Submitted:
02 September 2024
Posted:
03 September 2024
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Abstract
Keywords:
1. Introduction
2. The Langevin Equation
3. Fast and Slow Variables
4. The reduced equilibrium distribution of the slow amplitudes
5. The Langevin Equation for the Slow Amplitudes
6. A Reduced Description Using the Original Variables
7. Conclusions
- i)
- At any time scale one has a natural choice of variables for which the relaxation from an initial state and the fluctuations are described in the usual way.
- ii)
- If one reduces a description by elimination of fast variables both the linear (Onsager) coefficients and the equilibrium distribution change their values.
- iii)
- The reduced Onsager matrix and the correlation matrix are not trivially obtained from ℓ and . For this one needs the eigenvectors of .
- iv)
- The Onsager matrix for the slow variables and the correlation matrix are symmetric.
- v)
- Accept for the case that one can do experiments on the fast and the slow time scale, there is no need to do this reduction. One simply uses a set of independent variables which have not relaxed and constructs , and on the basis of physical arguments alone.
- vi)
- The initial state, equilibrium distribution and entropy depend on the time scale one considers. On each time scale it will be such that processes that decay on a faster time scale have equilibrated when the experiment or simulation is started.
- vii)
- The initial state, equilibrium distribution and entropy for the reduced description cannot be found by substituting the equilibrium values of the fast variables in the more extended description.
Acknowledgments
References
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