Summary

Accretion discs around young stellar objects serve as the birthplaces of planets, comprising gas and dust in a rotating structure governed by the transport of angular momentum and viscous forces. Material from the disc spirals inward to feed the central protostar, while radial temperature gradients establish condensation fronts—so-called snow lines—that control the phase of key volatiles. Within this environment, micron-sized dust grains collide and coagulate into pebbles and planetesimals, setting the stage for planetary assembly. Observations at millimetre and infrared wavelengths have revealed substructures such as rings, gaps and vortices, indicative of embedded planets or intrinsic hydrodynamic and magnetic instabilities. The interaction between dust growth, gas dynamics, thermal structure and stellar irradiation determines disc lifetimes, mass accretion rates and the delivery of water and organics to forming worlds, thus shaping the diversity of planetary systems.

Research from Nature Portfolio

Recent studies have employed the James Webb Space Telescope to characterise water vapour in the inner regions of a disc hosting a confirmed protoplanet. These observations reveal substantial water column densities within the terrestrial planet-forming zone, implying efficient in situ synthesis and self-shielding against ultraviolet photodissociation. The simultaneous detection of CO₂ emission underscores a chemically rich milieu, while marked variability in the mid-infrared spectral energy distribution points to dynamic changes in inner disc geometry. This work demonstrates that large gaps carved by nascent planets do not preclude the retention of volatile reservoirs essential for habitability.

Research from all publishers

A comprehensive review of protoplanetary disc chemistry emphasises how both inherited and local chemical pathways set the abundances of volatiles. Observed deviations of elemental ratios from stellar compositions reflect a combination of condensation, chemical reactions and radial transport, offering powerful probes of disc structure and evolution.

High-resolution interferometric measurements have constrained turbulence levels across diverse discs, revealing that turbulent motions are weaker than classical models predicted yet remain present at levels sufficient to mix material and contribute to angular momentum transport. These findings challenge pure viscous accretion theories and point towards roles for magnetic winds or hydrodynamic instabilities.

Mid-infrared spectroscopy of compact discs highlights excess cool water emission near the snow line, consistent with enhanced inward drift and sublimation of icy pebbles. The signature of this process provides direct evidence for the transport of solids across condensation fronts and opens new avenues for studies of chemical enrichment in planet-forming regions.

Accretion Disks in Protoplanetary Systems publication trend

The graph below shows the total number of articles in accretion disks in protoplanetary systems across all publications each year (not limited to Nature Index journals).

Technical terms

Accretion disk: A rotating assembly of gas and dust that feeds a central object through viscous and gravitational processes.

Snow line: The radial distance in a disc beyond which temperatures are low enough for volatiles to condense into ice.

Pebble drift: The inward migration of millimetre- to centimetre-sized solids driven by aerodynamic drag against the gas.

Turbulence: Chaotic, small-scale gas motions within the disc that facilitate mixing and angular momentum transfer.

Sublimation: The transition of solid material directly into gas as it moves across temperature thresholds.

References

  1. Water in the terrestrial planet-forming zone of the PDS 70 disk. Nature (2023).
  2. Protoplanetary Disk Chemistry. Annual Review of Astronomy and Astrophysics (2023).
  3. Empirical constraints on turbulence in proto-planetary discs. New Astronomy Reviews (2023).
  4. JWST Reveals Excess Cool Water near the Snow Line in Compact Disks, Consistent with Pebble Drift. The Astrophysical Journal Letters (2023).

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