Interaction of a Cylindrical Shock With a Heavy Gas Layer with Perturbed Outer Surfacee

Author(s):  
Juchun Ding ◽  
Zhigang Zhai ◽  
Ting Si ◽  
Xisheng Luo
Keyword(s):  
2013 ◽  
Vol 25 (11) ◽  
pp. 114101 ◽  
Author(s):  
G. C. Orlicz ◽  
S. Balasubramanian ◽  
K. P. Prestridge

2019 ◽  
Vol 878 ◽  
pp. 277-291 ◽  
Author(s):  
Juchun Ding ◽  
Jianming Li ◽  
Rui Sun ◽  
Zhigang Zhai ◽  
Xisheng Luo

The evolution of an $\text{SF}_{6}$ layer surrounded by air is experimentally studied in a semi-annular convergent shock tube by high-speed schlieren photography. The gas layer with a sinusoidal outer interface and a circular inner interface is realized by the soap-film technique such that the initial condition is well controlled. Results show that the thicker the gas layer, the weaker the interface–coupling effect and the slower the evolution of the outer interface. Induced by the distorted transmitted shock and the interface coupling, the inner interface exhibits a slow perturbation growth which can be largely suppressed by reducing the layer thickness. After the reshock, the inner perturbation increases linearly at a growth rate independent of the initial layer thickness as well as of the outer perturbation amplitude and wavelength, and the growth rate can be well predicted by the model of Mikaelian (Physica D, vol. 36, 1989, pp. 343–357) with an empirical coefficient of 0.31. After the linear stage, the growth rate decreases continuously, and finally the perturbation freezes at a constant amplitude caused by the successive stagnation of spikes and bubbles. The convergent geometry constraint as well as the very weak compressibility at late stages are responsible for this instability freeze-out.


2020 ◽  
Vol 886 ◽  
Author(s):  
Yu Liang ◽  
Lili Liu ◽  
Zhigang Zhai ◽  
Ting Si ◽  
Chih-Yung Wen
Keyword(s):  


2020 ◽  
Vol 902 ◽  
Author(s):  
Rui Sun ◽  
Juchun Ding ◽  
Zhigang Zhai ◽  
Ting Si ◽  
Xisheng Luo

Abstract


Author(s):  
K. Fukushima ◽  
N. Kohyama ◽  
A. Fukami

A film-sealed high resolution environmental cell(E.C) for observing hydrated materials had been developed by us(l). Main specification of the E.C. is as follows: 1) Accelerated voltage; 100 kV. 2) Gas in the E.C.; saturated water vapour with carrier gas of 50 Torr. 3) Thickness of gas layer; 50 μm. 4) Sealing film; evaporated carbon film(20 nm thick) with plastic microgrid. 5) Resolving power; 1 nm. 6) Transmittance of electron beam; 60% at 100 kV. The E.C. had been successfully applied to the study of hydrated halloysite(2) (3). Kaolin minerals have no interlayer water and are basically non-expandable but form intercalation compounds with some specific chemicals such as hydrazine, formamide and etc. Because of these compounds being mostly changed in vacuum, we tried to reveal the structure changes between in wet air and in vacuum of kaolin minerals intercalated with hydrazine and of hydrated state of montmori1lonite using the E.C. developed by us.


2008 ◽  
Vol 6 ◽  
pp. 132-136
Author(s):  
O.R. Nurislamov

The paper deals with the problem of wall boundary flow with the formation of a thin vapor-gas layer near its surface. The possibility of reducing the resistance to liquid motion by means of the injection of a hot vapor-gas mixture from its surface is investigated.


Fuel ◽  
2010 ◽  
Vol 89 (11) ◽  
pp. 3193-3206 ◽  
Author(s):  
F.Y.A. El Kady ◽  
M.G. Abd El Wahed ◽  
S. Shaban ◽  
A.O. Abo El Naga

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