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The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) 外柯伊伯带亚结构(ARKS)的ALMA调查
IF 6.5 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS Pub Date : 2026-01-20 DOI: 10.1051/0004-6361/202556568
J. B. Lovell, A. S. Hales, G. M. Kennedy, S. Marino, J. Olofsson, A. M. Hughes, E. Mansell, B. C. Matthews, T. D. Pearce, A. A. Sefilian, D. J. Wilner, B. Zawadzki, M. Booth, M. Bonduelle, A. Brennan, C. del Burgo, J. M. Carpenter, G. Cataldi, E. Chiang, A. Fehr, Y. Han, Th. Henning, A. V. Krivov, P. Luppe, J. P. Marshall, S. Mac Manamon, J. Milli, A. Moór, M. C. Wyatt, S. Ertel, M. R. Jankovic, Á. Kóspál, M. A. MacGregor, L. Matrà, S. Pérez, P. Weber
<i>Context<i/>. Asymmetries in debris discs provide unique clues to understand the evolution and architecture of planetary systems. Previous studies of debris discs at (sub)millimetre wavelengths have suggested the presence of asymmetries in a wide variety of systems, yet the lack of sufficiently sensitive high-resolution observations means that the typical properties of debris disc asymmetries have not been studied at the population level. The aim of the ALMA survey to Resolve exoKuiper belt Substructures (ARKS) is to expand our understanding of radial and vertical dust structures, as well as gas distributions and kinematics, in debris discs. The ARKS sample of 24 highly resolved targets in ALMA’s Bands 6 and 7 (1.1–1.4 mm and 0.8–1.1 mm, respectively) provided a unique opportunity to study their asymmetries.<i>Aims<i/>. Here, in ARKS VI, we present a systematic analysis of the asymmetries and stellocentric offsets present in the ALMA continuum data for the ARKS survey. Our aims are to (i) identify asymmetries in debris disc dust distributions, (ii) quantify debris disc asymmetry properties, and (iii) discuss the potential origins of debris disc asymmetries. This work is the first systematic analysis of asymmetries in a large sample of well-resolved discs at (sub)millimetre wavelengths.<i>Methods<i/>. We utilised empirical methods to identify emission asymmetries (relative to disc major and minor axes, and azimuthal disc locations) and the presence of offset emission between disc centres and the locations of the host stars, via an analysis of their calibration procedures and disc properties. We associated observational asymmetry types (offset, major and/or minor axis, azimuthal) and plausible physical classes (arcs, eccentricities, and possible clumps and warps) associated with each source.<i>Results<i/>. We show that there are ten systems, almost half of the ARKS sample, that host either a continuum emission asymmetry or offset emission. Three systems host offsets (HD 15115, HD 32297, and HD 109573 (HR 4796)), four host azimuthal asymmetries (HD 9672 (49 Ceti), HD 92945, HD 107146, and HD 121617), two host an asymmetry in their major axis (HD 10647 (q<sup>1<sup/> Eri), and HD 39060 (<i>β<i/> Pic)), and one hosts an asymmetry in their minor axis (HD 61005). We attribute the offset asymmetries to non-zero eccentricities, and three of the azimuthal asymmetries to arcs. The presence of an asymmetry or offset in the ARKS sample appears to be correlated with the fractional luminosity of cold dust. We tentatively suggest that continuum asymmetries are more prevalent in CO-rich debris discs, suggesting that gas interactions may drive debris dust asymmetries. We identify seven other tentative asymmetries, including four in distinct ARKS systems and three in systems with otherwise significant asymmetries.<i>Conclusions<i/>. This study demonstrates that debris disc asymmetries in the ARKS sample are common, and plausibly so in the wider population of debr
上下文。碎片盘的不对称性为理解行星系统的演化和结构提供了独特的线索。先前对(亚)毫米波长的碎片盘的研究表明,在各种各样的系统中都存在不对称,但缺乏足够敏感的高分辨率观测意味着碎片盘不对称的典型特性尚未在种群水平上进行研究。ALMA调查外柯伊伯带亚结构(ARKS)的目的是扩大我们对径向和垂直尘埃结构的理解,以及碎片盘中的气体分布和运动学。ARKS采样了ALMA波段6和7(分别为1.1-1.4 mm和0.8-1.1 mm)的24个高分辨率目标,为研究它们的不对称性提供了独特的机会。这里,在ARKS VI中,我们对ARKS调查中ALMA连续体数据中的不对称性和星心偏移进行了系统分析。我们的目标是(i)确定碎片盘尘埃分布中的不对称性,(ii)量化碎片盘的不对称性特性,以及(iii)讨论碎片盘不对称性的潜在起源。这项工作是第一次系统地分析(亚)毫米波长下高分辨率圆盘的不对称性。我们利用经验方法来识别发射不对称性(相对于盘主轴和小轴,以及盘的方位角位置),以及盘中心和主星位置之间存在的偏移发射,通过分析它们的校准程序和盘的特性。我们将观测到的不对称类型(偏移、主轴和/或小轴、方位角)和与每个源相关的合理物理类别(弧线、偏心、可能的团块和翘曲)联系起来。我们表明,有10个系统,几乎一半的ARKS样本,宿主连续发射不对称或抵消发射。三个系统主机偏移(HD 15115, HD 32297和HD 109573 (HR 4796)),四个主机方位角不对称(HD 9672 (49 Ceti), HD 92945, HD 107146和HD 121617),两个主机在其长轴上具有不对称(HD 10647 (q1 Eri)和HD 39060 (β Pic)),一个主机在其小轴上具有不对称(HD 61005)。我们将偏移不对称归因于非零偏心,并将三个方位角不对称归因于弧。ARKS样品中不对称或偏移的存在似乎与冷尘埃的分数光度有关。我们初步认为,连续体不对称在富含co的碎片盘中更为普遍,这表明气体相互作用可能导致碎片尘埃不对称。我们确定了其他7个暂定不对称,包括4个不同的ARKS系统和3个具有其他显著不对称的系统。这项研究表明,ARKS样本中的碎片盘不对称是常见的,而且在(亚)毫米波长的更广泛的碎片盘中似乎也是如此。这意味着,当我们以更高的灵敏度和分辨率探测这些碎片盘时,(亚)毫米的不对称可能会等待发现。在整个过程中,我们强调了未来的研究,以进一步调查碎片盘不对称的起源,并建立在这里提出的工作。
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引用次数: 0
The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) 外柯伊伯带亚结构(ARKS)的ALMA调查
IF 6.5 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS Pub Date : 2026-01-20 DOI: 10.1051/0004-6361/202556523
J. Milli, J. Olofsson, M. Bonduelle, R. Bendahan-West, J. P. Marshall, E. Choquet, A. A. Sefilian, Y. Han, B. Zawadzki, S. Mac Manamon, E. Mansell, C. del Burgo, J. M. Carpenter, A. M. Hughes, M. Booth, E. Chiang, S. Ertel, Th. M. Esposito, Th. Henning, J. Hom, M. R. Jankovic, A. V. Krivov, J. B. Lovell, P. Luppe, M. A. MacGregor, S. Marino, B. C. Matthews, L. Matrà, A. Moór, N. Pawellek, T. D. Pearce, S. Pérez, V. Squicciarini, P. Weber, D. J. Wilner, M. C. Wyatt
Context. Debris discs are analogues to our own Kuiper belt around main-sequence stars and are therefore referred to as exoKuiper belts. They have been resolved at high angular resolution at wavelengths spanning the optical/near-infrared to the submillimetre-millimetre regime. Short wavelengths can probe the light scattered by such discs, which is dominated by micron-sized dust particles, while millimetre wavelengths can probe the thermal emission of millimetre-sized particles. Determining differences in the dust distribution between millimetre- and micron-sized dust is fundamental to revealing the dynamical processes affecting the dust in debris discs.Aims. We aim to compare the scattered light from the discs of the ‘ALMA survey to Resolve exoKuiper belt Substructures’ (ARKS) with the thermal emission probed by ALMA. We focus on the radial distribution of the dust, and we also put constraints on the presence of giant planets in those systems.Methods. We used high-contrast scattered light observations obtained with VLT/SPHERE, GPI, and the HST to uniformly study the dust distribution in those systems and compare it to the dust distribution extracted from the ALMA observations carried out in the course of the ARKS project. We also set constraints on the presence of planets by using these high-contrast images combined with exoplanet evolutionary models.Results. Fifteen of the 24 discs comprising the ARKS sample are detected in scattered light, with TYC 9340-437-1 being imaged for the first time at near-infrared wavelengths. For six of those 15 discs, the dust surface density seen in scattered light peaks farther out compared to that observed with ALMA. These six discs except one are known to also host cold CO gas. Conversely, the systems without significant offsets are not known to host gas, except one. Moreover, with our scattered light near-infrared images, we achieve typical sensitivities to planets from 1 to 10 MJup beyond 10 to 20 au, depending on the system age and distance.Conclusions. This observational study suggests that the presence of gas in debris discs may affect the small and large grains differently, pushing the small dust to greater distances where the gas is less abundant.
