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Uncertainties of the dust grain size in protoplanetary disks retrieved from millimeter continuum observations

Earth and Planetary Astrophysics · Submitted 5 Oct 2024

abstract compiled · 2026-09-23 · no language-model review

The authors' main claim When taking all of the four images into account, degeneracies between different parameters are highly reduced, and consequently the best-fit grain sizes are consistent with the reference setup at almost all radii.

how it is stated · asserted 0.98 read the record →

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arXiv ID2410.04079 (version 1)
Pith ID2XU2WRTV, Pith's permanent record of this paper and its review
CitationDafa Li, Hongchi Wang, Lei Wang, Min Fang, Yao Liu. "Uncertainties of the dust grain size in protoplanetary disks retrieved from millimeter continuum observations." arXiv:2410.04079 (2024). https://pith.science/paper/2XU2WRTV
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Compiled by classifier-1.13.0 via TypeSafe API, question bank abstract-p1-20260923, 2026-09-23: 1 request, 8,844 input tokens.

What the abstract itself states, as probabilities: claims first 0.03 · states limitation 0.94 · human participants 0.01 · controlled comparison 0.23 · randomized assignment 0.01 · states quantitative result 0.94 · compares with prior results 0.31 · mentions code or data availability 0.02.

The abstract, sentence by sentence

arXiv listing abstract v1. Results and the main claim are underlined; .

Investigating the dust grain size and its dependence on substructures in protoplanetary disks is a crucial step in understanding the initial process of planet formation. Spectral indices derived from millimeter observations are used as a common probe for grain size. Converting observed spectral indices into grain sizes is a complex task that involves solving the radiative transfer equation, taking into account the disk structure and dust properties. In this work, we ran reference radiative transfer models with known disk properties, and generated four synthetic images at wavelengths of 0.8, 1.3, 3, and 7.8 mm, representing high-resolution continuum observations. Rings and gaps were considered in the setup. We fit the synthetic images using the analytic solution of the radiative transfer equation to investigate the circumstances under which the input grain sizes can be recovered. The results show that fitting images at only two wavelengths is not sufficient to retrieve the grain size. Fitting three images improves the retrieval of grain size, but the dust surface density is still not well recovered. When taking all of the four images into account, degeneracies between different parameters are highly reduced, and consequently the best-fit grain sizes are consistent with the reference setup at almost all radii. We find that the inclination angle has a significant impact on the fitting results. For disks with low inclinations, the analytic approach works quite well. However, when the disk is tilted above about 60 degree, neither the grain size nor the dust surface density can be constrained, as the inclination effect will smooth out all substructures in the radial intensity profile of the disk.

background contribution method result interpretation main claim

What the classifier reports for each sentence. The number is the probability it gave the label.
#sentencerolethe authors' own workstates the main conclusionstrength
s0 Investigating the dust grain size and its dependence on substructures in protoplanetary disks is a crucial step in understanding the initial process of planet formation. background 1.00 0.04 0.02 asserted 1.00
s1 Spectral indices derived from millimeter observations are used as a common probe for grain size. background 0.99 0.06 0.02 asserted 1.00
s2 Converting observed spectral indices into grain sizes is a complex task that involves solving the radiative transfer equation, taking into account the disk structure and dust properties. background 1.00 0.05 0.02 asserted 1.00
s3 In this work, we ran reference radiative transfer models with known disk properties, and generated four synthetic images at wavelengths of 0.8, 1.3, 3, and 7.8 mm, representing high-resolution continuum observations. method 0.96 0.97 0.03 asserted 0.99
s4 Rings and gaps were considered in the setup. method 0.99 0.79 0.01 asserted 0.96
s5 We fit the synthetic images using the analytic solution of the radiative transfer equation to investigate the circumstances under which the input grain sizes can be recovered. method 0.98 0.96 0.03 asserted 0.86
s6 The results show that fitting images at only two wavelengths is not sufficient to retrieve the grain size. result 1.00 0.92 0.20 asserted 1.00
s7 Fitting three images improves the retrieval of grain size, but the dust surface density is still not well recovered. result 1.00 0.93 0.09 asserted 1.00
s8 When taking all of the four images into account, degeneracies between different parameters are highly reduced, and consequently the best-fit grain sizes are consistent with the reference setup at almost all radii. result 0.99 0.94 0.61 asserted 0.98
s9 We find that the inclination angle has a significant impact on the fitting results. result 1.00 0.92 0.11 asserted 1.00
s10 For disks with low inclinations, the analytic approach works quite well. result 0.89 0.85 0.07 asserted 0.95
s11 However, when the disk is tilted above about 60 degree, neither the grain size nor the dust surface density can be constrained, as the inclination effect will smooth out all substructures in the radial intensity profile of the disk. result 0.75 0.86 0.22 asserted 1.00

What kind of paper the classifier reports this is: simulation study 1.00 · evidence from simulation or computation 1.00.

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  • references and citing sentences
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Every quoted sentence on this record is the authors'. Every label is from Pith's closed vocabulary, with the probability shown beside it. Every number in the measurements table is the authors', checked by code. Record as JSON

The paper
Original abstract

Investigating the dust grain size and its dependence on substructures in protoplanetary disks is a crucial step in understanding the initial process of planet formation. Spectral indices derived from millimeter observations are used as a common probe for grain size. Converting observed spectral indices into grain sizes is a complex task that involves solving the radiative transfer equation, taking into account the disk structure and dust properties. In this work, we ran reference radiative transfer models with known disk properties, and generated four synthetic images at wavelengths of 0.8, 1.3, 3, and 7.8 mm, representing high-resolution continuum observations. Rings and gaps were considered in the setup. We fit the synthetic images using the analytic solution of the radiative transfer equation to investigate the circumstances under which the input grain sizes can be recovered. The results show that fitting images at only two wavelengths is not sufficient to retrieve the grain size. Fitting three images improves the retrieval of grain size, but the dust surface density is still not well recovered. When taking all of the four images into account, degeneracies between different parameters are highly reduced, and consequently the best-fit grain sizes are consistent with the reference setup at almost all radii. We find that the inclination angle has a significant impact on the fitting results. For disks with low inclinations, the analytic approach works quite well. However, when the disk is tilted above about 60 degree, neither the grain size nor the dust surface density can be constrained, as the inclination effect will smooth out all substructures in the radial intensity profile of the disk.

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2 arXiv papers cite this in 2 sentences

Each citing sentence is taken from the citing paper's LaTeX source and typed by Pith's classifier. A label appears at probability 0.8 or more (0.95 for support), a contest at 0.7 or more; the quoted words are the citing authors'. How each label was checked · JSON

What it cites · 4 sentences without a confident label

Cites as background 1 paper
  • It is generally believed that micron-sized dust grains collide and stick together by van der Waals forces, forming large aggregates up to the scale of millimeters, and that the gravitational force between kilometer-sized planetesimals is enough to accrete surrounding dust, making the bodies grow to larger sizes [ref] .

    Dust growth and evolution in protoplanetary disks · Introduction · 0.90

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