REVIEW 2 major objections 5 minor 2 cited by
MINDS. JWST-MIRI reveals a peculiar CO$_2$-rich chemistry in the drift-dominated disk CX Tau
T0 review · 2 major / 5 minor · reviewed 2026-08-11 · deepseek-v4-flash
Pith's one-line read JWST-MIRI observations of CX Tau show that radial drift of icy pebbles is actively setting the inner-disk chemistry, producing a bright CO2-rich phase with cold 13CO2 and H2O emission near the snowlines.
desk verdict Solid MINDS data paper with a plausible drift/CO2-rich story; the cold 13CO2 pillar is softer than the text claims, but the cold H2O component and the CO2 excess keep the paper worth publishing. read the letter →
The pith
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
The reading
What carries the argument
The load-bearing tool is the 0D LTE slab model, which fits each molecule's emission with three parameters: line-of-sight column density $N$, temperature $T$, and emitting area $A$, converted to a radius through $A=\pi R^2$, with a fixed Gaussian line width of 4.7 km s$^{-1}$. The model is applied sequentially to $^{12}$CO$_2$, H$_2$O, C$_2$H$_2$, $^{13}$CO$_2$, OH, and HCN in the 13.5-17.5 $\mu$m region, with H$_2$O also fit separately at 5.5-8.5 $\mu$m. The argument for drift-driven chemistry rests on comparing the $^{12}$CO$_2$ and $^{13}$CO$_2$ Q-branch shapes: the temperature-sensitive broadening shows they trace different gas, with the optically thinner isotopologue revealing a cold component near the CO$_2$ snowline, and the diagnostic H$_2$O line ratios at 23.8-23.9 $\mu$m revealing a cold $\sim$200 K water component.
What would settle it
Take a higher-S/N MIRI spectrum of CX Tau and fit the 13.5-17.5 $\mu$m region and the 21-24 $\mu$m H$_2$O lines with a two-temperature LTE model or a non-LTE model; if the $\sim$200 K $^{13}$CO$_2$ and H$_2$O components disappear or move to different temperatures, the drift interpretation loses its main evidence. Separately, sub-2 au ALMA imaging can test the predicted small inner cavity: if no $\sim$2 au cavity is found, radial drift remains the preferred explanation; if one is found, the CO$_2$ enhancement could be cavity-induced instead.
Extended reading notes
Core claim
CX Tau, a disk around a low-mass M2.5 star, shows mid-infrared molecular emission that is peculiar for a compact, drift-dominated disk: instead of the bright H$_2$O expected from efficient radial drift, its spectrum is dominated by a bright CO$_2$ feature. Slab-model fits find optically thick $^{12}$CO$_2$ emission at $\sim$450 K from an equivalent radius of $\sim$0.05 au, while $^{13}$CO$_2$ traces a colder $\sim$200 K component over a larger emitting area; H$_2$O shows a warm $\sim$500-600 K component plus a cold $\sim$200 K component at longer wavelengths. The cold $^{13}$CO$_2$ and H$_2$O components are interpreted as direct evidence that icy pebbles are drifting across the CO$_2$ and H$_2$O snowlines and sublimating, enriching the inner disk. The authors argue the bright CO$_2$ reflects an evolutionary stage in which H$_2$O-rich gas has already advected onto the star and CO$_2$-rich gas is now arriving, with the relatively weak warm H$_2$O explained by the star's low accretion luminosity. They also consider, but disfavor, an alternative in which a small $\sim$2 au inner cavity outside the H$_2$O snowline produces the CO$_2$ enhancement.
Load-bearing premise
The whole cold-component interpretation rests on the slab models that assign each molecule a single temperature and a fixed 4.7 km s$^{-1}$ line width; if the real emission has multiple temperature components or non-LTE excitation, the cold $\sim$200 K $^{13}$CO$_2$ and H$_2$O signals could be fitting artifacts rather than evidence for drifting ice, a limitation the paper itself notes for most species.
Editorial extensions
If this is right
- If CX Tau is in a CO$_2$-rich phase, compact drift-dominated disks should show a time sequence in their inner-disk volatile chemistry: an early H$_2$O-rich stage, then a CO$_2$-rich stage, then carbon-rich gas, with the CO$_2$/H$_2$O ratio acting as a clock for how much ice has drifted inward and drained onto the star.
- The cold $\sim$200 K $^{13}$CO$_2$ and H$_2$O components make rare isotopologues of CO$_2$ and the long-wavelength H$_2$O rotational lines practical probes of snowline sublimation, since they isolate gas that is otherwise hidden behind optically thick $^{12}$CO$_2$ emission.
