Simulations of Winds. Daniel Proga University of Nevada, Las Vegas Princeton University

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Transcription:

Simulations of Winds Daniel Proga University of Nevada, Las Vegas Princeton University

Collaborators J. Stone, T. Kallman, J. Raymond, M. Begelman, J. Ostriker, R. Kurosawa, J. Drew, A. Janiuk, M. Moscibrodzka, B. Czerny, A. Siemiginowska, S. Sim, A. Dorodnityn, S. Sim, S. Luketic, T. Waters, M. Giustini, and many more

OUTLINE

OUTLINE 1. Introduction

OUTLINE 1. Introduction 2. Multidimensional, time-dependent simulations of disk winds driven by:

OUTLINE 1. Introduction 2. Multidimensional, time-dependent simulations of disk winds driven by: - thermal expansion

OUTLINE 1. Introduction 2. Multidimensional, time-dependent simulations of disk winds driven by: - thermal expansion - radiation pressure

OUTLINE 1. Introduction 2. Multidimensional, time-dependent simulations of disk winds driven by: - thermal expansion - radiation pressure - magnetic fields (please see other talks in this session)

OUTLINE 1. Introduction 2. Multidimensional, time-dependent simulations of disk winds driven by: - thermal expansion - radiation pressure - magnetic fields (please see other talks in this session) - and in some combinations.

OUTLINE 1. Introduction 2. Multidimensional, time-dependent simulations of disk winds driven by: - thermal expansion - radiation pressure - magnetic fields (please see other talks in this session) - and in some combinations. 3. Conclusions

What can drive an outflow?

What can drive an outflow? Thermal expansion (evaporation, hydrodynamical escape)

What can drive an outflow? Thermal expansion (evaporation, hydrodynamical escape) Radiation pressure (gas, dust)

What can drive an outflow? Thermal expansion (evaporation, hydrodynamical escape) Radiation pressure (gas, dust) Magnetic fields

What can drive an outflow? Thermal expansion (evaporation, hydrodynamical escape) Radiation pressure (gas, dust) Magnetic fields In most cases, rotation plays a key role (directly or indirectly) especially in AD.

Accretion Disks vs Stars

Accretion Disks vs Stars

Accretion Disks vs Stars

Accretion Disks vs Stars

Accretion Disks vs Stars See a poster by Tim Waters

Accretion Disks in Various Objects Two examples:

Thermal Disk Winds

GRS 1915-105 Neilsen & Lee (2009) fig. from DP s 2009 News & Views

X-ray Transient Sources Most of the accretion energy is emitted in X-rays. The radiation energy is still too low to drive an outflow from the inner disk. But the radiation from the inner disk can heat up the outer disk. However, spectral features of disk winds have not been seen from these systems until recently (Schulz & Brandt 2002; Miller et al. 2006, 2008; Kubota et al. 2007; Neilsen & Lee 2009). Thank you Chandra, XMM-Newton, and Suzaku...!!! future... ATHENA? GRO J1655 40 Observations: Miller et al. (2006)

X-ray Transient Sources GRO J1655 40 Interpretation and spectral modeling: Miller et al. (2006, 2008), Netzer (2006), Kallman et al. (2009). Dedicated hydrodynamical simulations (Luketic et al. 2010) Observations: Miller et al. (2006)

The equations of hydrodynamics Dρ Dt + ρ v = 0 ρ Dv = P + ρg + ρ f rad Dt ρ D e = P v + ρl Dt ρ P = (γ 1)e

The equations of hydrodynamics Dρ Dt + ρ v = 0 ρ Dv = P + ρg + ρ f rad Dt ρ D e = P v + ρlρ Dt ρ P = (γ 1)e

X-ray and UV source

Luketic et al. (2010)

GRO J1655 40

GRO J1655 40

GRO J1655 40 The thermal wind is not dense enough to account for the observed wind. But does it mean that the thermal wind is unimportant? Maybe not because the wind mass lose rate can be as high as 5 times the disk accretion rate (see also Neilsen & Lee 2009)!

