Nonlinear Effects, Accompanying Seismic Waves Propagation

1983 ◽  
pp. 391-396
Author(s):  
A. A. Gvozdev ◽  
M. A. Grinfeld ◽  
N. V. Zvolinski
Author(s):  
Gyulnara Voskoboynikova ◽  
Kholmatzhon Imomnazarov ◽  
Aleksander Mikhailov ◽  
Jian-Gang Tang

2015 ◽  
Author(s):  
V.A. Tcheverda ◽  
V.G. Khaidukov ◽  
V.V. Lisitsa ◽  
G.V. Reshetova

Author(s):  
Н.И. Хохлов

Основной задачей, стоящей перед сейсмической разведкой, является восстановление структуры и свойств подповерхностного пространства на основе регистрации колебаний земной поверхности. Для этого необходимо решить обратную задачу, что, в свою очередь, требует решения серии прямых задач с последовательно изменяющейся моделью геологического массива. В связи с открытием нетрадиционных месторождений (например, Баженовская свита), актуальной становится задача интерпретации сейсмического сигнала, обусловленной неоднородной структурой трещиноватых пластов. В настоящей работе была построена трещиноватая модель, отражающая некоторые особенности нефтеносных геологических сред. Проведено численное моделирование распространения сейсмических волн и получены синтетические площадные сейсмограммы. Также был проведен анализ сейсмического отклика. The key objective of seismic exploration is the recreation of the subsoil structure and properties by registering the surface waves. To solve a reverse problem, several direct problems shall be solved as the rock model is gradually changed. As nonconventional deposits are discovered (like the Bazhenov suite), it becomes necessary to interpret the seismic response caused by the heterogeneous structure of the fractured rock. This study presents a fractured rock model that represents some features of oilbearing geology. The seismic waves propagation was simulated, and composed widepatch seismic records were produced. The seismic response was also analyzed.


Geophysics ◽  
1996 ◽  
Vol 61 (6) ◽  
pp. 1935-1938 ◽  
Author(s):  
Ningya Cheng

Elastic nonlinear effects in rocks are observed widely in laboratory experiments. For example, Toksöz et al. (1976) measured the pressure dependence of wave speed in the rocks. In crystalline rock and sandstone, Johnson et al. (1987) and Johnson and Shankland (1989) have demonstrated the nonlinear generation of elastic waves. The importance of nonlinear effects in seismic waves in the earth in regard to models of the source is given in Johnson and McCall (1994). The evolution of the harmonic spectrum of a single frequency wave propagated in Berea Sandstone was shown in Meegan et al. (1993). The structural defects contained in rock, such as microcracks and grain‐to‐grain contacts, give rise to this strong elastic nonlinearity (e.g., Gist, 1994). A new theoretical model is developed in McCall and Guyer (1994) to describe elastic behavior of hysteretic nonlinear materials, such as rock. In general, the third‐order elastic constants of the rocks have much larger values than ordered solids.


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