirs significantly affect reservoir flow properties in subsequent years, which means that fracture characteristics such as preferred orientation, crack density or fracture compliance, what filling is in the fractures and so on are of great importance for reservoir development. When fractures are vertical, aligned and their dimensions are small relative to the seismic wavelength, the medium can be considered to be an equivalent horizontal transverse isotropic (HTI) medium. However, geophysical data acquired over naturally fractured reservoirs often reveal the presence of multiple fracture sets. We investigate a case where there are two vertical sets of fractures having differing length scales. One fracture set has length scale that is much smaller than the seismic wavelength but the other has length scale that is similar to the seismic wavelength. We use synthetic data to investigate the ability to infer the properties of the small-scale fractures in the presence of the large-scale fracture set. We invert for the Thomsen-type anisotropic coefficients of the small-scale fracture set by using the difference of the P wave amplitudes at two azimuths, which makes the inversion convex. Then we investigate the influence of the presence of the large-scale fractures on our ability to infer the properties of the small-scale fracture set. Surprisingly, we find that we can reliably infer the fracture density of the small-scale fractures even in the presence of large-scale fractures having significant compliance values. Although the inversion results for Thomsen-type anisotropic coefficients of small-scale fractures for one model are not good enough to figure out whether it is gas-filled or fluid-filled, we can find a big change of Thomsen-type anisotropic coefficient epsilon((V)) between the models in which small-scale fractures are filled with gas and fluid.
机译:以后几年中,储层中的裂缝会显着影响储层的流动性,这意味着诸如择优取向,裂缝密度或裂缝顺应性,裂缝中的充填物等裂缝特征对于储层开发至关重要。当裂缝是垂直的,对齐的并且其尺寸相对于地震波长较小时,该介质可以视为等效的水平横向各向同性(HTI)介质。然而,在天然裂缝性储层上获得的地球物理数据通常显示出多个裂缝组的存在。我们调查了一种情况,其中有两组垂直裂缝具有不同的长度尺度。一个裂缝组的长度尺度远小于地震波长,而另一个裂缝组的长度尺度与地震波长相似。我们使用合成数据来研究在存在大型裂缝集的情况下推断小型裂缝性质的能力。利用两个方位角P波振幅的差值,对小尺度裂缝集合的Thomsen型各向异性系数进行反演,使得反演凸出。然后,我们研究了大型裂缝的存在对我们推断小型裂缝组属性的能力的影响。出乎意料的是,我们发现即使存在具有显着柔度值的大型裂缝,我们也可以可靠地推断出小型裂缝的裂缝密度。尽管对于一个模型,小尺寸裂缝的Thomsen型各向异性系数的反演结果不足以判断是充气还是流体填充的,但我们可以发现Thomsen型各向异性系数ε发生了很大变化( (V))之间的模型,其中小规模裂缝充满了气体和流体。

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