scholarly journals One electron molecules with relativistic kinetic energy: Properties of the discrete spectrum

1984 ◽  
Vol 94 (4) ◽  
pp. 523-535 ◽  
Author(s):  
Ingrid Daubechies



2020 ◽  
Vol 98 (2) ◽  
pp. 142-147
Author(s):  
Marco Fedi

Relativistic mass change with speed is considered here as the effect of a viscous, dilatant vacuum, whose apparent viscosity is related to the Lorentz factor. Transient solid-like vacuum due to shear stress is presented as the reason why vacuum prevents the speed of massive objects from being indefinitely increased. Such a vacuum – that in a previous study allowed to exactly calculate the Pioneer anomaly, Mercury’s perihelion precession, and was shown to be compatible with stable planetary orbits – leads here to a quantum formula for the relativistic kinetic energy. A formula which distinguishes between the case of accelerated charges in a vacuum, for which a Stokes–Einstein radius comes into play, and the case of accelerated macroscopic bodies, for which the quantum potential term vanishes. In this way, incidentally, one obtains again correct results for the Pioneer 10, confirming the role of vacuum’s viscous force. This description of a quantum mechanism underlying the relativistic kinetic energy may be also helpful in constructing a theory of quantum relativity and may even tell us more about the interactions of matter with the Higgs field and the dark sector: two issues which can be themselves linked to a dilatant vacuum.







2002 ◽  
Vol 16 (23n24) ◽  
pp. 901-906 ◽  
Author(s):  
V. F. TARASOV

The total relativistic kinetic energy of the Thomas–Fermi atom is Ekr = Ek + Er, where Ek = κk ∫ ρ5/3dv and Er = -κr ∫ ρ7/3dv + o(α2), [Formula: see text]. The minimum pressure of a relativistic degenerate electron gas is [Formula: see text]. In just the same way, the cases x = pμ / mc = 1 and x > 1 are explicitly considered.



2008 ◽  
Vol 15 ◽  
pp. 17-22 ◽  
Author(s):  
M. V. Kurgansky

Abstract. In a forced-dissipative barotropic model of the atmosphere on a spherical planet, by following mathematical techniques in (Thompson, P. D.: The equilibrium energy spectrum of randomly forced two-dimensional turbulence, Journal of the Atmospheric Sciences, 30, 1593–1598, 1973) but applying them in a novel context of the discrete spectrum on a rotating sphere, the "minus 2" energy spectrum for wavenumbers much greater than a characteristic wavenumber of the baroclinic forcing has been obtained if the forcing is taken in the simplest and most fundamental form. Some observation-based atmospheric kinetic energy spectra, with their slopes lying between "minus 2" and "minus 3" laws, are discussed from the perspective of the deduced "minus 2" energy spectrum.



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