| Literature DB >> 33265548 |
Gerhard Grössing1, Siegfried Fussy1, Johannes Mesa Pascasio1, Herbert Schwabl1.
Abstract
In the quest for an understanding of nonlocality with respect to an appropriate ontology, we propose a "cosmological solution". We assume that from the beginning of the universe each point in space has been the location of a scalar field representing a zero-point vacuum energy that nonlocally vibrates at a vast range of different frequencies across the whole universe. A quantum, then, is a nonequilibrium steady state in the form of a "bouncer" coupled resonantly to one of those (particle type dependent) frequencies, in remote analogy to the bouncing oil drops on an oscillating oil bath as in Couder's experiments. A major difference to the latter analogy is given by the nonlocal nature of the vacuum oscillations. We show with the examples of double- and n-slit interference that the assumed nonlocality of the distribution functions alone suffices to derive the de Broglie-Bohm guiding equation for N particles with otherwise purely classical means. In our model, no influences from configuration space are required, as everything can be described in 3-space. Importantly, the setting up of an experimental arrangement limits and shapes the forward and osmotic contributions and is described as vacuum landscaping.Entities:
Keywords: Schrödinger equation; de Broglie–Bohm theory; nonequilibrium thermodynamics; zero-point field
Year: 2018 PMID: 33265548 PMCID: PMC7512975 DOI: 10.3390/e20060458
Source DB: PubMed Journal: Entropy (Basel) ISSN: 1099-4300 Impact factor: 2.524
Figure 1Scheme of interference at a double-slit. Considering an incoming beam of electrons with wave number impinging on a wall with two slits, two beams with wave numbers and , respectively, are created, which one may denote as “pre-determined” velocities Taking into account the influences of the osmotic momentum field , one has to combine all the velocities/momenta at a given point in space and time in order to compute the resulting, or emergent, velocity/momentum field . This, then, provides the correct intensity distributions and average trajectories (lower plane).
Figure 2Classical computer simulation of the interference pattern: intensity distribution with increasing intensity from white through yellow and orange, with trajectories (red) for two Gaussian slits, and with large dispersion (evolution from bottom to top; ). From [16].
Figure 3Classical computer simulation of the interference pattern: intensity distribution with increasing intensity from white through yellow and orange, with trajectories (red) for two Gaussian slits, and with small dispersion (evolution from bottom to top; ). From [16].