1-20 OF 720 RESULTS FOR

Frechet derivative

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Journal: Geophysics
Published: 01 October 2018
Geophysics (2018) 83 (6): R581–R595.
...Pan Zhang; Ru-Shan Wu; Liguo Han ABSTRACT Seismic envelope inversion (EI) uses low-frequency envelope data to recover long-wavelength components of the subsurface media. Conventional EI uses the same waveform Fréchet derivative as conventional full-waveform inversion. Due to linearization...
FIGURES
First thumbnail for: Source-independent seismic envelope inversion base...
Second thumbnail for: Source-independent seismic envelope inversion base...
Third thumbnail for: Source-independent seismic envelope inversion base...
Journal Article
Journal: Geophysics
Published: 31 December 2008
Geophysics (2009) 74 (1): E75–E91.
... validated a new inversion method to estimate 2D parametric spatial distributions of electrical resistivity from array-induction measurements acquired in a vertical well. The central component of the method is an efficient approximation to Fréchet derivatives where both the incident and adjoint fields...
FIGURES
First thumbnail for: Fast 2D inversion of large borehole EM induction d...
Second thumbnail for: Fast 2D inversion of large borehole EM induction d...
Third thumbnail for: Fast 2D inversion of large borehole EM induction d...
Journal Article
Journal: Geophysics
Published: 01 January 2001
Geophysics (2001) 66 (5): 1364–1371.
...Tsili Wang; Alberto Mezzatesta Abstract Frechet derivatives provide the vital information for parametric resistivity inversion, but the calculation for a multidimensional problem is often computer intensive. This paper presents a new technique for fast calculation of the Frechet derivatives...
FIGURES
First thumbnail for: Fast <span class="search-highlight">Frechet</span>...
Second thumbnail for: Fast <span class="search-highlight">Frechet</span>...
Third thumbnail for: Fast <span class="search-highlight">Frechet</span>...
Journal Article
Journal: Geophysics
Published: 01 December 1990
Geophysics (1990) 55 (12): 1589–1595.
...David E. Boerner; J. S. Holladay Abstract Frechet derivatives play dual roles in electromagnetic (EM) methods as averaging functions relating conductivity to EM fields and as sensitivity functions relating conductivity perturbations to changes in these fields. For one-dimensional EM inductive...
Journal Article
Journal: Geophysics
Published: 10 April 2009
Geophysics (2009) 74 (3): F31–F43.
...S. A. Greenhalgh; B. Zhou; M. Greenhalgh; L. Marescot; T. Wiese Abstract We have developed explicit expressions for the Fréchet derivatives or sensitivity functions in resistivity imaging of a heterogeneous and fully anisotropic earth. The formulation involves the Green's functions...
FIGURES
First thumbnail for: Explicit expressions for the <span class="search-h...
Second thumbnail for: Explicit expressions for the <span class="search-h...
Third thumbnail for: Explicit expressions for the <span class="search-h...
Journal Article
Journal: Geophysics
Published: 28 September 2009
Geophysics (2009) 74 (5): WB153–WB163.
...Bing Zhou; Stewart Greenhalgh Abstract We present a perturbation method and a matrix method for formulating the explicit Fréchet derivatives for seismic body-wave waveform inversion in 3D general anisotropic, heterogeneous media. Theoretically, the two methods yield the same explicit formula valid...
FIGURES
First thumbnail for: On the computation of the <span class="search-high...
Second thumbnail for: On the computation of the <span class="search-high...
Third thumbnail for: On the computation of the <span class="search-high...
Image
The rms sum of the Fréchet derivative using the (a) TT model (Figure 18a) and (b and c) EAWI-MF-DU final model (Figure 21g). The maximum time window T used in Fréchet derivative calculation is depicted in the text boxes. Higher values indicate better constraint of the velocity model in that location. The Fréchet derivative suggests significantly better constraint of the model in the upper 10 m.
Published: 31 October 2022
Figure 24. The rms sum of the Fréchet derivative using the (a) TT model (Figure  18a ) and (b and c) EAWI-MF-DU final model (Figure  21g ). The maximum time window T used in Fréchet derivative calculation is depicted in the text boxes. Higher values indicate better constraint of the velocity
Image
Longitudinal conductivity Fréchet derivative dG∕dσl variations in the subsurface for an anisotropic model having longitudinal conductivity of 0.1S∕m, transverse conductivity of 0.025S∕m, and strike of the symmetry axis of 0°. The various sensitivity plots are for different dips of the symmetry axis θ0 for 0°, 15°, 45°, 75°, and 90°. The profiles are perpendicular to the strike of the plane of stratification. The electrodes are again at (5,0,0) and (10,0,0).
Published: 10 April 2009
Figure 4. Longitudinal conductivity Fréchet derivative d G ∕ d σ l variations in the subsurface for an anisotropic model having longitudinal conductivity of 0.1 S ∕ m , transverse conductivity of 0.025 S ∕ m , and strike of the symmetry axis of 0°. The various
Image
Fréchet derivative dG∕dσt plots at the surface (z=0) for the same model and electrode configuration as in Figure 6. All patterns are symmetrical about the x-axis. In the case of zero dip, the sensitivity is zero.
Published: 10 April 2009
Figure 7. Fréchet derivative d G ∕ d σ t plots at the surface ( z = 0 ) for the same model and electrode configuration as in Figure 6 . All patterns are symmetrical about the x -axis. In the case of zero dip, the sensitivity is zero.
Image
Fréchet derivative dG∕dσ for an isotropic model having a conductivity of 0.1S∕m. The current source is at (5,0,0) and the potential electrode is at (10,0,0). (a) The cross-sectional view at y=0 and two horizontal depth slices at (b) z=0 and (c) z=0.5 depicting sensitivity variations in plan view are shown. For the z=0.5 depth slice, the electrode positions (white diamonds) have been projected onto this plane.
