P-wave modulus

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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). Template:ISBN

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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, provided both for 3D materials (first part of the table) and for 2D materials (second part).
3D formulae K= E= λ= G= ν= M= Notes
(K,E) 3K(3K−E)9K−E 3KE9K−E 3K−E6K 3K(3K+E)9K−E
(K,λ) 9K(K−λ)3K−λ 3(K−λ)2 λ3K−λ 3K−2λ
(K,G) 9KG3K+G K−2G3 3K−2G2(3K+G) K+4G3
(K,ν) 3K(1−2ν) 3Kν1+ν 3K(1−2ν)2(1+ν) 3K(1−ν)1+ν
(K,M) 9K(M−K)3K+M 3K−M2 3(M−K)4 3K−M3K+M
(E,λ) E+3λ+R6 E−3λ+R4 2λE+λ+R E−λ+R2 R=E2+9λ2+2Eλ
(E,G) EG3(3G−E) G(E−2G)3G−E E2G−1 G(4G−E)3G−E
(E,ν) E3(1−2ν) Eν(1+ν)(1−2ν) E2(1+ν) E(1−ν)(1+ν)(1−2ν)
(E,M) 3M−E+S6 M−E+S4 3M+E−S8 E−M+S4M S=±E2+9M2−10EM

There are two valid solutions.
The plus sign leads to ν≥0.

The minus sign leads to ν≤0.

(λ,G) λ+2G3 G(3λ+2G)λ+G λ2(λ+G) λ+2G
(λ,ν) λ(1+ν)3ν λ(1+ν)(1−2ν)ν λ(1−2ν)2ν λ(1−ν)ν Cannot be used when ν=0⇔λ=0
(λ,M) M+2λ3 (M−λ)(M+2λ)M+λ M−λ2 λM+λ
(G,ν) 2G(1+ν)3(1−2ν) 2G(1+ν) 2Gν1−2ν 2G(1−ν)1−2ν
(G,M) M−4G3 G(3M−4G)M−G M−2G M−2G2M−2G
(ν,M) M(1+ν)3(1−ν) M(1+ν)(1−2ν)1−ν Mν1−ν M(1−2ν)2(1−ν)
2D formulae K2D= E2D= λ2D= G2D= ν2D= M2D= Notes
(K2D,E2D) 2K2D(2K2D−E2D)4K2D−E2D K2DE2D4K2D−E2D 2K2D−E2D2K2D 4K2D24K2D−E2D
(K2D,λ2D) 4K2D(K2D−λ2D)2K2D−λ2D K2D−λ2D λ2D2K2D−λ2D 2K2D−λ2D
(K2D,G2D) 4K2DG2DK2D+G2D K2D−G2D K2D−G2DK2D+G2D K2D+G2D
(K2D,ν2D) 2K2D(1−ν2D) 2K2Dν2D1+ν2D K2D(1−ν2D)1+ν2D 2K2D1+ν2D
(E2D,G2D) E2DG2D4G2D−E2D 2G2D(E2D−2G2D)4G2D−E2D E2D2G2D−1 4G2D24G2D−E2D
(E2D,ν2D) E2D2(1−ν2D) E2Dν2D(1+ν2D)(1−ν2D) E2D2(1+ν2D) E2D(1+ν2D)(1−ν2D)
(λ2D,G2D) λ2D+G2D 4G2D(λ2D+G2D)λ2D+2G2D λ2Dλ2D+2G2D λ2D+2G2D
(λ2D,ν2D) λ2D(1+ν2D)2ν2D λ2D(1+ν2D)(1−ν2D)ν2D λ2D(1−ν2D)2ν2D λ2Dν2D Cannot be used when ν2D=0⇔λ2D=0
(G2D,ν2D) G2D(1+ν2D)1−ν2D 2G2D(1+ν2D) 2G2Dν2D1−ν2D 2G2D1−ν2D
(G2D,M2D) M2D−G2D 4G2D(M2D−G2D)M2D M2D−2G2D M2D−2G2DM2D




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