The Chemistry of PPN
1 / 13

The Chemistry of PPN - PowerPoint PPT Presentation

  • Uploaded on

The Chemistry of PPN. T. J. Millar & P. M. Woods, School of Physics and Astronomy, University of Manchester. The Chemistry of PPN. Short time scales, ~ 1000 yr Fast bipolar outflows, up to 200 km s -1 in CRL 618 Interacting stellar winds model Hot central object, 10,000 – 30,000 K

I am the owner, or an agent authorized to act on behalf of the owner, of the copyrighted work described.
Download Presentation

PowerPoint Slideshow about 'The Chemistry of PPN' - veta

An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.

- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -
Presentation Transcript

The Chemistry of PPN

T. J. Millar & P. M. Woods, School of Physics and Astronomy, University of Manchester

The chemistry of ppn
The Chemistry of PPN

  • Short time scales, ~ 1000 yr

  • Fast bipolar outflows, up to 200 km s-1 in CRL 618

  • Interacting stellar winds model

  • Hot central object, 10,000 – 30,000 K

  • Strong increasing central UV field, ~ 105 – 107 F(ISM)

  • Previous high mass loss rate but current mass loss ceased

  • Dense gas, n(H2) ~ 107 – 109 cm-3

  • Evolution of AGB molecular envelope

  • Over 20 molecules detected

Molecular line observations of ppn
Molecular Line Observations of PPN

Decrease in complexity from AGB → PPN → PN

50 → 20 → 8 molecules

Large increase in HCO+ abundance in PPN

CN and HNC abundances increase in the post-AGB phase

Importance of UV increases, of shocks decrease as PPN evolve

Molecular line observations of ppn1
Molecular Line Observations of PPN

CRL 618 (Cernicharo et al. 2001a,b; Herpin & Cernicharo 2000) intermediate age PPN, 200-1000 yr old, B0 star, Teff ~ 30,000 K, compact HII region, confined by a dense torus, bipolar outflow at ~ 200 km s-1, CSE expansion at ~ 20 km s-1

- Large hydrocarbon species

CH4, C2H2, C4H2, C6H2, CH3CCH, CH3C4H, C6H6

- Cyanopolyynes


- Oxygen-bearing molecules


Modelling the chemistry of ppn
Modelling the Chemistry of PPN

Photon-dominated Chemistry

UV photons dissociate molecules formed in AGB envelope, produce radicals which then form new species, primarily carbon chains

UV radiation dissociates CO which injects O atoms into chemistry

Shock Chemistry

Interaction of HV outflow with remnant AGB envelope. High temperature chemistry converts O into OH and H2O

AGB Envelope

The remnant of the AGB CSE, dilution due to expansion, photochemistry by internal and external UV photons

The chemistry of ppn1
The Chemistry of PPN

CRL 618

Herpin & Cernicharo, ApJ, 530, L129 (2000) identified three main molecular components – a torus (with PDR), a HV outflow and the AGB CSE

The chemistry of ppn2
The Chemistry of PPN

Cernicharo, ApJ, 608, L41 (2004) models the PDR precursor (PDRP)

Zone I – G0 = 104, AV = 1 mag

Zone II – AV = 2 mag, H2 self-shielded, CO photodissociated

Zone III – AV = 3 mag, CO not photodissociated

In all zones, T = 300K, n(H2) = 107 cm-3, zone thickness = 1014 cm,

initial molecules H2, CO, C2H2, CH4, C2H4 and HCN

Abundance peaks ~ 0.2 yr

Steady state ~ few yr

Faster than expansion of HII region

High fractional abundances of carbon chains, etc in Zones II and III

O freed from CO forms OH, H2O, CO2, H2CO in Zones I, II, III

The chemistry of ppn3
The Chemistry of PPN

Woods et al. ApJL, 574, L167 (2002) & A&A, 402, 189, (2003)

Modelled a thin slab of high-density gas as it moved away from central object – the expanding inner edge of the remnant AGB circumstellar envelope

Constant thickness, Δr, density n(r) ~ r-2, AUV ~ r-2

Expansion velocity 5 km s-1 (if v = 20 km s-1, dilution is rapid and photodissociation dominates; no complex molecules formed)

Equivalent mass-loss rate, 3 10-3 solar masses per yr

Initial radius, 2.5 1015 cm

Initial H2 abundance, 1.6 109 cm-3

Initial extinction, AV = 160 mags

Initial UV flux enhancement, 3.2 106

Initial CR rate enhancement, 500

Initial temperature, 250 K

C/O = 1.2

Initial abundances from AGB observations and calculations

The chemistry of ppn4
The Chemistry of PPN

‘No’ chemistry when AV is less than about 10 mags – photodestruction dominates – ‘radiation catastrophe’

Collision times very short ~ 0.1 s, so complex species are formed rapidly once parent species start to break down

The chemistry of ppn5
The Chemistry of PPN

CRL 618: Observed (heavy) and model (light) abundances, calculated at 9 1015 cm

The chemistry of ppn6
The Chemistry of PPN

Woods et al. Molecules in Bipolar Proto-Planetary Nebulae, A&A, in press

SEST observations of IRAS16594-4656 (~ 400 yr old) and 17150-3224(~ 200 yr old)

Other than CO, only HCN and CN detected; many upper limits

conclude that these 2 PPN are molecule-poor

Chemical model: Calculate radial distributions in a C-rich CSE

Expansion velocity = 14 kms-1

Mass-loss rate = 10-5 solar masses per yr

X-ray and CRP ionisation included

Envelope heating as central star evolves

The chemistry of ppn8
The Chemistry of PPN

  • Summary:

  • Importance of photons

  • CO dissociation leads to OH and H2O formation

  • High-densities, short time-scales, seconds to years

  • Rich organic chemistry driven by acetylene parent

  • Shock chemistry may be important in some PPN

  • Fine balance between UV as a promoter of molecular complexity and as a destructive force – radiation catastrophe

  • UV eventually destroys molecules – PN stage is molecule poor