上下文。碎片盘类似于我们在主序星周围的柯伊伯带,因此被称为外柯伊伯带。它们已经在光学/近红外到亚毫米-毫米波段的波长上以高角分辨率进行了分辨。短波可以探测由微米大小的尘埃颗粒散射的光,而毫米波长可以探测毫米大小颗粒的热辐射。确定毫米级和微米级尘埃分布的差异,对于揭示影响碎片盘中尘埃的动力学过程至关重要。我们的目的是比较“ALMA外柯伊伯带亚结构调查”(ARKS)中来自圆盘的散射光与ALMA探测的热发射。我们关注的是尘埃的径向分布,我们也对这些系统中巨行星的存在进行了限制。我们利用VLT/SPHERE、GPI和HST获得的高对比度散射光观测数据对这些系统中的尘埃分布进行了均匀研究,并将其与ARKS项目中ALMA观测数据提取的尘埃分布进行了比较。我们还通过将这些高对比度图像与系外行星演化模型相结合,对行星的存在设定了限制。在包含ARKS样本的24个圆盘中,有15个是在散射光下检测到的,TYC 9340-437-1是首次在近红外波长下成像。在这15个圆盘中,有6个圆盘的尘埃表面密度在散射光中达到峰值,比ALMA观测到的更远。除了一个盘外,这六个盘已知也含有冷CO气体。相反,没有显著偏移的系统不知道有气体,除了一个。此外,根据我们的散射光近红外图像,我们获得了对行星的典型灵敏度,从1到10 MJup到10到20 au,这取决于系统的年龄和距离。这项观测研究表明,碎片盘中气体的存在可能会对大小颗粒产生不同的影响,将小尘埃推到气体较少的更远的地方。
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引用次数: 0
The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) 外柯伊伯带亚结构(ARKS)的ALMA调查
IF 6.5 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS Pub Date : 2026-01-20 DOI: 10.1051/0004-6361/202556493
S. Marino, V. Gupta, P. Weber, T. D. Pearce, A. Brennan, S. Pérez, S. Mac Manamon, L. Matrà, J. Milli, M. Booth, C. del Burgo, G. Cataldi, E. Chiang, Y. Han, Th. Henning, A. M. Hughes, M. R. Jankovic, Á. Kóspál, J. B. Lovell, P. Luppe, E. Mansell, M. A. MacGregor, A. Moór, J. Olofsson, A. A. Sefilian, D. J. Wilner, M. C. Wyatt, B. Zawadzki
Context. ExoKuiper belts around young A-type stars often host CO gas, whose origin is still unclear. The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) includes six of these gas-bearing belts, to characterise their dust and gas distributions and investigate the gas origin.Aims. As part of ARKS, we observed the gas-rich system HD 121617 with a 0′′ 12 (14 au) resolution and discovered an arc of enhanced dust density. In this paper, we analyse in detail the dust and gas distributions and the gas kinematics of this system.Methods. We extracted radial and azimuthal profiles of the dust (in the millimetre and near-infrared) and gas emission (12CO and 13CO) from reconstructed images. To constrain the morphology of the arc, we fitted an asymmetric model to the dust emission. To characterise the gas kinematics, we fitted a Keplerian model to the velocity map and extracted the gas azimuthal velocity profile by deprojecting the data.Results. We find that the dust arc is narrow (1–5 au wide at a radius of 75 au), azimuthally extended with a full width at half maximum of ~90°, and asymmetric; the emission is more azimuthally compact in the direction of the system’s rotation, and represents 13% of the total dust mass (0.2 M). From analysis of the scattered light and CO images, we conclude that the arc is much less pronounced or absent for small grains and gas. Finally, we find strong non-Keplerian azimuthal velocities at the inner and outer wings of the ring, as was expected due to strong pressure gradients.Conclusions. The dust arc resembles the asymmetries found in protoplanetary discs, often interpreted as the result of dust trapping in vortices. If the gas disc mass is high enough (≳20 M, requiring a primordial gas origin), both the radial confinement of the ring and the azimuthal arc may result from dust grains responding to gas drag. Alternatively, it could result from planet-disc interactions via mean motion resonances. Further studies should test these hypotheses and may provide a dynamical gas mass estimate in this CO-rich exoKuiper belt.
