1999
DOI: 10.1029/1999gl900281
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Diamagnetic effect produced by the Fluxus‐1 and ‐2 artificial plasma jet

Abstract: Abstract. The purpose of the Fluxus-1 and-2 active experiments is to study plasma jets injected parallel to the magnetic field and to study the interaction of these jets with the magnetic field. The experiments were conducted using a shaped-charge device, known as an explosive type generator (ETG), that produced an artificial aluminum plasma jet. In Fluxus -1 and-2 the jet was injected nearly parallel to the geomagnetic field at an altitude of 140 km toward an instrumented diagnostic payload located about 100 … Show more

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Cited by 22 publications
(7 citation statements)
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“…A similar effect was observed during the Fluxus 1 and 2 experiments. 11 In addition, an enhancement in the magnetic field was observed in front of the jet. This is possibly a result of a "snowplow" effect, where magnetic field lines are concentrated in front of the jet or a magnetosonic wave.…”
Section: Magnetic and Electric Fieldsmentioning
confidence: 97%
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“…A similar effect was observed during the Fluxus 1 and 2 experiments. 11 In addition, an enhancement in the magnetic field was observed in front of the jet. This is possibly a result of a "snowplow" effect, where magnetic field lines are concentrated in front of the jet or a magnetosonic wave.…”
Section: Magnetic and Electric Fieldsmentioning
confidence: 97%
“…The first plasma-jet experiment (ETG-1) occurred near apogee at an altitude of 360 km, and the second plasma-jet experiment (ETG-2) occurred on the downward trajectory at an altitude of 280 km ( Table 1). A canister of compressed air was released prior to the first plasma-jet experiment to investigate the role of the neutral atmosphere on jet ionization and to connect the results to the previous Fluxus experiments, 10,11 conducted at 150-km altitude.…”
Section: Experiments Overviewmentioning
confidence: 99%
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“…The problem of interest is to investigate the possibility of an appearance of charged dust particles in active rocket experiments which involve the release of some gaseous substance in near-Earth space. This can be reached using the scheme of the experiments analogous to that of the "Fluxus" and "North Star" experiments carried out in the ionosphere at altitudes of 140, 280, and 360 km [18][19][20]. The source for the charged particle release in the ionosphere in these experiments is the generator of high-speed plasma jets.…”
Section: Active Rocket Experimentsmentioning
confidence: 99%
“…Therefore, the plasma of the dusty ionosphere can be considered as a dusty (complex) plasma [5,13]. Dusty plasma in the ionosphere can also be formed [17] during active geophysical rocket experiments, which, e.g., use the scheme of the experiments "Fluxus" [18,19] and/or "North Star" [20] and involve the release of some gaseous substance in near-Earth space. Dusty plasmas present even in the lower atmosphere.…”
Section: Introductionmentioning
confidence: 99%