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Challenges in Planet Formation (1610.07202v2)

Published 23 Oct 2016 in astro-ph.EP

Abstract: Over the past two decades, large strides have been made in the field of planet formation. Yet fundamental questions remain. Here we review our state of understanding of five fundamental bottlenecks in planet formation. These are: 1) the structure and evolution of protoplanetary disks; 2) the growth of the first planetesimals; 3) orbital migration driven by interactions between proto-planets and gaseous disk; 4) the origin of the Solar System's orbital architecture; and 5) the relationship between observed super-Earths and our own terrestrial planets. Given our lack of understanding of these issues, even the most successful formation models remain on shaky ground.

Citations (109)

Summary

  • The paper identifies bottlenecks in planet formation by critiquing the limitations of the α-disk model and traditional aggregation mechanisms.
  • It examines issues in protoplanetary disk turbulence, early planetesimal assembly, and rapid inward migration that conflict with observational data.
  • The work advocates for refined modeling of disk viscosity and migration halting regions to reconcile Solar System architecture with exoplanetary findings.

Challenges in Planet Formation

In the paper titled "Challenges in Planet Formation," the authors, Alessandro Morbidelli and Sean N. Raymond, provide a critical review of significant bottlenecks in the theoretical understanding of planet formation. The insights presented address complex issues that impede a full understanding of how planetary systems, including our Solar System, have come into existence. Despite progress in the field, these bottlenecks reveal that even the most successful models encounter fundamental challenges that persist due to inadequate comprehension of underlying processes.

Protoplanetary Disk Structure

One of the primary challenges discussed involves the structure and evolution of protoplanetary disks. Despite longstanding adoption of the α\alpha-disk model to describe these disks, the paper highlights that this model does not adequately capture the complexities observed in actual systems. Recent research suggests that magneto-rotational instability, previously considered a key driver of turbulence in disks, may not be universally applicable. The concept of a "dead zone" where turbulence is reduced contrasts with regions of active MRI, complicating the understanding of material transport and disk evolution.

Formation of the First Planetesimals

The accretion process that gives rise to the first generation of planetesimals remains a significant mystery. The authors emphasize the inadequacies of traditional aggregation models in overcoming barriers such as the "bouncing barrier" and "meter-size barrier," which inhibit the growth of larger bodies. Proposed mechanisms, such as the turbulent concentration and self-gravity-driven collapse of particulate matter, face challenges primarily due to the dependency on disk conditions which are not well-constrained.

Planetary Migration

The dynamics of planetary migration, where forming planets change their orbits considerably due to interactions with the gas disk, present both theoretical and observational puzzles. Current models greatly struggle to reconcile the rapid inward Type I migration expected from theory with the array of observed exoplanet configurations. Findings suggest regions within the disk, driven by complex disk morphology and temperature gradients, where migration could be halted or reversed. However, a comprehensive solution for the multitude of observed systems remains underdeveloped.

Solar System’s Orbital Architecture

The specific configuration of our Solar System, where terrestrial planets are separated from gas giants by an asteroid belt, raises questions about commonality versus uniqueness in planetary architectures. While hypotheses like the Grand Tack model provide mechanisms for forming such structures via significant migration of Jupiter and Saturn, alternative interpretations that rely less on migratory history also provide plausible explanations.

Comparison of Super-Earths and Terrestrial Planets

The paper questions whether super-Earths, which are prevalent in observed exoplanetary systems, are fundamentally different from Earth-like planets. The distinction is clouded by differences in initial conditions and formation timelines between systems. The significant mass and proximity of short-period super-Earths compared to Earth's formation raise questions about common processes and environmental conditions.

Implications and Future Directions

The paper underlines the need for further sophistication in disk models and a deeper understanding of embryo growth dynamics via pebble accretion and other processes. It speculates that the gaps in current knowledge, particularly regarding disk viscosity and structure, migration mechanisms, and planetesimal formation, are pivotal in restricting a complete synthesis of planet formation theories. Furthermore, elucidating how our Solar System’s configuration compares to diverse extrasolar systems could inform broader theories of planetary system evolution.

In conclusion, while the identified bottlenecks pose significant challenges, they also frame future research directions in astrophysics and planet formation, crucial for developing an integrated theory that aligns with empirical observations.

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