It is common to explain viscoelastic materials with spring and dashpot 1D constructions, e.g:
which represents a Maxwell rheology, usually explained by saying that $ \sigma = \eta \dot{\epsilon}_1 = k \epsilon_2$, and $\epsilon = \epsilon_1+\epsilon_2$. Differentiating the $\epsilon_2$ part and summing, one does get $\frac{\eta}{k}\dot{\sigma}+\sigma=\eta\dot{\epsilon}$
While I have well been aware of the caveats of these convenient representations before extrapolating to 2 or 3D continuum materials, I am surprised to realise now that there seems to be a first one which holds even when keeping very close to what is represented: strain rates shouldn't sum...?
If we relate strain rates with the length $l_i$ of each element ($i=1,2$), $\dot{\epsilon}_i = \dot{l}_i/l_i$ while $\dot{\epsilon}=\frac{\dot l_1+\dot l_2}{l_1+l_2}$, which I find difficult to reduce to an approximation of $\dot{\epsilon}_1+\dot{\epsilon}_2$ with reasonable assumptions.
I am aware that the overall answer is that these are only toys to help conceive how models derived otherwise do work, however I'm wondering if there's any more precise reason why they work so relatively well in these conditions. Can one state explicitly the limits of validity of these toy models? Is one e.g. reduced to consider that we are around some reference state $l_i=l_i^0$, and if so how can such a model provide information on liquid-like systems?