9:00-9:40 |
Sergei Nayakshin |
Invited Talk: Planets and non-ideal MHD disc winds in FUOR eruptions |
9:40-10:00 |
Eduard Vorobyov (remote) |
The mystery of FU Orionis resolved
FU-Orion-type objects are characterized by short (tens of years) episodic outbursts, during which their luminosity increases by orders of magnitude. A possible cause of such flares may be a gravitational perturbation of a circumstellar disks during close encounters in young star-forming regions. Numerical simulations show that to generate a burst with characteristics close to that of FU Orionis, a close flyby with a periastron no larger than several tens of AU is required. However, the separation between the two known components of FU Orionis amounts to several hundreds of AU. Considering that the burst occurs near the periastron, simple mathematical estimates show that the components of FU Orionis must have an extremely high relative velocity to account for such a large separation, which is an order of magnitude higher than the observed velocity dispersion in young star clusters. Using numerical hydrodynamics modeling we showed that flybys with a much larger periastron on the order of 500 AU can lead to luminosity bursts, but these bursts are not triggered by a mere gravitational perturbation of the circumstellar disk by the intruder star. Instead, a gravitational disturbance in the form of a pressure wave from a passing-by star can trigger a cascade process, during which the thermal instability first develops in the inner disk, followed by the magnetorotational instability. As a result, a sharp increase in the mass accretion rate onto the star occurs, which is also manifested in an increase in luminosity by more than 2 orders of magnitude. This cascade mechanism of FU Orionis outburst relaxes strict requirements on the relative velocity of the FU Orionis components and raises the likelihood of such events.
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10:00-10:20 |
Troels Haugbolle |
Late infall and accretion rejuvenating protoplanetary disks
Protoplanetary systems are traditionally believed to acquire their mass and angular momentum during the protostellar phase, strongly constraining disk evolution, planet formation, and the inclination and spin in the system. Recent findings, however, suggest that material from the protostellar environment is added through accretion streamers and late infall. This process not only increases the mass but also introduces significant angular momentum, potentially altering the star-disk systems orientation and allow late disks to maintain their size in a wind-driven scenario, without the need for viscous expansion.
Based on ab initio simulations of a star forming region and theoretical derivations, I will argue that the orientation of star-disk systems can change considerably during accretion, in particular for higher mass stars. While the change in orientation varies with stellar mass, it is consistent across different stars relative to their mass accrual. The post-collapse accretion phase tends to be more anisotropic than the initial collapse phase, aligning with the idea that infall occurs via streamers along a preferred direction, unlike the more isotropic early collapse. Environmental factors leads to a large variation in mass accretion history, with some stars gaining most of their mass during initial collapse and others receiving over half of their final mass from late infall. Stars experiencing significant late infall have higher angular momentum budgets, correlating with larger disk sizes. Late accretors, due to their significant infall, can appear younger than they are, being classified as Class 0 objects despite being 1 Myr old. This new understanding, supported by our magnetohydrodynamical models and recent observations of late infall, requires significant revisions in late-time disk and planet formation theories.~
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10:20-10:40 |
Vardan Elbakyan (remote) |
Accretion bursts in high-mass protostars
Recent observations of high-mass young stellar objects (HMYSOs) with masses M∗≥10 M⊙ uncovered outbursts with accretion rates exceeding ~10−3 M⊙ yr−1. We utilise 1D time-dependent models of protoplanetary discs around HMYSOs to study burst properties. We find that discs around HMYSOs are much hotter than those around their low-mass cousins. As a result, a much more extended region of the disc is prone to the thermal hydrogen ionisation and magnetorotational (MRI) activation instabilities. The outbursts triggered by these instabilities, however, always have too low accretion rates and are one to several orders of magnitude too long compared to those observed from HMYSOs to date. On the other hand, bursts generated by tidal disruptions of gaseous giant planets formed by the gravitational instability of the protoplanetary discs yield properties commensurate with observations, provided that the clumps are in the post-collapse configuration with planet radius Rp≥10 Jupiter radii.