上下文。年轻的a型恒星周围的柯伊伯带通常含有CO气体,其来源尚不清楚。ALMA对太阳系外柯伊伯带亚结构(ARKS)的调查包括6个这样的含气带,以表征它们的尘埃和气体分布,并研究气体的来源。作为ARKS的一部分,我们用0⋅”12 (14 au)分辨率观测了富含气体的HD 121617系统,并发现了尘埃密度增强的弧线。本文详细分析了该系统的粉尘和气体分布及气体运动学。我们从重建图像中提取了尘埃(毫米和近红外)和气体排放(12CO和13CO)的径向和方位角剖面。为了约束弧的形态,我们拟合了一个不对称的尘埃发射模型。为了描述气体的运动学特征,我们将开普勒模型拟合到速度图上,并通过对数据的解投影提取出气体的方位速度剖面。我们发现尘埃弧很窄(半径为75 au,宽1-5 au),沿方位延伸,最大半宽约为90°,且不对称;在系统旋转的方向上,发射物在方位角上更加致密,占总尘埃质量的13% (0.2 M⊕)。通过对散射光和CO图像的分析,我们得出结论,对于小颗粒和气体来说,弧不那么明显或不存在。最后,我们在环的内外翼发现了强大的非开普勒方位角速度,正如预期的那样,由于强大的压力梯度。尘埃弧类似于原行星盘中发现的不对称,通常被解释为尘埃困在漩涡中的结果。如果气体盘质量足够高(≥20 M⊕,需要原始气体的起源),环的径向限制和方位弧都可能是由尘埃颗粒对气体阻力的响应造成的。或者,它可能是行星与圆盘通过平均运动共振相互作用产生的。进一步的研究应该验证这些假设,并可能提供这个富含co的外柯伊伯带的动态气体质量估计。
{"title":"The ALMA survey to Resolve exoKuiper belt Substructures (ARKS)","authors":"S. Marino, V. Gupta, P. Weber, T. D. Pearce, A. Brennan, S. Pérez, S. Mac Manamon, L. Matrà, J. Milli, M. Booth, C. del Burgo, G. Cataldi, E. Chiang, Y. Han, Th. Henning, A. M. Hughes, M. R. Jankovic, Á. Kóspál, J. B. Lovell, P. Luppe, E. Mansell, M. A. MacGregor, A. Moór, J. Olofsson, A. A. Sefilian, D. J. Wilner, M. C. Wyatt, B. Zawadzki","doi":"10.1051/0004-6361/202556493","DOIUrl":"https://doi.org/10.1051/0004-6361/202556493","url":null,"abstract":"<i>Context<i/>. ExoKuiper belts around young A-type stars often host CO gas, whose origin is still unclear. The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) includes six of these gas-bearing belts, to characterise their dust and gas distributions and investigate the gas origin.<i>Aims<i/>. As part of ARKS, we observed the gas-rich system HD 121617 with a 0<sub>⋅<sub/><sup>′′<sup/> 12 (14 au) resolution and discovered an arc of enhanced dust density. In this paper, we analyse in detail the dust and gas distributions and the gas kinematics of this system.<i>Methods<i/>. We extracted radial and azimuthal profiles of the dust (in the millimetre and near-infrared) and gas emission (<sup>12<sup/>CO and <sup>13<sup/>CO) from reconstructed images. To constrain the morphology of the arc, we fitted an asymmetric model to the dust emission. To characterise the gas kinematics, we fitted a Keplerian model to the velocity map and extracted the gas azimuthal velocity profile by deprojecting the data.<i>Results<i/>. We find that the dust arc is narrow (1–5 au wide at a radius of 75 au), azimuthally extended with a full width at half maximum of ~90°, and asymmetric; the emission is more azimuthally compact in the direction of the system’s rotation, and represents 13% of the total dust mass (0.2 <i>M<i/><sub>⊕<sub/>). From analysis of the scattered light and CO images, we conclude that the arc is much less pronounced or absent for small grains and gas. Finally, we find strong non-Keplerian azimuthal velocities at the inner and outer wings of the ring, as was expected due to strong pressure gradients.<i>Conclusions<i/>. The dust arc resembles the asymmetries found in protoplanetary discs, often interpreted as the result of dust trapping in vortices. If the gas disc mass is high enough (≳20 <i>M<i/><sub>⊕<sub/>, requiring a primordial gas origin), both the radial confinement of the ring and the azimuthal arc may result from dust grains responding to gas drag. Alternatively, it could result from planet-disc interactions via mean motion resonances. Further studies should test these hypotheses and may provide a dynamical gas mass estimate in this CO-rich exoKuiper belt.","PeriodicalId":8571,"journal":{"name":"Astronomy & Astrophysics","volume":"276 1","pages":""},"PeriodicalIF":6.5,"publicationDate":"2026-01-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146006201","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"物理与天体物理","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Validating a non-local stellar convection model with 3D hydrodynamics simulations 用三维流体力学模拟验证非局部恒星对流模型
IF 6.5 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS Pub Date : 2026-01-20 DOI: 10.1051/0004-6361/202554956
F. Ahlborn, J. Higl, R. Andrassy, G. Leidi, A. Weiss, F. Röpke
Context. The efficient transport of energy and chemical elements by convective motions has a profound effect on the structure and evolution of stars. These motions occur on the relatively short dynamical timescale of convection and are intrinsically multi-dimensional. Stellar models usually rely on the one-dimensional mixing-length approximation of these processes, which is known to break down at convective boundaries. The Kuhfuß, R. (1987, Dissertation, Technische Universität München, München) convection model has been shown to handle convective boundaries in a more consistent way.Aims. We test the assumptions that enter the Kuhfuß model using multi-dimensional hydrodynamics simulations, and we compare the results with existing one-dimensional models. Where possible, we also aim to calibrate the parameters of the Kuhfuß model using the simulations.Methods. We computed one-dimensional stellar models employing the Kuhfuß model of a 3 M main-sequence star. These models were compared to three-dimensional hydrodynamic simulations obtained with the code called SEVEN-LEAGUE HYDRO and using the Reynolds-averaged Navier Stokes analysis. We analysed the global convective variables and individual contributions to the equations of the convection model.Results. The turbulent kinetic energy as predicted by the Kuhfuß model agrees well with the simulation results. Towards the boundary of the convective core, the simulations show a layer of a positive entropy gradient that coincides with a positive convective flux, as predicted by the convection model. The terms involving pressure fluctuations are found to have a non-negligible magnitude.Conclusions. The agreement of the turbulent kinetic energy equation for the convection model and the simulation is an important sign that the convection model is physically accurate. The gradient of the mean entropy that we found in the multi-dimensional simulations and in the Kuhfuß model confirms the existence of a Deardorff layer, that is, of a layer with a subadiabtic temperature stratification and positive convective flux. This is not predicted by the mixing-length theory. The assumption that turbulence is isotropic and that pressure fluctuations are negligible needs to be revisited in the convection model.
上下文。能量和化学元素通过对流运动的有效传输对恒星的结构和演化有着深远的影响。这些运动发生在相对较短的对流动力学时间尺度上,本质上是多维的。恒星模型通常依赖于这些过程的一维混合长度近似值,众所周知,这种近似值在对流边界处会崩溃。Kuhfuß, R. (1987, Dissertation, Technische Universität m nchen, m nchen)对流模型已被证明以更一致的方式处理对流边界。我们使用多维流体力学模拟来检验进入Kuhfuß模型的假设,并将结果与现有的一维模型进行比较。在可能的情况下,我们还打算使用模拟方法校准Kuhfuß模型的参数。我们用Kuhfuß模型计算了一个3 M⊙主序星的一维恒星模型。这些模型与三维流体动力学模拟进行了比较,这些模拟是用名为SEVEN-LEAGUE HYDRO的代码获得的,并使用了reynolds -average Navier Stokes分析。我们分析了整体对流变量和个体对对流模式方程的贡献。Kuhfuß模型预测的湍流动能与模拟结果吻合较好。在对流核边界处,模拟结果显示出一层正熵梯度,与对流模型预测的正对流通量相吻合。发现涉及压力波动的项具有不可忽略的量级。对流模型湍流动能方程与模拟结果的一致性是对流模型物理精度的重要标志。我们在多维模拟和Kuhfuß模型中发现的平均熵梯度证实了Deardorff层的存在,即具有亚绝热温度分层和正对流通量的层。这是混合长度理论无法预测的。紊流是各向同性和压力波动可以忽略不计的假设需要在对流模型中重新考虑。
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引用次数: 0
The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) 外柯伊伯带亚结构(ARKS)的ALMA调查
IF 6.5 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS Pub Date : 2026-01-20 DOI: 10.1051/0004-6361/202556505
B. Zawadzki, A. Fehr, A. M. Hughes, E. Mansell, J. Kittling, Y. Han, C. Hou, M. Pan, J. Milli, J. Olofsson, T. Pearce, A. A. Sefilian, A. Nurmohamed, J. Lee, Y. Mpofu, M. Bonduelle, M. Booth, A. Brennan, C. del Burgo, J. M. Carpenter, G. Cataldi, E. Chiang, S. Ertel, Th. Henning, M. R. Jankovic, G. M. Kennedy, Á. Kóspál, A. V. Krivov, J. B. Lovell, P. Luppe, M. A. MacGregor, S. Mac Manamon, S. Marino, J. P. Marshall, L. Matrà, A. Moór, S. Pérez, P. Weber, D. J. Wilner, M. C. Wyatt
Context. Debris disks – collisionally sustained belts of dust and sometimes gas around main sequence stars – are remnants of planet formation processes and are found in systems ≳10 Myr old. Millimeter-wavelength observations are particularly important, as the grains probed by these observations are not strongly affected by radiation pressure and stellar winds, allowing them to probe the dynamics of large bodies producing dust. The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) is analyzing high-resolution observations of 24 debris disks to enable the characterization of debris disk substructures across a large sample for the first time.Aims. For the most highly inclined disks, it is possible to recover the vertical structure of the disk. We aim to model and analyze the most highly inclined systems in the ARKS sample in order to uniformly extract the vertical dust distributions for a sample of well-resolved debris disks.Methods. We employed both parametric and nonparametric methods to constrain the vertical dust distributions for the most highly inclined ARKS targets.Results. We find a broad range of aspect ratios, revealing a wide diversity in vertical structure, with a range of best-fit parametric values of 0.0026 ≤ hHWHM ≤ 0.193 and a median best-fit value of hHWHM = 0.021. The results obtained by nonparametric modeling are generally consistent with the parametric modeling results. We find that five of the 13 disks are consistent with having total disk masses less than that of Neptune (17 M), assuming stirring by internal processes (self-stirring and collisional and frictional damping). Furthermore, most systems show a significant preference for a Lorentzian vertical profile rather than a Gaussian.
