Abstract

Abstract. We are presenting a semi-classical theory of the impact polarization due to a quadrupolar electric excitation, which is the case of this forbidden line. In addition, this line is also radiatively forbidden being a triplet-singlet transition. This last feature is overcome by scaling the semi-classical result to a full quantum calculation at a single energy value. The cross-section and impact polarization are thus obtained as a function of energy, in agreement with the quantum calculations that exist only for the cross-section. The behavior of the impact polarization is found to be quite different than that of the usual dipolar electric interaction. Let us denote as radial the polarization parallel to the incident beam or magnetic field, and as tangential the perpendicular polarization. In the case of the dipolar electric interaction (permitted lines), the polarization is radial at low energy, and tangential at high energy, and it vanishes at energy about twelve times the threshold energy. In the case of the quadrupolar electric interaction, we observe quite different behavior, with the polarization vanishing point much closer to the threshold energy. This leads us to reanalyze the auroral red line polarization observation by Lilensten et al. (2008). From polarization observations made at Svalbard, they conclude to a rather strong tangential polarization observed during a 4-h recording including two auroral events. The existence of tangential polarization is questioned by our new theory, which leads to reconsidering the contribution of scattered parasitic light from a neighboring city that was mentioned but discarded by the authors. Finally, we conclude that the line is only weakly radially polarized by electron impact, and only during the auroral events. The weak polarization level leads to taking the competing depolarization by collisions with the neighboring O atoms into account, and by the competing isotropical (thus depolarizing) processes for populating the line upper level: the dissociative recombination of O2+ colliding with thermal electrons, and above all the reaction N(2D)+O2. The final diagnostic could be a density determination by depolarization, but it may be rather complicated because it involves several species.

Highlights

  • Since the auroral intense red and green lines, which are forbidden lines of neutral Oxygen, are formed by collisional excitation due to electrons coming from the Sun and propagating along the local magnetic field lines, they are prime candidates for displaying impact polarization as a result of their excitation by directed particles

  • In the case of the dipolar electric interaction, the polarization is radial at low energy, and tangential at high energy, and it vanishes at energy about twelve times the threshold energy

  • The agreement between our results and the ones of Barklem (2007) shows that the behavior of the crosssection and impact polarization as a function of the energy of the incoming electron can be confidently modelled with our approach in which a single energy point is taken from the full quantum calculation

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Summary

Introduction

Since the auroral intense red and green lines, which are forbidden lines of neutral Oxygen, are formed by collisional excitation due to electrons coming from the Sun and propagating along the local magnetic field lines, they are prime candidates for displaying impact polarization as a result of their excitation by directed particles. Only m = 0 excitation occurs that leads to π polarization emission (i.e. parallel to the quantization axis which is the electron propagation average direction, which is the magnetic field direction) This result, valid for a permitted line, has to be sign changed (tangential polarization) for dipolar magnetic emissions like the auroral red line. It has to vanish in between and this occurs at the energy about twelve times the threshold energy, regardless of whatever element can be seen in all these figures Assuming that this remains valid for the O I red line, but changing the sign of the polarization according to the dipolar magnetic character of this line emission, the conclusion of Lilensten et al (2006, 2008) would be supported with tangential polarization at low incident electron energy that weakens when the energy increases. This is the object of the present paper, which is organized as follows: Sect. 2 is devoted to model the impact polarization, and Sect. 3 to the reanalysis of the observations of Lilensten et al (2008)

The O I 6300 Aline: a doubly forbidden line
Taking into account the triplet-singlet transition
The results: the cross-section
The results: the impact polarization
Auroræ physics: reinterpretation of the observations
Duncan’s observation
Conclusion
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