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Luca Belluzzi 1 and Javier Trujillo Bueno 2

A possible mechanism for understanding the enigmatic scattering polarization signals observed in the solar Na I and Ba II D 1 lines. Luca Belluzzi 1 and Javier Trujillo Bueno 2. 1 Istituto Ricerche Solari Locarno, Switzerland 2 Instituto de Astrofísica de Canarias, Tenerife, Spain.

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Luca Belluzzi 1 and Javier Trujillo Bueno 2

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  1. A possible mechanism for understanding the enigmatic scattering polarization signals observed in the solar NaI and BaII D1 lines Luca Belluzzi1 and Javier Trujillo Bueno2 1 Istituto Ricerche Solari Locarno, Switzerland 2 Instituto de Astrofísica de Canarias, Tenerife, Spain COST Action MP1104 WG2 Meeting: Theory and modelling of polarisation in astrophysics Prague, Czech Republic, 5–8 May 2014

  2. Observations of the NaI D1 line (5896Å) Observations in quiet regions close to the limb (=0.1) with ZIMPOL at NSO Kitt Peak From Stenflo & Keller 2000, A&A, 355, 789 Observation near the north polar limb (3 April 1995). From Stenflo & Keller 2000, A&A, 355, 789 Thick line (smaller peak): same as left panel. Thin lines (larger peaks): two observations at different locations near the south polar limb (12 September 1996).

  3. Observations of the BaII D1 line (4934Å) Observations in quiet regions close to the limb (=0.1) with ZIMPOL at NSO Kitt Peak From Stenflo & Keller 2000, A&A, 355, 789 Two observations at different locations near the north polar limb (4 and 5 April 1995). Three observations at different locations near the south polar limb (12 September 1996). Thick line: average profile From Stenflo & Keller 1997, A&A, 355, 789 Observation near the north polar limb (April 1995).

  4. Observations from the atlas of the Second Solar Spectrum Observations in quiet regions close to the limb (=0.1) with ZIMPOL at IRSOL Na I D1 Ba II D1 From Gandorfer 2000, The Second Solar Spectrum, vol.I From Gandorfer 2000, The Second Solar Spectrum, vol.I

  5. A recent observation of the NaI D1 line at IRSOL Observation in a quiet region close to the north polar limb (=0.1) with ZIMPOL3 at IRSOL Observation carried out on March 13, 2014 Exposure time: 1400s (~23min) Signal averaged over about 8 arcsec

  6. Non-LTE RT calculations in FAL-C Sodium (1 stable isotope) 23Na (100%)I=3/2 Ju=1/2 Fu= 2 Fu= 1 Barium (7 stable isotopes) 130Ba (0.1%)I=0 132Ba (0.1%)I=0 134Ba (2.4%)I=0 Fu= 2 135Ba (6.6%)I=3/2 Jl=1/2 136Ba (7.9%)I=0 137Ba (11.2%)I=3/2 138Ba (71.7%)I=0 Fu= 1 How can atomic alignment be induced in the upper HFS levels? Intrinsically unpolarizable line for linear polarization The atomic transition Levels with J=1/2 cannot harbour atomic alignment (population umbalances between sublevels with different values of |M|)

  7. No alignment can be induced in the upper HFS F-levels =0 (K=2, Ju=1/2) =0 (K=2, Ju=1/2) CRD theory of polarization (see Landi Degl’Innocenti & Landolfi 2004) • Hypotheses: • the various HFS components are “pumped” by the same radiation field (hypothesis required by the CRD theory to hold when F-state interference is included) • no atomic polarization is present in the lower level (ground level)

  8. No alignment can be induced in the upper HFS F-levels Wavelength position of the 4 HFS components Metalevel theory (coherent scattering) (see Landi Degl’Innocenti et al. 1997) • Hypotheses: • the various HFS components are “pumped” by the same radiation field • no atomic polarization is present in the lower level (ground level)

