Shear modulus

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Shear modulus
Common symbols
G, S, μ
SI unitPa
Derivations from
other quantities
G = τ / γ = E / [2(1 + ν)]
Shear strain

In solid mechanics, the shear modulus or modulus of rigidity, denoted by G, or sometimes S or μ, is a measure of the elastic shear stiffness of a material and is defined as the ratio of shear stress to the shear strain:[1]

G =def τxyγxy=F/AΔx/l=FlAΔx

where

τxy=F/A = shear stress
F is the force which acts
A is the area on which the force acts
γxy = shear strain. In engineering :=Δx/l=tanθ, elsewhere :=θ
Δx is the transverse displacement
l is the initial length of the area.

The derived SI unit of shear modulus is the pascal (Pa), although it is usually expressed in gigapascals (GPa) or in thousand pounds per square inch (ksi). Its dimensional form is M1L−1T−2, replacing force by mass times acceleration.

Explanation

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Material Typical values for
shear modulus (GPa)
(at room temperature)
Diamond[2] 478.0
Steel[3] 79.3
Iron[4] 52.5
Copper[5] 44.7
Titanium[3] 41.4
Glass[3] 26.2
Aluminium[3] 25.5
Polyethylene[3] 0.117
Rubber[6] 0.0006
Granite[7][8] 24
Shale[7][8] 1.6
Limestone[7][8] 24
Chalk[7][8] 3.2
Sandstone[7][8] 0.4
Wood 4

The shear modulus is one of several quantities for measuring the stiffness of materials. All of them arise in the generalized Hooke's law:

  • Young's modulus E describes the material's strain response to uniaxial stress in the direction of this stress (like pulling on the ends of a wire or putting a weight on top of a column, with the wire getting longer and the column losing height),
  • the Poisson's ratio ν describes the response in the directions orthogonal to this uniaxial stress (the wire getting thinner and the column thicker),
  • the bulk modulus K describes the material's response to (uniform) hydrostatic pressure (like the pressure at the bottom of the ocean or a deep swimming pool),
  • the shear modulus G describes the material's response to shear stress (like cutting it with dull scissors).

These moduli are not independent, and for isotropic materials they are connected via the equations[9]

E=2G(1+ν)=3K(12ν)

The shear modulus is concerned with the deformation of a solid when it experiences a force perpendicular to one of its surfaces while its opposite face experiences an opposing force (such as friction). In the case of an object shaped like a rectangular prism, it will deform into a parallelepiped. Anisotropic materials such as wood, paper and also essentially all single crystals exhibit differing material response to stress or strain when tested in different directions. In this case, one may need to use the full tensor-expression of the elastic constants, rather than a single scalar value.

One possible definition of a fluid would be a material with zero shear modulus.

Shear waves

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File:SpiderGraph ShearModulus.GIF
Influences of selected glass component additions on the shear modulus of a specific base glass.[10]

In homogeneous and isotropic solids, there are two kinds of waves, pressure waves and shear waves. The velocity of a shear wave, (vs) is controlled by the shear modulus,

vs=Gρ

where

G is the shear modulus
ρ is the solid's density.

Shear modulus of metals

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Shear modulus of copper as a function of temperature. The experimental data[11][12] are shown with colored symbols.

The shear modulus of metals is usually observed to decrease with increasing temperature. At high pressures, the shear modulus also appears to increase with the applied pressure. Correlations between the melting temperature, vacancy formation energy, and the shear modulus have been observed in many metals.[13]

Several models exist that attempt to predict the shear modulus of metals (and possibly that of alloys). Shear modulus models that have been used in plastic flow computations include:

  1. the Varshni-Chen-Gray model developed by[14] and used in conjunction with the Mechanical Threshold Stress (MTS) plastic flow stress model.[15][16]
  2. the Steinberg-Cochran-Guinan (SCG) shear modulus model developed by[17] and used in conjunction with the Steinberg-Cochran-Guinan-Lund (SCGL) flow stress model.
  3. the Nadal and LePoac (NP) shear modulus model[12] that uses Lindemann theory to determine the temperature dependence and the SCG model for pressure dependence of the shear modulus.

Varshni-Chen-Gray model

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The Varshni-Chen-Gray model (sometimes referred to as the Varshni equation) has the form:

μ(T)=μ0Dexp(T0/T)1

where μ0 is the shear modulus at T=0K, and D and T0 are material constants.

SCG model

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The Steinberg-Cochran-Guinan (SCG) shear modulus model is pressure dependent and has the form

μ(p,T)=μ0+μppη13+μT(T300);η:=ρρ0

where, μ0 is the shear modulus at the reference state (T = 300 K, p = 0, η = 1), p is the pressure, and T is the temperature.

NP model

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The Nadal-Le Poac (NP) shear modulus model is a modified version of the SCG model. The empirical temperature dependence of the shear modulus in the SCG model is replaced with an equation based on Lindemann melting theory. The NP shear modulus model has the form:

μ(p,T)=1𝒥(T^)[(μ0+μppη13)(1T^)+ρCmT];C:=(6π2)233f2

where

𝒥(T^):=1+exp[1+1/ζ1+ζ/(1T^)]forT^:=TTm[0,6+ζ],

and μ0 is the shear modulus at absolute zero and ambient pressure, ζ is an area, m is the atomic mass, and f is the Lindemann constant.

