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CONTINUUM MECHANICS for ENGINEERS

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FIGURE 9.8<br />

Applied stress histories: (a) stepped stress; (b) arbitrary stress.<br />

9.5 Superposition Principle, Hereditary Integrals<br />

For linear viscoelasticity, the principle of superposition is valid just as in elasticity.<br />

In the context of stress/strain relationships under discussion here, the<br />

principle asserts that the total strain (stress) resulting from the application<br />

of a sequence of stresses (strains) is equal to the sum of the strains (stresses)<br />

caused by the individual stresses (strains). Thus, <strong>for</strong> the stepped stress history<br />

in simple shear displayed in Figure 9.8a<br />

when applied to a material<br />

having a creep function J(<br />

t)<br />

, the resulting strain will be<br />

( )<br />

2<br />

γ ()= t ∆σ J()+ t ∆σ J( t−t )+ ∆σ J( t−t )= ∆σ<br />

J t−t 12 o 1 1 2 2 ∑ i i<br />

i=<br />

0<br />

(9.5-1)<br />

and by an obvious generalization to the arbitrary stress loading considered<br />

as an infinity of infinitesimal step loadings, Figure 9.8b,<br />

the strain is given by<br />

γ<br />

12<br />

t<br />

⎡dσ12<br />

t′<br />

⎤<br />

()= t J( t− t′<br />

) ⎢ dt<br />

⎣ dt′<br />

⎥ ′ ∫<br />

⎦<br />

−∞<br />

(9.5-2)<br />

which is called a hereditary integral since it expresses the strain at time t as<br />

a function of the entire stress history from time t = – ∞.<br />

If there is an initial<br />

discontinuity in the stress at time t = 0, and if the stress is zero up until that<br />

time (Figure 9.9), the strain becomes<br />

( )

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