- Accretion luminosity must be folded into any disk size-chemistry comparison: CX Tau's H$_2$O flux is unremarkable once its low accretion rate is accounted for, so disk compactness alone does not guarantee bright water emission.
- The potential detection of CO$^{18}$O, if confirmed, would provide an optically thin measurement of the total CO$_2$ column density and a cleaner tracer of the cold component than $^{13}$CO$_2$.
- Higher-angular-resolution ALMA observations can discriminate between the drift scenario and the alternative explanation of a small inner cavity: a $\sim$2 au cavity should be directly detectable with sub-2 au resolution, while absence of such a cavity would leave radial drift as the preferred explanation.
Reading between the lines
- One consequence the authors leave implicit: if drift-driven chemistry cycles CO$_2$ through the inner disk, the gas accreting onto the star and the solids building planets may shift between oxygen-rich and carbon-rich compositions on timescales shorter than the disk lifetime, so CX Tau-like disks are natural laboratories for the volatile delivery stage of planet formation.
- A direct testable extension would be a survey of compact versus extended disks measuring the same diagnostic ratios (the 1500/3600 K versus 3600/6000 K H$_2$O line ratio plane, and the $^{13}$CO$_2$/$^{12}$CO$_2$ Q-branch contrast); the drift scenario predicts that compact, high R$_{\mathrm{gas}}$/R$_{\mathrm{dust}}$ disks cluster in the CO$_2$-rich corner of that plane.
- The single-temperature slab fits leave large degeneracies, so the cold-component claim would be strengthened by fitting the full 13.5-17.5 $\mu$m region with a two-temperature LTE model or a non-LTE excitation model, something the paper identifies as needed future work.
- If the CO$_2$-rich phase is real, the same drift mechanism should also enhance other volatiles with icelines in the outer disk (e.g., hydrocarbons) at later stages, so CX Tau may be an early snapshot in a sequence that ends with a carbon-rich inner disk.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The paper presents JWST MIRI/MRS observations of CX Tau, a compact protoplanetary disk with a high gas-to-dust radius ratio indicative of strong radial drift. The authors detect H2O, 12CO2, 13CO2, C2H2, HCN, OH, H2, and possibly CO18O, and fit the molecular features with 0D LTE slab models. They find warm, optically thick 12CO2 emission at ~450 K and warm H2O at ~500-600 K, together with evidence for colder ~200 K components in 13CO2 and H2O. They interpret the bright CO2 and the cold components as signs that radial drift of icy pebbles has moved CX Tau into a CO2-rich evolutionary phase, while also discussing alternative explanations involving an inner cavity or a low gas-to-dust ratio.
Significance. If the cold 13CO2 and cold H2O components are real, the paper provides one of the clearest observational links between radial drift, snowline ice sublimation, and inner-disk chemistry in a compact disk. The work is valuable for connecting ALMA-derived disk size ratios with JWST molecular inventories, and it explicitly places CX Tau in the context of time-dependent drift models (Mah et al. 2023; Sellek et al. 2024). The paper is generally careful with weak detections, includes an MCMC cross-check of the step-by-step fitting, and quantifies CX Tau's CO2 excess relative to the Banzatti et al. (2020) sample. The principal weakness is that the two cold components that carry the central interpretation are inferred from visual or semi-quantitative comparisons rather than from formally quoted confidence intervals.
major comments (2)
- [Sect. 3.2.1, Fig. 3, Appendix A.1] The claim that the 13CO2 emission is constrained to a cold temperature below 300 K is not supported by the uncertainties stated in the manuscript. Appendix A.1 says that for all species except 12CO2, temperatures are constrained only to within about 100-200 K; with a best-fit temperature near 180-200 K, the 1-sigma interval includes 300-400 K. The visual comparison in Fig. 3 uses fixed-column-density models scaled in radius to the same peak flux, which is not the same as a 1-sigma exclusion from the chi-squared map. Please show the 1-sigma and 3-sigma marginal contours for the 13CO2 temperature from Fig. A.4 or the MCMC posterior in Fig. A.5 and state explicitly whether T > 300 K is excluded. If it is not excluded, the conclusion that 13CO2 is significantly colder than 12CO2, and the drift interpretation built on that difference, need to be reworded or downgraded.