Shear relaxation modulus

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The shear relaxation modulus G(t) is the time-dependent generalization of the shear modulus[18] G:

G=limtG(t).

See also

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References

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  1. ^ IUPAC, Compendium of Chemical Terminology, 5th ed. (the "Gold Book") (2025). Online version: (2006–) "shear modulus, G". Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  2. ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  3. ^ a b c d e Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  4. ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  5. ^ Material properties
  6. ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  7. ^ a b c d e Hoek, Evert, and Jonathan D. Bray. Rock slope engineering. CRC Press, 1981.
  8. ^ a b c d e Pariseau, William G. Design analysis in rock mechanics. CRC Press, 2017.
  9. ^ [Landau LD, Lifshitz EM. Theory of Elasticity, vol. 7. Course of Theoretical Physics. (2nd Ed) Pergamon: Oxford 1970 p13]
  10. ^ Shear modulus calculation of glasses
  11. ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  12. ^ a b Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  13. ^ March, N. H., (1996), Electron Correlation in Molecules and Condensed Phases, Springer, Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value). p. 363
  14. ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  15. ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  16. ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  17. ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  18. ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
Homogeneous isotropic linear elastic materials have their elastic properties uniquely determined by any two quantities 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
Knowns Bulk modulus (K) Young's modulus (E) Lamé's first parameter (λ) Shear modulus (G) Poisson's ratio (ν) P-wave modulus (M) Notes
(K, E) 3KE/3 − E/3K E/3 − E/3K 1/2E/6K 3K + E/3 − E/3K
(K, λ) 9K(K − λ)/3K − λ 3(K − λ)/2 λ/3K − λ 3K − 2λ
(K, G) 9KG/3K + G K2G/3 3K − 2G/6K + 2G K + 4G/3
(K, ν) 3K(1 − 2ν) 3/1 + ν 3K(1 − 2ν)/2(1 + ν) 3K(1 − ν)/1 + ν
(K, M) 9K(MK)/3K + M 3KM/2 3(MK)/4 3KM/3K + M
(E, λ) E + 3λ + R/6 E − 3λ + R/4 E + R/1/4 E − λ + R/2 R = ±(E2 + 9λ2 + 2Eλ)1/2
(E, G) EG/3(3GE) G(E − 2G)/3GE E/2G − 1 G(4GE)/3GE
(E, ν) E/3 − 6ν /(1 + ν)(1 − 2ν) E/2(1 + ν) E(1 − ν)/(1 + ν)(1 − 2ν)
(E, M) 3ME + S/6 ME + S/4 3M + ES/8 E + S/4M1/4 S = ±(E2 + 9M2 − 10EM)1/2
(λ, G) λ + 2G/3 G(3λ + 2G)/λ + G λ/2(λ + G) λ + 2G
(λ, ν) λ/3(1 + 1/v) λ(1/ν − 2ν − 1) λ(1/2ν − 1) λ(1/ν − 1)
(λ, M) M + 2λ/3 (M − λ)(M+2λ)/M + λ M − λ/2 λ/M + λ
(G, ν) 2G(1 + ν)/3 − 6ν 2G(1 + ν) 2 G ν/1 − 2ν 2G(1 − ν)/1 − 2ν
(G, M) M4G/3 G(3M − 4G)/MG M − 2G M − 2G/2M − 2G
(ν, M) M(1 + ν)/3(1 − ν) M(1 + ν)(1 − 2ν)/1 − ν M ν/1 − ν M(1 − 2ν)/2(1 − ν)
2D Formulae
Knowns (K) (E) (λ) (G) (ν) (M) Notes
(K2D, E2D) 2K2D(2K2DE2D)/4K2DE2D K2DE2D/4K2DE2D 2K2DE2D/2K2D 4K2D^2/4K2DE2D
(K2D, λ2D) 4K2D(K2D − λ2D)/2K2D − λ2D K2D − λ2D λ2D/2K2D − λ2D 2K2D − λ2D
(K2D, G2D) 4K2DG2D/K2D + G2D K2DG2D K2DG2D/K2D + G2D K2D + G2D
(K2D, ν2D) 2K2D(1 − ν2D) 2K2Dν2D/1 + ν2D K2D(1 − ν2D)/1 + ν2D 2K2D/1 + ν2D
(E2D, G2D) E2DG2D/4G2DE2D 2G2D(E2D − 2G2D)/4G2DE2D E2D/2G2D − 1 4G2D^2/4G2DE2D
(E2D, ν2D) E2D/2(1 − ν2D) E2Dν2D/(1 + ν2D)(1 − ν2D) E2D/2(1 + ν2D) E2D/(1 + ν2D)(1 − ν2D)
2D, G2D) λ2D + G2D 4G2D2D + G2D)/λ2D + 2G2D λ2D/λ2D + 2G2D λ2D + 2G2D
2D, ν2D) λ2D(1 + ν2D)/2ν2D λ2D(1 + ν2D)(1 − ν2D)/ν2D λ2D(1 − ν2D)/2ν2D λ2D/ν2D
(G2D, ν2D) G2D(1 + ν2D)/1 − ν2D 2G2D(1 + ν2D) 2 G2D ν2D/1 − ν2D 2G2D/1 − ν2D
(G2D, M2D) M2DG2D 4G2D(M2DG2D)/M2D M2D − 2G2D M2D − 2G2D/M2D

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