Abstract
This study investigates planet formation in M-Dwarf stellar systems using a comprehensive model considering multiple factors. By simulating a proto-planetary disc with turbulence, snowlines, planet migration, and pebble traps, we examine planet formation and evolution. Our results show that disc mass and turbulence strongly affect planet mass and density. Comparing simulations with observations, we find good agreement within the interquartile range for high and low-density planets. However, discrepancies in the low-density range suggest the importance of gas accretion. This study provides insights into complex processes during planet formation and lays the foundation for future research directions such as considering different-sized solids, planet-planet interactions, and gas accretion.
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