Successful Discoveries Using Novel DHI Technology Based on Seismic Resonance and Dispersion

Kristofer Skantze
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Abstract

A new technology that analyses dispersion events in seismic data is presented. The technology aims at identifying both reservoirs and also the likelihood of any presence of liquid hydrocarbons within them. This paper details the science on which the technology is based and empirical results from usage of the technology. Presence of strong wave dispersion in seismic data has analytically and in tests been seen to correlate with high porosity and permeability formations. A lack of dispersion has conversely been seen to correlate with low porosity systems. Furthermore, a high viscosity fluid in a poro-elastic system has been seen to cause higher dispersion effects compared to brine. This permits derisking of reservoirs to identify locations with high chance of liquid hydrocarbon. Resonance wave systems are abundant in sedimentary rock. The measurement of resonance waves permits the study of otherwise weak frequency shifts in seismic data, which can then be used to search for reservoir rock and liquid hydrocarbon. Velocity dispersion and resonance wave analysis of seismic data requires carefully selected wavelet based spectral decomposition methods. Results from a commercially available technology presented in this paper have shown a need to prioritize high accuracy spectral decomposition methods that are able to identify minute dispersion events. These methods are often very computationally demanding. Therefore, those methods need to be selected that ensure highest accuracy while optimizing for speed. A dispersive event occurs when an incoming P-wave propagates through a heterogeneous porous media due to mesoscopic flow. Dispersivity contributions may also stem from localized effects such as Krauklis waves. The level of dispersivity has in models and field tests been identified as a function of the reservoir porosity, permeability and fluid viscosity. Empirical results from the technology presented here, suggest the ability to identify reservoirs and frequently also their fluid content using dispersion analysis of seismic data. Case study results using the commercial technology are presented over both discovery and dry wells in Norway and Oman. The results show how new insights into poro-elastic lithology can be provided and also the technology's potential to contribute to an improved overall prospect derisking and field delineation with respect to fluid content. The technology demonstrates the ability to extract additional information from seismic data sets and thereby further the geological and geophysical subsurface interpretation and modelling.
基于地震共振和色散的新型DHI技术的成功发现
提出了一种分析地震资料中频散事件的新技术。该技术旨在识别储层以及储层中存在液态碳氢化合物的可能性。本文详细介绍了该技术所依据的科学以及该技术使用的实证结果。在分析和测试中发现,地震资料中存在的强波频散与高孔隙度和高渗透率地层有关。相反,分散的缺乏被认为与低孔隙度系统有关。此外,与卤水相比,多孔弹性体系中的高粘度流体具有更高的分散效果。这可以降低储层的风险,从而识别出液态烃可能性高的位置。沉积岩中有丰富的共振波系。共振波的测量允许研究地震数据中微弱的频移,然后可以用来寻找储层岩石和液态烃。地震资料的速度频散和共振波分析需要仔细选择基于小波的频谱分解方法。本文提出的一种商用技术的结果表明,需要优先考虑能够识别微小色散事件的高精度光谱分解方法。这些方法通常对计算量要求很高。因此,需要选择在优化速度的同时确保最高精度的方法。当入射纵波在非均质多孔介质中传播时,由于介观流动而发生色散事件。色散的贡献也可能源于局域效应,如克劳克利斯波。在模型和现场测试中,分散性水平被确定为储层孔隙度、渗透率和流体粘度的函数。本文介绍的经验结果表明,利用地震数据的离散分析,可以识别储层,通常还可以识别储层的流体含量。介绍了在挪威和阿曼的发现井和干井中使用商业技术的案例研究结果。研究结果表明,该技术可以提供有关孔隙弹性岩性的新见解,并有助于提高整体勘探风险和油田流体含量圈定的潜力。该技术证明了从地震数据集中提取额外信息的能力,从而进一步进行地质和地球物理地下解释和建模。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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