- [Sect. 3.2.3, Fig. 5] The cold ~200 K H2O component is a second pillar of the drift interpretation, but it is currently established only through visual line-ratio comparisons and a rescaled comparison to DR Tau, with no chi-squared fit or quoted uncertainty. Please provide measured fluxes and uncertainties for the diagnostic H2O lines near 23.8-23.9 um and for the line ratios used in Fig. 8, and test explicitly whether a single-temperature warm model can be rejected at a formal confidence level. Without this, the statement that the cold H2O component is "clearly detected" (Sect. 3.2.3) overstates the quantitative support.
minor comments (5)
- [Abstract] The phrase "and even demonstrate a potential detection" is slightly contradictory; consider "and even present evidence for a potential detection" or "and possibly detect".
- [Sect. 3.2.3] The sentence "The latter have an upper level energy" should read "The latter lines have upper level energies" or similar.
- [Fig. 5 caption and text] In the discussion of the left and middle panels, the terms "the former model" and "the latter" are ambiguous because three models (warm H2O, cold H2O, OH) are listed. Please refer to them explicitly as "the warm H2O model" and "the cold H2O model."
- [Sect. 3.2.1 vs Fig. A.6] The column density assumed for the CO18O model is given as 5 x 10^16 cm^-2 in Sect. 3.2.1 but as 10^16 cm^-2 in the Fig. A.6 caption. Please reconcile these values.
- [Sect. 3.2.4] The text says "We find evidence of OH prompt emission" after initially labeling it a "potential detection"; the Conclusions correctly list it as potential, but the main text should maintain the same level of hedging throughout.
Circularity Check
No significant circularity: the spectral temperatures and column densities are empirical fits, and the drift interpretation is a comparative model scenario with explicit alternatives rather than a by-construction prediction.
full rationale
The paper's derivation chain is: JWST MIRI spectrum -> continuum subtraction -> 0D LTE slab fits -> best-fit T, N, R for each molecule -> comparison with thermochemical model predictions for CO2/H2O ratios. The cold 13CO2 (~200 K) and cold H2O (~200 K) components are fitted from the data, not imposed by the drift framework; the slab model assumptions (single temperature, fixed 4.7 km/s line width, A=pi R^2) are stated and the fits are explicitly acknowledged to be weakly constrained for most species (Sect. 3.2, Appendix A.1). The interpretation leans on modeling work by Sellek et al. (2024), Mah et al. (2023), and Vlasblom et al. (2024), which share some authors with this paper, but those are independent thermochemical simulations with parameter-free, qualitative predictions (e.g., a CO2-rich evolutionary phase), and the paper openly weighs alternatives: a small inner cavity (Sect. 4.2) and a reduced gas-to-dust ratio (Sect. 4.3). The claim that the 13CO2 Q-branch shape constrains T<300 K relies partly on visual model comparison, and the quoted uncertainties (100-200 K in temperature for non-12CO2 species) mean the cold component could be less robust; however, that is a statistical robustness concern, not a circular reduction. No equation or fitted parameter is reused as its own prediction, and no load-bearing result is forced by self-citation. The paper is therefore self-contained on the observational side, with only a mild, non-load-bearing self-citation pattern in the interpretive discussion.
Assumptions & free parameters
free parameters (16)
- 12CO2 temperature =
~450 K
- 12CO2 column density =
~8 x 10^17 cm^-2
- 12CO2 emitting radius =
~0.05 au
- 13CO2 temperature =
~180-200 K
- 13CO2 column density =
~2 x 10^17 cm^-2
- 13CO2 emitting radius =
~0.2 au
- H2O rotational temperature =
~500-600 K
- H2O rotational column density =
~10^19 cm^-2 (or ~10^18 with narrower windows)
- H2O rotational emitting radius =
~0.05 au
- H2O ro-vibrational parameters =
T ~500-600 K, N >10^20 cm^-2, R slightly smaller than 0.05 au
- Cold H2O component temperature =
~200 K
- C2H2 temperature =
warm, unconstrained
- HCN slab parameters =
unconstrained
- OH LTE slab temperature =
>1500 K
- CO18O column density =
5 x 10^16 cm^-2 (assumed)
- CO18O temperature =
~200 K
assumptions (9)
- domain assumption The molecular emission is in local thermodynamic equilibrium, describable by a single excitation temperature for each species.
- domain assumption Line profiles are Gaussian with FWHM = 4.7 km/s.
- domain assumption Disk isotope ratios equal ISM values (12C/13C = 68, 16O/18O = 500).
- domain assumption CX Tau's small dust disk relative to gas disk (Rgas/Rdust ~ 5) is caused by efficient radial drift.
- domain assumption Literature stellar parameters (M* = 0.37 Msun, L* = 0.22 Lsun, Teff = 3483 K, distance = 127.9 pc, inclination = 55 deg) are accurate.
