The excitation of O(1S) and O2 bands in the nightglow: a brief review and preview

1986 ◽  
Vol 64 (12) ◽  
pp. 1626-1630 ◽  
Author(s):  
I. C. McDade ◽  
E. J. Llewellyn

Recent laboratory and in situ studies of the processes involved in the excitation of O(1S) and the five strongest systems of molecular oxygen in the terrestrial nightglow are reviewed. In spite of the significant advances that have been made during the last few years, it is not yet possible to reconcile rocket and satellite photometric observations with expectations based on laboratory kinetic data. Even in the most extensively studied O2 system, the Herzberg-I system, serious discrepancies exist between the kinetic parameters measured in the laboratory and those deduced from the airglow observations. It is only in the case of the O2 Atmospheric system that the laboratory and in situ studies have converged on a consistent view of the overall excitation mechanism. In the case of the O(1S) green line, most evidence would now appear to support the Barth mechanism, but progress towards a conclusive identification of the Barth precursor state, or states, is seriously hindered by the inadequacies in current understanding of the molecular oxygen systems.


2021 ◽  
Author(s):  
Claire Chassagne ◽  
Zeinab Safar ◽  
Zhirui Deng ◽  
Qing He ◽  
Andy Manning

Modelling the flocculation of particles in a natural environment like an estuary is a challenging task owing to the complex particle-particle and particle-hydrodynamic interactions involved. In this chapter a summary is given of recent laboratory and in-situ studies regarding flocculation. A flocculation model is presented and the way to implement it in an existing sediment transport model is discussed. The model ought to be parametrized, which can be done by performing laboratory experiments which are reviewed. It is found, both from laboratory and in-situ studies, that flocculation between mineral sediment and organic matter is the dominant form of flocculation in estuarine systems. Mineral sediment in the water column is < 20 μm in size and its settling velocity is in the range [0–0.5] mm/s. Flocs can then be categorized in two types: flocs of size [20–200] μm and flocs of size > 200 μm. The origin of these two types is discussed. The two types of flocs are found at different positions in the water column and both have settling velocities in the range [0.5–10] mm/s.



Author(s):  
J. V. Maskowitz ◽  
W. E. Rhoden ◽  
D. R. Kitchen ◽  
R. E. Omlor ◽  
P. F. Lloyd

The fabrication of the aluminum bridge test vehicle for use in the crystallographic studies of electromigration involves several photolithographic processes, some common, while others quite unique. It is most important to start with a clean wafer of known orientation. The wafers used are 7 mil thick boron doped silicon. The diameter of the wafer is 1.5 inches with a resistivity of 10-20 ohm-cm. The crystallographic orientation is (111).Initial attempts were made to both drill and laser holes in the silicon wafers then back fill with photoresist or mounting wax. A diamond tipped dentist burr was used to successfully drill holes in the wafer. This proved unacceptable in that the perimeter of the hole was cracked and chipped. Additionally, the minimum size hole realizable was > 300 μm. The drilled holes could not be arrayed on the wafer to any extent because the wafer would not stand up to the stress of multiple drilling.



1997 ◽  
Author(s):  
L. D. Marks
Keyword(s):  


2003 ◽  
Author(s):  
J. Bredow ◽  
S.P. Gogineni ◽  
K. Jezek
Keyword(s):  




2020 ◽  
Vol 30 ◽  
pp. 53-58
Author(s):  
Kirill Kurgan ◽  
Anatoliy Klopotov ◽  
Vasiliy Klimenov ◽  
Michael Slobodyan ◽  
Artem Ustinov ◽  
...  


2019 ◽  
Vol 9 (7) ◽  
pp. 1310 ◽  
Author(s):  
Kerstin Hauke ◽  
Johannes Kehren ◽  
Nadine Böhme ◽  
Sinje Zimmer ◽  
Thorsten Geisler

In the last decades, Raman spectroscopy has become an important tool to identify and investigate minerals, gases, glasses, and organic material at room temperature. In combination with high-temperature and high-pressure devices, however, the in situ investigation of mineral transformation reactions and their kinetics is nowadays also possible. Here, we present a novel approach to in situ studies for the sintering process of silicate ceramics by hyperspectral Raman imaging. This imaging technique allows studying high-temperature solid-solid and/or solid-melt reactions spatially and temporally resolved, and opens up new avenues to study and visualize high-temperature sintering processes in multi-component systems. After describing in detail the methodology, the results of three application examples are presented and discussed. These experiments demonstrate the power of hyperspectral Raman imaging for in situ studies of the mechanism(s) of solid-solid or solid-melt reactions at high-temperature with a micrometer-scale resolution as well as to gain kinetic information from the temperature- and time-dependent growth and breakdown of minerals during isothermal or isochronal sintering.





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