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Gas chemistry in the dust depleted inner regions of protoplanetary disks. I. Near-IR spectra and overtones

J. Bethlehem, Ch. Rab, I. Kamp, M. Flock, G. Bourdarot, P. Caselli

Abstract

The molecular composition inside the dust sublimation zones of protoplanetary disks is mostly unknown but important to understanding terrestrial planet formation. A few molecules have been observed from this region, specifically CO, H2O, OH and SiO. The small surface area makes observing this region difficult, hence modeling is required to disentangle the innermost disk from regions further out. We model a protoplanetary disk around a Herbig-type star including the dust depleted inner region (approx. 0.1-0.3 au) and aim to investigate the chemistry of this region and explain existing and future observations. Methods. We post-process the dust and gas distribution of a magnetohydrostatic model with the radiation thermochemical code ProDiMo to study the chemistry and to produce observables. We find that the dust free inner disk is a molecular rich environment, where besides CO we also find H2, H2O and SiO. The gas temperature profile is complex and fluctuates between 700 and 2000 K, which is warm enough to produce CO overtone line emission. Next to the CO overtone lines we also find strong high J-level fundamental CO lines between 4.3 and 4.6 micron. The elemental enrichment of Si due to dust sublimation leads to 2 orders of magnitude more SiO abundance. The SiO gas has average temperatures of approx. 1000 K resulting in strong SiO overtone emission in the spectral range between 4 and 4.3 micron. We predict that the gas density in the dust depleted inner disk is high enough to allow for H2 formation, resulting in an molecular rich environment. For our representative Herbig model, the dust-depleted inner disk is responsible for at least 90% of the line emission for CO and H2O between 1 and 28 micron. Next to CO overtone lines, SiO overtone lines are expected to be an important tracer of a dust free inner disk.

Gas chemistry in the dust depleted inner regions of protoplanetary disks. I. Near-IR spectra and overtones

Abstract

The molecular composition inside the dust sublimation zones of protoplanetary disks is mostly unknown but important to understanding terrestrial planet formation. A few molecules have been observed from this region, specifically CO, H2O, OH and SiO. The small surface area makes observing this region difficult, hence modeling is required to disentangle the innermost disk from regions further out. We model a protoplanetary disk around a Herbig-type star including the dust depleted inner region (approx. 0.1-0.3 au) and aim to investigate the chemistry of this region and explain existing and future observations. Methods. We post-process the dust and gas distribution of a magnetohydrostatic model with the radiation thermochemical code ProDiMo to study the chemistry and to produce observables. We find that the dust free inner disk is a molecular rich environment, where besides CO we also find H2, H2O and SiO. The gas temperature profile is complex and fluctuates between 700 and 2000 K, which is warm enough to produce CO overtone line emission. Next to the CO overtone lines we also find strong high J-level fundamental CO lines between 4.3 and 4.6 micron. The elemental enrichment of Si due to dust sublimation leads to 2 orders of magnitude more SiO abundance. The SiO gas has average temperatures of approx. 1000 K resulting in strong SiO overtone emission in the spectral range between 4 and 4.3 micron. We predict that the gas density in the dust depleted inner disk is high enough to allow for H2 formation, resulting in an molecular rich environment. For our representative Herbig model, the dust-depleted inner disk is responsible for at least 90% of the line emission for CO and H2O between 1 and 28 micron. Next to CO overtone lines, SiO overtone lines are expected to be an important tracer of a dust free inner disk.
Paper Structure (26 sections, 11 figures, 6 tables)

This paper contains 26 sections, 11 figures, 6 tables.

Figures (11)

  • Figure 1: Chemical relaxation timescale $\tau_{chem}$ (top) and cooling relaxation timescale $\tau_{cool}$ (bottom) for our model including a dust free inner environment. The blue dashed line indicates where the visual extinction reaches unity ($A_V = 1$).
  • Figure 2: Gas and dust density of a typical ProDiMo Herbig disk model. The red hatched area is generally not modeled as it is beyond the expected dust rim at 0.3 au. The blue dashed line indicates where the visual extinction reaches unity ($A_V = 1$), the white dashed contours align with the values on the colorbar. The yellow dashed line indicates where $n_{\langle H \rangle} = 10^{12}$ cm^-3.
  • Figure 3: Gas density, dust density and the dust-to-gas ratio of our model with the dust depleted inner disk included. The red vertical dotted line indicates where the standard model is cut. The blue dashed line indicates where the visual extinction reaches unity ($A_V = 1$), the white dashed contours align with the values on the colorbar and the red dashed contour in the bottom panel indicates the outer boundary of the dust depleted inner disk. The yellow dashed line indicates where $n_{\langle H \rangle} = 10^{12}$ cm^-3.
  • Figure 4: The top panel shows the temperature profile of a standard ProDiMo model and the bottom shows the temperature profile of our model that includes a dust depleted inner disk and increased inner disk gas-phase elemental abundances (see Table \ref{['Elemental composition']}). The blue dashed line indicates where the visual extinction reaches unity ($A_V = 1$), the white contours show the gas temperatures of 100, 1000 and 10000 K. The red vertical line indicates where the temperature is analyzed in Fig. \ref{['Heat_cool_abundance']} and the red dot is the grid point at which the chemistry is analyzed (Fig. \ref{['Reaction_network']}).
  • Figure 5: Vertical cut of the disk at r = 0.165 au, showing the gas temperature and molecular abundances with respect to the gas and number density. The left axis indicates the gas temperature and the right axis shows the relative molecular abundance for selected species important to the heating and cooling balance. The midplane is the left y-axis at $\rho_{\text{gas}} \approx 2.15 \times 10^{-10}$ [g cm^-3].
  • ...and 6 more figures