galaxy scale agn outflows two puzzles two solutions
play

Galaxy-Scale AGN Outflows: Two Puzzles, Two Solutions Claude-Andr - PowerPoint PPT Presentation

Galaxy-Scale AGN Outflows: Two Puzzles, Two Solutions Claude-Andr Faucher-Gigure UC Berkeley Miller Institute for Basic Research in Science with Eliot Quataert & Norm Murray The possible roles of AGN feedback Establish correlations


  1. Galaxy-Scale AGN Outflows: Two Puzzles, Two Solutions Claude-André Faucher-Giguère UC Berkeley Miller Institute for Basic Research in Science with Eliot Quataert & Norm Murray

  2. The possible roles of AGN feedback Establish correlations between Truncate star formation SMBH and galaxy properties Salim+07 Gultekin+09 Models that assume f ~5% L AGN couples to ISM are successful in explaining in these observations

  3. Observational breakthroughs on AGN outflows Mrk 231 • km/s Massive, galaxy-scale AGN outflows in local ULIRGs ➡ neutral, ionized, CO, OH, HCN, ... Rupke & Veilleux 11 • Herschel, E-VLA, ALMA, ... to kpc CO revolutionize this field 0.03 0.02 • 0.01 Physical conditions in QSO outflows using low-ion BALs ( ⇒ energetics) 0 Feruglio+10 -1000 -500 0 500 1000 Velocity [Km/s]

  4. Physical conditions in luminous QSO atomic outflows • Photoionization modeling particularly constraining in QSOs with FeII* broad line absorption ( T ~10 4 K, v ~5,000 km/s; FeLoBALs): SDSS J0318-0600 n e ~ 10 4 cm -3 Δ R ~0.01 pc (absorber thickness) N H ~ 10 20-21 cm -2 R~ 1-3 kpc (distance from SMBH) ionization param Dunn+10 Observations from Moe+09, Dunn+10, Bautista+10, Arav 10

  5. Physical conditions in luminous QSO atomic outflows • Photoionization modeling particularly constraining in QSOs with FeII* broad line absorption ( T ~10 4 K, v ~5,000 km/s; FeLoBALs): n e ~ 10 4 cm -3 Δ R ~0.01 pc (absorber thickness) N H ~ 10 20-21 cm -2 R~ 1-3 kpc (distance from SMBH) ionization param Observations from Moe+09, Dunn+10, Bautista+10, Arav 10

  6. Physical conditions in luminous QSO atomic outflows • Photoionization modeling particularly constraining in QSOs with FeII* broad line absorption ( T ~10 4 K, v ~5,000 km/s; FeLoBALs): ⇒ Δ R/R ~10 -5 n e ~ 10 4 cm -3 Jupiter mass! Δ R ~0.01 pc (absorber thickness) N H ~ 10 20-21 cm -2 R~ 1-3 kpc (distance from SMBH) ionization param Observations from Moe+09, Dunn+10, Bautista+10, Arav 10

  7. Physical conditions in luminous QSO atomic outflows • Photoionization modeling particularly constraining in QSOs with FeII* broad line absorption ( T ~10 4 K, v ~5,000 km/s; FeLoBALs): ⇒ Δ R/R ~10 -5 n e ~ 10 4 cm -3 Jupiter mass! Δ R ~0.01 pc (absorber thickness) N H ~ 10 20-21 cm -2 R~ 1-3 kpc (distance from SMBH) ionization param 1. What are these things? 2. How can we use them to measure outflow energetics? Observations from Moe+09, Dunn+10, Bautista+10, Arav 10

  8. Compact absorbers must form in situ, at R ~kpc from SMBHs • If they traveled from the SMBH to their implied location... ◆ − 1 ✓ ◆ ✓ t flow ≈ R R v v ≈ 3 × 10 5 yr 10 , 000 km s − 1 3 kpc • But destroyed by hydro instabilities and thermal evaporation in t KH , t evap ∼ few × 10 3 yr Not a direct accretion disk wind! CAFG, Quataert, & Murray 12

  9. Radiative shock model • Form in interaction of the QSO blast wave with an ISM clump: v sh v sh v sh T sh ~ v sh 2 T sh ~ v sh 2 n H c,i , T c i v sh,c a n H c,f , T c f n H pre , T pre Shock wave propagates in cloud on At t>t KH , t drag , original cloud is shredded QSO blast wave encounters moderately crushing time t cc , cloud is destroyed into cloudlets traveling at ~v sh and cloud crushing by QSO dense ISM cloud. by K-H in t KH ~20t cc , and is accelerated compressed by hot post-shock gas. absorption by transient, to ~v sh in t drag . blast, accel by ram pre-existing ISM cloud compressed shreds pressure CAFG, Quataert, & Murray 12

  10. Radiative shock model • Form in interaction of the QSO blast wave with an ISM clump: v sh v sh v sh T sh ~ v sh 2 T sh ~ v sh 2 n H c,i , T c i v sh,c a n H c,f , T c f n H pre , T pre Shock wave propagates in cloud on At t>t KH , t drag , original cloud is shredded QSO blast wave encounters moderately crushing time t cc , cloud is destroyed into cloudlets traveling at ~v sh and cloud crushing by QSO dense ISM cloud. by K-H in t KH ~20t cc , and is accelerated compressed by hot post-shock gas. absorption by transient, to ~v sh in t drag . blast, accel by ram pre-existing ISM cloud compressed shreds pressure CAFG, Quataert, & Murray 12