- domain assumption The fitted emitting area maps to a physical radius as A = pi R^2.
- domain assumption The continuum subtraction (IRSQR, quantile 0.1, knots every 25 points) does not bias the weak molecular features.
- domain assumption Chemical evolution models of Sellek et al. (2024) and Mah et al. (2023) are applicable to CX Tau.
- domain assumption OH prompt emission from H2O photodissociation preferentially populates A' symmetry states.
Cite this review
Pith. "Pith review of MINDS. JWST-MIRI reveals a peculiar CO$_2$-rich chemistry in the drift-dominated disk CX Tau." pith.science (2026). https://pith.science/paper/2CG56JQR
@misc{pith2026241212715,
author = {Pith},
title = {Pith review of: MINDS. JWST-MIRI reveals a peculiar CO$_2$-rich chemistry in the drift-dominated disk CX Tau},
year = {2026},
howpublished = {\url{https://pith.science/paper/2CG56JQR}},
note = {Machine review of arXiv:2412.12715}
}
abstract
Radial drift of icy pebbles can have a large impact on the chemistry of the inner regions of protoplanetary disks. Compact dust disks ($\lesssim$50 au) are suggested to have a higher (cold) H$_2$O flux than more extended disks, likely due to efficient radial drift bringing H$_2$O-rich material to the inner disk, where it can be observed with JWST. We present JWST MIRI/MRS observations of the disk CX Tau taken as a part of the Mid-INfrared Disk Survey (MINDS) GTO program, a prime example of a drift-dominated disk. This compact disk seems peculiar: the source possesses a bright CO$_2$ feature instead of the bright H$_2$O expected based on its efficient radial drift. We aim to provide an explanation for this finding. We detect molecular emission from H$_2$O, $^{12}$CO$_2$, $^{13}$CO$_2$, C$_2$H$_2$, HCN, and OH in this disk, and even demonstrate a potential detection of CO$^{18}$O. Analysis of the $^{12}$CO$_2$ and $^{13}$CO$_2$ emission shows the former to be tracing a temperature of $\sim$450 K, whereas the $^{13}$CO$_2$ traces a significantly colder temperature ($\sim$200 K). H$_2$O is also securely detected both at shorter and longer wavelengths, tracing a similar temperature of $\sim$500-600 K as the CO$_2$ emission. We also find evidence for a colder, $\sim$200 K H$_2$O component at longer wavelengths, which is in line with this disk having strong radial drift. The cold $^{13}$CO$_2$ and H$_2$O emission indicate that radial drift of ices likely plays an important role in setting the chemistry of the inner disk of CX Tau. Potentially, the H$_2$O-rich gas has already advected onto the central star, which is now followed by an enhancement of comparatively CO$_2$-rich gas reaching the inner disk, explaining the enhancement of CO$_2$ emission in CX Tau. The comparatively weaker H$_2$O emission can be explained by the source's low accretion luminosity. (abridged)
Figures
Figures from the paper (5 more)
Forward citations
Cited by 2 Pith papers
-
JWST/MIRI Detection of Molecular H$_2$ Winds from an Edge-on Class II Source HV Tau C
The edge-on Class II disk HV Tau C hosts a spatially extended, wide-angled molecular hydrogen wind with warm (~600 K) and hot (~2000 K) components and a mass-loss rate near 1e-8 solar masses per year.
-
Compact protoplanetary discs can be produced by dead zones
Fragile dust destroyed beyond a dead zone limits mm-dust emission to the dead zone radius, naturally producing the compact discs seen around young stars.
Reference graph
Works this paper leans on
-
[1]
, " * write output.state after.block = add.period write newline
ENTRY address archiveprefix author booktitle chapter edition editor howpublished institution eprint journal key month note number organization pages publisher school series title type volume year label extra.label sort.label short.list INTEGERS output.state before.all mid.sentence after.sentence after.block FUNCTION init.state.consts #0 'before.all := #1 ...
-
[2]
write newline
" write newline "" before.all 'output.state := FUNCTION n.dashify 't := "" t empty not t #1 #1 substring "-" = t #1 #2 substring "--" = not "--" * t #2 global.max substring 't := t #1 #1 substring "-" = "-" * t #2 global.max substring 't := while if t #1 #1 substring * t #2 global.max substring 't := if while FUNCTION word.in bbl.in " " * FUNCTION format....
