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82nd EAGE Annual Conference & Exhibition最新文献

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Second-Order Perturbation Approximation of HTI Medium based on Azimuthal Observation 基于方位观测的HTI介质二阶微扰近似
Pub Date : 1900-01-01 DOI: 10.3997/2214-4609.202112729
J. Shan, G. Wu, H. Liu, S. Yang
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引用次数: 0
Near-surface multi-parameter estimation for VTI media by first-arrival stereotomography VTI介质初到立体成像近地表多参数估计
Pub Date : 1900-01-01 DOI: 10.3997/2214-4609.202112766
H. Sun, K. Yang, H. Wang, T. Shu
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引用次数: 0
Joint reflection and diving FWI using graph-space optimal transport and structure-guided smoothing on benchmark data 基于图空间最优传输和基准数据结构导向平滑的联合反射和潜水FWI
Pub Date : 1900-01-01 DOI: 10.3997/2214-4609.202112779
G. Provenzano, L. Métivier, R. Brossier
Introduction Joint full waveform inversion (JFWI, Zhou et al., 2015) builds a P-wave velocity (Vp) macromodel exploiting simultaneously the information carried by diving waves and reflections (e.g. in RWI, Brossier et al., 2015), thus obtaining deep Vp-updates while enforcing the constraint on the shallow subsurface. Here we devise an acoustic JFWI+Impedance-WI (IpWI) strategy on the Chevron-2014 benchmark limited-offset reflection elastic dataset. JFWI is performed using a graph-space optimal transport objective function (GSOT, Métivier et al., 2019) and takes advantage from along-structure smoothing based on the impedance reflective image. We compare GSOT and L2 objective functions, and show the benefits of structure-oriented smoothing (Trinh et al., 2017). Finally, the JFWI solution is used as starting model of a multi-scale Vp-FWI, attaining an excellent match with the virtual log, a satisfactory focusing of the common image gathers (CIGs), and an improved stationarity of the source wavelet estimation.
联合全波形反演(JFWI, Zhou et al., 2015)建立了纵波速度(Vp)宏观模型,同时利用潜水波和反射(如RWI, Brossier et al., 2015)所携带的信息,从而在对浅层地下进行约束的同时获得深层Vp更新。在这里,我们设计了一种基于Chevron-2014基准有限偏移反射弹性数据集的声学JFWI+阻抗wi (IpWI)策略。JFWI使用图空间最优传输目标函数(GSOT, m等人,2019)执行,并利用基于阻抗反射图像的沿结构平滑。我们比较了GSOT和L2目标函数,并展示了面向结构的平滑的好处(Trinh et al., 2017)。最后,将JFWI解决方案作为多尺度Vp-FWI的起始模型,获得了与虚拟日志的良好匹配,公共图像集(CIGs)的令人满意的聚焦,并且提高了源小波估计的平稳性。
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引用次数: 0
Reverse time migration with frequency-dependent Q compensation accelerated with GPU computing 基于频率相关Q补偿的逆时偏移,通过GPU计算加速
Pub Date : 1900-01-01 DOI: 10.3997/2214-4609.202112710
J. Cheng, J. Chen, W. Wu, M. Guo, X. Wu, N. Dai
It is well known that the earth strata are far from perfectly elastic but demonstrate the properties of viscoelasticity, in which seismic waves suffer wavelet shape distortion and energy loss during propagation. Seismic attenuation is commonly characterized by the quality factor Q. The linear model of wave attenuation with frequency independent Q is widely used in exploration seismology (Kjartansson, 1979). Based on this theory, different frequency components of seismic waves propagate in anelastic materials with a frequency-dependent phase velocity, while in elastic media all frequency components travel with the same phase velocity. In anelastic media the energy loss is approximately proportional to the frequency. In general, higher frequency components in seismic waves tend to travel faster than low frequency components, and their amplitudes decay more quickly. Seismic imaging without proper accounting of dispersion and amplitude loss produces images with distorted phases, dimmed amplitudes and reduced resolutions, especially for deeper horizons under low quality factor (low Q) strata, making it more difficult to do AVO interpretation analysis and to tie seismic horizons to well data.