Published: 10 April 2009
Figure 3. Fréchet derivative d G ∕ d σ for an isotropic model having a conductivity of 0.1 S ∕ m . The current source is at (5,0,0) and the potential electrode is at (10,0,0). (a) The cross-sectional view at y = 0 and two horizontal depth slices at (b) z = 0
Image
Transverse conductivity Fréchet derivative dG∕dσt variations for the same anisotropic model and electrode configuration as in Figure 4. The various sensitivity plots are for differing dips of the symmetry axis, as indicated. The profiles are perpendicular to the strike of the plane of stratification.
Published: 10 April 2009
Figure 6. Transverse conductivity Fréchet derivative d G ∕ d σ t variations for the same anisotropic model and electrode configuration as in Figure 4 . The various sensitivity plots are for differing dips of the symmetry axis, as indicated. The profiles are perpendicular
Image
Fréchet derivative dG∕dσl plots at the surface (z=0) for the same model and electrode configuration as Figure 4. Note the symmetry of the plots and the decrease in sensitivity with increasing dip.
Published: 10 April 2009
Figure 5. Fréchet derivative d G ∕ d σ l plots at the surface ( z = 0 ) for the same model and electrode configuration as Figure 4 . Note the symmetry of the plots and the decrease in sensitivity with increasing dip.
Image
Velocity model for comparing the analytic Fréchet derivative with the numerical Fréchet derivative.
Published: 22 March 2005
Figure 1. Velocity model for comparing the analytic Fréchet derivative with the numerical Fréchet derivative.
Image
Comparison of the analytic and numerical Fréchet derivative of traveltime, where the shot is located at (a) 1.5 km, (b) 2.5 km, and (c) 4.5 km, respectively. FDM = finite-difference method.
Published: 22 March 2005
Figure 2. Comparison of the analytic and numerical Fréchet derivative of traveltime, where the shot is located at (a) 1.5 km, (b) 2.5 km, and (c) 4.5 km, respectively. FDM = finite-difference method.
Image
Comparison of the analytic and numerical Fréchet derivative of amplitude where the shot is located at (a) 1.5 km, (b) 2.5 km, and (c) 4.5 km, respectively. FDM = finite-difference method.
Published: 22 March 2005
Figure 3. Comparison of the analytic and numerical Fréchet derivative of amplitude where the shot is located at (a) 1.5 km, (b) 2.5 km, and (c) 4.5 km, respectively. FDM = finite-difference method.
Image
The 3-D sensitivity function (Frechét derivative) of normalised apparent resistivity for the pole-pole array with a pole-pole distance of 1 m presented as horisontal depth slices at z = 0.01, 0.25, 0.5, 0.75, 1.0, and 1.5 m. The electrodes are located at (−0.5, 0, 0) m and (0.5, 0, 0) m. Each slice is shown as a surface plot and a contoured picture. The same logarithmic scale with three intervals per decade is used in the contouring of all slices, but the vertical axis in the surface plots is changed as the maximum of the Frechét derivative decreases rapidly with depth. All distances are in meters. Figure from Møller (1996).
Published: 01 January 2002
F IG . 12. The 3-D sensitivity function (Frechét derivative) of normalised apparent resistivity for the pole-pole array with a pole-pole distance of 1 m presented as horisontal depth slices at z = 0.01, 0.25, 0.5, 0.75, 1.0, and 1.5 m. The electrodes are located at (−0.5, 0, 0) m and (0.5, 0, 0
Image
2-D form of the Fréchet derivative for an electrode configuration with current and potential electrodes placed at x = −15 m (A), x = 15 m (B), x = −25 m (M), and x = 45 m (N) (configuration s6 in Figure 4). Light gray indicates negative values; dark gray, positive values. Contour intervals are −0.010, −0.003, −0.001, 0, 0.001, 0.003, 0.010.
Published: 01 January 2001
F IG . 2. 2-D form of the Fréchet derivative for an electrode configuration with current and potential electrodes placed at x = −15 m ( A ), x = 15 m ( B ), x = −25 m ( M ), and x = 45 m ( N ) (configuration s6 in Figure 4 ). Light gray indicates negative values; dark gray, positive
Image
The Frechet derivatives with respect to Rxo in the layer between 60.96 and 63.40 m. The first track shows the model resistivity variations in depth. The shaded area in the second track shows the location of the invasion zone for which the Frechet derivatives are shown. The third to fifth tracks show the Frechet derivatives of the potential (V4, VA, and VG), the first potential difference (F23, F56, and FFG), and the second potential difference (S234, S789, and SEFG) data, respectively. The solid lines show the results calculated by the ASAM, and the shaded lines show the results calculated by the PPM with 5% perturbation.
Published: 01 January 2001
F IG . 4. The Frechet derivatives with respect to R xo in the layer between 60.96 and 63.40 m. The first track shows the model resistivity variations in depth. The shaded area in the second track shows the location of the invasion zone for which the Frechet derivatives are shown. The third
Journal Article
Journal: Geophysics
Published: 22 March 2005
Geophysics (2005) 70 (2): U1–U7.
...Figure 1. Velocity model for comparing the analytic Fréchet derivative with the numerical Fréchet derivative. ...
FIGURES
First thumbnail for: Refraction traveltime tomography using damped mono...
Second thumbnail for: Refraction traveltime tomography using damped mono...
Third thumbnail for: Refraction traveltime tomography using damped mono...
Image
Fréchet derivatives computed from the Green’s functions in Figure 8.
Published: 19 April 2016
Figure 9. Fréchet derivatives computed from the Green’s functions in Figure  8 .