Radiation-Driven Winds

The equations of hydrodynamics Dρ Dt + ρ v = 0 ρ Dv = P + ρg + ρ f rad Dt ρ D e = P v + ρl Dt ρ P = (γ 1)e

The equations of hydrodynamics Dρ Dt + ρ v = 0 ρ Dv = P + ρg + ρ f rad Dt ρ D e = P v + ρl Dt ρ P = (γ 1)e

L(disk)=3 L(star)=0

L(disk)=3 L(star)=0 L(disk)=3 L(star)=3

HD simulations and their line profiles

HD simulations and their line profiles

HD simulations and their line profiles

HD simulations and observations

HD simulations and observations L = D 23.4L, SUN L = WD 0.25L, D M = a 8 3 10 M SUN 1 yr

HD simulations and observations L = D 23.4L, SUN L = WD 0.25L, D M = a 8 3 10 M SUN 1 yr

HD simulations and observations L = D 23.4L, SUN L = WD 0.25L, D M = a 8 3 10 M SUN 1 yr CIV 1549 for IX Vel (Hartley et al. 2001); models Proga (2003b)

HD simulations and observations L = D 23.4L, SUN L = WD 0.25L, D M = a 8 3 10 M SUN 1 yr CIV 1549 for IX Vel (Hartley et al. 2001); models Proga (2003b)

HD simulations and observations L = D 23.4L, SUN L = WD 0.25L, D M = a 8 3 10 M SUN 1 yr CIV 1549 for IX Vel (Hartley et al. 2001); models Proga (2003b)

Drew & Proga (1999)

Drew & Proga (1999)

Drew & Proga (1999)

a M = 8 1 10 M Sun M = WD 1M Sun 1 yr Drew & Proga (1999)

Thermal and Radiation- Driven Winds

The equations of hydrodynamics Dρ Dt + ρ v = 0 ρ Dv = P + ρg + ρ f rad Dt ρ D e = P v + ρl Dt ρ P = (γ 1)e

The equations of hydrodynamics Dρ Dt + ρ v = 0 ρ Dv = P + ρg + ρ f rad Dt ρ D e = P v + ρlρ Dt ρ P = (γ 1)e

The equations of hydrodynamics Dρ Dt + ρ v = 0 ρ Dv = P + ρg + ρ f rad Dt ρ D e = P v + ρlρ Dt ρ P = (γ 1)e

M = 8 BH Γ = 0.6 10 Msun

DP, Stone, & Kallman (2000) DP & Kallman (2004)

DP, Stone, & Kallman (2000) DP & Kallman (2004)

DP, Stone, & Kallman (2000) DP & Kallman (2004)

Paola Rodriguez-Hidalgo, DP, F. Hamann

Broad band spectra for various l.o.s. Schurch, Done, & DP (2009)

Broad band spectra for various l.o.s. Schurch, Done, & DP (2009)

Broad band spectra for various l.o.s. Schurch, Done, & DP (2009)

Broad band spectra for various l.o.s. 50 o 57 o 62 o 65 o 67 o Schurch, Done, & DP (2009)

Broad band spectra for various l.o.s. 50 o 57 o 62 o 65 o 67 o Schurch, Done, & DP (2009)

Broad band spectra for various l.o.s. 50 o 57 o 62 o 65 o 67 o Schurch, Done, & DP (2009)

Broad band spectra for various l.o.s. 50 o 57 o 62 o 65 o 67 o Schurch, Done, & DP (2009)

Broad band spectra for various l.o.s. Sim et al. (2010)

Broad band spectra for various l.o.s. Sim et al. (2010)

Broad band spectra for various l.o.s. Sim et al. (2010)

Broad band spectra for various l.o.s. Sim et al. (2010)

Quasar Irradiation

Quasar Irradiation

Quasar Irradiation

Quasar Irradiation?

