Planetesimal collisions as a chondrule forming event
Shigeru Wakita, Yuji Matsumoto, Shoichi Oshino, Yasuhiro Hasegawa

TL;DR
This study uses numerical simulations to investigate planetesimal collisions as a mechanism for chondrule formation, finding that such collisions can produce significant amounts of chondrules consistent with observed data, influenced by impact velocity and target composition.
Contribution
It demonstrates that planetesimal-planetesimal collisions can produce chondrules in amounts comparable to protoplanet collisions, highlighting the importance of impact velocity and target composition.
Findings
Planetesimal collisions produce ~1% chondrules, similar to protoplanet collisions.
Higher impact velocities increase chondrule production.
Deeper regions of large bodies can eject chondrule progenitors.
Abstract
Chondritic meteorites contain unique spherical materials named chondrules: sub-mm sized silicate grains once melted in a high temperature condition in the solar nebula. We numerically explore one of chondrule forming processes, planetesimal collisions. Previous studies found that impact jetting via protoplanet-planetesimal collisions make chondrules with an amount of 1 % of impactors' mass, when impact velocity exceeds 2.5 km s. Based on the mineralogical data of chondrules, undifferentiated planetesimals would be more suitable for chondrule-forming collisions than potentially differentiated protoplanets. We examine planetesimal-planetesimal collisions using a shock physics code and find two things: one is that planetesimal-planetesimal collisions produce the nearly same amount of chondrules as protoplanet-planetesimal collisions ( 1 %). The other is that the amount of…
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