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Foundations of classical physics
2007We choose the classical canonical theory of Liouville because of the best match with the q-theory—a genuine statistical theory. Also this is why we devote the particular Sect. 2.4 to the measurement of the physical quantities.
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Physical Aging of Classical Oscillators
Physical Review Letters, 2014Aging is a familiar phenomenon from glassy systems like spin glasses and materials with slow relaxation processes, breaking of time-translation invariance, and dynamical scaling. We study aging in active rotators and Kuramoto oscillators that are coupled with frustrated bonds.
Florin, Ionita +1 more
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2013
The cell method presented in the previous chapters can be applied to different classes of physical problems. Some of these classes are presented in this chapter, in both static and time-varying formulations, together with a short explanation of their main characteristics.
Alotto, Piergiorgio +3 more
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The cell method presented in the previous chapters can be applied to different classes of physical problems. Some of these classes are presented in this chapter, in both static and time-varying formulations, together with a short explanation of their main characteristics.
Alotto, Piergiorgio +3 more
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Classical physical abstraction
Erkenntnis, 1993An informal theory is set forth of relations between abstract entities, includingcolors, physical quantities, times, andplaces in space, and the concrete things thathave them, or areat orin them, based on the assumption that there are close analogies between these relations and relations between abstractsets and the concrete things that aremembers of ...
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1997
Abstract Hertz’s experiment. The atom as an elementary source of light. The classical model of the atom. Emission from a charge and Emission conditions. Calculation of the vortical component of the field. A rigorous solution of the problem of dipole emission. Harmonic oscillations of a dipole. The total power of dipole radiation.
S A Akhmanov, S YU Nikitin
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Abstract Hertz’s experiment. The atom as an elementary source of light. The classical model of the atom. Emission from a charge and Emission conditions. Calculation of the vortical component of the field. A rigorous solution of the problem of dipole emission. Harmonic oscillations of a dipole. The total power of dipole radiation.
S A Akhmanov, S YU Nikitin
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2010
Geodesy can be defined as the science of the figure of the Earth and its gravitational field, as well as their determination. Even though today the figure of the Earth, understood as the visible Earth’s surface, can be determined purely geometrically by satellites, using Global Positioning System (GPS) for the continents and satellite altimetry for the
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Geodesy can be defined as the science of the figure of the Earth and its gravitational field, as well as their determination. Even though today the figure of the Earth, understood as the visible Earth’s surface, can be determined purely geometrically by satellites, using Global Positioning System (GPS) for the continents and satellite altimetry for the
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2017
This chapter presents the basics of classical physical geodesy, starting from the definitions of the gravity potential and gravity. The normal gravity potential is derived as the potential of a level ellipsoid plus the rotational potential of the ellipsoid.
Lars E. Sjöberg, Mohammad Bagherbandi
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This chapter presents the basics of classical physical geodesy, starting from the definitions of the gravity potential and gravity. The normal gravity potential is derived as the potential of a level ellipsoid plus the rotational potential of the ellipsoid.
Lars E. Sjöberg, Mohammad Bagherbandi
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Fast Algorithms for Classical Physics
Science, 1994Some of the recently developed fast summation methods that have arisen in scientific computing are described. These methods require an amount of work proportional to N or N log N to evaluate all pairwise interactions in an ensemble of N ...
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