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Introduction to Acoustics

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34 Part A Propagation of Sound<br />

Part A 3.2<br />

initially a small box (∆x by ∆y by ∆z)is<br />

δ[Work]= �<br />

� �<br />

∂<br />

σii δξi ∆x∆y∆z<br />

∂xi<br />

i<br />

+ �<br />

� �<br />

∂<br />

σij δξi ∆x∆y∆z , (3.58)<br />

∂x j<br />

i�= j<br />

where here σij is interpreted as the i-th component of the<br />

force per unit area on a surface whose outward normal<br />

is in the direction of increasing x j. With use of the<br />

symmetry of the stress tensor and of the definition of the<br />

strain tensor components, one obtains the incremental<br />

strain energy per unit volume as<br />

δÍ = �<br />

σijδɛij . (3.59)<br />

ij<br />

If the reference state, where Í = 0, is taken as that in<br />

which the strain is zero, and given that each stress component<br />

is a linear combination of the strain components,<br />

then the above integrates <strong>to</strong><br />

Í = �<br />

ij<br />

1<br />

2 σijɛij . (3.60)<br />

Here the stresses are unders<strong>to</strong>od <strong>to</strong> be given in terms of<br />

the strains by an appropriate stress–strain relation of the<br />

general form of (3.57).<br />

Because of the symmetry of both the stress tensor<br />

and the strain tensor, the internal energy Í per unit<br />

can be regarded as a function of only the six distinct<br />

strain components: ɛxx, ɛyy, ɛzz, ɛxy, ɛyz, andɛxz. Consequently,<br />

with such an understanding, it follows from<br />

the differential relation (3.59)that<br />

∂Í<br />

= σxx ;<br />

∂ɛxx<br />

∂Í<br />

∂ɛxy<br />

= 2σxy , (3.61)<br />

with analogous relations for derivatives with respect <strong>to</strong><br />

the other distinct strain components.<br />

Isotropic Solids<br />

If the properties of the solid are such that they are<br />

independent of the orientation of the axes of the Cartesian<br />

coordinate system, then the solid is said <strong>to</strong> be<br />

isotropic. This idealization is usually regarded as good<br />

if the solid is made up of a random assemblage of<br />

many small grains. The tiny grains are possibly crystalline<br />

with directional properties, but the orientation<br />

of the grains is random, so that an element composed<br />

of a large number of grains has no directional orientation.<br />

For such an isotropic solid the number of<br />

y<br />

x<br />

�(x)<br />

x+ �(x)<br />

Fig. 3.5 Displacement field vec<strong>to</strong>r ξ in a solid. A material<br />

point normally at x is displaced <strong>to</strong> x + ξ(x)<br />

different coefficients in the stress–strain relation (3.57)<br />

is only two, and the relation can be taken in the general<br />

form<br />

σij = 2µLɛij + λLδij<br />

3�<br />

ɛkk . (3.62)<br />

k=1<br />

This involves two material constants, termed the<br />

Lamè constants, and here denoted by λL and µL<br />

(the latter being the same as the shear modulus<br />

G).<br />

Equivalently, one can express the strain components<br />

in terms of the stress components by the inverse of the<br />

above set of relations. The generic form is sometimes<br />

written<br />

ɛij =<br />

1 + ν<br />

E σij − ν<br />

E<br />

�<br />

σkkδij , (3.63)<br />

k<br />

where E is the elastic modulus and ν is Poisson’s ratio.<br />

The relation of these two constants <strong>to</strong> the Lamè constants<br />

is such that<br />

νE<br />

,<br />

(1 + ν)(1 − 2ν)<br />

(3.64)<br />

E<br />

µL = G = .<br />

2(1 + ν)<br />

(3.65)<br />

λL =<br />

In undergraduate texts on the mechanics of materials,<br />

the relations (3.63) are often written out separately<br />

for the diagonal and off-diagonal strain elements, so<br />

x

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