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Poisson Ratio and Lithology
0.5
Water
0.45
0.4
North Sea
Shale
Clays
0.35
Calcite
North S ea
Chalk
high
porosity
0.3
Brine sand
Halite
0.25
32% Porosity Sand
0.2
0.15
Gas sand
0.1
Quartz
0.05
0
0
5
10
15
20
AI (km/s . g/cm 3 )
Fig. 5.2
Poisson's ratio vs acoustic impedance.
Energy Partitioning at an Interface
Reflected
Compressional
Reflected
Shear
Transmitted
Compressional
Transmitted
Shear
Critical
angle
Angle of
incidence
Critical
angle
Described by the
Zoeppritz
Equations
V p 12 800 ft/s
V s 8000 ft/s
ρ 2.4 g/cm 3
θ
V p 21 000 ft/s
V s 12 000 ft/s
ρ
2.65 g/cm 3
Fig. 5.3 Energy partitioning at an interface, after Dobrin (1976), Introduction to Geophysical
Prospecting , reproduced with permission of the McGraw-Hill Companies.
 
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