A Maxwell material is the most simple model viscoelastic material showing properties of a typical liquid. It shows viscous flow on the long timescale, but additional elastic resistance to fast deformations.[1] It is named for James Clerk Maxwell who proposed the model in 1867.[2] [3] It is also known as a Maxwell fluid. A generalization of the scalar relation to a tensor equation lacks motivation from more microscopic models and does not comply with the concept of material objectivity. However, these criteria are fulfilled by the Upper-convected Maxwell model.
The Maxwell model is represented by a purely viscous damper and a purely elastic spring connected in series,[4] as shown in the diagram. If, instead, we connect these two elements in parallel, we get the generalized model of a solid Kelvin–Voigt material.
In Maxwell configuration, under an applied axial stress, the total stress,
\sigmaTotal
\varepsilonTotal
\sigmaTotal=\sigma\rm=\sigma\rm
\varepsilonTotal=\varepsilon\rm+\varepsilon\rm
where the subscript D indicates the stress–strain in the damper and the subscript S indicates the stress–strain in the spring. Taking the derivative of strain with respect to time, we obtain:
d\varepsilonTotal | |
dt |
=
d\varepsilon\rm | |
dt |
+
d\varepsilon\rm | |
dt |
=
\sigma | |
η |
+
1 | |
E |
d\sigma | |
dt |
where E is the elastic modulus and η is the material coefficient of viscosity. This model describes the damper as a Newtonian fluid and models the spring with Hooke's law.
In a Maxwell material, stress σ, strain ε and their rates of change with respect to time t are governed by equations of the form:
1 | |
E |
d\sigma | |
dt |
+
\sigma | |
η |
=
d\varepsilon | |
dt |
or, in dot notation:
| |||
E |
+
\sigma | |
η |
=
\varepsilon |
The equation can be applied either to the shear stress or to the uniform tension in a material. In the former case, the viscosity corresponds to that for a Newtonian fluid. In the latter case, it has a slightly different meaning relating stress and rate of strain.
The model is usually applied to the case of small deformations. For the large deformations we should include some geometrical non-linearity. For the simplest way of generalizing the Maxwell model, refer to the upper-convected Maxwell model.
If a Maxwell material is suddenly deformed and held to a strain of
\varepsilon0
η | |
E |
The picture shows dependence of dimensionless stress
\sigma(t) | |
E\varepsilon0 |
E | |
η |
t
If we free the material at time
t1
\varepsilonback=-
\sigma(t1) | |
E |
=\varepsilon0\exp\left(-
E | |
η |
t1\right).
Since the viscous element would not return to its original length, the irreversible component of deformation can be simplified to the expression below:
\varepsilonirreversible=\varepsilon0\left[1-\exp\left(-
E | |
η |
t1\right)\right].
If a Maxwell material is suddenly subjected to a stress
\sigma0
\varepsilon(t)=
\sigma0 | |
E |
+t
\sigma0 | |
η |
If at some time
t1
\varepsilonreversible=
\sigma0 | |
E, |
\varepsilonirreversible=t1
\sigma0 | |
η. |
The Maxwell model does not exhibit creep since it models strain as linear function of time.
If a small stress is applied for a sufficiently long time, then the irreversible strains become large. Thus, Maxwell material is a type of liquid.
If a Maxwell material is subject to a constant strain rate
\epsilon |
\sigma=η
\varepsilon |
In general
\sigma(t)=η
\varepsilon |
(1-e-Et/η)
The complex dynamic modulus of a Maxwell material would be:
E*(\omega)=
1 | |
1/E-i/(\omegaη) |
=
Eη2\omega2+i\omegaE2η | |
η2\omega2+E2 |
Thus, the components of the dynamic modulus are :
E1(\omega)=
Eη2\omega2 | |
η2\omega2+E2 |
=
(η/E)2\omega2 | |
(η/E)2\omega2+1 |
E=
\tau2\omega2 | |
\tau2\omega2+1 |
E
and
E2(\omega)=
\omegaE2η | |
η2\omega2+E2 |
=
(η/E)\omega | |
(η/E)2\omega2+1 |
E=
\tau\omega | |
\tau2\omega2+1 |
E
\tau\equivη/E
Blue curve | dimensionless elastic modulus
| |||
Pink curve | dimensionless modulus of losses
| |||
Yellow curve | dimensionless apparent viscosity
| |||
X-axis | dimensionless frequency \omega\tau |