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The Dust and Snow Surfaces of IRAS 04302+2247

A look into the dust settling and conditions around a young star.

― 7 min read


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In the vast universe, stars and Planets are born in massive clouds of gas and Dust. One of the fascinating aspects of this process is how dust settles in these early environments. Understanding how dust behaves in these forming stars can give us insights into how planets develop. This article explores the dust settling and snow surfaces of a specific young star known as IRAS 04302+2247, which is located in a dense region of the Taurus constellation.

The Setting: IRAS 04302+2247

IRAS 04302+2247, often called the "Butterfly Star" due to its beautiful surrounding nebula, is a young protostar in the Class I category. This means it is in an early stage of development, where it is still gathering material and forming. Researchers have pointed powerful telescopes at this star to learn more about its dust and gas.

As the star develops, it gathers material from its environment. Much of this material comes in the form of microscopic dust particles. When we look at the dust around this star, we see that it behaves differently than the gas surrounding it. The gas is often much taller and spread out, while dust can settle lower in the disk around the star.

How Dust Settles

Dust settling is a process influenced by gravity and turbulence. When dust particles become disconnected from the gas, they tend to fall down toward the star due to gravity. However, this process is often interrupted by turbulence, which can mix the dust back into the gas.

In many cases, the dust remains in a thick layer above the star, leading to challenges in understanding how planets might form. If dust settles well, it could gather into larger clumps, eventually forming planets. Understanding the balance between settling and turbulence is crucial for uncovering the conditions that lead to planet formation.

Observing IRAS 04302

To investigate the dust around IRAS 04302, researchers used the Atacama Large Millimeter/submillimeter Array (ALMA) to take detailed images. These images allow scientists to see the structure of the dust disk and assess how settled it is.

At a high resolution of about 8 astronomical units (au), the dust appears thick and uneven. This indicates that dust has not settled as much as it could. The images reveal a clear asymmetry in brightness along the minor axis of the disk, suggesting that one side may be more populated with dust than the other.

The Snow Surfaces

In addition to the dust, researchers explored what are known as snow surfaces. A snow surface is the boundary where certain Gases freeze into solid ice. For example, the cold Temperatures in certain regions can lead to carbon monoxide (CO) freezing out of the gas phase and forming ice on dust particles.

In the case of IRAS 04302, scientists managed to define the area where CO transitions from gas to solid. This area gives clues about the conditions present in the disk around the star. They estimated that the snow line for CO is located about 130 au from the star.

The Role of Temperature

Temperature plays a significant role in determining where dust and gas will settle. In general, the closer you are to the star, the warmer it is, causing gas to stay in a gaseous state. As you move away, temperatures drop and certain gases freeze, forming ice. Researchers found that the temperature needed to keep CO in gas form is around 20 K.

The shape of the observations reveals a V-structure formed by the frozen-out regions of CO and the gas, which is warmer and remains in gaseous form beyond the snow line. The complexity of this structure provides researchers with valuable information about the temperature and density in the disk.

What About the Gaps?

One of the common features in disks around other young stars is the presence of gaps and rings. These can indicate the presence of forming planets, which can clear paths through the dust. However, in the observations of IRAS 04302, no clear gaps or rings were found. This could be because the dust is still too mixed with the gas or because the thick layer of dust is obscuring any potential gaps.

The Characteristics of Dust

Researchers found that the dust in IRAS 04302 is qualitatively different from the gas. The dust has not settled significantly, with a scale height of around 6 au at a distance of 100 au from the star. This indicates that the dust remains in a relatively thick layer, which can affect the dynamics of potential planet formation.

The gas, on the other hand, has a different scale height. This disparity suggests that the dust particles have not yet fully separated from the gas, a critical phase for the growth of solid bodies in the disk.

The Connection to Planet Formation

Understanding the current state of dust and gas around a young star like IRAS 04302 can give us clues about how planets may eventually form. If dust can settle and gather into larger structures, it could lead to the formation of planetesimals, the building blocks of planets.

The observations show that IRAS 04302 is still in a relatively early stage, with Turbulent mixing keeping the dust and gas intertwined. This finding emphasizes the need to continue studying the transitional phases between Class I and Class II protostars to grasp how planets are born.

