1981
DOI: 10.1029/ja086ia04p02443
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Unstable potential of geosynchronous spacecraft

Abstract: The potential of a geosynchronous spacecraft and of various portions of its surface may become unstable and undergo large potential jumps. A time varying strongly non‐Maxwellian plasma and secondary electron emission play key roles in the theory.

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Cited by 11 publications
(5 citation statements)
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References 3 publications
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“…The concept of critical temperature T., although derived for environments modeled with single Maxwellian distributions, remains useful and important when the plasma environment is described as double Maxwellian [Besse, 1981;Laframboise and Kamitsuma, 1983]. The applicability of this concept is developed here by showing that the current JT behaves as illustrated in Figure 1 These data are chosen because during the data period the lower-temperature Maxwellian electron density steadily decreases by as much as a decade while all other environmental parameters, n2, T•, and T2, practically remain constant.…”
Section: The Role Of Critical Temperaturementioning
confidence: 99%
See 1 more Smart Citation
“…The concept of critical temperature T., although derived for environments modeled with single Maxwellian distributions, remains useful and important when the plasma environment is described as double Maxwellian [Besse, 1981;Laframboise and Kamitsuma, 1983]. The applicability of this concept is developed here by showing that the current JT behaves as illustrated in Figure 1 These data are chosen because during the data period the lower-temperature Maxwellian electron density steadily decreases by as much as a decade while all other environmental parameters, n2, T•, and T2, practically remain constant.…”
Section: The Role Of Critical Temperaturementioning
confidence: 99%
“…ambient charged particles (see, for example, Garrett [1981]). The triple-root current-voltage characteristic has a simple explanation in terms of the concepts of critical temperature and double Maxwellian distributions [Besse, 1981;Laframboise et al, 1982;Laframboise and Kamitsuma, 1983]. The relation between current and voltage can be given by a simple plasma probe model [Mott-Smith and Langmuir, 1926], which we use because of its simplicity.…”
mentioning
confidence: 99%
“…In this paper we shall examine another type of differential charging due to the fact that in non-Maxwellian plasmas certain material may have double-valued potentials [Prokopenko and Laframboise, 1980;Sanders and lnouye, 1978;Besse, 1981]. This implies that adjacent isolated surfaces made of the same material may follow different charging histories and end up on different solutions of the current balance condition.…”
Section: Introductionmentioning
confidence: 99%
“…The zero current points at -18 V and +3100 V correspond to stable equilibria. The zero current point at 17 V is unstable; if secondary electrons can escape, a surface that starts at a voltage below 17 V will go toward -18 V; a surface that starts above 17 V will go towards +3100 V. (The existence of multiple roots has been discussed previously by several authors [Prøkopenko and Lafrarnboise, 1977;Besse, 1981] for non-Maxwellian spectra.) However, as we saw in the positive ground calculations, the highest possible positive voltage equilibrium point is frequently not achieved because as the Surface voltage nears that of the underlying ground, the direction of the surface electric field changes sign, suppressing the secondary electron emission.…”
Section: Solar Cell 'Snapover'mentioning
confidence: 89%