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10:40-11:10 |
30 min coffee break |
11:10-11:30 |
Michael Cecil |
2D radiation hydrodynamic evolution of the inner PPD undergoing episodic accretion
Our two dimensional radiation hydrodynamic models show the evolution of the vertical thermal and dynamic structure of the inner protoplanetary disk impacted by thermal instability-induced episodic accretion events. We describe the evolution of the thermal instability as a consequence of MRI activation in the dead zone on the basis of S-curves, investigate the disk's dust content in the burst regions and the emergence of pressure maxima, and analyse the occurring small-scale modulation of the accretion rate in addition to the large-scale outbursts. Our models highlight different important aspects of the inner disk evolution during and in between episodic accretion events and can incentivise further theoretical and observational investigations.
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11:30-11:50 |
Arpan Ghosh |
Simultaneous NIR and Radio monitoring of YSOs to probe connection between accretion and outflows
Accretion and Outflows are the fundamental processes in the formation of low mass stars that remain poorly understood. Initially, it was understood that the Pre-Main sequence (PMS) stars accrete at steady rate from their circumstellar envelope. However, the works of Kenyon et al. 1990 and Evans et al. 2009 revealed that the predicted luminosity of low mass Class I young stellar objects (YSOs) based on steady accretion rate is an order lower than the observed luminosities. The most promising solution to this apparent paradox is episodic accretion as a widespread phenomenon among YSOs. Indeed, accretion bursts have been known for decades to occur in ‘peculiar’ objects like FU Oris. Systematic optical and infrared surveys are being conducted to test and quantify accretion variations. In the radio part of the spectrum, the jet emanating from YSOs is known to have faint free-free emission. These ‘thermal radio jets’ have also been found to be variable and/or to have episodic ejections. The radio data permits to directly obtain the mass-loss rate from the wind/jet emission, but it does not provide direct information on accretion variations. Therefore to test this in a systematic way, we started in 2012 a radio monitoring of a few nearby star formation regions using JVLA in coordination with the KMOS-VLT to observe the variations of NIR lines and the radio continuum respectively. The goals of our current work is to probe the connection between accretion and ejection in an evolutionary unbiased sample of YSOs, and to test for episodic accretion/ejection and in this platform we wish to show our results.~
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11:50-12:10 |
Foteini Lykou (remote) |
A compact disk and jet-like signatures in the eruptive star V900 Mon
Eruptive young stars experience fast increases in brightness in the visual and near-IR due to enhanced accretion from their circumstellar disks. Their status on whether they constitute a sub-class of pre-MS stars or they are a typical step in early-type stellar evolution is under debate. FUori-type eruptive young stars experience a rapid brightening (e.g., ~200x brighter than in quiescence) that can last from a few months to years, caused sudden spikes in mass accretion rates as high as 1e-4 Msun/yr, followed by a very slow dimming. This long-term variability makes them ideal laboratories in studying the evolution of protoplanetary disks within a few years after an eruptive event. V900 Mon is one such star, whose irregular reflection nebula was discovered by an amateur astronomer. It is thought to have erupted in the 1990s and has yet to return to quiescence. Sub-mm observations probed a wide-angled bipolar outflow and a compact disk. We have now harnessed the power of mid-infrared interferometry with MATISSE/VLTI and integral field spectroscopy with MUSE/VLT to study the protoplanetary disk and outflow of V900 Mon. In this talk, we will discuss our recent results (Lykou et al. 2024) and potential implications in disk-wind interaction in FUors based on the jet-like signature that was discovered with MUSE, and the MATISSE data that could indicate sub-micron dust at the bottom of said outflow.~
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12:10-12:30 |
Patrick Sheehan |
Sub-mm Variability in the Envelope & Warped Protostellar Disk of the Class 0 Protostar HOPS 358
The JCMT Transient Survey recently discovered that the Class 0 protostar HOPS 358 decreased in 350 GHz continuum brightness by ~25% over the course of four years before brightening again for the next four. Intriguingly, the JCMT lightcurve can be fit by a long period sinusoid with a period roughly eight years and an amplitude of 10% the mean flux. A shorter period overtone is also apparent with a period of 1.75 years and a smaller 3\% amplitude. I will present a study of nine epochs of ALMA observations of HOPS 358 taken over the course of the decline and subsequent rise in brightness seen with the JCMT to test whether the variation seen on ~15", covering both disk and envelope, is also observed on smaller, <1" scales that primarily probe HOPS 358's protostellar disk. With images covering a range of spatial scales, I will discuss the interesting structure we find in the protostellar disk, and further consider how this structure may inform and/or be related to planet formation at early times.