上下文。碎片盘——围绕在主序星周围的持续碰撞的尘埃带,有时是气体带——是行星形成过程的残余物,发现于年龄在10myr以上的星系中。毫米波长的观测特别重要,因为这些观测探测到的颗粒不受辐射压力和恒星风的强烈影响,这使他们能够探测产生尘埃的大型天体的动力学。ALMA调查解决外柯伊伯带子结构(ARKS)正在分析24个碎片盘的高分辨率观测结果,以便首次在大样本中对碎片盘子结构进行表征。对于最高度倾斜的磁盘,可以恢复磁盘的垂直结构。我们的目标是模拟和分析ARKS样本中最高度倾斜的系统,以便均匀地提取一个分辨率很高的碎片盘样本的垂直尘埃分布。我们采用参数和非参数两种方法来约束最高度倾斜的ARKS目标的垂直粉尘分布。研究发现,长宽比的范围很广,揭示了垂直结构的多样性,最佳拟合参数值的范围为0.0026≤hHWHM≤0.193,中位数最佳拟合值为hHWHM = 0.021。非参数化建模得到的结果与参数化建模得到的结果基本一致。我们发现13个圆盘中有5个圆盘的总质量小于海王星(17 M⊕),假设有内部过程的搅拌(自搅拌、碰撞和摩擦阻尼)。此外,大多数系统表现出对洛伦兹垂直剖面的显著偏好,而不是高斯剖面。
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引用次数: 0
The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) 外柯伊伯带亚结构(ARKS)的ALMA调查
IF 6.5 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS Pub Date : 2026-01-20 DOI: 10.1051/0004-6361/202556566
A. Brennan, L. Matrà, S. Mac Manamon, S. Marino, G. Cataldi, A. M. Hughes, P. Weber, Y. Han, J. P. Marshall, B. Zawadzki, P. Luppe, A. A. Sefilian, A. Moór, M. A. MacGregor, J. B. Lovell, A. Kóspál, M. Bonduelle, E. Mansell, M. C. Wyatt, T. D. Pearce, J. M. Carpenter, D. J. Wilner, C. del Burgo, S. Pérez, T. Henning, J. Milli, E. Chiang
Context. CO gas has been detected in ~20 debris discs, typically classified as CO-poor or CO-rich. We present observations of the CO-rich HD 121617 debris disc as part of the ALMA survey to Resolve exoKuiper belt Substructures (ARKS).Aims. We model local CO line profiles in the HD 121617 debris disc to investigate optical depth, CO mass, and temperature. HD 121617 is a well-suited ARKS target due to its previously detected CO emission and moderate inclination, reducing the effect of Keplerian shear.Methods. Using high-resolution ALMA Band 7 observations of 12CO J=3–2 (26 m s−1, 0′′ 1), we create local line profiles by aligning and stacking spectra in concentric annuli of 0′′ 02 width. These profiles are modelled with both a toy model and a RADMC-3D model that includes projection effects and Keplerian shear.Results. The resulting local profiles are Gaussian-shaped and broad due to the effect of Keplerian shear. Fitting a RADMC-3D model to the 13CO data, we find that an optically thick model (temperature of 38 K and mass of 2 × 10−3 M) reproduces the data, particularly the enhanced intensity at orbital azimuths of ~±45° and ±135°, which forms an X-shape in the velocity integrated intensity map, as well as the broader 12CO linewidth compared to 13CO. Scaling this model by the ISM abundance ratio (~77) also reproduces the 12CO data, but high optical depths and model assumptions limit mass constraints.Conclusions. Keplerian shear causes azimuthally averaged line profiles to appear Gaussian regardless of optical depth; therefore, we caution against using the local line profiles to distinguish between optically thin and thick emission. We constrain the mean molecular weight to 12.6−1.1+1.3, dependent on model assumptions. Although model dependent, our 13CO results indicate that C18O might also be optically thick in CO-rich debris discs, contrary to previous assumptions, and that the mean molecular weight is significantly higher than if H2 were the dominant gas species, suggesting a non-primordial composition.
