使用线性规划稀疏尖峰反演和深度前馈神经网络技术估算荷兰 F3 区块的岩石物理属性:案例研究

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS pure and applied geophysics Pub Date : 2024-03-14 DOI:10.1007/s00024-024-03439-7
Raghav Singh, Prabodh Kumar Kushwaha, S. P. Maurya, Piyush Rai
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摘要

本研究采用线性规划(l1-norm)稀疏尖峰反演(LPSSI)方法确定了荷兰 F3 区块地下的声阻抗(P-阻抗)分布。该研究的目标是描述砂道特征,并从低分辨率地震数据中提取高分辨率地下岩石特征。为了从地震数据中估算岩石属性,有多种传统的叠后地震反演技术可供选择。然而,LPSSI 技术是一种相当快速且易于计算的地下模型,可用于定量和定性解释。该方法分为两个步骤:首先,检索靠近油井位置的复合轨迹并反演声学 P-阻抗,然后通过与油井测井阻抗的比较来优化 LPSSI 参数。根据对复合地震道的分析,该算法性能良好,平均相关性高(0.98)。第二阶段利用 F3 区块地震数据,采用 LPSSI 方法估计地下声阻抗的分布。在反演声阻抗分析中,1380-1400 毫秒时间间隔内的沙道状低阻抗异常明显,范围为 3800-7400 m/s g/cc。然后,利用深度前馈神经网络(DFNN)估算了井间区域的许多其他关键岩石参数,包括孔隙度、密度和 P 波速度,以证实砂道的存在。在对这些岩石物理特性进行分析之后,1380-1400 毫秒时间间隔内出现了高孔隙度区(24-40%)、低密度区(1.9-2.02 克/立方厘米)和低 P 波速度区(1700-2300 米/秒),这与低阻抗区一致,验证了砂道的存在。
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Estimation of Petrophysical Properties Using Linear Programming Sparse Spike Inversion and Deep Feed-Forward Neural Network Techniques Over F3 Block, Netherlands: A Case Study

In this study, acoustic impedance (P-impedance) distribution in the subsurface of the F3 block, Netherlands is determined using the linear programming (l1-norm) sparse spike inversion (LPSSI) method. The objectives of the study are to characterize the sand channel and extract high-resolution subsurface rock features from the low-resolution seismic data. To estimate rock properties from seismic data, a variety of conventional post-stack seismic inversion techniques are available. However, the LPSSI technique is a reasonably quick and easy-to-compute subsurface model that can be employed for both quantitative and qualitative interpretation. The method is employed in two steps: first, composite traces close to well locations are retrieved and inverted for acoustic P-impedance, and then optimization of the LPSSI parameters is done using comparison with well log impedance. According to the analysis of the composite traces, the algorithm performs well and has a high average correlation (0.98). The F3 block seismic data are utilized in the second stage to estimate the distribution of acoustic impedance in the subsurface by using the LPSSI method. A sand channel-like low impedance anomaly with a range of 3800–7400 m/s g/cc is evident in the inverted acoustic impedance analysis at the 1380–1400 ms time interval. Then, using a deep feed-forward neural network (DFNN), many other crucial rock parameters, including porosity, density, and P-wave velocity, were estimated in the inter-well region to corroborate the sand channel. Following the analysis of these petrophysical properties, a high porosity zone (24–40%), low-density zone (1.9–2.02 g/cc), and low P-wave velocity zone (1700–2300 m/s) are present in the 1380–1400 ms time interval, which aligns with the low impedance zone and validates the presence of the sand channel.

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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
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