-
[3]
R., Williams , J
Anderson , A. R., Williams , J. P., & Blake , G. A. 2024, , submitted
2024
-
[4]
M., Huang , J., P \'e rez , L
Andrews , S. M., Huang , J., P \'e rez , L. M., et al. 2018, , 869, L41
2018
-
[5]
P., Trapman , L., et al
Ansdell , M., Williams , J. P., Trapman , L., et al. 2018, , 859, 21
2018
-
[6]
M., Kamp , I., Henning , T., et al
Arabhavi , A. M., Kamp , I., Henning , T., et al. 2024, Science, 384, 1086
2024
-
[7]
R., et al
Argyriou , I., Glasse , A., Law , D. R., et al. 2023, , 675, A111
2023
-
[8]
Ballering , N. P. & Eisner , J. A. 2019, , 157, 144
2019
Show all 119 references
-
[9]
D., et al
Banzatti , A., Pascucci , I., Bosman , A. D., et al. 2020, , 903, 124
2020
-
[10]
M., Carr , J
Banzatti , A., Pontoppidan , K. M., Carr , J. S., et al. 2023 a , , 957, L22
2023
-
[11]
M., P \'e re Ch \'a vez , J., et al
Banzatti , A., Pontoppidan , K. M., P \'e re Ch \'a vez , J., et al. 2023 b , , 165, 72
2023
-
[12]
M., et al
Banzatti , A., Salyk , C., Pontoppidan , K. M., et al. 2024, arXiv e-prints, arXiv:2409.16255
2024 arXiv
-
[13]
& Mah , J
Bitsch , B. & Mah , J. 2023, , 679, A11
2023
-
[14]
& Wurm , G
Blum , J. & Wurm , G. 2008, , 46, 21
2008
-
[15]
A., Clarke , C
Booth , R. A., Clarke , C. J., Madhusudhan , N., & Ilee , J. D. 2017, , 469, 3994
2017
-
[16]
D., Appelgren , J., Bergin , E
Bosman , A. D., Appelgren , J., Bergin , E. A., Lambrechts , M., & Johansen , A. 2023, , 944, L53
2023
-
[17]
D., Bergin , E
Bosman , A. D., Bergin , E. A., Calahan , J., & Duval , S. E. 2022 a , , 930, L26
2022
-
[18]
D., Bergin , E
Bosman , A. D., Bergin , E. A., Calahan , J. K., & Duval , S. E. 2022 b , , 933, L40
2022
-
[19]
D., Bergin , E
Bosman , A. D., Bergin , E. A., Loomis , R. A., et al. 2021, , 257, 15
2021
-
[20]
D., Bruderer , S., & van Dishoeck , E
Bosman , A. D., Bruderer , S., & van Dishoeck , E. F. 2017, , 601, A36
2017
-
[21]
2001, , 375, 950
Bouwman , J., Meeus , G., de Koter , A., et al. 2001, , 375, 950
2001
-
[22]
2023, JWST Calibration Pipeline
Bushouse , H., Eisenhamer , J., Dencheva , N., et al. 2023, JWST Calibration Pipeline
2023
-
[23]
Carnall , A. C. 2017, arXiv e-prints, arXiv:1705.05165
2017 arXiv
-
[24]
Carr , J. S. & Najita , J. R. 2014, , 788, 66
2014
-
[25]
Charnley , S. B. 1997, , 481, 396
1997
-
[26]
2023, The Journal of Open Source Software, 8, 4774
Christiaens , V., Gonzalez , C., Farkas , R., et al. 2023, The Journal of Open Source Software, 8, 4774
2023
-
[27]
2024, MINDS: Hybrid pipeline for the reduction of JWST/MIRI-MRS data , Astrophysics Source Code Library, record ascl:2403.007
Christiaens , V., Samland , M., Gasman , D., Temmink , M., & Perotti , G. 2024, MINDS: Hybrid pipeline for the reduction of JWST/MIRI-MRS data , Astrophysics Source Code Library, record ascl:2403.007
2024
-
[28]
A., Ru \' z-Rodr \' guez , D., Hales , A., et al
Cieza , L. A., Ru \' z-Rodr \' guez , D., Hales , A., et al. 2019, , 482, 698
2019
-
[29]
Dawson , R. I. & Johnson , J. A. 2018, , 56, 175
2018
-
[30]
2022, pybaselines : A Python library of algorithms for the baseline correction of experimental data
Erb , D. 2022, pybaselines : A Python library of algorithms for the baseline correction of experimental data
