Impact of mass transfer on the orbital evolution of a white dwarf close to an intermediate-mass black hole
Yang Yang, Jie Yang, Xian Chen, Zihan Zhang
TL;DR
We address WD EMRIs around spinning IMBHs and show that phase-dependent MT, resolved with a perturbed Kepler approach plus PN corrections, can compete with GW-driven inspiral. MT can increase orbital period and eccentricity, potentially preventing complete tidal disruption and producing detectable GW phase shifts of order $1$ rad over multi-year observations; it may also explain QPE variability or disappearance. By deriving MT accelerations from angular-momentum considerations and incorporating GR corrections to Roche geometry, the work demonstrates the necessity of jointly modeling relativistic dynamics and MT for WD–IMBH systems and highlights observable GW signatures that accompany mass transfer. The results have direct implications for multi-messenger astronomy and the interpretation of QPEs, emphasizing that MT feedback can significantly alter EMRI evolution and GW waveforms.
Abstract
Extreme mass ratio inspirals (EMRIs) of low-mass white dwarfs (WDs, 0.1 - 0.3 Msun) around spinning intermediate-mass black holes (IMBHs, 10^3 - 10^5 Msun) offer unique opportunities for multi-messenger astronomy, emitting both gravitational waves (GWs) and electromagnetic (EM) signals. Yet, despite their astrophysical relevance, theoretical models often omit key interactions between relativistic dynamics and phase-dependent mass transfer (MT). In this study, we integrate a perturbed Keplerian formalism with post-Newtonian (PN) corrections to simulate the relativistic orbit of a WD around a rotating IMBH, explicitly resolving the narrow phase near pericentre where Roche-lobe overflow initiates MT. We find that GW emission and MT exert competing influences on the orbit: MT episodes can increase both orbital period and eccentricity, potentially enabling the WD to avoid complete tidal disruption and even escape. We further quantify the GW phase evolution induced by MT, identifying parameter regimes in which GW detectors could observe a one-radian phase shift over observational timescales. Finally, we propose that the orbital expansion driven by MT may lead to the disappearance of quasi-periodic eruptions (QPEs). Our results underscore the necessity of jointly modeling relativistic effects and dynamic mass transfer in WD-IMBH systems.
