791 |
Ion transport theory for a strongly rotating beam injected tokamak plasmaNeeley, Gary William 05 1900 (has links)
No description available.
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792 |
Particle and momentum confinement in tokamak plasmas with unbalanced neutral beam injection and strong rotationMalik, Muhammad Afzaal 08 1900 (has links)
No description available.
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793 |
Generation of induction heated, seeded hydrogen plasmas at one atmosphere pressure.Benns, Robert Allan 08 1900 (has links)
No description available.
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794 |
Particle transport theory with ICRH and ECRh in tokamaksIndireshkumar, K. 12 1900 (has links)
No description available.
|
795 |
Spectroscopic diagnostics of a plasma in a rotating magnetic fieldFrierson, Robert V., Jr. 12 1900 (has links)
No description available.
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796 |
Plasma torch interaction with a melting substrateHill, S. D. 08 1900 (has links)
No description available.
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797 |
An experimental study of ion behavior in the advanced toroidal facilityWade, Mickey Ray 12 1900 (has links)
No description available.
|
798 |
Radiation absorption correction in the measurement of temperature in a 30 atmosphere air arcSalmon, Joseph Thaddeus 05 1900 (has links)
No description available.
|
799 |
A three-dimensional mechanistic model of steam condensers using porous medium formulationAl-johani, Mohammed S. 05 1900 (has links)
No description available.
|
800 |
A study of atmospheric properties and their impact on the use of the nocturnal boundary layer budget technique for trace gas measurement /Mathieu, Nathalie January 2004 (has links)
While most micrometeorological measurement techniques are only suitable for windy conditions, the Nocturnal Boundary Layer Technique can be used to measure trace gas flux during calm, clear nights as the nighttime stability enables gas emitted at the ground to accumulate. The difference between two measurements over the whole depth of this layer is believed to integrate emissions from a large area representative of, in this study, an agricultural farm. A tethersonde and infrared gas analyzer attached to a blimp carrying a bag sampling system monitored atmospheric variables for each ascent during two summer field campaigns. A mini-SODAR was installed in the field to obtain the wind flowfield. Strong accumulation was observed under low level jets suggesting that this feature acts as a good lid for trace gases. An average background vertical motion different from zero seemed to have more influence on gas propagation than did intermittent turbulence. On at least one night, a density current created by the nearby St-Lawrence River was observed to influence measurements.
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