上下文。在约20个碎片盘中检测到CO气体,通常分为贫CO和富CO两类。我们提出了对富含co的HD 121617碎片盘的观测,作为ALMA调查的一部分,以解决外柯伊伯带亚结构(ARKS)。我们模拟了HD 121617碎片盘中的局部CO线剖面,以研究光学深度、CO质量和温度。HD 121617是一个非常适合的ARKS目标,因为它以前检测到CO发射和适度的倾角,减少了开普勒剪切的影响。利用高分辨率ALMA Band 7观测12CO J= 3-2 (26 m s−1,0⋅”1),我们通过对齐和叠加光谱在0⋅”02宽度的同心环空中创建局部线剖面。这些剖面用玩具模型和RADMC-3D模型建模,其中包括投影效果和开普勒剪切。由于开普勒剪切的影响,得到的局部剖面是高斯形的,而且很宽。将RADMC-3D模型拟合13CO数据,我们发现一个光学厚模型(温度为38 K,质量为2 × 10−3 M⊕)再现了数据,特别是在轨道方位角为~±45°和±135°处的强度增强,在速度综合强度图中形成x形,并且与13CO相比,12CO线宽更宽。用ISM丰度比(~77)对该模型进行缩放也能再现12CO的数据,但较高的光学深度和模型假设限制了质量约束。无论光学深度如何,开普勒剪切都会导致方位平均线轮廓呈现高斯分布;因此,我们警告不要使用局部线轮廓来区分光学薄和厚发射。根据模型假设,我们将平均分子量限制为12.6−1.1+1.3。虽然依赖于模型,但我们的13CO结果表明,在富含co的碎片盘中,C18O也可能具有光学厚度,这与之前的假设相反,并且平均分子量明显高于H2为主要气体的情况,表明其非原始成分。
{"title":"The ALMA survey to Resolve exoKuiper belt Substructures (ARKS)","authors":"A. Brennan, L. Matrà, S. Mac Manamon, S. Marino, G. Cataldi, A. M. Hughes, P. Weber, Y. Han, J. P. Marshall, B. Zawadzki, P. Luppe, A. A. Sefilian, A. Moór, M. A. MacGregor, J. B. Lovell, A. Kóspál, M. Bonduelle, E. Mansell, M. C. Wyatt, T. D. Pearce, J. M. Carpenter, D. J. Wilner, C. del Burgo, S. Pérez, T. Henning, J. Milli, E. Chiang","doi":"10.1051/0004-6361/202556566","DOIUrl":"https://doi.org/10.1051/0004-6361/202556566","url":null,"abstract":"<i>Context<i/>. CO gas has been detected in ~20 debris discs, typically classified as CO-poor or CO-rich. We present observations of the CO-rich HD 121617 debris disc as part of the ALMA survey to Resolve exoKuiper belt Substructures (ARKS).<i>Aims<i/>. We model local CO line profiles in the HD 121617 debris disc to investigate optical depth, CO mass, and temperature. HD 121617 is a well-suited ARKS target due to its previously detected CO emission and moderate inclination, reducing the effect of Keplerian shear.<i>Methods<i/>. Using high-resolution ALMA Band 7 observations of <sup>12<sup/>CO J=3–2 (26 m s<sup>−1<sup/>, 0<sub>⋅<sub/>′′ 1), we create local line profiles by aligning and stacking spectra in concentric annuli of 0<sub>⋅<sub/>′′ 02 width. These profiles are modelled with both a toy model and a RADMC-3D model that includes projection effects and Keplerian shear.<i>Results<i/>. The resulting local profiles are Gaussian-shaped and broad due to the effect of Keplerian shear. Fitting a RADMC-3D model to the <sup>13<sup/>CO data, we find that an optically thick model (temperature of 38 K and mass of 2 × 10<sup>−3<sup/> M<sub>⊕<sub/>) reproduces the data, particularly the enhanced intensity at orbital azimuths of ~±45° and ±135°, which forms an X-shape in the velocity integrated intensity map, as well as the broader <sup>12<sup/>CO linewidth compared to <sup>13<sup/>CO. Scaling this model by the ISM abundance ratio (~77) also reproduces the <sup>12<sup/>CO data, but high optical depths and model assumptions limit mass constraints.<i>Conclusions<i/>. Keplerian shear causes azimuthally averaged line profiles to appear Gaussian regardless of optical depth; therefore, we caution against using the local line profiles to distinguish between optically thin and thick emission. We constrain the mean molecular weight to 12.6<sub>−1.1<sub/><sup>+1.3<sup/>, dependent on model assumptions. Although model dependent, our <sup>13<sup/>CO results indicate that C<sup>18<sup/>O might also be optically thick in CO-rich debris discs, contrary to previous assumptions, and that the mean molecular weight is significantly higher than if H<sub>2<sub/> were the dominant gas species, suggesting a non-primordial composition.","PeriodicalId":8571,"journal":{"name":"Astronomy & Astrophysics","volume":"31 1","pages":""},"PeriodicalIF":6.5,"publicationDate":"2026-01-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146006176","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"物理与天体物理","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) 外柯伊伯带亚结构(ARKS)的ALMA调查
IF 6.5 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS Pub Date : 2026-01-20 DOI: 10.1051/0004-6361/202556605
S. Mac Manamon, L. Matrà, S. Marino, A. Brennan, Y. Han, M. R. Jankovic, P. Weber, M. Bonduelle, J. M. Carpenter, G. Cataldi, A. M. Hughes, A. Kóspál, J. P. Marshall, B. C. Matthews, J. Milli, A. Moór, K. Öberg, S. Pérez, A. A. Sefilian, D. J. Wilner, M. C. Wyatt, E. Chiang, A. S. Hales, J. B. Lovell, P. Luppe, M. A. MacGregor, T. Pearce, M. Booth, C. del Burgo, A. Fehr, E. Mansell, B. Zawadzki
Context. CO gas is detected in a significant number (~20) of debris discs (exoKuiper belts), but understanding its origin and evolution remains elusive. Crucial pieces of evidence are its mass and spectro-spatial distribution, which are coupled through optical depth and have only been analysed at low to moderate resolution so far. The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) is the first ALMA large program to target debris discs at high spectro-spatial resolution.Aims. We used 12CO and 13CO J=3-2 line data of 18 debris belts observed by ARKS, 5 of which were already known to be gas-bearing, in order to analyse the spectro-spatial distribution of CO and constrain the gas mass in discs that were known to host gas previously, and to search for gas in the remaining 13 discs without previous CO detections.Methods. We developed a line-imaging pipeline for ARKS CO data with a high spectro-spatial resolution. Using this tool, we produced line cubes for each of the ARKS targets, with a spatial resolution down to about 70 mas and a spectral resolution of 26 m s−1. We used spectro-spatial shifting and stacking techniques to produce a gallery of maps with the highest possible signal-to-noise ratio (S/N) and with radial and spectral profiles that reveal the distribution and kinematics of gas in five gas-bearing discs at unprecedented detail.Results. For each of the five gas-bearing discs (HD 9672/49 Ceti, HD 32297, HD 121617, HD 131488, and HD 131835), we constrained the inner radius of the 12CO (rmin ~ 3-68 au), and we found that the radial brightness profile of CO peaked interior to the dust ring, but that CO was also more radially extended than the dust. In a second-generation scenario, this would require significant shielding of CO that would allow it to viscously spread to the observed widths. We present the first radially resolved 12CO/13CO isotopologue flux ratios in five gas-bearing debris discs and found them to be constant with radius for the majority (four out of five) of systems. This indicates that 12CO and 13CO are both optically thick or optically thin throughout the discs. We report CO line fluxes or upper limits for all systems and optical depth dependant masses for the five systems with detected CO. Finally, we analysed the 12CO J=3-2 line luminosities for a range of ARKS debris discs and for debris discs from the literature. We confirm that gas is mostly detected in young systems. However, the high scatter seen in young/high fractional luminosity systems indicates no trend within the systems with detected gas. This could be caused by different system properties and/or evolution pathways.
