“…We point out that evolution equations () and () are rate equations, where the Onsager operator
, or more generally, the non‐linear operator
maps the thermodynamic driving force
to a rate
. Other examples for gradient systems can be found for example in [
12] for the porous medium equation, in [
9, 10] for complex fluids, in [
39, 58–60] for (slow & fast) reaction‐diffusion systems with detailed balance, in [
61] for the Fokker–Planck equation, and in [
62, 63] in the context of large deviations. Mathematical properties of gradient flows are discussed in [
11].…”