众所周知,地层并不是完全弹性的,而是表现出粘弹性的特性,在这种特性下,地震波在传播过程中会发生小波形状畸变和能量损失。地震衰减通常用质量因子Q来表示,与频率无关的Q波衰减线性模型在勘探地震学中得到广泛应用(Kjartansson, 1979)。根据这一理论,地震波的不同频率分量在非弹性材料中以频率相关的相速度传播,而在弹性介质中,所有频率分量以相同的相速度传播。在非弹性介质中,能量损失近似与频率成正比。一般来说,地震波中的高频分量往往比低频分量传播得更快,其振幅衰减得更快。没有适当考虑频散和振幅损失的地震成像会产生相位失真、振幅变暗和分辨率降低的图像,特别是对于低质量因子(低Q)地层下的较深层位,这使得进行AVO解释分析以及将地震层位与井数据联系起来变得更加困难。
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引用次数: 0
Ultra-resolution near surface FWI within a transmission surface-consistent scheme 传输面一致方案下的超分辨率近地表FWI
Pub Date : 1900-01-01 DOI: 10.3997/2214-4609.202112727
D. Colombo, E. Sandoval-Curiel, E. Turkoglu, A. Kontakis, D. Rovetta
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引用次数: 0
A matrix-free reformulation of the multi-parameter descent and conjugate-gradient method for isotropic elastic iterative reverse-time migration 各向同性弹性迭代逆时偏移的无矩阵多参数下降和共轭梯度法
Pub Date : 1900-01-01 DOI: 10.3997/2214-4609.202112725
W. Mulder
Multi-parameter inversion of linear systems appears in many problems. The focus here is on isotropic elastic iterative reverse-time migration for three position-dependent subsurface model parameters, which amounts to data fitting of processed seismic data with synthetics from the Born approximation of the elastic wave equation. In that case, the matrix of the linear system is the hessian. As it is impractical to form, a matrix-free formulation is needed, which is readily derived for the gradient descent method. For single-parameter inversion, the conjugate-gradient (CG) method is generally more efficient than simple descent. However, the multiple-parameter CG method has a significantly higher cost than the descent method. Here, first a matrix-free data-domain reformulation is derived. Then, its performance is compared to the simple descent method to see of its faster convergence justifies the higher cost. A comparison on a marine 2-D toy problem with a salt body and sea-bottom receivers shows that the multiple-parameter descent method wins in terms of efficiency if the number of iterations is limited and that the single-parameter CG method is even faster.
线性系统的多参数反演出现在许多问题中。本文的重点是三个位置相关地下模型参数的各向同性弹性迭代逆时偏移,这相当于将处理过的地震数据与弹性波动方程的Born近似合成的数据拟合。在这种情况下,线性系统的矩阵就是黑森矩阵。由于不实际的形成,需要一个无矩阵的公式,这是很容易导出的梯度下降法。对于单参数反演,共轭梯度法(CG)通常比简单下降法更有效。然而,与下降法相比,多参数CG法的代价要高得多。在这里,首先推导了一个无矩阵的数据域重构公式。然后,将其性能与简单下降法进行比较,以证明其更快的收敛速度证明了较高的成本是合理的。对含盐体和海底接收机的海洋二维玩具问题进行了比较,结果表明,在迭代次数有限的情况下,多参数下降法的求解效率更高,单参数CG法的求解速度更快。
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引用次数: 0
Testing CO2 compatibility of a glauconitic reservoir: Case study from depleted Nini Field, Danish North Sea 海绿石油藏CO2相容性测试:以丹麦北海枯竭Nini油田为例
Pub Date : 1900-01-01 DOI: 10.3997/2214-4609.202112758
S. Mohammadkhani, D. Olsen, H. Holmslykke, H. Lorentzen, R. Weibel, N. Andrianov, N. Schovsbo
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引用次数: 2
The estimation of permeability using grain size distribution and pore space analysis 利用粒度分布和孔隙空间分析估算渗透率
Pub Date : 1900-01-01 DOI: 10.3997/2214-4609.202112713
R. Masumura, H. Mikada, J. Takekawa, S. Xu
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引用次数: 0
Rock Physics attributes as potential rock-fluid discriminants for carbonate reservoirs in Central Luconia 岩石物理属性是中卢科尼亚碳酸盐岩储层的潜在判别因素
Pub Date : 1900-01-01 DOI: 10.3997/2214-4609.202112743
R. Leite, F. Azuddin, N. Mohsin, M. Z. Kashim, S. Shah, Z. Bakar, A.H. Goodman, M. Rashidi, S. Ali, P. Tiwari
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引用次数: 1
Research and Application of Uphole Constrained Tomographic Static Correction Technology 微井约束层析静校正技术的研究与应用
Pub Date : 1900-01-01 DOI: 10.3997/2214-4609.202112705
S. Zang, X. Wang, J. Wu, Zhang Tao, Y. Yong
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引用次数: 0
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82nd EAGE Annual Conference & Exhibition
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