上下文。CO气体在相当数量(~20)的碎片盘(外柯伊伯带)中被检测到,但对其起源和演化的理解仍然难以捉摸。关键的证据是它的质量和光谱空间分布,它们是通过光学深度耦合的,到目前为止只在低到中等分辨率下进行了分析。ALMA调查外柯伊伯带子结构(ARKS)是ALMA第一个以高光谱空间分辨率瞄准碎片盘的大型项目。我们利用ARKS观测到的18个碎片带的12CO和13CO J=3-2线数据,其中5个已经已知含气,以分析CO的光谱空间分布,并限制先前已知含有气体的圆盘中的气体质量,并在其余13个先前未检测到CO的圆盘中寻找气体。我们开发了一种具有高光谱空间分辨率的ARKS CO数据线成像管道。使用该工具,我们为每个ARKS目标生成了线立方,空间分辨率低至约70 mas,光谱分辨率为26 m s - 1。我们使用光谱空间移位和叠加技术,以最高可能的信噪比(S/N)和径向和光谱剖面制作了一个图库,以前所未有的细节揭示了五个含气圆盘中的气体分布和运动学。对于5个含气盘(HD 9672/49 Ceti、HD 32297、HD 121617、HD 131488和HD 131835),我们限制了12CO的内部半径(rmin ~ 3-68 au),我们发现CO的径向亮度剖面在尘埃环内部达到峰值,但CO也比尘埃更径向延伸。在第二代方案中,这将需要CO的大量屏蔽,使其能够粘性地扩散到观察到的宽度。我们首次在5个含气岩屑盘中径向解析了12CO/13CO同位素通量比,并发现它们在大多数(5个中的4个)系统中随半径不变。这表明12CO和13CO在整个光盘上都是光学厚或光学薄。我们报告了所有系统的CO线通量或上限以及检测到CO的五个系统的光学深度依赖质量。最后,我们分析了一系列ARKS碎片盘和文献中碎片盘的12CO J=3-2线光度。我们确认气体主要在年轻的系统中被探测到。然而,在年轻/高分数光度系统中看到的高散射表明,在检测到气体的系统中没有趋势。这可能是由不同的系统特性和/或进化途径引起的。
{"title":"The ALMA survey to Resolve exoKuiper belt Substructures (ARKS)","authors":"S. Mac Manamon, L. Matrà, S. Marino, A. Brennan, Y. Han, M. R. Jankovic, P. Weber, M. Bonduelle, J. M. Carpenter, G. Cataldi, A. M. Hughes, A. Kóspál, J. P. Marshall, B. C. Matthews, J. Milli, A. Moór, K. Öberg, S. Pérez, A. A. Sefilian, D. J. Wilner, M. C. Wyatt, E. Chiang, A. S. Hales, J. B. Lovell, P. Luppe, M. A. MacGregor, T. Pearce, M. Booth, C. del Burgo, A. Fehr, E. Mansell, B. Zawadzki","doi":"10.1051/0004-6361/202556605","DOIUrl":"https://doi.org/10.1051/0004-6361/202556605","url":null,"abstract":"<i>Context<i/>. CO gas is detected in a significant number (~20) of debris discs (exoKuiper belts), but understanding its origin and evolution remains elusive. Crucial pieces of evidence are its mass and spectro-spatial distribution, which are coupled through optical depth and have only been analysed at low to moderate resolution so far. The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) is the first ALMA large program to target debris discs at high spectro-spatial resolution.<i>Aims<i/>. We used <sup>12<sup/>CO and <sup>13<sup/>CO J=3-2 line data of 18 debris belts observed by ARKS, 5 of which were already known to be gas-bearing, in order to analyse the spectro-spatial distribution of CO and constrain the gas mass in discs that were known to host gas previously, and to search for gas in the remaining 13 discs without previous CO detections.<i>Methods<i/>. We developed a line-imaging pipeline for ARKS CO data with a high spectro-spatial resolution. Using this tool, we produced line cubes for each of the ARKS targets, with a spatial resolution down to about 70 mas and a spectral resolution of 26 m s<sup>−1<sup/>. We used spectro-spatial shifting and stacking techniques to produce a gallery of maps with the highest possible signal-to-noise ratio (S/N) and with radial and spectral profiles that reveal the distribution and kinematics of gas in five gas-bearing discs at unprecedented detail.<i>Results<i/>. For each of the five gas-bearing discs (HD 9672/49 Ceti, HD 32297, HD 121617, HD 131488, and HD 131835), we constrained the inner radius of the <sup>12<sup/>CO (<i>r<i/><sub>min<sub/> ~ 3-68 au), and we found that the radial brightness profile of CO peaked interior to the dust ring, but that CO was also more radially extended than the dust. In a second-generation scenario, this would require significant shielding of CO that would allow it to viscously spread to the observed widths. We present the first radially resolved <sup>12<sup/>CO/<sup>13<sup/>CO isotopologue flux ratios in five gas-bearing debris discs and found them to be constant with radius for the majority (four out of five) of systems. This indicates that <sup>12<sup/>CO and <sup>13<sup/>CO are both optically thick or optically thin throughout the discs. We report CO line fluxes or upper limits for all systems and optical depth dependant masses for the five systems with detected CO. Finally, we analysed the <sup>12<sup/>CO J=3-2 line luminosities for a range of ARKS debris discs and for debris discs from the literature. We confirm that gas is mostly detected in young systems. However, the high scatter seen in young/high fractional luminosity systems indicates no trend within the systems with detected gas. This could be caused by different system properties and/or evolution pathways.","PeriodicalId":8571,"journal":{"name":"Astronomy & Astrophysics","volume":"64 1","pages":""},"PeriodicalIF":6.5,"publicationDate":"2026-01-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146006173","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"物理与天体物理","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) 外柯伊伯带亚结构(ARKS)的ALMA调查
IF 6.5 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS Pub Date : 2026-01-20 DOI: 10.1051/0004-6361/202556489
S. Marino, L. Matrà, A. M. Hughes, J. Ehrhardt, G. M. Kennedy, C. del Burgo, A. Brennan, Y. Han, M. R. Jankovic, J. B. Lovell, S. Mac Manamon, J. Milli, P. Weber, B. Zawadzki, R. Bendahan-West, A. Fehr, E. Mansell, J. Olofsson, T. D. Pearce, A. Bayo, B. C. Matthews, T. Löhne, M. C. Wyatt, P. Ábrahám, M. Bonduelle, M. Booth, G. Cataldi, J. M. Carpenter, E. Chiang, S. Ertel, A. S. Hales, Th. Henning, Á. Kóspál, A. V. Krivov, P. Luppe, M. A. MacGregor, J. P. Marshall, A. Moór, S. Pérez, A. A. Sefilian, A. G. Sepulveda, D. J. Wilner
Context. The outer regions of planetary systems host dusty debris discs analogous to the Kuiper belt (exoKuiper belts), which provide crucial constraints on planet formation and evolution processes. ALMA dust observations have revealed a great diversity in terms of radii, widths, and scale heights. At the same time, ALMA has also shown that some belts contain CO gas, whose origin and implications are still highly uncertain. Most of this progress, however, has been limited by low angular resolution observations that hinder our ability to test existing models and theories.Aims. High-resolution observations of these belts are crucial for understanding the detailed distribution of solids and for constraining the gas distribution and kinematics.Methods. We conducted the first ALMA large programme dedicated to debris discs: the ALMA survey to Resolve exoKuiper belt Substructures (ARKS). We selected the 24 most promising belts to best address our main objectives: analysing the detailed radial and vertical structure, and characterising the gas content. The data were reduced and corrected to account for several systematic effects, and then imaged. Using parametric and non-parametric models, we constrained the radial and vertical distribution of dust, as well as the presence of asymmetries. For a subset of six belts with CO gas, we constrained the gas distribution and kinematics. To interpret these observations, we used a wide range of dynamical models.Results. The first results of ARKS are presented as a series of ten papers. We discovered that up to 33% of our sample exhibits substructures in the form of multiple dusty rings that may have been inherited from their protoplanetary discs. For highly inclined belts, we found that non-Gaussian vertical distributions are common and could be indicative of multiple dynamical populations. Half of the derived scale heights are small enough to be consistent with self-stirring in low-mass belts (MbeltMNeptune). We also found that 10 of the 24 belts present asymmetries in the form of density enhancements, eccentricities, or warps. We find that the CO gas is radially broader than the dust, but this could be an effect of optical depth. At least one system shows non-Keplerian kinematics due to strong pressure gradients, which may have triggered a vortex that trapped dust in an arc. Finally, we find evidence that the micron-sized grains may be affected by gas drag in gas-rich systems, pushing the small grains to wider orbits than the large grains.Conclusions. ARKS has revealed a great diversity of radial and vertical structures in exoKuiper belts that may arise when they are formed in protoplanetary discs or subsequently via interactions with planets and/or gas. We encourage the community to explore the reduced data and data products that we have made public through a dedicated website.