2022
-
[31]
2013, , 762, 62
Espaillat , C., Ingleby , L., Furlan , E., et al. 2013, , 762, 62
2013
-
[32]
C., Thanathibodee , T., Pittman , C
Espaillat , C. C., Thanathibodee , T., Pittman , C. V., et al. 2023, , 958, L4
2023
-
[33]
Facchini , S., Birnstiel , T., Bruderer , S., & van Dishoeck , E. F. 2017, , 605, A16
2017
-
[34]
F., Manara , C
Facchini , S., van Dishoeck , E. F., Manara , C. F., et al. 2019, , 626, L2
2019
-
[35]
2018, , 868, 28
Fang , M., Pascucci , I., Edwards , S., et al. 2018, , 868, 28
2018
-
[36]
2024, , 687, A96
Franceschi , R., Henning , T., Tabone , B., et al. 2024, , 687, A96
2024
-
[37]
2006, , 165, 568
Furlan , E., Hartmann , L., Calvet , N., et al. 2006, , 165, 568
2006
-
[38]
L., Espaillat , C., et al
Furlan , E., Luhman , K. L., Espaillat , C., et al. 2011, , 195, 3
2011
-
[39]
Gaia Collaboration , Brown , A. G. A., Vallenari , A., et al. 2018, , 616, A1
2018
-
[40]
F., Grant , S
Gasman , D., van Dishoeck , E. F., Grant , S. L., et al. 2023, , 679, A117
2023
-
[41]
E., Najita , J
Glassgold , A. E., Najita , J. R., & Igea , J. 2007, , 656, 515
2007
-
[42]
A., Wertz , O., Absil , O., et al
Gomez Gonzalez , C. A., Wertz , O., Absil , O., et al. 2017, , 154, 7
2017
-
[43]
L., Kurtovic , N
Grant , S. L., Kurtovic , N. T., van Dishoeck , E. F., et al. 2024, , 689, A85
2024
-
[44]
L., van Dishoeck , E
Grant , S. L., van Dishoeck , E. F., Tabone , B., et al. 2023, , 947, L6
2023
-
[45]
J., Kamp , I., Waters , L
Greenwood , A. J., Kamp , I., Waters , L. B. F. M., Woitke , P., & Thi , W. F. 2019, , 631, A81
2019
-
[46]
1998, , 492, 323
Gullbring , E., Hartmann , L., Brice \ n o , C., & Calvet , N. 1998, , 492, 323
1998
-
[47]
& Blum , J
Gundlach , B. & Blum , J. 2015, , 798, 34
2015
-
[48]
P., Kreuzig , C., et al
Gundlach , B., Schmidt , K. P., Kreuzig , C., et al. 2018, , 479, 1273
2018
-
[49]
1998, , 495, 385
Hartmann , L., Calvet , N., Gullbring , E., & D'Alessio , P. 1998, , 495, 385
1998
-
[50]
N., Bosman , A
Heays , A. N., Bosman , A. D., & van Dishoeck , E. F. 2017, , 602, A105
2017
-
[51]
2024, , 136, 054302
Henning , T., Kamp , I., Samland , M., et al. 2024, , 136, 054302
2024
-
[52]
Herczeg , G. J. & Hillenbrand , L. A. 2008, , 681, 594
2008
-
[53]
Herczeg , G. J. & Hillenbrand , L. A. 2014, , 786, 97
2014
-
[54]
& Gorti , U
Hollenbach , D. & Gorti , U. 2009, , 703, 1203
2009
-
[55]
M., Dullemond , C
Huang , J., Andrews , S. M., Dullemond , C. P., et al. 2018, , 869, L42
2018
-
[56]
C., \'A lvarez-M \'a rquez , J., Sloan , G
Jones , O. C., \'A lvarez-M \'a rquez , J., Sloan , G. C., et al. 2023, , 523, 2519
2023
-
[57]
Kaeufer , T., Min , M., Woitke , P., Kamp , I., & Arabhavi , A. M. 2024, , 687, A209
2024
-
[58]
2023, , 954, 66
Kalyaan , A., Pinilla , P., Krijt , S., et al. 2023, , 954, 66
2023
-
[59]
D., & Banzatti , A
Kalyaan , A., Pinilla , P., Krijt , S., Mulders , G. D., & Banzatti , A. 2021, , 921, 84
2021
-
[60]
M., et al
Kamp , I., Henning , T., Arabhavi , A. M., et al. 2023, Faraday Discussions, 245, 112
2023
-
[61]
2024, , 689, A231
Kanwar , J., Kamp , I., Jang , H., et al. 2024, , 689, A231
2024
-
[62]
P., et al