Quasar Irradiation?

An outflow from an inflow

M = 8 BH 10 M SUN M = 26 D 10 g/ s =1.6M SUN T = X 8 x 7 10 K ρ( r o )= 10 21 3 g/ cm f = UV f = X 0.5 / yr

M = 8 BH 10 M SUN M = 26 D 10 g/ s =1.6M SUN T = X 8 x 7 10 K ρ( r o )= 10 21 3 g/ cm f = UV f = X 0.5 / yr Proga (2007)

M = 8 BH 10 M SUN M = 26 D 10 g/ s =1.6M SUN T = X 8 x 7 10 K ρ( r o )= 10 21 3 g/ cm f = UV 0.95 f = X 0.05 / yr

M = 8 BH 10 M SUN M = 26 D 10 g/ s =1.6M SUN T = X 8 x 7 10 K ρ( r o )= 10 21 3 g/ cm f = UV 0.95 f = X 0.05 / yr

M = 8 BH 10 M SUN M = 26 D 10 g/ s =1.6M SUN T = X 8 x 7 10 K ρ( r o )= 10 21 3 g/ cm f = UV 0.95 f = X 0.05 / yr Proga (2007)

M = 8 BH 10 M SUN M = 26 D 10 g/s =1.6M SUN/ yr T = X 8 x 7 10 K ρ( r o )= 10 21 3 g/ cm f = UV 0.95 f = X 0.05

Effects of gas rotation, optical depth and X-ray background radiation

Effects of gas rotation, optical depth and X-ray background radiation DP, Ostriker, Kurosawa (2007)

Effects of gas rotation, optical depth and X-ray background radiation no rotation DP, Ostriker, Kurosawa (2007)

Effects of gas rotation, optical depth and X-ray background radiation no rotation rotation DP, Ostriker, Kurosawa (2007)

Effects of gas rotation, optical depth and X-ray background radiation no rotation rotation rotation and opt. thick DP, Ostriker, Kurosawa (2007)

Effects of gas rotation, optical depth and X-ray background radiation no rotation rotation no X-ray background rotation and opt. thick DP, Ostriker, Kurosawa (2007)

Effects of gas rotation, optical depth and X-ray background radiation no rotation rotation no X-ray background rotation and opt. thick X-ray background DP, Ostriker, Kurosawa (2007)

Dynamical model for clouds in NLR!?

Dynamical model for clouds in NLR!?

Dynamical model for clouds in NLR!?

3-diminesional simulations Kurosawa & DP (2009a)

Clouds properties density map temperature map Kurosawa & DP (2009a)

What is the limit for the mass supply rate? Kurosawa & DP (2009b)

What is the limit for the mass supply rate? Kurosawa & DP (2009b)

What is the limit for the mass supply rate? Kurosawa & DP (2009b)

What is the limit for the mass supply rate? Kurosawa & DP (2009b)

What is the limit for the mass supply rate? Kurosawa & DP (2009b)

What is the geometry of the outflow?

What is the geometry of the outflow? jet like

What is the geometry of the outflow? jet like i/o

What is the geometry of the outflow? jet like i/o disk-wind like

How efficient are the outflows? Kurosawa, DP, & Nagamine (2009)

How efficient are the outflows? 10^-4 Kurosawa, DP, & Nagamine (2009)

AGN feedback

AGN feedback Watt centrifugal governor of 1788

?

?

?

Ciotti, Ostriker, & DP (2010)

Conclusions

Conclusions Simulations of accretion flows and their outflows provide important insights into the dynamics and geometry of the material that produces radiation. In particular, we can use the simulations to assess the effects of radiation on the flow properties. We can also explore coupling between accretion flows and they outflows as well as mass supply (e.g., various forms of feedback).

