scholarly journals Influence of atomic motion on the collective effects in dense and cold atomic ensembles

2020 ◽  
Vol 101 (3) ◽  
Author(s):  
A. S. Kuraptsev ◽  
I. M. Sokolov
2021 ◽  
Vol 104 (1) ◽  
Author(s):  
Sofia Ribeiro ◽  
Thomas F. Cutler ◽  
Charles S. Adams ◽  
Simon A. Gardiner

1988 ◽  
Vol 156 (9) ◽  
pp. 3-46 ◽  
Author(s):  
S.A. Kazantsev ◽  
N.Ya. Polinovskaya ◽  
L.N. Pyatnitskii ◽  
S.A. Edel'man
Keyword(s):  

2000 ◽  
Vol 170 (3) ◽  
pp. 331 ◽  
Author(s):  
S.A. Gusev ◽  
Yu.N. Nozdrin ◽  
M.V. Sapozhnikov ◽  
A.A. Fraerman

2010 ◽  
Vol 82 (6) ◽  
Author(s):  
Y. Kobayashi ◽  
Y. Shiraishi ◽  
A. Hatakeyama
Keyword(s):  

2012 ◽  
Vol 10 (01) ◽  
pp. 1250007 ◽  
Author(s):  
NOUR ZIDAN ◽  
S. ABDEL-KHALEK ◽  
M. ABDEL-ATY

In this paper, we investigate the geometric phase of the field interacting with a moving four-level atom in the presence of Kerr medium. The results show that the atomic motion, the field-mode structure and Kerr medium play important roles in the evolution of the system dynamics. As illustration, we examine the behavior of the geometric phase and entanglement with experimentally accessible parameters. Some new aspects are observed and discussed.


1957 ◽  
Vol 35 (1) ◽  
pp. 21-37 ◽  
Author(s):  
J. D. Jackson

The Monte Carlo calculations of McManus and Sharp (unpublished) for the prompt nuclear processes occurring upon bombardment of heavy elements by 400 Mev. protons are combined with a description of the subsequent neutron evaporation to determine spallation cross sections for comparison with experiment. The model employed is a schematic one which suppresses the detailed characteristics of individual nuclei, but gives the over-all behavior to be expected. Many-particle and collective effects such as alpha particle emission and fission are ignored. The computed cross sections are presented in a variety of different graphical forms which illustrate quantitatively the qualitative picture of high energy reactions first given by Serber (1947). The calculations are in general agreement with existing data when fission is not an important effect, but the agreement does not imply a very stringent test of the various features of the model.


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