Temperature Behavior of Plasma Reflection Spectra of (Bi2–xSbx)Te3 (0 < х < 1) Crystals in the Temperature Interval 80–300 K

2018 ◽  
Vol 61 (8) ◽  
pp. 1429-1434 ◽  
Author(s):  
N. P. Stepanov ◽  
L. É. Stepanova ◽  
A. S. Lozovskaya
2019 ◽  
Vol 64 (2) ◽  
pp. 173
Author(s):  
O. O. Gomonnai ◽  
M. Ludemann ◽  
A. V. Gomonnai ◽  
I. Yu. Roman ◽  
A. G. Slivka ◽  
...  

The unpolarized Raman spectra of TlIn(S0.95Se0.05)2 single crystals in the frequency interval 16–340 cm−1 are studied in the temperature interval 30 ≤ T ≤ 293 K. The Raman spectra are analyzed by a multipeak simulation using Lorentzian contours. The temperature behavior of the vibrational band parameters (half-width, intensity, and frequency) is studied with the emphasis on the temperature range, where changes related to phase transformations are revealed.


Author(s):  
E.D. Zhuzha ◽  
◽  
D.A. Vyrodov ◽  
A.P. Vyrodova ◽  
◽  
...  

2018 ◽  
Vol 56 (4) ◽  
pp. 527-532
Author(s):  
L. Kamaeva ◽  
◽  
A. Korepanov ◽  
V. Ladyanova ◽  
◽  
...  
Keyword(s):  

1991 ◽  
Vol 56 (12) ◽  
pp. 2786-2790 ◽  
Author(s):  
Václav Svoboda ◽  
Milan Zábranský

Molar heat capacities of 2,3,6-trimethylpyridine, 2,4,6-trimethylpyridine and 3-methoxypropionitrile in the liquid state were measured at the constant atmospheric pressure in the temperature interval of 300.60 to 328.35 K. The static type of adiabatic calorimeter was used for the measurements.


2021 ◽  
Vol 13 (6) ◽  
Author(s):  
Tabea J. Koch ◽  
Patrick Schmidt

AbstractBirch tar is the oldest manmade adhesive dating back to the European Middle Palaeolithic. Its study is of importance for understanding the cognitive capacities and technical skills of Neanderthals and the aceramic production systems employed in the European Palaeolithic and Mesolithic. Several methods may have been used to make birch tar, the most common proposition being dry distillation in oxygen-depleted atmospheres. One of the major impediments for our understanding of the conditions employed to make Neanderthal birch tar, and ultimately the technique used, is that it remains unknown at which temperatures exactly birch tar forms. The relationship between heating duration and tar formation is also unknown. To address these questions, we conduct a laboratory heating experiment, using sealed glass tubes and an electric furnace. We found that birch tar is only produced at a narrow temperature interval (350 °C and 400 °C). Heating times longer than 15 min have no effect on the quantity of tar produced. These findings, notwithstanding previous propositions of necessarily long heating times and larger tolerances for temperature, have important implications for our understanding of the investment in time needed for Palaeolithic birch tar making.


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