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- homogeneous earth, then iteratively remove the responses of by cash flow than by the amount20 KB (3,148 words) - 11:09, 18 October 2016
- ...ismic amplitudes. By mapping changes in fluid saturation, changes in fluid flow directions may also be inferred and used for planning of production wells. ...er|7.0-4}} A subsurface model consisting of a dipping plane interface in a homogeneous medium. Line ''A'' is in the dip direction, line ''B'' is in the strike dir279 KB (43,590 words) - 09:31, 29 August 2014
- ...is applied to model shot profiles recorded over a water layer on top of a homogeneous elastic half space. Raypaths corresponding to multiple reflections, direct [[file:ch06_figF-6.png|thumb|{{figure number|F-6}} Processing flow for inversion of refraction profiles.]]70 KB (10,953 words) - 15:05, 9 October 2014
- ...ased on fitting a hyperbola to CMP traveltimes associated with a laterally homogeneous earth model. If there are [[lateral velocity variations]] in layers above t ...ed into a reservoir simulation scheme to predict the geometry of the fluid flow from the given reservoir parameters.278 KB (43,816 words) - 14:40, 10 September 2014
- ...a, Lumley, D. E., 1995a, Seismic time-lapse monitoring of subsurface fluid flow: Ph. D. thesis, Stanford University.</ref>,<ref name=ch11r56>Lumley, 1995b, # Determining flow properties of sealing or leaking faults, and395 KB (60,721 words) - 14:42, 10 September 2014
- ...p>4</sup> terms to specify the stress strain relationship for an arbitrary homogeneous material. Conservation of angular momentum requires the stress tensor to b It is important to note that these velocities assume a homogeneous, isotropic, perfectly elastic material. All energy associated with deformat39 KB (5,997 words) - 14:03, 11 September 2020
- [[File:Resistance.png|thumbnail|center|Current flow I through a piece of conductive material over which a potential difference ...tential difference [V] imposed over a closed loop and the magnitude of its flow depends on the resistance of the loop's material. For most materials, inclu7 KB (1,086 words) - 19:10, 23 February 2017
- ''ka << 0.01 (quasi-homogeneous medium)'' - no significant scattering;<br /> ...dstone shows greater attenuation despite the fact that a macroscopic fluid flow is compromised.5 KB (741 words) - 15:19, 19 March 2018
- ...ial balance equation (MBE) methods are used to calculate if a reservoir is homogeneous and to predict its production behavior by providing values of its propertie === '''Flow Model''' ===11 KB (1,519 words) - 07:50, 17 May 2021
- ...edev. "Seismic wave attenuation and dispersion resulting from wave-induced flow in porous rocks—A review." Geophysics 75, no. 5 (2010): 75A147-75A164.</r ...Berryman, and Jerry M. Harris. "Seismic attenuation due to wave‐induced flow." Journal of Geophysical Research: Solid Earth 109, no. B1 (2004).</ref>.12 KB (1,739 words) - 13:27, 21 August 2018
- ...ray to be the unattainable limit on the narrowness of such a beam. Within homogeneous isotropic materials, a ray is a straight line because, by symmetry, there i ...arrive at <math>S^{'}</math> in the same time <math>t^{'}</math>. Within a homogeneous isotropic medium, the velocity of propagation is identical in all direction14 KB (2,173 words) - 14:39, 30 April 2021
- ...us (i.e., consisting of points all of the same kind) or inhomogeneous (not homogeneous). In an isotropic medium, rays constitute orthogonal trajectories of the wa ...<math>\Delta t</math>. This is true even if the wavefronts travel from one homogeneous isotropic medium into another, and it simply means that every point on <mat5 KB (675 words) - 13:26, 22 April 2021
- ...us (i.e., consisting of points all of the same kind) or inhomogeneous (not homogeneous). In an isotropic medium, rays constitute orthogonal trajectories of the wa ...<math>\Delta t</math>. This is true even if the wavefronts travel from one homogeneous isotropic medium into another, and it simply means that every point on <mat5 KB (699 words) - 13:26, 22 April 2021
- ...us (i.e., consisting of points all of the same kind) or inhomogeneous (not homogeneous). In an isotropic medium, rays constitute orthogonal trajectories of the wa ...<math>\Delta t</math>. This is true even if the wavefronts travel from one homogeneous isotropic medium into another, and it simply means that every point on <mat5 KB (687 words) - 07:47, 7 May 2021
- ...ray to be the unattainable limit on the narrowness of such a beam. Within homogeneous isotropic materials, a ray is a straight line because, by symmetry, there i968 bytes (173 words) - 14:39, 30 April 2021
- ...ray to be the unattainable limit on the narrowness of such a beam. Within homogeneous isotropic materials, a ray is a straight line because, by symmetry, there i ...arrive at <math>S^{'}</math> in the same time <math>t^{'}</math>. Within a homogeneous isotropic medium, the velocity of propagation is identical in all direction13 KB (2,128 words) - 15:16, 19 May 2021
- ...ray to be the unattainable limit on the narrowness of such a beam. Within homogeneous isotropic materials, a ray is a straight line because, by symmetry, there i ...arrive at <math>S^{'}</math> in the same time <math>t^{'}</math>. Within a homogeneous isotropic medium, the velocity of propagation is identical in all direction14 KB (2,113 words) - 14:40, 30 April 2021