Dust Polarization. J.Ph. Bernard Institut de Recherche en Astrophysique et Planetologie (IRAP) Toulouse

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Transcription:

Dust Polarization J.Ph. Bernard Institut de Recherche en Astrophysique et Planetologie (IRAP) Toulouse 1

Layout - Dust polarization (Extinction) - Dust polarization (Emission) - Dust polarization observational evidences - Planck results on dust polarization (what can be shown) - Instrumental considerations 2

The Planck Consortium The Planck Collaboration, includes individuals from more than 50 scientific institutes in Europe, the USA and Canada Planck is a project of the European Space Agency -- ESA -- with instruments provided by two scientific Consortia funded by ESA member states (in particular the lead countries: France and Italy) with contributions from NASA (USA), and telescope reflectors provided in a collaboration between ESA and a scientific Consortium led and funded by Denmark. 3

Dust Emission There is no single model to explain dust emission Compiegne et al., (2011) PAH VSG BG There is a consensus that NIR emission is produced by large molecules or very small dust particles (PAH) MIR is due to intermediate size grains, which nature is uncertain Even for Big Grains, the composition is uncertain BG necessarily include Silicates Silicates in BG is amorphous (from extinction) BG also probably include Carbonaceous material (Amorphous Carbon, Graphite,...) It is currently unclear if these 2 components are separate or part of the same dust grains 4

Dust Polarization BG: - Rotating, elongated and align partially on B - Produce polarized emission & extinction extinction // to B From extinction polarization: - 2200 Å bump and FUV rise, DIBs not polarized ==> PAH & VSG: are unlikely to be aligned (too small) - 3.4 mic feature not polarized ==> Carbonaceous BG may not align or may be spherical - 10-20 mic feature is polarized ==> Silicate grains aligned and elongated emission to B Draine & Fraisse 2009 Possible alignment mechanisms: - Paramagnetic relaxation alignment - Radiative Alignment Torques Grain disalignment by: - Gas/grain collisions - Plasma drag 5

Dust Polarization Compiegne et al., (2011) Draine & Fraisse 2009 PAH VSG BG Spherical Graphite Same b/a polarization in emission is predicted ~10-15% Compiegne et al., (2011) Various possible models lead to different predictions in polarization Variations of polarization fraction with frequency will help constrain dust models 6

Submm Emissivity Variations Large variations of the sub-mm emissivity are observed between the MW, the LMC and the SMC Such variations also seem to happen within the MW Planck Collaboration 2011, A&A 536, A17 LMC SMC MW The dust emissivity law seem to flatten above ~500 microns (MW, some low metalicity galaxies) The origin is unclear and could in principle be due to: - Existence of extremely cold dust - Modified optical dust properties In dense regions, dust aggregates, which also changes its emissivity properties Normalized at 100 µm Paradis et al. 2009 β 2.8 β=1.2 β=1.5 β=1.8 β 2.1 Neutral Molecular Very Small Grains Large Grains HERSCHEL PLANCK 7

Exemple of SMC SMC: 70 GHz SMC: CMB subtracted SMC excess map (3mm) - Free-Free contribution subtracted, extrapolated from Hα emission, assuming no extinction - Submm excess follows the spatial distribution of thermal dust at high frequencies - Best fit obtained for a combination of the Two-Level System (TLS) model and spinning dust - Amorphous grains with similar parameters as MW, but more amorphous than in MW - Spinning dust parameters compatible with PAH emission in the SMC TLS+spinning Planck Collaboration 2011, A&A 536, A17 (C. Author J.-Ph. Bernard) 8

Dust Polarization Two-Level Systems Planck Collaboration 2011, A&A 536, A17 Magnetic nanoparticles Draine et al. 2011, 2012 TLS+spinning Various possible models lead to different predictions in polarization For instance : - The TLS model would not require variations of p with frequency (same grains) - Free-flying magnetic nanoparticle model will produce larger p at long wavelengths - Magnetic nanoparticle inclusion in BG will produce lower p at long wavelengths See presentation by B. Draine 9

