Ejected mass in FQ Cir’s nova outbursts

Determine the ejected mass (M_ejecta) in classical nova eruptions of FQ Circini with usable accuracy sufficient to compare against the inter-eruption accreted mass (M_accreted), in order to assess whether the white dwarf grows or erodes over time.

Background

Assessing whether a white dwarf can approach the Chandrasekhar limit requires knowing if it retains more mass than it ejects over repeated nova cycles. The authors emphasize that traditional methods for estimating M_ejecta suffer from 2–3 orders of magnitude uncertainty and explicitly note that no usable measurement exists for FQ Cir (and rapid recurrent novae).

A reliable determination of M_ejecta for FQ Cir would constrain mass-retention efficiency and help clarify whether HMCVs with ONe cores can reach conditions for AIC.

References

The huge problem with checking whether $M_{\rm ejecta}$ is more-or-less than $M_{\rm accreted}$ is that all the usual and traditional methods for estimating $M_{\rm ejecta}$ have 2--3 orders-of-magnitude real uncertainty. Importantly, for M31N 2008-12a, we have no measure of $M_{\rm ejecta}$ to any useable accuracy, and the same is true for all the RRNe and FQ Cir.

During classical nova eruptions, the WD loses mass, and between recurrent nova eruptions it gains mass through accretion; whether a nova WD mass overall increases or decreases over its life-time is, however, still a matter of debate.

The instantaneous mass accretion rate of novae in quiescence: - an archival ultraviolet optical spectral analysis  (2608.18037 - Godon et al., 18 Aug 2026) in Section 1, Introduction