2021A&A...650A.180N


Query : 2021A&A...650A.180N

2021A&A...650A.180N - Astronomy and Astrophysics, volume 650A, 180-180 (2021/6-1)

X-ray-induced chemistry of water and related molecules in low-mass protostellar envelopes.

NOTSU S., VAN DISHOECK E.F., WALSH C., BOSMAN A.D. and NOMURA H.

Abstract (from CDS):


Context. Water is a key molecule in star- and planet-forming regions. Recent water line observations toward several low-mass protostars suggest low water gas fractional abundances (<10–6 with respect to total hydrogen density) in the inner warm envelopes (r<102au). Water destruction by X-rays is thought to influence the water abundances in these regions, but the detailed chemistry, including the nature of alternative oxygen carriers, is not yet understood.
Aims. Our aim is to understand the impact of X-rays on the composition of low-mass protostellar envelopes, focusing specifically on water and related oxygen-bearing species.
Methods. We computed the chemical composition of two proto-typical low-mass protostellar envelopes using a 1D gas-grain chemical reaction network. We varied the X-ray luminosities of the central protostars, and thus the X-ray ionization rates in the protostellar envelopes.
Results. The protostellar X-ray luminosity has a strong effect on the water gas abundances, both within and outside the H2O snowline (Tgas∼102K, r∼102au). Outside, the water gas abundance increases with LX, from ∼10–10 for low LX to ∼10–8-10–7 at LX>1030erg/s. Inside, water maintains a high abundance of ∼10–4 for LX≤1029-1030erg/s, with water and CO being the dominant oxygen carriers. For LX≥1030-1031erg/s, the water gas abundances significantly decrease just inside the water snowline (down to ∼10–8-10–7) and in the innermost regions with Tgas≥250K (∼10–6). For these cases, the fractional abundances of O2 and O gas reach ∼10–4 within the water snowline, and they become the dominant oxygen carriers. In addition, the fractional abundances of HCO+ and CH3OH, which have been used as tracers of the water snowline, significantly increase and decrease, respectively, within the water snowline as the X-ray fluxes become larger. The fractional abundances of some other dominant molecules, such as CO2, OH, CH4, HCN, and NH3, are also affected by strong X-ray fields, especially within their own snowlines. These X-ray effects are larger in lower-density envelope models.
Conclusions. X-ray-induced chemistry strongly affects the abundances of water and related molecules including O, O2, HCO+, and CH3OH, and can explain the observed low water gas abundances in the inner protostellar envelopes. In the presence of strong X-ray fields, gas-phase water molecules within the water snowline are mainly destroyed with ion-molecule reactions and X-ray-induced photodissociation. Future observations of water and related molecules (using, e.g., ALMA and ngVLA) will access the regions around protostars where such X-ray-induced chemistry is effective.

Abstract Copyright: © ESO 2021

Journal keyword(s): astrochemistry - ISM: molecules - stars: formation - stars: protostars - protoplanetary disks

Simbad objects: 16

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Number of rows : 16
N Identifier Otype ICRS (J2000)
RA
ICRS (J2000)
DEC
Mag U Mag B Mag V Mag R Mag I Sp type #ref
1850 - 2024
#notes
1 IRAS 03222+3034 Y*O 03 25 22.32 +30 45 13.9           ~ 149 0
2 NAME LDN 1455 IRS 4 cor 03 27 43.23 +30 12 28.9           ~ 74 0
3 [JCC87] IRAS 2A Y*O 03 28 55.55 +31 14 36.7           ~ 459 3
4 [JCC87] IRAS 4A Y*O 03 29 10.49 +31 13 30.8           ~ 715 1
5 [JCC87] IRAS 4B Y*O 03 29 12.058 +31 13 02.05           ~ 600 0
6 NAME Perseus Cloud SFR 03 35.0 +31 13           ~ 1365 0
7 TMC-1 MoC 04 41 45.9 +25 41 27           ~ 1676 0
8 V* V2457 Ori Or* 05 35 26.97000 -05 09 54.4644         18.858 ~ 151 0
9 HOPS 383 Y*O 05 35 29.8407 -04 59 51.006           ~ 68 0
10 V* V883 Ori Or* 05 38 18.1018261392 -07 02 26.017707120           F:I: 213 0
11 [B2001b] IRS 1 Y*O 12 01 36.53040 -65 08 51.9180           ~ 153 0
12 BHR 71 MoC 12 01 37 -65 08.8           ~ 154 0
13 NAME IRAS 16293-2422B Y*O 16 32 22.63 -24 28 31.8           ~ 283 0
14 LDN 483 DNe 18 17 35 -04 39.8           ~ 315 0
15 V* V371 Ser Or* 18 29 51.21240 +01 16 39.4860           ~ 119 1
16 LDN 663 DNe 19 36 55 +07 34.4           ~ 646 0

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