上下文。行星系统的外部区域拥有类似于柯伊伯带(外柯伊伯带)的尘埃碎片盘,这对行星的形成和演化过程提供了关键的限制。ALMA尘埃观测揭示了在半径、宽度和尺度高度方面的巨大差异。同时,ALMA也显示了一些带含有CO气体,其来源和含义仍然高度不确定。然而,这些进展大多受到低角度分辨率观测的限制,这阻碍了我们测试现有模型和理论的能力。这些带的高分辨率观测对于了解固体的详细分布以及约束气体分布和运动学方法至关重要。我们进行了第一个专门研究碎片盘的ALMA大型项目:ALMA调查以解决外柯伊伯带子结构(ARKS)。我们选择了24个最有希望的带,以最好地实现我们的主要目标:分析详细的径向和垂直结构,并表征气体含量。数据经过简化和校正,以解释几个系统效应,然后成像。使用参数和非参数模型,我们限制了尘埃的径向和垂直分布,以及不对称的存在。对于含有CO气体的六个带的子集,我们对气体分布和运动学进行了约束。为了解释这些观察结果,我们使用了广泛的动力学模型。ARKS的第一个结果以一系列10篇论文的形式呈现。我们发现,高达33%的样本显示出多个尘埃环形式的亚结构,这些亚结构可能是从它们的原行星盘继承下来的。对于高度倾斜的带,我们发现非高斯垂直分布是常见的,并且可以指示多个动态种群。在低质量带(Mbelt≤MNeptune)中,推导出的尺度高度有一半小到足以与自搅拌相一致。我们还发现,24个带中有10个以密度增强、偏心或翘曲的形式呈现不对称。我们发现CO气体在径向上比尘埃宽,但这可能是光学深度的影响。由于强大的压力梯度,至少有一个系统显示出非开普勒运动,这可能引发了一个漩涡,将尘埃困在一个弧形中。最后,我们发现证据表明,在富气系统中,微米级颗粒可能受到气体阻力的影响,使小颗粒比大颗粒更宽的轨道。ARKS揭示了外柯伊伯带的径向和垂直结构的多样性,这些结构可能是在它们形成于原行星盘或随后与行星和/或气体相互作用时产生的。我们鼓励社会各界探索我们在一个专门的网站上公布的精简数据和数据产品。
{"title":"The ALMA survey to Resolve exoKuiper belt Substructures (ARKS)","authors":"S. Marino, L. Matrà, A. M. Hughes, J. Ehrhardt, G. M. Kennedy, C. del Burgo, A. Brennan, Y. Han, M. R. Jankovic, J. B. Lovell, S. Mac Manamon, J. Milli, P. Weber, B. Zawadzki, R. Bendahan-West, A. Fehr, E. Mansell, J. Olofsson, T. D. Pearce, A. Bayo, B. C. Matthews, T. Löhne, M. C. Wyatt, P. Ábrahám, M. Bonduelle, M. Booth, G. Cataldi, J. M. Carpenter, E. Chiang, S. Ertel, A. S. Hales, Th. Henning, Á. Kóspál, A. V. Krivov, P. Luppe, M. A. MacGregor, J. P. Marshall, A. Moór, S. Pérez, A. A. Sefilian, A. G. Sepulveda, D. J. Wilner","doi":"10.1051/0004-6361/202556489","DOIUrl":"https://doi.org/10.1051/0004-6361/202556489","url":null,"abstract":"<i>Context<i/>. The outer regions of planetary systems host dusty debris discs analogous to the Kuiper belt (exoKuiper belts), which provide crucial constraints on planet formation and evolution processes. ALMA dust observations have revealed a great diversity in terms of radii, widths, and scale heights. At the same time, ALMA has also shown that some belts contain CO gas, whose origin and implications are still highly uncertain. Most of this progress, however, has been limited by low angular resolution observations that hinder our ability to test existing models and theories.<i>Aims<i/>. High-resolution observations of these belts are crucial for understanding the detailed distribution of solids and for constraining the gas distribution and kinematics.<i>Methods<i/>. We conducted the first ALMA large programme dedicated to debris discs: the ALMA survey to Resolve exoKuiper belt Substructures (ARKS). We selected the 24 most promising belts to best address our main objectives: analysing the detailed radial and vertical structure, and characterising the gas content. The data were reduced and corrected to account for several systematic effects, and then imaged. Using parametric and non-parametric models, we constrained the radial and vertical distribution of dust, as well as the presence of asymmetries. For a subset of six belts with CO gas, we constrained the gas distribution and kinematics. To interpret these observations, we used a wide range of dynamical models.<i>Results<i/>. The first results of ARKS are presented as a series of ten papers. We discovered that up to 33% of our sample exhibits substructures in the form of multiple dusty rings that may have been inherited from their protoplanetary discs. For highly inclined belts, we found that non-Gaussian vertical distributions are common and could be indicative of multiple dynamical populations. Half of the derived scale heights are small enough to be consistent with self-stirring in low-mass belts (<i>M<i/><sub>belt<sub/> ≤ <i>M<i/><sub>Neptune<sub/>). We also found that 10 of the 24 belts present asymmetries in the form of density enhancements, eccentricities, or warps. We find that the CO gas is radially broader than the dust, but this could be an effect of optical depth. At least one system shows non-Keplerian kinematics due to strong pressure gradients, which may have triggered a vortex that trapped dust in an arc. Finally, we find evidence that the micron-sized grains may be affected by gas drag in gas-rich systems, pushing the small grains to wider orbits than the large grains.<i>Conclusions<i/>. ARKS has revealed a great diversity of radial and vertical structures in exoKuiper belts that may arise when they are formed in protoplanetary discs or subsequently via interactions with planets and/or gas. We encourage the community to explore the reduced data and data products that we have made public through a dedicated website.","PeriodicalId":8571,"journal":{"name":"Astronomy & Astrophysics","volume":"63 1","pages":""},"PeriodicalIF":6.5,"publicationDate":"2026-01-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146006202","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"物理与天体物理","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) 外柯伊伯带亚结构(ARKS)的ALMA调查
IF 6.5 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS Pub Date : 2026-01-20 DOI: 10.1051/0004-6361/202556450
Yinuo Han, Elias Mansell, Jeff Jennings, Sebastian Marino, A. Meredith Hughes, Brianna Zawadzki, Anna Fehr, Jamar Kittling, Catherine Hou, Aliya Nurmohamed, Junu Lee, Allan Cheruiyot, Yamani Mpofu, Mark Booth, Richard Booth, Myriam Bonduelle, Aoife Brennan, Carlos del Burgo, John M. Carpenter, Gianni Cataldi, Eugene Chiang, Steve Ertel, Thomas Henning, Marija R. Jankovic, Ágnes Kóspál, Alexander V. Krivov, Joshua B. Lovell, Patricia Luppe, Meredith A. MacGregor, Sorcha Mac Manamon, Jonathan P. Marshall, Luca Matrà, Julien Milli, Attila Moór, Johan Olofsson, Tim Pearce, Sebastián Pérez, Antranik A. Sefilian, Philipp Weber, David J. Wilner, Mark C. Wyatt
Context. Debris discs are populated by belts of planetesimals, whose structure carries dynamical imprints of planets and the formation and evolutionary history of the planetary system. The relatively faint emission of debris discs has previously made it challenging to obtain a large sample of high-resolution ALMA images to characterise their substructures.Aims. The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) was recently completed to cover the lack of high-resolution observations and to investigate the prevalence of substructures such as radial gaps and rings in a sample of 24 debris discs. This study characterises the radial structure of debris discs in the ARKS programme.Methods. We modelled all discs with a range of non-parametric and parametric approaches, including those that deconvolve and deproject the image or fit the visibilities directly, in order to identify and quantify the disc substructures.Results. Across the sample we find that of the 24 discs, 5 host multiple rings, 7 are single rings that display halos or additional low-amplitude rings, and 12 are single rings with at most tentative evidence of additional substructures. The fractional ring widths that we measured are significantly narrower than previously derived values, and they follow a distribution similar to the fractional widths of individual rings resolved in protoplanetary discs. However, there exists a population of rings in debris discs that are significantly wider than those in protoplanetary discs. We also find that discs with steep inner edges consistent with planet sculpting tend to be found at smaller (<100 au) radii, while more radially extended discs tend to have shallower edges more consistent with collisional evolution. An overwhelming majority of discs have radial profiles that are well-described by either a double power law or double-Gaussian parametrisation.Conclusions. While our findings suggest that it may be possible for some debris discs to inherit their structures directly from pro-toplanetary discs, there exists a sizeable population of broad debris discs that cannot be explained in this way. Assuming that the distribution of millimetre dust reflects the distribution of planetesimals, mechanisms that cause rings in protoplanetary discs to migrate or debris discs to broaden soon after formation may be at play, possibly mediated by planetary migration or scattering.
