Exozodiacal discs with infrared interferometry

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Exozodiacal discs with infrared interferometry First results and perspectives * (post-doc at LAOG, Grenoble) and E. Di Folco (Obs. Geneva), J.C. Augereau (LAOG), V. Coudé du Foresto (Obs. Paris), A. Mérand (CHARA), D. Defrère (U. Liège)

Debris discs: towards warm dust Detected debris discs Far-IR, sub-mm, visible Cold and distant (~100 AU) Massive (few 100s Kuiper belt) Evidences for inner holes Zodiacal disc analogues? Inner planetary region Spitzer: first evidence for warm dust (~300 K) Sensitivity ~ 1000 zodi! Goal: direct imaging of exozodiacal discs Towards Darwin / TPF Marsh et al. 2005 (350 µm) 150 AU T 75 K 150 AU (150 AU 20 at 7.7 pc) Stapelfeldt et al. 2004 Kalas et al. 2005 (0.8 µm) Observing Planetary Systems ESO 5 March 2007 2

The challenges of direct imaging High contrast ( 1:100) Small angular separation Inner disc: a few 10 mas Requires IR interferometry? 40 K? 15 1500 300 K Macintosh et al. 2003 (Keck AO) Vega s SED (courtesy J-C Augereau) Observing Planetary Systems ESO 5 March 2007 3

Debris discs by interferometry Disc larger than angular resolution (λ/b) incoherent flux Induces a loss visibility at all baselines Best detected at short baselines (~10-30m) Flux ratio V 2 2 2J1( πbθ / λ) ( 1 2 f ) πbθ / λ Requires very good accuracy (~1%) Observing Planetary Systems ESO 5 March 2007 4

CHARA FLUOR Centre for High Angular Resolution Astronomy 34m Fibre Linked Unit for Optical Recombination K band (2.2µm) FoV: 1 arcsec 330m Our first target: Vega 1m collectors Observing Planetary Systems ESO 5 March 2007 5

Fitting a uniform-disc photosphere Vega Observing Planetary Systems ESO 5 March 2007 6

Fitting photosphere + debris disc Absil et al. 2006 Vega 3σ Observing Planetary Systems ESO 5 March 2007 7

Possible sources of near-ir excess Point-like source? RV and astrometry stable no companion Very low probability for background star Stellar wind? A stars: very weak winds (~10-12..14 M /yr) Circumstellar dust? Thermal emission & reflected flux Most probable explanation Need to check compatibility with literature Observing Planetary Systems ESO 5 March 2007 8

Reproducing the global Vega SED Using the debris disc models of Augereau et al. (1999) Absil et al. 2006 Observing Planetary Systems ESO 5 March 2007 9

Best-fit disc properties χ 2 maps for various disc models 2 fit parameters: minimum grain size (a min ) and inner radius (r 0 ) Small grains (mostly < 1 µm) at distances ~ 0.1 0.5 AU Highly refractive grains, no silicate feature carbons 50% Steep density power law: Σ(r) ~ r -4 (Solar System: r -0.3 ) χ 2 map 6 10-8 M 5 10-4 L 0.5 AU Observing Planetary Systems ESO 5 March 2007 10

Absil et al, in prep Survey: early-type stars 6-σ detection! α Crb A0V ζ Aql A0V γ Oph A0V β UMa A1V Observing Planetary Systems ESO 5 March 2007 11

Survey: early-type stars Absil et al, in prep σ Boo F2V η Crv F2V Vega is not an isolated case! Akeson et al: excess also around β Leo (A2V) Non-detections have a healthy behaviour Detection is not an instrumental effect! Observing Planetary Systems ESO 5 March 2007 12

Di Folco et al, in prep Survey: solar-type stars τ Cet G8V ε Eri K2V τ Cet (~10Gyr, G8V): also small C-rich grains! Where does all this dust come from? Small very short lifetime (radiation pressure) Need high replenishment rate Solar F-corona and zodiacal cloud are much weaker Augereau et al, in prep Observing Planetary Systems ESO 5 March 2007 13

Origin of the dust 1 st scenario: Falling Evaporating Bodies Proposed for β Pic (Beust & Morbidelli 2000) Local disc perturbation by a planet Production of star-grazing comets Needs replenishment (migration?) Secular perturbations in 4:1 MMR Courtesy H. Beust Observing Planetary Systems ESO 5 March 2007 14

Origin of the dust 2 nd scenario: Late Heavy Bombardment Dynamical re-arrangement of planets Global disc perturbation Injection of bodies from asteroid and Kuiper belts Collisions and evaporation Gomes et al. 2003 Reche et al., in prep Observing Planetary Systems ESO 5 March 2007 15

AMBER What s s next: VLTI (J), H and K band Good accuracy (FINITO) + closure phases MIDI N band silicates? Limited accuracy bright discs only 2 nd generation instruments VSI (near-ir) & MATISSE (mid-ir) More baselines increased efficiency Larger surveys are considered Observing Planetary Systems ESO 5 March 2007 16

Perspectives: nulling interferometry Cancel starlight by destructive interference VLTI-GENIE End-to-end simulation sensitivity: 50 100 zodi Instrument now discarded by ESA/ESO Dome C: ALADDIN Sensitivity: ~ 20 zodi (Absil et al., in prep) Towards Darwin Alcatel Alenia Space Observing Planetary Systems ESO 5 March 2007 17