ALMA chemical survey of disk-outflow sources in Taurus (ALMA-DOT) VII: the layered molecular outflow from HL Tau and its relationship with the ringed disk
F. Bacciotti, T. Nony, L. Podio, C. Dougados, A. Garufi, S. Cabrit, C. Codella, N. Zimniak, J. Ferreira
TL;DR
This work analyzes the HL Tau disk-outflow system with ALMA-DOT CO (2-1) data at ~0.28" resolution to map the outer wind and relate it to the disk’s ring structure. Through tomographic reconstruction of channel maps and PV diagrams, the authors identify nested rotating wind shells whose footpoints align with dust rings at 58, 72, and 86 au, consistent with magnetized disk winds launching over a broad disk region. The wind parameters imply a magnetic lever arm λ in the range ~4–5 and a launching region extending to ~90 au, suggesting that magnetic effects can drive angular-momentum transport and influence disk evolution and planet formation, possibly without invoking planets to explain rings. The results support non-ideal MHD scenarios where magnetic instabilities organize rings and a layered wind, while highlighting the need for extended modeling and observation of the outer disk wind.
Abstract
The ringed disk around HL Tau stands out as the iconic signature of planet formation, but the origin of the substructures is still debated. The HL Tau system also drives a powerful bipolar wind, and we analyze its outermost component traced by CO emission, to determine the relationship of the flow with the disk and its substructures. We use ALMA observations of the ${}^{12}$CO (2-1) line at 1.3 mm, with 0.2 km/s and ~ 0.28" resolution, conducted within the ALMA-DOT project. The channel maps and position-velocity diagrams show a rich structure of concatenated bubble- and arc-shaped features, whose size and distance from the source increase with velocity. The superposition of the features generates the apparent conical shape. The tomographic reconstruction of the morphology and kinematics of the red-shifted lobe suggests the presence of distinct nested shells having higher velocity and steeper velocity gradient for shells closer to the axis, rotating in the same sense of the disk. Such configuration can be justified by different classes of models. In this paper we compare the derived wind parameters with the predictions of magnetohydrodynamic (MHD) disk winds. Under this hypothesis, the launch radii of the three outermost shells are found to be at about the position of three adjacent dust rings in the disk at 58, 72 and 86 au. The wind may be capable of removing angular momentum from the outer disk, and we derive a magnetic lever arm of $λ\sim 4 - 5$, higher than that commonly adopted for MHD winds from these regions. Interpretations are discussed. The arrangement of the wind in nested shells with brighter emission rooted at the location of ring substructures could support the results of non-ideal MHD simulations according to which magnetic instabilities can generate the disk ring-gap system with a connected layered wind, alternatively to the action of yet undetected protoplanets.
