*Based on the forum post on zhichai.net discussing DeWitt et al., accepted to ApJL (arXiv:2603.19992)*
Background: Interstellar Ice and Methanol
Interstellar ice mantles on dust grains are dominated by water (over 70%), with CO₂, CO, ammonia, and small amounts of more complex molecules. Methanol (CH₃OH) — the simplest "complex organic molecule" and a gateway to prebiotic chemistry — has long been measured at less than 10% of water abundance in interstellar ices.
The Target: SVS 13-A
- A Class I protostellar binary in the NGC 1333 cloud, Perseus, at ~300 pc (~1,000 light-years)
- Components VLA 4A and VLA 4B separated by ~90 AU, each with its own disk, embedded in a circumbinary disk with spiral arms
- Both host hot corinos — regions above ~100 K where ice mantles sublimate, releasing complex organics (methanol, acetaldehyde, dimethyl ether, formamide)
- Chemistry differs between the two components: nitrogen-bearing molecules are more abundant around VLA 4A
- SOFIA (Stratospheric Observatory for Infrared Astronomy), a 2.7-m telescope aboard a modified Boeing 747SP, flew above 99% of atmospheric water vapor before its retirement in September 2022
- The EXES spectrograph (Echelon-Cross-Echelle Spectrograph), R ≈ 70,500, targeted H₂O and CH₃OH absorption near 26 μm
- N(CH₃OH) ≈ 2.09 × 10¹⁷ cm⁻²
- N(H₂O) ≈ 4.9 × 10¹⁶ cm⁻²
- DeWitt et al. (2026), arXiv:2603.19992, accepted to ApJL
- Bianchi et al. (2022), ApJL, 928, L3
- Diaz-Rodriguez et al. (2022), A&A
- Tinacci et al. (2023); Bariosco et al. (2025)
- Ceccarelli et al. (2017), ARA&A
- NASA SOFIA history report (SP-2025-4901)
The Observation: SOFIA's Last Look
The Surprise: Methanol Wins
LTE slab model fitting gave excitation temperatures of ~168 K (water) and ~141 K (methanol) — consistent with a common ice-sublimation environment. But the column densities were startling:
Methanol is ~4× more abundant than water — reversing the canonical interstellar ice recipe.
Proposed Explanations
The authors suggest the mid-IR absorption probes a cold outer skin of the hot corino (the layer outside the dust τ = 1 photosphere), unlike millimeter emission from the hot inner core. In this transition zone:
1. Selective desorption: quantum-chemical studies (Tinacci et al. 2023; Bariosco et al. 2025) show binding-energy *distributions*, not fixed values; below ~60 K, methanol desorbs more readily than water, enriching the gas phase by roughly a factor of 2 2. Differential re-condensation: water sticks back onto grains faster than methanol, amplifying the gas-phase ratio by an additional ~1.5× 3. Layered ice structure: ices form as a stratified "layer cake"; absorption may sample a methanol-rich outer layer while water remains trapped deeper
Why It Matters
Planets inherit their chemistry from the natal envelope. Solar System comets show methanol/water ratios of only a few percent; a region at 400% implies a very different chemical legacy for any planets forming around SVS 13-A — with potential consequences for prebiotic chemistry. Caveats remain: the binary geometry, jets, streamers, and circumbinary spiral structure make this a complex, dynamic system, and the 4:1 ratio may be a snapshot of one moment and viewing angle.
Outlook
SOFIA has ceased flying, but its data archive continues to yield results. Future JWST mid-IR spectroscopy and higher-resolution ALMA imaging should test whether selective desorption, ice stratification, or another mechanism explains this anomaly.