Physical origin of the present-day compositional asymmetry

Determine whether the large-scale segregation between Ne-rich and Si-enhanced O-rich ejecta in Cassiopeia A primarily reflects spatially heterogeneous presupernova shell-merger burning, asymmetric ejecta transport during the explosion, or subsequent remnant evolution.

Background

The study finds that Ne-rich ejecta are concentrated preferentially toward the north and northeast, whereas Si-enhanced O-rich ejecta are more prominent in the southeast. Comparisons with one-dimensional presupernova models suggest distinct degrees of O-shell processing, but the current observations cannot uniquely determine whether the observed spatial arrangement was established before collapse or substantially modified during and after the explosion.

The authors propose a physically motivated scenario involving direction-dependent fuel entrainment and convective-reactive burning followed by asymmetric transport associated with Fe-rich plumes, while explicitly acknowledging that the scenario is not unique. Higher-resolution soft-X-ray observations are identified as necessary to distinguish among the competing origins.

References

Such observations could identify faint O-rich plasma in the highly absorbed western region, resolve velocity and ionization components within the different compositional classes, and determine whether the observed asymmetry primarily reflects the presupernova burning structure, asymmetric ejecta transport, or subsequent remnant evolution.

— Remnant-wide mapping of heterogeneous presupernova burning histories in the O-rich ejecta of Cassiopeia A  (2610.09612 - Kuboike et al., 7 Oct 2026) in Section 4.2, “Origin of the O-rich Ejecta Asymmetry”; Summary and Conclusions