Conclusions Simulations of accretion flows and their outflows provide important insights into the dynamics and geometry of the material that produces radiation. In particular, we can use the simulations to assess the effects of radiation on the flow properties. We can also explore coupling between accretion flows and they outflows as well as mass supply (e.g., various forms of feedback). The simulations can be and are used to compute synthetic spectra for direct comparison with the observations. As such, the simulations are useful in explaining specific spectral features as well as overall shape of the SED (not just pretty movies with complex equations/physics behind).

Future Works

Future Works Add effects of dust.

Future Works Add effects of dust. Add other modes of operation (e.g., radiatively inefficient accretion, magnetic).

Future Works Add effects of dust. Add other modes of operation (e.g., radiatively inefficient accretion, magnetic).

Future Works Add effects of dust. Add other modes of operation (e.g., radiatively inefficient accretion, magnetic). Follow interaction of disk winds with outer inflows/outflows and incorporate these type of simulations into cosmological simulations

Future Works Add effects of dust. Add other modes of operation (e.g., radiatively inefficient accretion, magnetic). Follow interaction of disk winds with outer inflows/outflows and incorporate these type of simulations into cosmological simulations

Future Works Add effects of dust. Add other modes of operation (e.g., radiatively inefficient accretion, magnetic). Follow interaction of disk winds with outer inflows/outflows and incorporate these type of simulations into cosmological simulations

Future Works Add effects of dust. Add other modes of operation (e.g., radiatively inefficient accretion, magnetic). Follow interaction of disk winds with outer inflows/outflows and incorporate these type of simulations into cosmological simulations Most importantly, keep comparing the model predictions with observations of AGN.

Quenching Disk Corona DP (2005)

Quenching Disk Corona Disk DP (2005)

Quenching Disk Corona Disk Disk and inflow/outflow DP (2005)

Quenching Disk Corona Disk Disk and inflow/outflow Disk and corona DP (2005)

Quenching Disk Corona Disk Disk and inflow/outflow Disk and corona Disk and??? DP (2005)

Where is the X-ray corona?

Where is the X-ray corona?

Where is the X-ray corona???

Where is the X-ray corona???

Where is the X-ray corona???

L = D 1 L = S 0 L = D 3 L = S 0 L = D 3 L = S 3 13 L = D 3 L = S 9 Proga, Stone & Drew (1998)

Black Hole Accretion -> Outflow

Black Hole Accretion -> Outflow

Multi-component flow

Multi-component flow torus

Multi-component flow torus corona torus

Multi-component flow torus wind torus corona torus

Multi-component flow torus wind torus corona torus low l inflow

Multi-component flow torus wind torus corona torus low l inflow outflow/jet

Multi-component flow torus wind torus corona torus low l inflow outflow/jet see Moscribrodzka et al for spectra predicted by such flows

Does it have to be so complex?

Does it have to be so complex?

Does it have to be so complex?

Does it have to be so complex? Proga (2005)

Does it have to be so complex? Answer: No, it does not. Proga (2005)

Ciotti, Ostriker, & Proga (2010)

Ciotti, Ostriker, & Proga (2010)

Ciotti, Ostriker, & Proga (2010)

MHD Driven Winds

MHD and Radiation Driven Winds

MHD-LD Disk Winds DP (2003a)

MHD-LD Disk Winds DP (2003a)

MHD-LD Disk Winds DP (2003a)

MHD-LD Disk Winds DP (2003a)

The mass loss rate in MHD-LD winds.

The mass loss rate in MHD-LD winds.

A big picture L Edd = 4πcGM a σ L = M M a G 2r a Γ = L M = a σ L Edd 8πcr a Γ UV = L UV L Edd

A big picture L Edd = 4πcGM a σ L = M M a G 2r a Γ = L M = a σ L Edd 8πcr a Γ UV = L UV L Edd Proga (2002)

A big picture 1/(TOTAL UV LINE OPACITY) L Edd = 4πcGM a σ L = M M a G 2r a Γ = L M = a σ L Edd 8πcr a Γ UV = L UV L Edd Proga (2002)

