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H3+ in irradiated protoplanetary disks: Linking far-ultraviolet radiation and water vapor

Javier R. Goicoechea, Octavio Roncero, Evelyne Roueff, John H. Black, Ilane Schroetter, Olivier Berné

TL;DR

The paper investigates H$_3^+$ formation and excitation in the externally irradiated outer disk and photoevaporative wind of the protoplanetary disk d203-506, using state-to-state quantum-dynamical rate constants for H$_2(v'')$ + HOC$^+$ and H$_2(v'')$ + H$^+$, as well as FUV photoionization of vibrationally excited H$_2$ (H$_2^*$, $v''\geq 4$). It demonstrates that FUV-driven chemistry in the PDR dominates H$_3^+$ production, largely independent of the cosmic-ray ionization rate, with H$_3^+$ peaking at $x({\rm H_3^+})\sim 10^{-8}$ and $N({\rm H_3^+})\sim 10^{13}$ cm$^{-2}$, particularly in a molecular PDR zone near the H/H$_2$ transition. Non-LTE excitation modeling shows that formation pumping from exoergic reactions can reproduce the JWST-detected H$_3^+$ lines, implying a formation temperature around $T_{\rm form} \approx 3000$ K and a ro-vibrational temperature $T_{\rm rot} \sim 1100$ K. The results imply H$_3^+$ is a diagnostic of external FUV fields ($G_0$) and disk photochemistry in strongly irradiated systems, with relevance to inner disks, exoplanet ionospheres, and early-Universe contexts.

Abstract

The likely JWST detection of vibrationally excited H3+ emission in Orion's irradiated disk system d203-506 raises the important question of whether cosmic-ray ionization is enhanced in disks within clustered star-forming regions, or whether alternative mechanisms contribute to H3+ formation and excitation. We present a detailed model of the photodissociation region (PDR) component of a protoplanetary disk -comprising the outer disk surface and the photoevaporative wind - exposed to strong external far-ultraviolet (FUV) radiation. We investigate key gas-phase reactions involving excited H2 that lead to the formation of H3+ in the PDR, including detailed state-to-state dynamical calculations of reactions H2(v>=0) + HOC+ -> H3+ + CO and H2(v>=0) + H+ -> H2+ + H. We also consider the effects of photoionization of vibrationally excited H2(v>=4), a process not previously included in PDR or disk models. We find that these FUV-driven reactions dominate the formation of H3+ in the PDR of strongly irradiated disks, largely independently of cosmic-ray ionization. The predicted H3+ abundance in the disk PDR peaks at x(H3+)~1E-8, coinciding with regions of enhanced HOC+ and water vapor abundances, and is linked to the strength of the external FUV field (G0). The predicted H3+ column density (~1E13 cm^-2) agrees with the presence of H3+ in the PDR of d203-506. We also find that formation pumping, resulting from exoergic reactions between excited H2 and HOC+, drives the vibrational excitation of H3+ in these regions. We expect this photochemistry to be highly active in disks where G_0 > 1E3. The H3+ formation pathways studied here may also be relevant in the inner disk region (near the host star), in exoplanetary ionospheres, and in the early Universe.

H3+ in irradiated protoplanetary disks: Linking far-ultraviolet radiation and water vapor

TL;DR

The paper investigates H formation and excitation in the externally irradiated outer disk and photoevaporative wind of the protoplanetary disk d203-506, using state-to-state quantum-dynamical rate constants for H + HOC and H + H, as well as FUV photoionization of vibrationally excited H (H, ). It demonstrates that FUV-driven chemistry in the PDR dominates H production, largely independent of the cosmic-ray ionization rate, with H peaking at and cm, particularly in a molecular PDR zone near the H/H transition. Non-LTE excitation modeling shows that formation pumping from exoergic reactions can reproduce the JWST-detected H lines, implying a formation temperature around K and a ro-vibrational temperature K. The results imply H is a diagnostic of external FUV fields () and disk photochemistry in strongly irradiated systems, with relevance to inner disks, exoplanet ionospheres, and early-Universe contexts.