上下文。碎片盘由星子带组成,其结构带有行星的动力学印记以及行星系统的形成和演化历史。碎片盘的发射相对微弱,这使得之前获得大量高分辨率ALMA图像样本以表征其亚结构具有挑战性。ALMA最近完成了对外柯伊伯带亚结构(ARKS)的调查,以弥补高分辨率观测的不足,并调查了24个碎片盘样本中径向间隙和环等亚结构的普遍存在。本研究在ARKS程序中描述了碎片盘的径向结构。我们用一系列非参数和参数方法对所有圆盘进行建模,包括那些对图像进行反卷积和去投影或直接拟合可见性的方法,以便识别和量化圆盘的子结构。在整个样本中,我们发现在24个圆盘中,有5个拥有多个环,7个是显示晕或附加低振幅环的单个环,12个是单个环,最多是附加子结构的初步证据。我们测量到的分数环宽度比之前得到的值要窄得多,它们的分布类似于原行星盘中单个环的分数宽度。然而,在碎片盘中存在着大量的环,它们比原行星盘中的环要宽得多。我们还发现,具有与行星雕刻一致的陡峭内缘的圆盘往往在较小的地方被发现。虽然我们的研究结果表明,一些碎片盘的结构可能直接继承自前行星盘,但仍有相当数量的宽碎片盘无法用这种方式解释。假设毫米尘埃的分布反映了星子的分布,那么导致原行星盘中的环迁移或碎片盘在形成后不久变宽的机制可能在起作用,可能是由行星迁移或散射介导的。
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引用次数: 0
The ALMA survey to Resolve exoKuiper belt Substructures (ARKS) 外柯伊伯带亚结构(ARKS)的ALMA调查
IF 6.5 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS Pub Date : 2026-01-20 DOI: 10.1051/0004-6361/202556637
M. R. Jankovic, N. Pawellek, J. Zander, T. Löhne, A. V. Krivov, J. Olofsson, A. Brennan, J. Milli, M. Bonduelle, M. C. Wyatt, A. A. Sefilian, T. D. Pearce, S. Mac Manamon, Y. Han, S. Marino, L. Matrà, A. Moór, M. Booth, E. Chiang, E. Mansell, P. Weber, A. M. Hughes, D. J. Wilner, P. Luppe, B. Zawadzki, C. del Burgo, Á. Kóspál, S. Pérez, J. M. Carpenter, T. Henning
Context. Dusty discs detected around main-sequence stars are thought to be signs of planetesimal belts in which the dust distribution is shaped by collisional and dynamical processes, including interactions with gas if present. The debris disc around the young A-type star HD 131835 is composed of two dust rings at ∼65 au and ∼100 au, a third unconstrained innermost component, and a gaseous component centred at ∼65 au. New ALMA observations show that the inner of the two dust rings is brighter than the outer one, in contrast with previous observations in scattered light.Aims. We explore two scenarios that could explain these observations: the two dust rings might represent distinct planetesimal belts with different collisional properties, or only the inner ring might contain planetesimals while the outer ring consists entirely of dust that has migrated outwards due to gas drag.Methods. To explore the first scenario, we employed a state-of-the-art collisional evolution code. To test the second scenario, we used a simple dynamical model of dust grain evolution in an optically thin gaseous disc. In each case we identified the parameters of the planetesimal and the gaseous disc that best reproduce the observational constraints.Results. Collisional models of two planetesimal belts cannot fully reproduce the observations by only varying their dynamical excitation, and matching the data through a different material strength requires an extreme difference in dust composition. The gas-driven scenario can reproduce the location of the outer ring and the brightness ratio of the two rings from scattered light observations, but the resulting outer ring is too faint overall in both scattered light and sub-millimetre emission.Conclusions. The dust rings in HD 131835 could be produced from two planetesimal belts, although how these belts would attain the required extremely different properties needs to be explained. The dust-gas interaction is a plausible alternative explanation and deserves further study using a more comprehensive model.
上下文。在主序星周围发现的尘埃盘被认为是星子带的标志,其中的尘埃分布是由碰撞和动力学过程形成的,如果存在的话,还包括与气体的相互作用。年轻的a型恒星HD 131835周围的碎片盘由两个位于~ 65 au和~ 100 au的尘埃环,第三个不受约束的最内层成分和一个位于~ 65 au的气体成分组成。新的ALMA观测结果表明,与之前的散射光观测结果相比,这两个尘埃环的内部比外部更亮。我们探索了两种可以解释这些观测结果的情景:两个尘埃环可能代表具有不同碰撞特性的不同的星子带,或者只有内环可能包含星子,而外环完全由由于气体阻力而向外迁移的尘埃组成。为了探索第一个场景,我们使用了最先进的碰撞演化代码。为了测试第二种情况,我们使用了一个简单的动力学模型来研究一个光学薄的气体盘中尘埃颗粒的演化。在每种情况下,我们都确定了最能再现观测约束结果的星子和气体盘的参数。两个星子带的碰撞模型不能仅仅通过改变它们的动力激励来完全再现观测结果,并且通过不同的物质强度来匹配数据需要在尘埃组成上有极大的差异。气体驱动情景可以从散射光观测中再现外环的位置和两个环的亮度比,但由此产生的外环在散射光和亚毫米辐射下总体上都太微弱。HD 131835中的尘埃环可能是由两条星子带产生的,尽管这两条星子带如何获得所需的截然不同的特性还需要解释。尘埃-气体相互作用是一种合理的替代解释,值得使用更全面的模型进行进一步研究。
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Astronomy & Astrophysics
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