A big picture 1/(TOTAL UV LINE OPACITY) AGN (SMBH) L Edd = 4πcGM a σ L = M M a G 2r a Γ = L M = a σ L Edd 8πcr a Γ UV = L UV L Edd Proga (2002)

A big picture 1/(TOTAL UV LINE OPACITY) AGN (SMBH) CV (WD) L Edd = 4πcGM a σ L = M M a G 2r a Γ = L M = a σ L Edd 8πcr a Γ UV = L UV L Edd Proga (2002)

A big picture 1/(TOTAL UV LINE OPACITY) FU Ori (MS S) AGN (SMBH) CV (WD) L Edd = 4πcGM a σ L = M M a G 2r a Γ = L M = a σ L Edd 8πcr a Γ UV = L UV L Edd Proga (2002)

A big picture 1/(TOTAL UV LINE OPACITY) FU Ori (MS S) AGN (SMBH) CV (WD) LMXB (NS) GBH (LM BH) L Edd = 4πcGM a σ L = M M a G 2r a Γ = L M = a σ L Edd 8πcr a Γ UV = L UV L Edd Proga (2002)

Conclusions

Conclusions A significant fraction of the inflowing matter can be expelled by radiation pressure and heating.

Conclusions A significant fraction of the inflowing matter can be expelled by radiation pressure and heating. The non-rotating flow settles into a steady inflow/outflow solution. Gas rotation and large optical depth can lead to time variability.

Conclusions A significant fraction of the inflowing matter can be expelled by radiation pressure and heating. The non-rotating flow settles into a steady inflow/outflow solution. Gas rotation and large optical depth can lead to time variability. In time variable flows, dense clouds form (as in NRL of AGN?).

Conclusions A significant fraction of the inflowing matter can be expelled by radiation pressure and heating. The non-rotating flow settles into a steady inflow/outflow solution. Gas rotation and large optical depth can lead to time variability. In time variable flows, dense clouds form (as in NRL of AGN?). The outflows are multi-temperature/phases (as in WA?).

Conclusions A significant fraction of the inflowing matter can be expelled by radiation pressure and heating. The non-rotating flow settles into a steady inflow/outflow solution. Gas rotation and large optical depth can lead to time variability. In time variable flows, dense clouds form (as in NRL of AGN?). The outflows are multi-temperature/phases (as in WA?). The I/O solution is quite robust but its characteristics are sensitive to the geometry and SED of the central object radiation.

Conclusions A significant fraction of the inflowing matter can be expelled by radiation pressure and heating. The non-rotating flow settles into a steady inflow/outflow solution. Gas rotation and large optical depth can lead to time variability. In time variable flows, dense clouds form (as in NRL of AGN?). The outflows are multi-temperature/phases (as in WA?). The I/O solution is quite robust but its characteristics are sensitive to the geometry and SED of the central object radiation. The mass supplied rate does not appear to be limited by the luminosity of AGN.

Conclusions A significant fraction of the inflowing matter can be expelled by radiation pressure and heating. The non-rotating flow settles into a steady inflow/outflow solution. Gas rotation and large optical depth can lead to time variability. In time variable flows, dense clouds form (as in NRL of AGN?). The outflows are multi-temperature/phases (as in WA?). The I/O solution is quite robust but its characteristics are sensitive to the geometry and SED of the central object radiation. The mass supplied rate does not appear to be limited by the luminosity of AGN. The outflow is inefficient in removing energy.

Conclusions A significant fraction of the inflowing matter can be expelled by radiation pressure and heating. The non-rotating flow settles into a steady inflow/outflow solution. Gas rotation and large optical depth can lead to time variability. In time variable flows, dense clouds form (as in NRL of AGN?). The outflows are multi-temperature/phases (as in WA?). The I/O solution is quite robust but its characteristics are sensitive to the geometry and SED of the central object radiation. The mass supplied rate does not appear to be limited by the luminosity of AGN. The outflow is inefficient in removing energy. Disk winds are much more efficient than the large scale outflows