Abstract

The likely JWST detection of vibrationally excited H3+ emission in Orion's irradiated disk system d203-506 raises the important question of whether cosmic-ray ionization is enhanced in disks within clustered star-forming regions, or whether alternative mechanisms contribute to H3+ formation and excitation. We present a detailed model of the photodissociation region (PDR) component of a protoplanetary disk -comprising the outer disk surface and the photoevaporative wind - exposed to strong external far-ultraviolet (FUV) radiation. We investigate key gas-phase reactions involving excited H2 that lead to the formation of H3+ in the PDR, including detailed state-to-state dynamical calculations of reactions H2(v>=0) + HOC+ -> H3+ + CO and H2(v>=0) + H+ -> H2+ + H. We also consider the effects of photoionization of vibrationally excited H2(v>=4), a process not previously included in PDR or disk models. We find that these FUV-driven reactions dominate the formation of H3+ in the PDR of strongly irradiated disks, largely independently of cosmic-ray ionization. The predicted H3+ abundance in the disk PDR peaks at x(H3+)~1E-8, coinciding with regions of enhanced HOC+ and water vapor abundances, and is linked to the strength of the external FUV field (G0). The predicted H3+ column density (~1E13 cm^-2) agrees with the presence of H3+ in the PDR of d203-506. We also find that formation pumping, resulting from exoergic reactions between excited H2 and HOC+, drives the vibrational excitation of H3+ in these regions. We expect this photochemistry to be highly active in disks where G_0 > 1E3. The H3+ formation pathways studied here may also be relevant in the inner disk region (near the host star), in exoplanetary ionospheres, and in the early Universe.

Paper Structure

This paper contains 22 sections, 20 equations, 18 figures, 2 tables.

Figures (18)

  • Figure 1: Physical (approximately vertical) structure of d203-506. Upper panels: Model profiles of gas density, gas temperature, and $a^{-3.5}$ grain-size distribution, showing the highest and lowest dust temperatures (corresponding to $a_{\rm min}$ and $a_{\rm max}$ grain radii, respectively) as a function of depth into the PDR. The green curve shows the density of H$_{2}^{*}$($v$$\geq$4). Lower panel: Abundance profiles of selected species. Bottom sketch: Simplified sketch illustrating the PDR component of an externally irradiated protoplanetary disk. The different colored regions correspond to the chemical zones discussed in Sect. \ref{['sec:chemistry']}.
  • Figure 2: Predicted $\lambda$-dependent FUV radiation field at different depth positions from the PDR surface into the disk. We show the local FUV energy density in units of erg cm$^{-3}$ Å$^{-1}$, from the Lyman cut to 12.6 eV.
  • Figure 3: Dominant H$_3^+$ formation and destruction pathways in different zones of a strongly irradiated protoplanetary disk (see Fig. \ref{['fig:chemical_model_d203-506']}). A thicker arrow represents a dominant chemical pathway. Red arrows show endoergic reactions. These reactions become fast at high $T_{\rm gas}$ and where significant H$_{2}^{*}$ exists. “CR” refers to ionization caused by cosmic rays and “$\gamma$” refers to FUV photons. Orange arrows represent ion-molecule and charge exchange reactions. Green arrows represent dissociative recombinations with electrons. Incomplete circles indicate that these are not the starting points of the chemistries.
  • Figure 4: Calculated vibrational-state-specific rate constants of reaction H$_2$($v$") + H$^+$$\rightarrow$ H$_2^+$ + H (reaction~\ref{['reaction_hp']}). The dashed curve represents the thermal$^6$ rate constant determined from thermal averages of these constants.
  • Figure 5: Calculated H$_2$ vibrational-state-specific rate constants of reaction H$_2$($v$") + HOC$^+$ producing H$_3^+$ + CO (left box) and HCO$^+$ + H$_2$ (right box). The dashed curves represent the thermal$^6$ rate constant determined from thermal averages of the state-dependent rates.
  • ...and 13 more figures