X-ray photoevaporation's limited success in the formation of planetesimals by the streaming instability
Barbara Ercolano (1,2), Jeff Jennings (1), Giovanni Rosotti (3),, Tilmann Birnstiel (1) ((1) Ludwig Maximilian University Munich, (2), Excellence Cluster Universe, (3) Institute of Astronomy, University of, Cambridge)

TL;DR
This study investigates whether X-ray photoevaporation can trigger planetesimal formation via the streaming instability, concluding it is generally ineffective for forming planetary cores but may contribute to debris disc creation.
Contribution
The paper provides a one-dimensional viscous disc evolution model showing limited dust-to-planetesimal conversion from X-ray photoevaporation, contrasting with previous FUV-driven models.
Findings
Dust mass converted into planetesimals is usually less than 1 Earth mass.
Photoevaporation's role is likely limited to debris disc formation.
Different photoevaporation profiles significantly affect outcomes.
Abstract
The streaming instability is often invoked as solution to the fragmentation and drift barriers in planetesimal formation, catalyzing the aggregation of dust on kyr timescales to grow km-sized cores. However there remains a lack of consensus on the physical mechanism(s) responsible for initiating it. One potential avenue is disc photoevaporation, wherein the preferential removal of relatively dust-free gas increases the disc metallicity. Late in the disc lifetime, photoevaporation dominates viscous accretion, creating a gradient in the depleted gas surface density near the location of the gap. This induces a local pressure maximum that collects drifting dust particles, which may then become susceptible to the streaming instability. Using a one-dimensional viscous evolution model of a disc subject to internal X-ray photoevaporation, we explore the efficacy of this process to build…
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