Spatial variations of p Dust Polarization - Ground submm measurements (restricted to bright regions) indicate low values (usually a few %) - However, Archeops claimed 10-15% in the plane (2nd Galactic Quadrant) - p variations are difficult to analyze because: + affected by on-sky B field geometry + affected by 2nd angle + affected by bias (noise dependent) - is there a single (intrinsic) true p value affected only by B structure? 850 µm OMC-3 in Orion A Archeops polarization map @ 353 GHz Data from Ponthieu et al. 2005 10

spatial variations of p Dust Polarization There should be large scale variations of p due to B field structure of the MW depolarization effect (G factor) as predicted by PSM Based mainly on Synchrotron measurements Delabrouille et al. in prep 11

spatial variations of p Variation of p with intensity Seen in most ground submm data Matthews et al. 2002 LBS 23N Dust Polarization Matthews et al. 2002 Correlation between p and tau (NH)? Correlation between p and T? Will be searched for systematically in Planck data could help dissociate if a B effect or alignment effect 12

spatial variations of p Variation of p with NH Cho & Lazarian 2005 Dust Polarization Cho et Lazarian (2005) Radiative Alignment Torques (RAT) in dense cores illuminated by external ISRF Depolarisation as a function of depth Also a function of grain size. Could explain existing observations Cho & Lazarian 2005 Variation of p could also be due to B field structure only Requires comparison to MHD & rad. transfer simulations 13

spatial variations of p Evidence for RATs? Around HD97300 (Chamaeleon I) Andersson et al. 2011 Dust Polarization colder & more polarized Andersson et al. 2011 warmer & less polarized Existing evidence in one object from Vis Will be searched for systematically with Planck 14

Variations of p with Wavelength? Dust Polarization This is probably the main question of interest for Polarization component separation. Some information in the dense ISM - Existing measurements indicate lowest p at around 250 microns - Requires 2 T components with higher T best aligned or difference in emissivity - This result is questionned (different instruments, objects,...) - p variations with wavelength are difficult to analyze because: + Affected by bias (noise dependent) which is strongly band dependent (steep dust SED) Little to no information in the diffuse ISM (Planck will do) 15

Dust Polarization Variation of p(wav) with NH From Vaillancourt 2008 P(850)/P(450) P(850)/P(450) drops at high NH in OMC-1 16

Is AME dust polarized? Dust Polarization This is also important for Polarization component separation. AME is likely Spinning dust Therefore likely due to PAH or VSG Therefore, should not be strongly polarized Existing measurement show p<2% (Battistelli et al., 2006; Lopez- Caraballo et al., 2011; Dickinson, Peel, & Vidal, 2011) As Planck measures AME very well, constraints on AME polarization should be quite efficient Planck Collaboration 2011, A&A 536, A20 (C. author C. Dickinson) 17

polar angle vs ISM filaments Dust Polarization Some ISM filamentary structure show apparent connection with magnetic field...... although the two examples shown here (only a few degrees apart on the sky) give opposite filament orientation w.r.t. B field The planck data will allow to test this with much more statistics than stellar absorption measurements allow. 18

From data to Stokes parameters Planck scanning the sky Planck/HFI focal plane Derivation of Stokes parameters (I, Q and U) involves the combination of two pairs of PSB bolometers that observe the same sky positions within a few seconds. The polarizers of the second pair are rotated by 45 with respect to the first pair. Multiple scans and multiple surveys provide Q and U measurements with different orientation. Maps of Q and U and their standard deviations are inferred from the multiple measurements. 19

Planck Polarization Sensitivity Pelkonen et al. 2007 353 GHz Limitations to Planck dust polar measurements? - Bandpass mismatch on Dust emission - CO contribution (100, 217, 353 GHz) - Effect of noise (and bias), in particular at low freq - Systematic effects : Optical effects (FSL, beams in Q vs U,...) Component separation (Dust vs CMB, Synch, free-free, AME,...) 20

Coming soon : Pilot Dust emission polarization at 240 and 500 microns First launch forseen in 2014 http://pilot.irap.omp.eu 21

Instrumental considerations propagation of linear polarization in the Pilot experiment (These C. Engel) - The propagation of polarization modes in a given instrument is a complex problem - Today, we have little automated tools to simulate this and run MC analysis to optimize instruments - Several problems arise in instruments (intercalibration, band mismatch, beam mismatch, etc...) - Such detailed models are also needed for data analysis - Full End-to-end tests of the instrument in polarization are needed 22

Conclusions Dust polarization results from complex processes Various possible models lead to different predictions in polarization We don t really know how difficult the foreground correction will be The main questions are : -1 How does p varies with frequency? -2 How stable is this on the sky? -3 What is the intensity of dust polarization? If 1 and 2 unfavorable, good physical understanding will be needed Planck will answer those questions Polarization is hard to measure. We probably miss dedicated optical software We need very precise end-to-end instrument calibration We miss precise natural and/or artificial calibration sources (p and angle) 23