A Brief Review of Elasticity and Viscoelasticity for Solids 1 Introduction
A Brief Review of Elasticity and Viscoelasticity for Solids 1 Introduction
A Brief Review of Elasticity and Viscoelasticity for Solids 1 Introduction
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46 H. T. Banks, S. H. Hu <strong>and</strong> Z. R. Kenz / Adv. Appl. Math. Mech., 3 (2011), pp. 1-51<br />
the modulus increases, we see that the wave begins its upward slope sooner, meaning<br />
the wave has arrived at the observation point sooner so wave speed has increased.<br />
Also, as the modulus increases, we see less displacement overall. In the case where<br />
density increases, we see that we also get less displacement overall, but the wave<br />
speed decreases. We clearly see the model demonstrates that soil parameters have<br />
multiple realistic effects on overall displacement <strong>and</strong> wave speed.<br />
In Fig. 23, we examine the situation where we increase both soil parameters. As expected,<br />
the effects <strong>of</strong> the parameter increases combine to reduce overall displacement.<br />
In the left pane <strong>of</strong> the figure, we see that the elastic modulus increases more rapidly<br />
than the density <strong>and</strong> the wave reaches the observation point sooner. In the right pane,<br />
we applied the same percentage increases to the parameters <strong>and</strong> so the wave reaches<br />
the observation point at the same time <strong>for</strong> all the parameter combinations. Thus, our<br />
model is able to demonstrate the effects <strong>of</strong> more complex parameter changes that one<br />
might see in applications. For example one might input multiple impacts at the same<br />
site, which would increase both soil density <strong>and</strong> stiffness from one impact to the next.<br />
(This in fact was realized in field experiments by scientific colleagues when testing <strong>for</strong><br />
repeatability <strong>of</strong> responses to interrogation impacts.)<br />
Displacement around z=0.3048m (z=1 ft)<br />
Displacement around z=0.3048m (z=1 ft)<br />
u(0.3048,t)) (units: m)<br />
12 x 10−4 t (units: s)<br />
10<br />
8<br />
6<br />
4<br />
2<br />
κ=102000000 ρ=1800<br />
κ=204000000 ρ=1800<br />
κ=408000000 ρ=1800<br />
u(0.3048,t)) (units: m)<br />
10 x 10−4 8<br />
6<br />
4<br />
2<br />
t (units: s)<br />
κ=204000000 ρ=1440<br />
κ=204000000 ρ=1800<br />
κ=204000000 ρ=2250<br />
0<br />
0<br />
−2<br />
0 0.002 0.004 0.006 0.008 0.01<br />
−2<br />
0 0.002 0.004 0.006 0.008 0.01<br />
Figure 22: Wave <strong>for</strong>m at z 10 with varying soil parameters individually (left: variable κ, constant ρ; right:<br />
constant κ, variable ρ).<br />
Displacement around z=0.3048m (z=1 ft)<br />
Displacement around z=0.3048m (z=1 ft)<br />
u(0.3048,t)) (units: m)<br />
14 x 10−4 t (units: s)<br />
12<br />
10<br />
8<br />
6<br />
4<br />
2<br />
κ=102000000 ρ=1440<br />
κ=204000000 ρ=1800<br />
κ=408000000 ρ=2250<br />
u(0.3048,t)) (units: m)<br />
12 x 10−4<br />
10<br />
8<br />
6<br />
4<br />
2<br />
t (units: s)<br />
κ=163200000 ρ=1440<br />
κ=204000000 ρ=1800<br />
κ=255000000 ρ=2250<br />
0<br />
0<br />
−2<br />
0 0.002 0.004 0.006 0.008 0.01<br />
−2<br />
0 0.002 0.004 0.006 0.008 0.01<br />
Figure 23: Wave <strong>for</strong>m at z 10 with both soil parameters κ <strong>and</strong> ρ varying.