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Journal Article
Seismic depth migration with the Dirac equation
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 01 June 1999
Geophysics (1999) 64 (3): 925–933.
...Ketil Hokstad; Rune Mittet Abstract We demonstrate the applicability of the Dirac equation in seismic wavefield extrapolation by presenting a new explicit one-way prestack depth migration scheme. The method is in principle accurate up to 90 degrees from the vertical, and it tolerates lateral...
Journal Article
Solving the nonlinear Riccati equation for the 1D plane-wave reflection response from a velocity gradient interface by a Heun to hypergeometric reduction
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 22 August 2022
Geophysics (2023) 88 (1): WA1–WA12.
... of the wavefield at that depth. In the case that the model is a velocity gradient interface expressed in terms of a smooth Heaviside function defined by the Fermi-Dirac function, the Riccati equation is shown to have an analytical solution for the reflection response. The solution accounts for all wave phenomena...
Journal Article
Challenges of complex media
Journal: The Leading Edge
Publisher: Society of Exploration Geophysicists
Published: 01 June 2002
The Leading Edge (2002) 21 (6): 587–592.
... migration with the Dirac equation” by Hokstad and Millet (G eophysics , 1999). “Optimum seismic illumination of hydrocarbon reservoirs” by Rietveld et al. (G eophysics , 1992). “Velocity estimation and downward-continuation by wavefront synthesis” by Schultz and Claerbout (G eophysics , 1978). For further...
Book: Basic Wave Analysis
Series: Geophysical Monograph Series
Publisher: Society of Exploration Geophysicists
Published: 24 August 2020
DOI: 10.1190/1.9781560803737.ch9
EISBN: 978-1-56080-373-7
... and later a visiting-turned-permanent Professor at Florida State University, he was considered to be precise and taciturn; it was said that his colleagues in Cambridge jokingly defined a unit called a “dirac,” which represented one word per hour. He was known for formulating the Dirac equation, which...
The Dirac delta function δ( t ) and the Heaviside unit step function θ( t ) are known as singularity functions. By definition, a stable function has finite energy. A stable time function h ( t ) and a stable space function g ( x ) have well-defined Fourier transforms, designated by H (ω) and G ( k ), respectively. However, the study of wave propagation involves functions that are not stable. For example, the function sin k 0 x does not have finite energy, so it is not stable. The Fourier transforms of such unstable functions are not well defined. Thus, in wave propagation, we must consider using quantities that involve a certain kind of infinity.
Journal Article
Time-domain behavior of wide-angle one-way wave equations
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 01 March 1991
Geophysics (1991) 56 (3): 382–384.
...A. H. Kamel Abstract The constant-coefficient inhomogeneous wave equation reads (1) ∂ 2 u ( x , z , t ) ∂ x 2 + ∂ 2 u ( x , z , t ) ∂ z 2 − 1 c 2 ∂ 2 u ( x , z , t ) ∂ t 2 = − δ ( t ) δ ( r ) , where t is the time; x , z are Cartesian coordinates; c is the sound speed; and δ(.) is the Dirac delta...
Image
Solution of the convection–dispersion equation assuming solute-free input t...
Published: 01 November 2006
Fig. 11. Solution of the convection–dispersion equation assuming solute-free input to a soil having a Dirac delta initial distribution at x = 5 cm; λ = dispersivity, D i = effective ionic diffusion coefficient, v = pore water velocity.
Journal Article
Adaptive traveltime inversion
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 20 June 2019
Geophysics (2019) 84 (4): U13–U29.
... and forces it to be a Dirac delta function. Unlike the crosscorrelation function of equation 2 for WTI, equation 9 of ATI does not crosscorrelate the predicted and measured data directly, which has the potential drawback of focusing on events with high amplitude. ATI uses crosscorrelation to measure...
Journal Article
Wave-equation-based image warping
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 08 October 2015
Geophysics (2016) 81 (1): V1–V6.
... p in equation 4 denotes that it is now considered as a dual-component complex vector in a quantum mechanical context defined as a spinor . To relate the observed image wavefield to the spinor space, the wavefield is projected onto the eigenspace of the Dirac operator: p = K [ p...
Image
A schematic showing the way the various parts of the Fractional MacroEvolut...
in The Fractional MacroEvolution Model: a simple quantitative scaling macroevolution model
> Paleobiology
Published: 01 May 2024
+ ), However, deterministic forcings such as bolide impacts are also discussed, shown here with both T and E + forced with a Dirac function of amplitude f 0,T , f 0,E+ , respectively. More general forcings can be used and their responses can be obtained using the impulse response functions. The middle
Book Chapter
Appendix A
Series: SEPM Special Publication
Publisher: SEPM Society for Sedimentary Geology
Published: 01 January 2009
EISBN: 9781565762008
... by keeping only n = 0 in the former sum Equation A5. Because is a sharply decreasing function for usual values of h 0 and v ( Table 1 ) we have that t – t ’ is less than 10 2 –10 4 s, a few hours. Therefore we can approximate also the exponential function as a Dirac delta function δ ( ξ – ρ...
