A Theory Of Seismic-Wave Propagation In Porous Rocks Çontaining Clays - Interrelation Between Seismic-Wave Attenuation And Permeability

1989 ◽  
Author(s):  
Theo Klimentos
Keyword(s):  
Wave Propagation ◽  
Seismic Wave ◽  
Wave Attenuation ◽  
Seismic Wave Propagation ◽  
Porous Rocks ◽  
Seismic Wave Attenuation

Experimental evidence for the Biot‐Gardner theory

Geophysics ◽  
1989 ◽  
Vol 54 (4) ◽  
pp. 524-527 ◽  
Author(s):  
R. Mörig ◽  
H. Burkhardt
Keyword(s):  
Experimental Evidence ◽  
Seismic Wave ◽  
Seismic Data ◽  
Seismic Waves ◽  
Wave Attenuation ◽  
Wide Spectrum ◽  
Seismic Energy ◽  
Porous Rocks ◽  
Saturation State ◽  
Seismic Wave Attenuation

Seismic wave attenuation has been a subject of interest during the last 40 years because it may be of use in interpreting seismic data. From this attenuation parameter, more detailed information about the lithology of the subsurface may be deduced if we understand the absorption mechanisms by which dissipation of seismic energy is governed. We are, therefore, studying in the laboratory the effects of different parameters such as porosity, permeability, pore fluid, and saturation state on the absorption of seismic waves in porous rocks over a wide spectrum ranging from seismic to ultrasonic frequencies (Burkhardt et al., 1986).

scholarly journals Does wettability influence seismic wave propagation in liquid-saturated porous rocks?

2015 ◽  
Vol 203 (3) ◽  
pp. 2182-2188 ◽  
Author(s):  
Zizhen Wang ◽  
Douglas R. Schmitt ◽  
Ruihe Wang
Keyword(s):  
Wave Propagation ◽  
Seismic Wave ◽  
Seismic Wave Propagation ◽  
Porous Rocks
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