Burning voltage of self-sustained volume discharge in CO2 laser irradiated SF6 and mixtures of SF6 with C2H6

2006 ◽  
Author(s):  
A. A. Belevtsev ◽  
K. N. Firsov ◽  
S. Yu. Kazantsev ◽  
I. G. Kononov
Keyword(s):  
Volume Discharge ◽  
Burning Voltage

Self-sustained volume discharge

2000 ◽  
Vol 170 (3) ◽  
pp. 225 ◽  
Author(s):  
V.V. Osipov
Keyword(s):  
Volume Discharge

Formation of ArCl(B) molecules in a transverse volume discharge

1999 ◽  
Vol 25 (6) ◽  
pp. 433-434 ◽  
Author(s):  
A. K. Shuaibov ◽  
L. L. Shimon ◽  
A. I. Dashchenko ◽  
Yu. Yu. Neimet ◽  
I. V. Shevera
Keyword(s):  
Volume Discharge ◽  
Transverse Volume Discharge ◽  
Transverse Volume

scholarly journals Design of testing Method of Fuels Filling Measurement Instrument

2020 ◽  
Vol 202 ◽  
pp. 11001
Author(s):  
Ratna Purwaningsih ◽  
Susatyo Nugroho Widyo Pramono ◽  
Farhan Atoilah ◽  
Aan Aria Nanda ◽  
Azizah Dewi Suryaningsih
Keyword(s):  
Fluid Flow ◽  
Flow Measurement ◽  
Reporting System ◽  
Measurement Instrument ◽  
Volume Discharge ◽  
Flow Meters ◽  
Testing Method ◽  
Measurement Results ◽  
Color Detection ◽  
Measurement Devices

In this paper we have proposed a technique as a testing method for the instrument of measuring the amount of fuel filled in motorbike fuel tank. The instrument used a fluid flow meter that can be used easily by consumers to check the accuracy of gas station filler gauge. The study aims to develop a prototype of fluid flow measurement devices and a digital reporting system through IoT. The research phase consists of designing a fluid flow equipment, designing a color detection device, and designing a reporting system with IoT. Reporting application uses the smartphone system as a display of measurement results from flow meters and color detectors. Testing the function of the accuracy of the flow sensor on the tool is done by using a calibration factor. The output of measurements are fuel volume discharge, type of fluid and the result are shown on smartphone which connected to the internet for its reporting system.

Initiation of a high-power nonself-sustained volume discharge in molecular gases by ultraviolet radiation from a plasma cathode

1982 ◽  
Vol 12 (8) ◽  
pp. 1105-1107 ◽  
Author(s):  
Yu I Bychkov ◽  
D Yu Zaroslov ◽  
Nikolai V Karlov ◽  
G P Kuz'min ◽  
V V Osipov ◽  
...  
Keyword(s):  
Ultraviolet Radiation ◽  
High Power ◽  
Volume Discharge ◽  
Plasma Cathode ◽  
Molecular Gases

N2O laser pumped by a self-sustained volume discharge

1989 ◽  
Vol 19 (7) ◽  
pp. 839-840 ◽  
Author(s):  
V V Apollonov ◽  
G G Baĭtsur ◽  
I G Kononov ◽  
A M Prokhorov ◽  
S K Semenov ◽  
...  
Keyword(s):  
Volume Discharge ◽  
N2o Laser

Vizualization of 3D non-stationary flow in shock tube using nanosecond volume discharge

Shock Waves ◽  
2009 ◽  
pp. 533-538
Author(s):  
I.A. Znamenskaya ◽  
I.V. Mursenkova ◽  
T.A. Kuli-Zade ◽  
A.N. Kolycheva
Keyword(s):  
Shock Tube ◽  
Stationary Flow ◽  
Volume Discharge

Initiation of glacier surges

1969 ◽  
Vol 6 (4) ◽  
pp. 919-928 ◽  
Author(s):  
G. de Q. Robin
Keyword(s):  
Water Film ◽  
Ice Thickness ◽  
Volume Discharge ◽  
Ablation Zone ◽  
Critical Limit ◽  
Bedrock Topography ◽  
Steady Rate ◽  
Compressive Flow ◽  
Glacier Surges ◽  
Glacier Flow

Three types of instability leading to glacier surges have been suggested, namely stress instabilities, temperature instabilities, and water-film instabilities. Evidence of approximately equal volumes of ice being involved in repeated surges of the same glacier favors stress instabilities as the most likely cause. Since for a steady rate of discharge a section of a glacier undergoing extending flow tends to be of the order of thirty meters thicker than for compressive flow under otherwise similar conditions, it is suggested that surges originate when the glacier flow switches between these two modes of flow. In the accumulation zone of a glacier, a surge would be triggered off by a change from extending to compressive flow over a length of the glacier. If the volume of ice and movement velocities involved are sufficiently large this could lead to repeated surging, although a tendency to stability appears to exist. In the ablation zone, the tendency to change modes of flow would be preceded by a period during which the lower part of the glacier acts as a rigid, sliding dam and increases ice thickness upstream. In this zone, if the volume discharge of the glacier increases beyond a critical limit that depends on bedrock topography, it would initiate a surge.

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