Comparing Different Stages

This young star gives researchers an opportunity to compare different stages of star formation. Class 0 stars, for instance, are even younger and often show a more chaotic structure, while Class II stars tend to have settled dust and more defined structures. The transition from Class 0 to Class I to Class II can reveal how the conditions around stars change over time.

As the observations showed, it is likely that IRAS 04302 is still gathering materials, indicating that it is not yet ready to form planets. This is in contrast to other Class II stars that have already formed planets and show clear signs of disk structure.

The Importance of Monitoring

Studying IRAS 04302 is important for building a broader understanding of star and planet formation. Continuous monitoring and analysis of such early stages help piece together the overall picture of how systems like our Solar System came to be.

Future observations using advanced techniques may provide further insights. By capturing images at different wavelengths and analyses, researchers can construct detailed models of how dust and gas behave in these environments, clarifying the transition from dust to planetesimal.

Conclusion

IRAS 04302+2247 serves as a captivating example of the processes at play in the early stages of star and planet formation. With its thick dust layer and distinct snow surfaces, it presents a wealth of information about how dust settles and the conditions around a young star.

Through exploring how dust interacts with gas and how temperatures affect the formation of snow surfaces, we gain valuable knowledge that informs our understanding of planetary systems. The ongoing work in this field continues to deepen our appreciation for the complex dynamics that shape the universe we see today.

By studying cases like IRAS 04302, we can continue to uncover the secrets of star formation and the processes that lead to the origin of planets, providing insights not only into our own Solar System but also into the myriad of systems scattered throughout the cosmos.

Original Source

Title: Early Planet Formation in Embedded Disks (eDisk). II. Limited Dust Settling and Prominent Snow Surfaces in the Edge-on Class I Disk IRAS 04302+2247

Abstract: While dust disks around optically visible, Class II protostars are found to be vertically thin, when and how dust settles to the midplane are unclear. As part of the Atacama Large Millimeter/submillimeter Array (ALMA) large program, Early Planet Formation in Embedded Disks, we analyze the edge-on, embedded, Class I protostar IRAS 04302+2247, also nicknamed the ``Butterfly Star." With a resolution of 0.05" (8~au), the 1.3 mm continuum shows an asymmetry along the minor axis which is evidence of an optically thick and geometrically thick disk viewed nearly edge-on. There is no evidence of rings and gaps, which could be due to the lack of radial substructure or the highly inclined and optically thick view. With 0.1" (16~au) resolution, we resolve the 2D snow surfaces, i.e., the boundary region between freeze-out and sublimation, for $^{12}$CO $J$=2--1, $^{13}$CO $J$=2--1, C$^{18}$O $J$=2--1, $H_{2}$CO $J$=$3_{0,3}$--$2_{0,2}$, and SO $J$=$6_{5}$--$5_{4}$, and constrain the CO midplane snow line to $\sim 130$ au. We find Keplerian rotation around a protostar of $1.6 \pm 0.4 M_{\odot}$ using C$^{18}$O. Through forward ray-tracing using RADMC-3D, we find that the dust scale height is $\sim 6$ au at a radius of 100~au from the central star and is comparable to the gas pressure scale height. The results suggest that the dust of this Class~I source has yet to vertically settle significantly.

Authors: Zhe-Yu Daniel Lin, Zhi-Yun Li, John J. Tobin, Nagayoshi Ohashi, Jes Kristian Jørgensen, Leslie W. Looney, Yusuke Aso, Shigehisa Takakuwa, Yuri Aikawa, Merel L. R. van 't Hoff, Itziar de Gregorio-Monsalvo, Frankie J. Encalada, Christian Flores, Sacha Gavino, Ilseung Han, Miyu Kido, Patrick M. Koch, Woojin Kwon, Shih-Ping Lai, Chang Won Lee, Jeong-Eun Lee, Nguyen Thi Phuong, Jinshi Sai, Rajeeb Sharma, Patrick Sheehan, Travis J. Thieme, Jonathan P. Williams, Yoshihide Yamato, Hsi-Wei Yen

Last Update: 2023-06-27 00:00:00

Language: English

Source URL: https://arxiv.org/abs/2306.15423

Source PDF: https://arxiv.org/pdf/2306.15423

Licence: https://creativecommons.org/licenses/by/4.0/

Changes: This summary was created with assistance from AI and may have inaccuracies. For accurate information, please refer to the original source documents linked here.

Thank you to arxiv for use of its open access interoperability.

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