Kessler-Silacci , J., Augereau , J.-C., Dullemond , C. P., et al. 2006, , 639, 275
2006
-
[63]
2023, , 945, L7
K \'o sp \'a l , \'A ., \'A brah \'a m , P., Diehl , L., et al. 2023, , 945, L7
2023
-
[64]
D., Zhang , K., et al
Krijt , S., Bosman , A. D., Zhang , K., et al. 2020, , 899, 134
2020
-
[65]
R., Bergin , E
Krijt , S., Schwarz , K. R., Bergin , E. A., & Ciesla , F. J. 2018, , 864, 78
2018
-
[66]
L., Bitsch , B., & Henning , T
Lienert , J. L., Bitsch , B., & Henning , T. 2024, , 691, A72
2024
-
[67]
J., Harsono , D., et al
Long , F., Herczeg , G. J., Harsono , D., et al. 2019, , 882, 49
2019
-
[68]
J., et al
Long , F., Pinilla , P., Herczeg , G. J., et al. 2018, , 869, 17
2018
-
[69]
2023, , 677, L7
Mah , J., Bitsch , B., Pascucci , I., & Henning , T. 2023, , 677, L7
2023
-
[70]
2024, , 686, L17
Mah , J., Savvidou , S., & Bitsch , B. 2024, , 686, L17
2024
-
[71]
F., Ansdell , M., Rosotti , G
Manara , C. F., Ansdell , M., Rosotti , G. P., et al. 2023, in Astronomical Society of the Pacific Conference Series, Vol. 534, Protostars and Planets VII, ed. S. Inutsuka , Y. Aikawa , T. Muto , K. Tomida , & M. Tamura , 539
2023
-
[72]
M., Mumma , M
Mandell , A. M., Mumma , M. J., Blake , G. A., et al. 2008, , 681, L25
2008
-
[73]
McClure , M. K. 2019, , 632, A32
2019
-
[74]
E., & Najita , J
Meijerink , R., Glassgold , A. E., & Najita , J. R. 2008, , 676, 518
2008
-
[75]
M., Blake , G
Meijerink , R., Pontoppidan , K. M., Blake , G. A., Poelman , D. R., & Dullemond , C. P. 2009, , 704, 1471
2009
-
[76]
N., Savage , C., Brewster , M
Milam , S. N., Savage , C., Brewster , M. A., Ziurys , L. M., & Wyckoff , S. 2005, , 634, 1126
2005
-
[77]
& Wurm , G
Musiolik , G. & Wurm , G. 2019, , 873, 58
2019
-
[78]
R., Carr , J
Najita , J. R., Carr , J. S., Pontoppidan , K. M., et al. 2013, , 766, 134
2013
-
[79]
R., Strom , S
Najita , J. R., Strom , S. E., & Muzerolle , J. 2007, , 378, 369
2007
-
[80]
A., Manoj , P., Tyagi , H., et al
Neufeld , D. A., Manoj , P., Tyagi , H., et al. 2024, , 966, L22
2024
-
[81]
\"O berg , K. I. & Bergin , E. A. 2021, , 893, 1
2021
-
[82]
I., Murray-Clay , R., & Bergin , E
\"O berg , K. I., Murray-Clay , R., & Bergin , E. A. 2011, , 743, L16
2011
-
[83]
C., van Dishoeck , E
Olofsson , J., Augereau , J. C., van Dishoeck , E. F., et al. 2010, , 520, A39
2010
-
[84]
C., van Dishoeck , E
Olofsson , J., Augereau , J. C., van Dishoeck , E. F., et al. 2009, , 507, 327
2009
-
[85]
2016, , 585, A35
Pinilla , P., Klarmann , L., Birnstiel , T., et al. 2016, , 585, A35
2016
-
[86]
M., Salyk , C., Banzatti , A., et al
Pontoppidan , K. M., Salyk , C., Banzatti , A., et al. 2024, , 963, 158
2024
-
[87]
2003, , 412, L43
Przygodda , F., van Boekel , R., \`A brah \`a m , P., et al. 2003, , 412, L43
2003
-
[88]
C., Bik , A., Cuijpers , L., et al
Ram \' rez-Tannus , M. C., Bik , A., Cuijpers , L., et al. 2023, , 958, L30
2023
-
[89]
H., Ressler , M
Rieke , G. H., Ressler , M. E., Morrison , J. E., et al. 2015, , 127, 665
2015
-
[90]
2015, , 801, 31
Rigliaco , E., Pascucci , I., Duchene , G., et al. 2015, , 801, 31
2015
-
[91]
E., Banzatti , A., \"O berg , K
Romero-Mirza , C. E., Banzatti , A., \"O berg , K. I., et al. 2024 a , , 975, 78
