pith:6VJSZ6OK
ALMA-IMF XXII. Role of core subfragmentation in the IMF origin: Hierarchical fragmentation cascade and CMF in W43-MM1
Gravity rather than turbulence drives fragmentation below 14 kau in W43-MM1 and keeps the high-mass end of the fragment mass function top-heavy.
arxiv:2604.14875 v2 · 2026-04-16 · astro-ph.GA
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Claims
Based on the fractality and efficiency values measured in W43-MM1, the gravo-turbulent model by Thomasson et al. predicts that its fragmentation below ~14 kau is not driven by turbulence but by gravity. [...] the fragment mass function, from which the IMF emerges, has a high-mass end which remains top-heavy.
The assumption of self-similarity across scales, allowing parameters measured at larger scales (14 kau to 270 au) to be extrapolated to smaller scales where the model is applied; also that the Thomasson et al. model accurately captures the physics without additional unaccounted processes.
Core subfragmentation in W43-MM1 preserves the top-heavy shape of the core mass function, implying it has minimal influence on the origin of the initial mass function.
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| First computed | 2026-07-14T01:20:59.143337Z |
|---|---|
| Builder | pith-number-builder-2026-05-17-v1 |
| Signature | Pith Ed25519
(pith-v1-2026-05) · public key |
| Schema | pith-number/v1.0 |
Canonical hash
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Canonical record JSON
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