Collisional influence on the differential Hanle effect method applied to the second solar spectrum of the A2Π-X2Σ+ (0, 0) band of MgH

Details Collisional influence on the differential Hanle effect method applied to the second solar spectrum of the A2Π-X2Σ+ (0, 0) band of MgH Collisional influence on the differential Hanle effect method applied to the second solar spectrum of the A2Π-X2Σ+ (0, 0) band of MgH

Nov 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006a%26a...458..625b&link_type=abstract

Astronomy and Astrophysics, Volume 458, Issue 2, November I 2006, pp.625-633

Astronomy and Astrophysics

Astrophysics

11

Sun: Magnetic Fields, Polarization

Scientific paper

Aims.This paper presents an analysis of the Q1,2(6-12) lines of the Q band of the A2Π-X2Σ+ (0, 0) transition of MgH, whose linear polarization was measured 4 arcsec inside the solar limb in a quiet region (North Pole) with THEMIS on 21 November 2004. Methods: .This analysis is performed as follows: a) the Hanle effect ΓH parameter is derived by applying the differential Hanle effect method between the two extreme pairs of lines. Assuming no depolarizing collisions, a magnetic field strength follows, which is found to be 9.2 Gauss, in agreement with previous observations of the same kind; b) this ΓH parameter is entered in a code solving the NLTE polarized radiative transfer equations, and the other depolarizing parameter, namely the depolarizing collision rate, is then derived by adjusting the computed polarization to the observed one. Thus an average value of the rate per colliding hydrogen atom α(2)=1.20 × 10-9 cm3 s-1 is obtained for the upper levels of the 12 lines (standard deviation 0.21 × 10-9 cm3 s-1). The corresponding model-dependent depolarizing rate is D(2)=(4.2 ± 0.7) × 107 s-1 at h=200 km; c) this depolarizing rate is now introduced in the conversion of the ΓH parameter in terms of magnetic field strength: an average turbulent field strength of 29 ± 12 Gauss is derived as the final value, at height h=200 ± 80 km where the polarization is formed. The Hönl-London factors of the lines under interest have been recalculated, leading to detect an error of a factor 2 in the recent literature. Results: .The derived value B=29 ± 12 Gauss at h=200 ± 80 km is in fairly good agreement with the previous determinations based on the interpretation of the Sr I 4607 Å limb polarization, which has led to fields in the range 35-60 Gauss. Conclusions: .Given the error bars, it seems unnecessary to put forward different formation regions for the Sr I and MgH lines.

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