scholarly journals Phase retrieval from experimental far-field intensity data

1990 ◽  
Vol 7 (3) ◽  
pp. 434 ◽  
Author(s):  
M. J. Pérez-Ilzarbe ◽  
M. Nieto-Vesperinas ◽  
R. Navarro
Optik ◽  
2020 ◽  
Vol 218 ◽  
pp. 164904
Author(s):  
Qian Ye ◽  
Dafei Xiao

2003 ◽  
Author(s):  
Eugenio R. Mendez ◽  
Demetrio Macias ◽  
Gustavo Olague

1997 ◽  
Vol 14 (12) ◽  
pp. 3155 ◽  
Author(s):  
C.-W. Liao ◽  
M. A. Fiddy ◽  
C. L. Byrne

2019 ◽  
Vol 2019 ◽  
pp. 1-10
Author(s):  
Huiliang Jin ◽  
Jianhui Huang ◽  
Qian Ye ◽  
Guoxiang Meng ◽  
Binbin Xiang ◽  
...  

The efficiency of a reflector antenna highly depends on its surface shape. In order to ensure a good convergence, the conventional phase retrieval based shape detection schemes require that several far-field intensities be scanned, focused, or defocused. For large reflector antennas, the scanning process is time consuming. This paper proposes a new shape detection method that requires only single far-field intensity. Unlike existing shape detection methods, it retrieves both the amplitude and the phase, based on the fact that a deformed shape causes change not only in the aperture phase but also in the aperture amplitude. Through even-odd decomposition analysis, it is found that in the case of small and smooth deformation, “odd-phase” and “even-amplitude” can be directly recovered from one focused far-field intensity. This leads to the recovery of both the odd and the even parts of the antenna surface shape simultaneously. By combining amplitude retrieval and phase retrieval, this work achieves for the first time the shape detection with only one scan.


1994 ◽  
Vol 37 (1) ◽  
Author(s):  
G. Mele ◽  
A. Meloni ◽  
P. Palangio

Significant variations in the absolute value of the geomagnetic field intensity related to tectonic events, as earthquakes and volcanic eruptions, have been observed in several cases. To detect such a tectonomagnetic effect related to seismic activity, a seismomagnetic network was installed by the Istituto Nazionale di Geofisica (ING) in the Abruzzi region (CentraI Italy), in July 1989. This area is being uplifting since the Pliocene. A logistic compromise between geophysical requirements and the electrified railway system tracks distribution led to the installation of five total magnetic field intensity data acquisition sites. From July 1989 to September 1992 geomagnetic intensity data were simultaneously recorded at all stations and compared to that recorded at the L'Aquila Observatory, located in the same area. A variation of about 10 nT in the absolute level of the geomagnetic field was measured at two stations located on the eastern side of the network. We suggest that the detected magnetic anomaly could resuIt from aseismic-changes in crustal stress during this time.


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