LACK OF THERMAL-EQUILIBRIUM BETWEEN H+ AND O+ TEMPERATURES IN THE VENUS NIGHTSIDE IONOSPHERE

Citation
Wc. Knudsen et al., LACK OF THERMAL-EQUILIBRIUM BETWEEN H+ AND O+ TEMPERATURES IN THE VENUS NIGHTSIDE IONOSPHERE, J GEO R-S P, 102(A2), 1997, pp. 2185-2191
Citations number
22
Categorie Soggetti
Geosciences, Interdisciplinary","Astronomy & Astrophysics","Metereology & Atmospheric Sciences
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
ISSN journal
21699380 → ACNP
Volume
102
Issue
A2
Year of publication
1997
Pages
2185 - 2191
Database
ISI
SICI code
2169-9380(1997)102:A2<2185:LOTBHA>2.0.ZU;2-8
Abstract
Analysis of orbiter retarding potential analyzer (ORPA) ion data recor ded in the nightside Venus hydrogen bulge region has revealed that the temperature of the H+ ions is substantially cooler by approximately 2 000 degrees K than that of the O+ ions above 200 km altitude. Below 20 0 km altitude the H+ and O+ temperatures cross, with the H+ temperatur e becoming the hotter temperature. Frequently, the velocity distributi on of the H+ ions appears to be non-Maxwellian with too large a fracti on of the ions having small velocities. We suggest that this may be th e result of H+ ions, created from charge exchange collisions, not havi ng completely thermalized with the ambient H+ gas. Charge exchange col lisions between cold neutral hydrogen atoms at a temperature of 100 de grees K and the hot O+ and H+ ion gases create H+ ions at a temperatur e of 100 degrees K. The temporal and spatial extent of the cooled H+ g as has not been investigated in this study. We have attempted to under stand the processes responsible for the observed temperature behavior by solving numerically the coupled electron, H+, and O+ energy equatio ns in one-dimensional form. Neglecting convective transport terms but including for the first time cooling processes resulting from charge e xchange between H+ and O+ ions with cold neutral hydrogen atoms and us ing separate H+, O+, and electron thermal conductivities corrected for collisions, we have obtained temperature profiles for the H+ and O+ g ases which are consistent with the observed profiles. The process prim arily responsible for the observed behavior of the H+ acid O+ temperat ures appears to be the difference in the thermal conductivity of the t wo ion gases with the thermal conductivity of H+ being several times l arger than that of O+ given the same temperature and density. This res ult must be tempered with the fact that several processes or condition s, which may be important, have been neglected.