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12:30-14:00 |
Lunch |
Wednesday Afternoon, Chairs: James Miley, Baobab Liu |
14:00-14:40 |
Ilse Cleeves |
Invited Talk: Energetic Processes' Role in the Chemistry of Planet Formation |
14:40-15:00 |
Zsófia M. Szabó |
The molecular inventory of a young eruptive star’s environment - Case study of the classical FUor, V1057 Cyg
Young stellar objects (YSOs) undergo accretion-driven episodic outbursts. Studying the impact of these outbursts on the environment is fundamental for our understanding of planet formation. The FU Orionis objects (briefly FUors) represent a small but rather pivotal class of YSOs, whose outbursts are primar- ily characterised by a rapid, multi-magnitude increase in brightness at optical and near-infrared wavelengths, attributed to the sudden increase of the accretion flow from the disk onto the protostar, a process lasting for several decades, likely centuries. These highly energetic outbursts may have a long-lasting influence on the chemistry and molecular inventory of disks around eruptive young stars and the elevated temperatures can, temporarily, increase abundances of complex organic molecules (COMs). Improvements in observational techniques and instrumentation have opened a new path for astrochemical research. Despite the growing number of observational studies and model predictions of molecular emission, there is a lack of dedicated line surveys for FUors over wide frequency ranges that cover multiple transitions of many molecules, which is required for deriving their column densities. We carried out the first dedicated (almost) continuous large band with millimeter line survey of a low-mass young eruptive star, the classical FUor V1057 Cyg, known to have the highest peak accretion rate ever observed in a FUor. This source has shown extraordinary multiple flares in the 1720 MHz OH maser transition, and NH3 observation have shown that it is still associated with its natal dense core, thus it is a good candidate to search for other molecular species. We performed a wide spectral line survey of this source, complemented by on-the-fly maps of selected molecules, with the IRAM 30-m and APEX 12-m telescopes from 73 to 263 GHz, of selected frequencies ranged centered around 227, 291, and 344 GHz. In this talk, I will present results of this survey, which provides the first in depth view at the molecular inventory of a young eruptive star’s environment. Due to the wide frequency coverage we detected emission from many molecular species (and isotopologues of several), covering multiple transitions for many. We identify simple molecules of C-, N-, O-, S-bearing species, deuterated species, ionic species, and complex organic molecules. Several molecular species trace large-scale structures in the environment of V1057 Cyg with hints of small-scale fragmentation. The position-velocity diagram shows concentrated peaks even in the single-dish data, indicating past outburst activity. We used population diagrams and a simple radiative transfer analysis to derive column densities and excitation temperatures, and position- velocity diagrams to get insight into the past outburst activity of the source. This study highlights the importance of using astrochemistry to study outbursting sources in different evolutionary stages, and reveals that V1057 Cyg is an excellent target for high angular resolution interferometric observations.
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15:00-15:20 |
Abygail Waggoner |
Observing an 'Explosion:' Monitoring Post-flare Chemistry and Physics in Real Time
Planets are not only 'born in fire', but they are born in a highly 'explosive' environment. Protostars are highly variable objects, as they commonly undergo flaring events, i.e. 'explosions', that temporarily increase light emission across the electromagnetic spectrum. Flares are thought to dramatically impact the physics and chemistry of surrounding disk, and therefore driving variations in the environment where planets form. However, there is limited observational evidence on this phenomenon. We present results from a multi-wavelength campaign designed to map the physics and chemistry of flaring events in real time in the Orion Nebula Cluster. Chandra was used to identify stars actively undergoing flaring events, which then triggered rapid (days or less) follow up observations by ground based telescopes. We monitored coronal mass ejections using the VLBA, magnetic activity with the Hobby-Ebberly telescope, and gas-phase chemistry and ionization with ALMA. This campaign reveals previously unexplored information on 'explosive' stars, thus providing a more complete picture of the highly dynamic regions where planet formation occurs.
