| Literature DB >> 35893000 |
Armen E Allahverdyan1,2, Edvard A Khalafyan3.
Abstract
Dynamical stabilization processes (homeostasis) are ubiquitous in nature, but the needed energetic resources for their existence have not been studied systematically. Here, we undertake such a study using the famous model of Kapitza's pendulum, which has attracted attention in the context of classical and quantum control. This model is generalized and rendered autonomous, and we show that friction and stored energy stabilize the upper (normally unstable) state of the pendulum. The upper state can be rendered asymptotically stable, yet it does not cost any constant dissipation of energy, and only a transient energy dissipation is needed. Asymptotic stability under a single perturbation does not imply stability with respect to multiple perturbations. For a range of pendulum-controller interactions, there is also a regime where constant energy dissipation is needed for stabilization. Several mechanisms are studied for the decay of dynamically stabilized states.Entities:
Keywords: Kapitza’s pendulum; asymptotic stability; dynamical stabilization; energy storage
Year: 2022 PMID: 35893000 PMCID: PMC9394353 DOI: 10.3390/e24081020
Source DB: PubMed Journal: Entropy (Basel) ISSN: 1099-4300 Impact factor: 2.738
Figure 1A schematic representation of the inverted pendulum. Angle is defined such that the upper (normally unstable) position refers to . The end point of the pendulum moves vertically with coordinate that is subject to a harmonic potential; cf. (3).
Figure 2(a) Angle variable (black, upper curve) and controller (blue, oscillating curve) as the numerical solutions of (6) and (9) versus time t. Red curve (in the middle) is the scaled energy that includes stored energy ; cf. (8) and (22). Parameters in (6) and (9) are: , (), (), , , . It is seen that quickly stabilizes at , which is normally an unstable state. The stabilization process takes a relatively small amount of energy. After stabilization, and decouple; continues oscillating, and scaled energy is then constant in time. Stability Condition (22) holds (the difference between its LHS and RHS is ). (b) The same parameters as in (a), but back-reaction parameter is slightly larger. We also display (green curve, third from top), where is the (scaled) energy related to the angle variable only; cf. (8). There is a rather long () period of metastability accompanied by a slow dissipation of energy. After this, stability is lost: quickly relaxes to the minimal of the potential, and loses all its energy and eventually stops moving (i.e., ). The whole stored energy dissipates. The physical reason of scenario in (b) is that fast oscillations around do not disappear, i.e., they persist in the metastable state, continuously dissipate energy [cf. (10)], and once the initial energy decreases sufficiently, and (relatively) suddenly move to global energy minima . Energy stored in decays in time. To confirm this, (b) also shows the scaled energy related to . It stays constant in time for the whole metastability period; see the green curve. A similar scenario happens, when the initial condition is out of the attraction basin of . However, here never reaches .
Figure 3(a) Angle (blue, piecewise constant curve) as the numerical solution of (6) and (9) versus time t, where to the RHS of (9) we added white noise with intensity ; see (23). Here, (orange, decaying curve) is the scaled energy; cf. (8). Parameters in (6) and (9) are: , , , , , . It is seen that is stabilized around in a metastable state whose lifetime is . During this lifetime, energy slowly decays till it is below some critical value, and then the metastable state suddenly decays. (b) The same as in (a), but for a stronger noise . Metastable decay is smeared, but still clearly visible.