How it Works
A sinusoidal displacement is driven at the left boundary. The simulation propagates a 1D shear wave through a Maxwell viscoelastic medium using the finite-difference time-domain method. The Maxwell model gives a frequency-dependent complex shear modulus G*(ω) = G·iωτ/(1+iωτ), which determines the complex wave number k(ω) = ω·sqrt(ρ/G*(ω)).
At low frequencies (ω << ωc = 1/τ) the imaginary part of k dominates — disturbances decay exponentially (diffusive regime). At high frequencies (ω >> ωc) the real part of k dominates — coherent waves travel at speed c = sqrt(G/ρ) (elastic regime). The lower panel shows the live dispersion curve.
ω_c = 1/τ = G/η [crossover frequency]
G*(ω) = G · iωτ / (1 + iωτ)
k = ω √(ρ / G*(ω))
Frequently Asked Questions
What is a viscoelastic material?
A viscoelastic material exhibits both viscous (liquid-like) and elastic (solid-like) behaviour depending on the timescale of deformation. Examples include polymer melts, biological gels, and silly putty.
What is the Maxwell viscoelastic model?
The Maxwell model represents viscoelasticity as a spring (elastic modulus G) and dashpot (viscosity η) in series. Stress relaxes exponentially with relaxation time τ = η/G.
What is relaxation time in viscoelasticity?
Relaxation time τ = η/G is the time for stress to decay to 1/e of its initial value after an imposed step strain. It separates the elastic (fast) regime from the viscous (slow) regime.
Why do waves diffuse at low frequency in a Maxwell fluid?
At frequencies below ωc = G/η = 1/τ, the material has time to relax and behaves as a viscous liquid. Disturbances decay diffusively rather than propagating as coherent waves.
Why do waves propagate at high frequency in a Maxwell fluid?
At frequencies above ωc, the material cannot relax before the wave passes and behaves elastically, supporting propagating shear waves at speed c = sqrt(G/ρ).
What is the dispersion relation for viscoelastic waves?
For a Maxwell fluid: k² = ρω²/G·(1 + i/(ωτ)). The real part gives phase speed, the imaginary part gives spatial attenuation.
What is attenuation in wave propagation?
Attenuation is the decay of wave amplitude with distance. In viscoelastic media it arises from viscous dissipation. The spatial attenuation coefficient α = Im(k) grows with viscosity.
What are practical examples of viscoelastic wave effects?
Viscoelastic wave phenomena are important in seismic attenuation in sedimentary rock, ultrasound in biological tissue, shock absorption in polymer foams, and vibration damping in composite structures.
What is the Deborah number?
The Deborah number De = τ/tobs compares the material relaxation time to the observation timescale. De >> 1 means elastic behaviour; De << 1 means viscous behaviour.
How does the Kelvin-Voigt model differ from the Maxwell model?
The Kelvin-Voigt model places spring and dashpot in parallel, giving a creep response but no stress relaxation. The Maxwell model places them in series, giving stress relaxation but unlimited creep.