  9. Fu= 3 Fu= 2 Ju=3/2 Fu= 1 Fu= 0 D2 Jl=1/2 Fu= 2 Presence of atomic alignment Ju=1/2 Fu= 1 D1 Fl= 2 Fl= 1 The results of Landi Degl’Innocenti (1998) (Nature, 392, 256) • Hypotheses: • Coherent scattering (metalevel theory) 2) D1+D2 system studied accounting for interference between magnetic sublevels of different F-levels, pertaining either the same J-level or to different J-levels 3) the various HFS components of each D-line are “pumped” by the same radiation field 4) YES atomic polarization in the lower level (parametrized) Repopulation pumping mechanism via the D2 line (Trujillo Bueno et al. 2002, Casini et al. 2002)

  10. (from Landi Degl’Innocenti, 1998) BUT: • The required amount of atomic polarization in the long-lived lower level is incompatible with the presence of inclined magnetic fields with intensities larger than about 0.01G (lower level Hanle effect). • (Landi Degl’Innocenti 1998) • This result was later refined by Trujillo Bueno et al. (2002) through a deeper analysis of the sensitivity of the atomic polarization in the levels of the D1 line to the presence of a magnetic field.

  11. (from Landi Degl’Innocenti, 1998) BUT: • Kerkeni and Bommier (2002) argued that the required amount of atomic polarization in the long-lived lower level appears to be incompatible with the rates of depolarizing collisions that they obtained through quantum chemistry calculations.

  12. Hypotheses: 1) Two-level model atom with HFS Jl=1/2 Fu= 2 Ju=1/2 Fu= 1 D1 Fl= 2 Fl= 1 Missing “ingredient”: accounting for the (small) variation of the incident radiation field among the various HFS components of the D1 line 2) Unpolarized and infinitely-sharp lower levels 3) Coherent scattering in the atom rest frame + Doppler redistribution in the observer’s frame (angle-averaged redistr. matrix derived from metalevel theory) 4) Numerical solution of the full non-LTE problem accounting for the variation of the incident field among the various HFS components.

  13. CRD vs CS calculations (FAL-C, =0.1) Physical origin of the Q/I signal in the CS calculations: different pumping radiation field in the various HFS components.

  14. Monochromatic anisotropy at the height where τ=1 for =0.1 The Q/I signal obtained in the BaII D1 line is much larger than the one obtained in the NaI D1 line because the HFS splitting of the lower level of BaII is about four times larger than that of the lower level of NaI

  15. Calculations in various atmospheric models (=0.1)

  16. Problems: 1) Although there is a dependence on the atmospheric model, this mechanism should always be at work, while observations do not always show clear scattering polarization signals in the core of these lines (in particular in the core of the BaII D1 line). Conclusions A mechanism capable of producing a scattering polarization signal in the core of the BaII and NaI D1 lines, which does not require the presence of atomic polarization in the lower level, has been identified. 2) The peak of the calculated profiles is slightly shifted with respect to the line center, were the calculated signal is still zero. The observed peaks (in particular the one of NaI D1) are centerd at the line center. 3) The amplitude of the calculated NaI D1 peak is smaller than that of the observations presented by Stenflo & Keller (1997, 2000).

  17. Conclusions Our calculations do not include: -depolarization and frequency redistribution effects due to collisions. These effects are expected to be more important in the line core of BaII D1, which forms deeper in the atmosphere than NaI D1 (need of a more appropriateRIII redistribution matrix for taking these effects into account). -depolarization effect due to a magnetic field (Hanle effect). -lower level polarization, which may in any case be present (mainly in NaI D1, though in a less amount than in Landi Degl’Innocenti 1998), and may contribute to produce a symmetric profile; -J-state interference, which, in the case of NaI D1, are known to significantly modify the overall Q/I pattern across D1; -frequencyredistribution of continuum radiation: as pointed out by Del Pino Aleman et al. (2014) redistribution phenomena of the continnum radiation are capable of producing observables symmetric signals in the core of intrinsically unpolarizable lines. This latter mechanism depends on the assumed atmospheric model, but it may well coexist with the mechanism presented in this talk.

  18. Ju=3/2 Ju=3/2 Ba II Ju=1/2 Ju=1/2 D2 D1 D2 D1 Na I Jm=5/2 Jm=3/2 Jl=1/2 Jl=1/2 Conclusions -the impact of metastable levels (for the case of BaII D1)

  19. PRD calculations: Core: PRD ≈ CS Wings: PRD CRD CRD vs CS vs PRD calculations

  20. PRD calculations in various atmospheric models (=0.1)

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