  11. Radiative shock model • Form in interaction of the QSO blast wave with an ISM clump: v sh v sh v sh T sh ~ v sh 2 T sh ~ v sh 2 n H c,i , T c i v sh,c a n H c,f , T c f n H pre , T pre Shock wave propagates in cloud on At t>t KH , t drag , original cloud is shredded QSO blast wave encounters moderately crushing time t cc , cloud is destroyed into cloudlets traveling at ~v sh and cloud crushing by QSO dense ISM cloud. by K-H in t KH ~20t cc , and is accelerated compressed by hot post-shock gas. absorption by transient, to ~v sh in t drag . blast, accel by ram pre-existing ISM cloud compressed shreds pressure CAFG, Quataert, & Murray 12

  12. Cloud crushing by shocks, Kelvin-Helmholtz instability • Well-studied problem for SNRs (e.g., Klein+94, Cooper+09) CAFG, Quataert, & Murray 12

  13. Requirements for radiative shocks explain properties of cool absorbers • Acceleration, cold gas: ◆ 4 . 2 ✓ t drag < t KH v sh N H & 10 20 cm − 2 ⇒ t cool < t cc 5 , 000 km s − 1 • Post-shock compression: ✓ T sh ◆ ∼ 10 4 cm − 3 ≈ 4 n pre n BAL 10 4 K H H ⇒ ∆ R ∼ N H /n H ∼ 0 . 01 pc • Also: super-thermal line widths, multiple v components, reddening, ... CAFG, Quataert, & Murray 12

  14. Energetics of QSO outflows • Outflows are multiphase n H pre • Most of kinetic power in hot flow: shocked ambient medium shocked ˙ M hot = 8 π Ω hot RN hot wind H µm p v hot v in FeLoBAL hot * QSO flow cool • Using radiative shock model: clumps ˙ E k ≈ 2 − 5% L AGN R sw ˙ M ≈ 1 , 000 − 2 , 000 M � / yr R c R s ˙ P ≈ 2 − 10 L AGN /c Observations from Moe+09, Dunn+10, Bautista+10, Arav 10 CAFG, Quataert, & Murray 12

  15. The puzzle of large momentum fluxes • If all photons scatter once & P is conserved, ˙ P ∼ L AGN /c • Observations indicate ˙ P ∼ 10 L AGN /c • Simulations also require ULIRG data from Sturm+10 ˙ P � L AGN /c to reproduce M ● - σ (DeBuhr+) CAFG & Quataert, in prep.

  16. Momentum driving forward shock t cool ≪ t flow with ambient medium No thermal pressure shocked reverse shock ambient in nuclear wind medium P final ~ P start shocked wind v in e.g., AGB wind Does this * QSO cool? Energy driving t cool ≫ t flow R sw Shocked gas does work R c P final ≫ P start R s e.g., Sedov-Taylor SNR CAFG & Quataert, in prep.

  17. Proposal: AGN outflows are energy-driven • Possible in ULIRGs despite extreme densities ➡ relevant criterion is cooling of reverse shock: T sw ~10 10 K for v in ~0.1c ➡ 2-T plasma inhibits IC cooling AGN shocked wind cooling example cooling cooling p + time 1- T time 2- T e - t (yr) CAFG & Quataert, in prep.

  18. Energy conservation naturally explains measured AGN momentum boosts • Predicts v in = 0 . 1 c ˙ P ✓ nuclear wind speed ◆ L AGN /c ∼ 1 2 galaxy wind speed E cons. • To be tested soon with Herschel, E-VLA, ALMA, ... P cons. (1 scatt limit) • galaxy wind speed (km/s) Analytic model will inform numerical implementations CAFG & Quataert, in prep.

  19. Robust to mixing, leakage • Stellar wind bubbles smaller & slower than in energy-conserving Carina nebula models (Castor) ➡ cooling due to mixing (McKee+84) ➡ hot gas vents out (H.-C. & Murray 09) • AGN winds more robust ➡ ~30 × wind mass of cool gas before catastrophic ff cooling Smith & Brooks 07 ➡ escape along paths <10 -3 under- dense can still boost P by factor >10 in ULIRGs CAFG & Quataert, in prep.

  20. Summary • Compact, cool absorbers form in radiative shocks • Energetics in good agreement with M ● - σ requirements • Observations of galaxy-scale AGN outflows suggest ˙ P � L AGN /c • Proposal: outflows are energy-conserving • Prediction: ˙ ✓ nuclear wind speed ◆ P L AGN /c ∼ 1 2 galaxy wind speed

Download Presentation
Download Policy: The content available on the website is offered to you 'AS IS' for your personal information and use only. It cannot be commercialized, licensed, or distributed on other websites without prior consent from the author. To download a presentation, simply click this link. If you encounter any difficulties during the download process, it's possible that the publisher has removed the file from their server.

Recommend


More recommend