Physics:P-wave modulus

From HandWiki

There are two kinds of seismic body waves in solids, pressure waves (P-waves) and shear waves. In linear elasticity, the P-wave modulus M, also known as the longitudinal modulus, or the constrained modulus, is one of the elastic moduli available to describe isotropic homogeneous materials. It is defined as the ratio of axial stress to axial strain in a uniaxial strain state. This occurs when expansion in the transverse direction is prevented by the inertia of neighboring material, such as in an earthquake, or underwater seismic blast.

σzz=Mϵzz

where all the other strains ϵ** are zero.

This is equivalent to stating that

Mx=ρxVP2,

where VP is the velocity of a P-wave and ρ is the density of the material through which the wave is propagating.


References

  • G. Mavko, T. Mukerji, J. Dvorkin. The Rock Physics Handbook. Cambridge University Press 2003 (paperback). ISBN:0-521-54344-4
Conversion formulae
Homogeneous isotropic linear elastic materials have their elastic properties uniquely determined by any two moduli among these; thus, given any two, any other of the elastic moduli can be calculated according to these formulas.
K= E= λ= G= ν= M= Notes
(K,E) 3K(3KE)9KE 3KE9KE 3KE6K 3K(3K+E)9KE
(K,λ) 9K(Kλ)3Kλ 3(Kλ)2 λ3Kλ 3K2λ
(K,G) 9KG3K+G K2G3 3K2G2(3K+G) K+4G3
(K,ν) 3K(12ν) 3Kν1+ν 3K(12ν)2(1+ν) 3K(1ν)1+ν
(K,M) 9K(MK)3K+M 3KM2 3(MK)4 3KM3K+M
(E,λ) E+3λ+R6 E3λ+R4 2λE+λ+R Eλ+R2 R=E2+9λ2+2Eλ
(E,G) EG3(3GE) G(E2G)3GE E2G1 G(4GE)3GE
(E,ν) E3(12ν) Eν(1+ν)(12ν) E2(1+ν) E(1ν)(1+ν)(12ν)
(E,M) 3ME+S6 ME+S4 3M+ES8 EM+S4M S=±E2+9M210EM

There are two valid solutions.
The plus sign leads to ν0.

The minus sign leads to ν0.

(λ,G) λ+2G3 G(3λ+2G)λ+G λ2(λ+G) λ+2G
(λ,ν) λ(1+ν)3ν λ(1+ν)(12ν)ν λ(12ν)2ν λ(1ν)ν Cannot be used when ν=0λ=0
(λ,M) M+2λ3 (Mλ)(M+2λ)M+λ Mλ2 λM+λ
(G,ν) 2G(1+ν)3(12ν) 2G(1+ν) 2Gν12ν 2G(1ν)12ν
(G,M) M4G3 G(3M4G)MG M2G M2G2M2G
(ν,M) M(1+ν)3(1ν) M(1+ν)(12ν)1ν Mν1ν M(12ν)2(1ν)