scholarly journals Optical Studies of 15 Hard X-Ray Selected Cataclysmic Binaries

2018 ◽  
Vol 155 (6) ◽  
pp. 247 ◽  
Author(s):  
Jules P. Halpern ◽  
John R. Thorstensen ◽  
Patricia Cho ◽  
Gabriel Collver ◽  
Mokhine Motsoaledi ◽  
...  
2019 ◽  
Vol 2019 ◽  
pp. 1-11 ◽  
Author(s):  
H. Letifi ◽  
Y. Litaiem ◽  
D. Dridi ◽  
S. Ammar ◽  
R. Chtourou

In this paper, we have reported a novel photocatalytic study of vanadium-doped SnO2 nanoparticles (SnO2: V NPs) in rhodamine B degradation. These NPs have been prepared with vanadium concentrations varying from 0% to 4% via the coprecipitation method. Structural, morphological, and optical properties of the prepared nanoparticles have been investigated by X-ray diffraction (XRD), Fourier transform infrared (FTIR) spectroscopy, transmission electron microscope (TEM), and UV-Vis and photoluminescence (PL) spectroscopy. Structural properties showed that both undoped and SnO2: V NPs exhibited the tetragonal structure, and the average crystal size has been decreased from 20 nm to 10 nm with the increasing doping level of vanadium. Optical studies showed that the absorption edge of SnO2: V NPs showed a redshift with the increasing vanadium concentration. This redshift leads to the decrease in the optical band gap from 3.25 eV to 2.55 eV. A quenching in luminescence intensity has been observed in SnO2: V NPs, as compared to the undoped sample. Rhodamine B dye (RhB) has been used to study the photocatalytic degradation of all synthesized NPs. As compared to undoped SnO2 NPs, the photocatalytic activity of SnO2: V NPs has been improved. RhB dye was considerably degraded by 95% within 150 min over on the SnO2: V NPs.


1985 ◽  
Vol 90 ◽  
pp. 410 ◽  
Author(s):  
H. Quintana ◽  
J. Melnick ◽  
L. Infante ◽  
B. Thomas

1974 ◽  
Vol 190 ◽  
pp. L1 ◽  
Author(s):  
C. A. Jones ◽  
T. Chetin ◽  
W. Liller
Keyword(s):  

Clay Minerals ◽  
1970 ◽  
Vol 8 (4) ◽  
pp. 435-444 ◽  
Author(s):  
M. J. Wilson ◽  
V. C. Farmer

AbstractThe weathering of hornblende in the Rehiran profile has been investigated by optical, X-ray, infrared and differential thermal methods. Optical studies of the fresh hornblende show that it contains discrete lamellar intergrowths of another amphibole which, from infrared evidence, is of an iron-rich nature. This minor phase is selectively weathered in the lower horizons and yields a clay mineral which was identified as interstratified swelling chlorite-saponite. The major hornblende component remains relatively unchanged. Single crystal photographs indicate that the formation of the clay mineral is not structurally controlled by the parent hornblende, although there is a tendency towards alignment along cleavage planes. The clay mineral becomes unstable in the upper part of the profile and could not be detected in the A horizon. Comparisons are made with the findings of other workers.


Author(s):  
Grigory Shirinyan ◽  
Karine L. Ovanesyan ◽  
Atom Eganyan ◽  
Ashot G. Petrosyan ◽  
Christian Pedrini ◽  
...  
Keyword(s):  

2000 ◽  
Vol 316 (1) ◽  
pp. 137-142 ◽  
Author(s):  
C. Zurita ◽  
J. Casares ◽  
T. Shahbaz ◽  
P. A. Charles ◽  
R. I. Hynes ◽  
...  
Keyword(s):  

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