Linear Waves in Homogeneous Media

2005 ◽  
pp. 45-53
Author(s):  
Mohamed S. Nasser ◽  
John A. McCorquodale
Keyword(s):  

2016 ◽  
Vol 11 (1) ◽  
pp. 119-126 ◽  
Author(s):  
A.A. Aganin ◽  
N.A. Khismatullina

Numerical investigation of efficiency of UNO- and TVD-modifications of the Godunov method of the second order accuracy for computation of linear waves in an elastic body in comparison with the classical Godunov method is carried out. To this end, one-dimensional cylindrical Riemann problems are considered. It is shown that the both modifications are considerably more accurate in describing radially converging as well as diverging longitudinal and shear waves and contact discontinuities both in one- and two-dimensional problem statements. At that the UNO-modification is more preferable than the TVD-modification because exact implementation of the TVD property in the TVD-modification is reached at the expense of “cutting” solution extrema.


2019 ◽  
Vol 20 (5) ◽  
pp. 1583-1650 ◽  
Author(s):  
Christoph Kehle ◽  
Yakov Shlapentokh-Rothman

2008 ◽  
Vol 55 (4) ◽  
pp. 295-301 ◽  
Author(s):  
J.P. Le Roux
Keyword(s):  

1999 ◽  
Vol 122 (3) ◽  
pp. 222-224 ◽  
Author(s):  
T. H. Dawson

Applicability of extreme-value theory in predicting the maximum crest amplitude in runs of ocean waves is demonstrated using data from extensive computer simulations of random linear waves. Extension of the theory to include wave crests in heavy seas is also made within the context of Stokes nonlinearities. Results are confirmed with scaled laboratory measurements. [S0892-7219(00)00803-7]


Geophysics ◽  
1997 ◽  
Vol 62 (4) ◽  
pp. 1226-1237 ◽  
Author(s):  
Irina Apostoiu‐Marin ◽  
Andreas Ehinger

Prestack depth migration can be used in the velocity model estimation process if one succeeds in interpreting depth events obtained with erroneous velocity models. The interpretational difficulty arises from the fact that migration with erroneous velocity does not yield the geologically correct reflector geometries and that individual migrated images suffer from poor signal‐to‐noise ratio. Moreover, migrated events may be of considerable complexity and thus hard to identify. In this paper, we examine the influence of wrong velocity models on the output of prestack depth migration in the case of straight reflector and point diffractor data in homogeneous media. To avoid obscuring migration results by artifacts (“smiles”), we use a geometrical technique for modeling and migration yielding a point‐to‐point map from time‐domain data to depth‐domain data. We discover that strong deformation of migrated events may occur even in situations of simple structures and small velocity errors. From a kinematical point of view, we compare the results of common‐shot and common‐offset migration. and we find that common‐offset migration with erroneous velocity models yields less severe image distortion than common‐shot migration. However, for any kind of migration, it is important to use the entire cube of migrated data to consistently interpret in the prestack depth‐migrated domain.


Author(s):  
Gyorgy Csaba ◽  
Adam Papp ◽  
Wolfgang Porod ◽  
Ramazan Yeniceri
Keyword(s):  

2015 ◽  
Vol 17 (44) ◽  
pp. 29465-29474 ◽  
Author(s):  
S. Mitzscherling ◽  
Q. Cui ◽  
W. Koopman ◽  
M. Bargheer

A simple two-phase environment model is used to calculate localized plasmon resonances in effective media, beyond the limit of homogeneous media.


Author(s):  
Babita Bisht ◽  
Priyank Bhardwaj ◽  
Manoj Giri ◽  
Sanjay Pant

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