Measurement techniques for the determination of doping and mobility profiles in GaAs epitaxial layers

1994 ◽  
Vol 74 (1-2) ◽  
pp. 21-30
Author(s):  
B. Szentpáli ◽  
B. Kovács ◽  
F. Riesz ◽  
V. V. Tuyen
Physchem ◽  
2021 ◽  
Vol 1 (2) ◽  
pp. 176-188
Author(s):  
Gregor Lipinski ◽  
Markus Richter

Efficient and environmentally responsible use of resources requires the development and optimization of gas separation processes. A promising approach is the use of liquids that are designed for specific tasks, e.g., the capture of carbon dioxide or other greenhouse gases. This requires an accurate determination of gas solubilities for a broad range of temperatures and pressures. However, state of the art measurement techniques are often very time consuming or exhibit other pitfalls that prevent their use as efficient screening tools. Here, we show that the application of Raman spectroscopy through a compact measuring system can simplify data acquisition for the determination of gas solubilities in liquids. To demonstrate that this approach is expedient, we determined gas solubilities of carbon dioxide in water for three isotherms T = (288.15, 293.15, 298.15) K over a pressure range from p = (0.5–5) MPa and in three imidazolium-based ionic liquids for one isotherm T = 298.15 K at pressures from p = (0.1–5) MPa. When compared to data in the literature, all results are within the reported uncertainties of the measurement techniques involved. The developed analysis method eliminates the need for a lengthy volume or mass calibration of the sample prior to the measurements and, therefore, allows for fast screening of samples, which can help to advance gas separation processes in scientific and industrial applications.


2020 ◽  
Vol 5 (6) ◽  
pp. 931-934
Author(s):  
Rayees Sheikh ◽  
Swapnil Hiremath ◽  
Edward G. Clark ◽  
Ayub Akbari ◽  
Christopher McCudden ◽  
...  

Author(s):  
Ejiro Emorhokpor ◽  
E.P. Carlson ◽  
Jian Wei Wan ◽  
Arnd Dietrich Weber ◽  
C. Basceri ◽  
...  

Author(s):  
William Lowrie

‘Gravity and the figure of the Earth’ discusses the measurement of gravity and its variation at the Earth’s surface and with depth. Gravity is about 0.5 per cent stronger at the poles than at the equator and it first increases with depth until the core–mantle boundary and then sinks to zero at the Earth’s centre. Using satellites to carry out geodetic and gravimetric observations has revolutionized geodesy, creating a powerful geophysical tool for observing and measuring dynamic processes on the Earth. The various measurement techniques employed fall in two categories: precise location of a position on the Earth (such as GPS) and accurate determination of the geoid and gravitational field. Bouguer and free-air gravity anomalies and isostasy are explained.


1979 ◽  
Vol 14 (5) ◽  
pp. 571-574 ◽  
Author(s):  
A. Tempel ◽  
B. Schumann

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