On the Evolution of the Snow Line in Protoplanetary Discs
Rebecca G. Martin, Mario Livio (STScI)

TL;DR
This paper models the evolution of the snow line in protoplanetary discs, considering both fully turbulent and dead zone scenarios, to explain planet formation and water distribution.
Contribution
It introduces a time-dependent disc model with dead zones, showing how the snow line's evolution affects planet formation and water delivery.
Findings
In fully turbulent discs, the snow line moves inside Earth's orbit, challenging water-devoid planet formation.
Dead zones slow disc evolution, allowing the outer snow line to stay outside Earth's orbit.
An inner icy region within the dead zone forms, enabling Earth-like planet formation and potential giant planet formation close to the star.
Abstract
We model the evolution of the snow line in a protoplanetary disc. If the magneto-rotational instability (MRI) drives turbulence throughout the disc, there is a unique snow line outside of which the disc is icy. The snow line moves closer to the star as the infall accretion rate drops. Because the snow line moves inside the radius of the Earth's orbit, the formation of our water-devoid planet is difficult with this model. However, protoplanetary discs are not likely to be sufficiently ionised to be fully turbulent. A dead zone at the mid-plane slows the flow of material through the disc and a steady state cannot be achieved. We therefore model the evolution of the snow line also in a time-dependent disc with a dead zone. As the mass is accumulating, the outer parts of the dead zone become self gravitating, heat the massive disc and thus the outer snow line does not come inside the radius…
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