The Maxwell model is represented by a purely
viscous damper and a purely
elastic spring connected in series, 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, \sigma_\mathrm{Total} and the total strain, \varepsilon_\mathrm{Total} can be defined as follows: :\sigma_\mathrm{Total}=\sigma_{\rm D} = \sigma_{\rm S} :\varepsilon_\mathrm{Total}=\varepsilon_{\rm D}+\varepsilon_{\rm S } 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: :\frac {d\varepsilon_\mathrm{Total}} {dt} = \frac {d\varepsilon_{\rm D}} {dt} + \frac {d\varepsilon_{\rm S}} {dt} = \frac {\sigma} {\eta} + \frac {1} {E} \frac {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: :\frac {1} {E} \frac {d\sigma} {dt} + \frac {\sigma} {\eta} = \frac {d\varepsilon} {dt} or, in dot notation: :\frac {\dot {\sigma}} {E} + \frac {\sigma} {\eta}= \dot {\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. == Effect of a sudden deformation ==