2024
-
[92]
E., \"O berg , K
Romero-Mirza , C. E., \"O berg , K. I., Banzatti , A., et al. 2024 b , , 964, 36
2024
-
[93]
M., Blake , G
Salyk , C., Pontoppidan , K. M., Blake , G. A., et al. 2008, , 676, L49
2008
-
[94]
M., Blake , G
Salyk , C., Pontoppidan , K. M., Blake , G. A., Najita , J. R., & Carr , J. S. 2011, , 731, 130
2011
-
[95]
R., Henning , T., Christiaens , V., et al
Schwarz , K. R., Henning , T., Christiaens , V., et al. 2024, , 962, 8
2024
-
[96]
D., Vlasblom , M., & van Dishoeck , E
Sellek , A. D., Vlasblom , M., & van Dishoeck , E. F. 2024, arXiv e-prints, arXiv:2412.01895
2024 arXiv
-
[97]
2017, , 844, 158
Simon , M., Guilloteau , S., Di Folco , E., et al. 2017, , 844, 158
2017
-
[98]
2012, , 759, 47
Szul \'a gyi , J., Pascucci , I., \'A brah \'a m , P., et al. 2012, , 759, 47
2012
-
[99]
F., et al
Tabone , B., Bettoni , G., van Dishoeck , E. F., et al. 2023, Nature Astronomy
2023
-
[100]
F., & Black , J
Tabone , B., van Dishoeck , E. F., & Black , J. H. 2024, , 691, A11
2024
-
[101]
C., van Dishoeck , E
Tabone , B., van Hemert , M. C., van Dishoeck , E. F., & Black , J. H. 2021, , 650, A192
2021
-
[102]
F., Gasman , D., et al
Temmink , M., van Dishoeck , E. F., Gasman , D., et al. 2024 a , , 689, A330
2024
-
[103]
F., Grant , S
Temmink , M., van Dishoeck , E. F., Grant , S. L., et al. 2024 b , , 686, A117
2024
-
[104]
R., et al
Trapman , L., Ansdell , M., Hogerheijde , M. R., et al. 2020, , 638, A38
2020
-
[105]
R., van Dishoeck , E
Trapman , L., Facchini , S., Hogerheijde , M. R., van Dishoeck , E. F., & Bruderer , S. 2019, , 629, A79
2019
-
[106]
F., Grant , S., Tabone , B., et al
van Dishoeck , E. F., Grant , S., Tabone , B., et al. 2023, Faraday Discussions, 245, 52
2023
-
[107]
F., Herbst , E., & Neufeld , D
van Dishoeck , E. F., Herbst , E., & Neufeld , D. A. 2013, Chemical Reviews, 113, 9043
2013
-
[108]
& van Hemert , M
van Harrevelt , R. & van Hemert , M. 2003, Chemical Physics Letters, 370, 706
2003
-
[109]
F., Tabone , B., & Bruderer , S
Vlasblom , M., van Dishoeck , E. F., Tabone , B., & Bruderer , S. 2024, , 682, A91
2024
-
[110]
2015, , 582, A88
Walsh , C., Nomura , H., & van Dishoeck , E. 2015, , 582, A88
2015
-
[111]
W., Glasse , A., et al
Wells , M., Pel , J. W., Glasse , A., et al. 2015, , 127, 646
2015
-
[112]
Wilson , T. L. 1999, Reports on Progress in Physics, 62, 143
1999
-
[113]
Wilson , T. L. & Rood , R. 1994, , 32, 191
1994
-
[114]
2016, , 586, A103
Woitke , P., Min , M., Pinte , C., et al. 2016, , 586, A103
2016
-
[115]
F., et al
Woitke , P., Min , M., Thi , W. F., et al. 2018, , 618, A57
2018
-
[116]
S., Rieke , G
Wright , G. S., Rieke , G. H., Glasse , A., et al. 2023, , 135, 048003
2023
-
[117]
S., Wright , D., Goodson , G
Wright , G. S., Wright , D., Goodson , G. B., et al. 2015, , 127, 595
2015
-
[118]
2024, Nature Astronomy [ [arXiv] 2312.14056 ]
Zannese , M., Tabone , B., Habart , E., et al. 2024, Nature Astronomy [ [arXiv] 2312.14056 ]
2024 arXiv
-
[119]
2015, Chem
Zhou , L., Xie , D., & Guo , H. 2015, Chem. Phys., 42, 124317
2015
Reviewed August 11, 2026 · model on record in the stance chip above.
Discussion (0). Continue with ORCID to comment.