Journal Article
The application of an optimal transport to a preconditioned data matching function for robust waveform inversion
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 28 October 2019
Geophysics (2019) 84 (6): R923–R945.
... use equation 13 to compute a band-limited Dirac delta function. The results of the proposed misfit function, AWI, and the l 2 -norm approaches are shown in Figure 18 . The reconstructed models shown in Figure 18a recover most of the details of the true model (Figure 15a ). The edges...
Journal Article
A robust waveform inversion using a global comparison of modeled and observed data
Journal: The Leading Edge
Publisher: Society of Exploration Geophysicists
Published: 01 March 2019
The Leading Edge (2019) 38 (3): 185–192.
... function insensitive to the amplitude of the matching filter, and thus, avoids the problem faced by the conventional matching-filter misfit function of equation 3 . When the model parameters are accurate, the resulting matching filter reduces to a Dirac delta function or a band-limited version...
Journal Article
Synergies in geophysical, medical, and space imaging
Journal: The Leading Edge
Publisher: Society of Exploration Geophysicists
Published: 01 June 2002
The Leading Edge (2002) 21 (6): 576–577.
... applications of wave equation prestack depth migration, Chengbin Peng Imaging with the Dirac equation in the presence of large lateral velocity variations, Anatoly Baumstein, John Anderson, and Tom Dickens Wavefield migration of 3D prestack data, Bertrand Duquet, Andreas Ehinger, P. Lailly, and B...
Journal Article
Robust source-independent elastic full-waveform inversion in the time domain
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 03 March 2016
Geophysics (2016) 81 (2): R29–R44.
... to Gaussian and spike noises, even for a Dirac wavelet. Finally, we applied our method to real seismic data. The similarity between the observed and modeled seismic data, the higher resolution of the migration image, and flatter common image gathers corresponding to the inverted models proved the relevance...
Journal Article
A new insight into the reciprocity principle
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 01 January 2000
Geophysics (2000) 65 (5): 1604–1612.
... experiments for single forces. The body forces are positioned at x 0 and x ' 0 . Also g x = g z = δ ( x - x 0 ) while g' x = g' z = δ ( x - x ' 0 ), where δ is Dirac's delta function. This equation reveals a fundamental symmetry of the wavefield in a viscoelastic medium: in any given...
Journal Article
3D ray+Born migration/inversion—Part 1: Theory
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 01 January 2003
Geophysics (2003) 68 (4): 1348–1356.
... are oriented. Jin et al. (1992) recognized the analogy between the Fourier integral expression of the Dirac function, (8) and the asymptotic approximation of the Hessian [equation ( 5 )]. The Hessian involves an oscillatory integral whose stationary points are on the diagonal. One can keep...
Journal Article
Tutorial on New Developments in the Physics of Rotational Motions
Publisher: Seismological Society of America
Published: 01 May 2009
Bulletin of the Seismological Society of America (2009) 99 (2B): 1028–1039.
... by the external 4D antisymmetric tensor (20) defined similarly to equation (8) with the help of the Dirac tensors and the following scalars: Equation (18b) for the symmetric deviatoric strain tensor is equivalent to that for the antisymmetric twist tensor (equation 19 ); the latter helps us...
Journal Article
Direct Fourier migration for vertical velocity variations
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 01 January 2001
Geophysics (2001) 66 (5): 1504–1514.
... length are assumed, this is exactly true and is demonstrated in the Appendix . The key part of the proof is to realize that M ( k x , ξ , ω ) [as given by equation ( 18 )] is actually a Dirac delta function: (20) Insertion of this result in equation ( 17 ) collapses the integration and forces...
Journal Article
Time-domain full-waveform inversion of exponentially damped wavefield using the deconvolution-based objective function
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 10 January 2018
Geophysics (2018) 83 (2): R77–R88.
... a Dirac delta function even when the modeled data are very close to the observed data. On the other hand, the deconvolution filter of equation 3 should admit a Dirac delta function when the modeled data are close to the observed data. As the threshold becomes larger, the discontinuity in equation 3...
Journal Article
Calculation of electrical potentials along a longitudinal section of a 2-D terrain
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 01 January 2002
Geophysics (2002) 67 (2): 511–516.
... A against domain Ω, and δ 3 ( A ) is a 3-D Dirac delta function centered at A . For a 2-D terrain, applying Fourier transformation (3) to the left sides of equations ( 9 ) and ( 10 ), we have (11) and (12) where is the 2-D Laplacian. Because (13) and (14) where δ ( A ) is a 2-D...
1