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15:20-15:50 |
30 min coffee break |
15:50-16:10 |
F. Cruz Sáenz de Miera |
The role of (out)bursts in shaping circumstellar disk chemistry
Disks around young stars are the birthplaces of planets, with their chemical compositions playing a crucial role in the materials available for planet formation. However, these disks are not static environments. The increased temperatures during accretion (out)bursts significantly perturb the chemistry of the disk.
In particular, molecular species in the midplane region of a quiescent disk are subjected to temperatures so low that they are frozen icy mantles encasing dust grains.
Once the disk temperature rises, these molecules quickly sublimate, hereby modifying the spatial distribution and chemical composition of the gas available for dust growth and planet formation. Here I will present our studies of the effects of (out)bursts in the chemistry of young protostellar disks.
I will show the serendipitous ALMA discovery of hot and compact emission of multiple complex organic molecules in four protostars with evidence of FUor-type accretion outbursts.
I will put these results into context by comparing our four targets, plus others outbursting young stars from the literature, with young stars considered to be in quiescence. Lastly, I will mention some ideas when designing future astrochemical studies of (out)bursting young stars.
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16:10-16:30 |
Margot Leemker (remote) |
Resolving the water snowline in disks and its effect on the chemical composition of planet forming material
Many bright disks show signs of ongoing planet formation such as deep cavities and rings. These may be carved by massive planets but how the planets form remains one of the biggest questions to date. On top of that, their chemical composition depends on their formation location with respect to the snowlines, the midplane radius where a major volatile freezes out. One possible solution to solve the planet formation puzzle is that planets form around the water snowline. We will resolve and locate the 2D water snow surface for the first time in a disk around a young outbursting star using HDO, an isotopologue of water observed with ALMA. In addition, we will use observations of another chemically rich disk to study the effect of the water snowline on the chemical composition of the planet forming material through freshly sublimated ices.
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16:30-16:50 |
Beatrice Kulterer |
Post Outburst Chemistry in the Very Low Luminosity Object in DC3272+18
The Very Low Luminosity Object (VeLLO) in the DC3272+18 cloud has undergone an outburst in the past ~10^4 yr. This is evident from the current position of its CO snowline, which is ~3 times further out than the present luminosity of the central protostar would allow for [1]. It is currently in the quiescent phase of the episodic accretion process, and has an internal luminosity of only 0.04 Lsun [1,2], but due to its past outburst (Lburst = 1-4 Lsun, [1]) a plethora of molecules has been detected in the gas phase with the Atacama Pathfinder Experiment [3]. In my talk I will discuss how we can utilize the line fluxes, column densities and abundance ratios of the detected molecules to characterize the different physical components of the VeLLO, a in general understudied group, and how the past outburst has influenced its chemical inventory. Detection highlights include molecules that have a) sublimated due to the increased temperature in the envelope during the heating event such as methanol (CH3OH), formaldehyde (H2CO), and sulfur oxide (SO), and b) freshly formed gas phase species that have formed from processed and sublimated ices such as nitric oxide (NO). I will argue how the detection of NO, which has been detected for the first time in a source of this type, can be directly linked to its formation at the position that the water snowline got shifted to during the burst, which suggests that NO could potentially be used to trace the water snowline in outbursting sources.
[1] Hsieh, T.-H., Murillo, N. M., Belloche, A. et al., 2018, ApJ, 854, 15
[2] Kim G., Lee, C. W., Maheswar, G. et al. 2019, ApJS, 240, 18
[3] Kulterer, B. M., Wampfler, S.-F., Ligterink, N. F. W. et al., 2024, „Post-Outburst Chemistry in a Very Low Luminosity Object: Does Nitric Oxide Trace the Water Snowline”, submitted to A&A
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16:50-17:30 |
Discussion session |
17:30 |
Conference Photo (don't run away!) |
18:00 |
Planetarium social event
Location
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