The Coulomb interference term in polarization analysis and the determination of the transition matrix

Author(s):  
Albrecht Lindner
1989 ◽  
Vol 50 (C1) ◽  
pp. C1-119-C1-125 ◽  
Author(s):  
S. BOUGOUFFA ◽  
X. C. CAO

2008 ◽  
Vol 42 (1) ◽  
pp. 69-84 ◽  
Author(s):  
J. R. Stewart ◽  
P. P. Deen ◽  
K. H. Andersen ◽  
H. Schober ◽  
J.-F. Barthélémy ◽  
...  

The technique of longitudinal neutron polarization analysis on a multi-detector neutron spectrometer (so-called `xyz'-polarization analysis) is presented. This technique allows the simultaneous and unambiguous determination of the nuclear, magnetic and nuclear spin-incoherent scattering cross sections as a function of both momentum transfer and energy transfer. The implementation ofxyz-polarization analysis on the recently upgraded D7 spectrometer at the Institut Laue–Langevin in Grenoble is described. Several examples of neutron polarization analysis studies of disordered systems on D7 are given, illustrating the valuable information which can be retrieved from the analysis of neutron diffraction patterns between the Bragg peaks.


1988 ◽  
Vol 27-28 ◽  
pp. 471-0 ◽  
Author(s):  
J.C. Osborn ◽  
T.J. Hicks ◽  
R.J. Hill

1984 ◽  
Vol 52 (21) ◽  
pp. 1876-1879 ◽  
Author(s):  
A. Saha ◽  
Kamal K. Seth ◽  
M. Artuso ◽  
B. Harris ◽  
R. Seth ◽  
...  

2020 ◽  
Vol 1 (1) ◽  
pp. 21
Author(s):  
Syahrial Ayub ◽  
Muhammad Zuhdi ◽  
Muhammad Taufik ◽  
Gunawan Gunawan

Volcanic earthquakes of mount Merapi have been investigated periodically. The investigation aims to determine the hypocenter and epicenter of mount Merapi's volcanic earthquake using wave polarization analysis. The analysis was carried out in three domains, which are the time domain, the frequency domain, and the space domain. The analysis in the time domain was conducted by the arrival time of the volcanic earthquake, and the analysis in the frequency domain was done by observing the spectrum to get information on source frequency and bandwidth passed from polarization analysis, while the analysis in the space domain was conducted especially on hypocenter determination of the volcanic earthquakes. The analysis leads to the frequency of source 6 Hz and a bandwidth of 0.1 Hz. Thus, the hypocenter of volcanic earthquakes by polarization analysis was distributed to depth from 670 m to 3250 m from Merapi's top


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