A strong shallow heat source in the accreting neutron star MAXI J0556-332

TL;DR

This paper investigates the unusually high shallow heat source in the neutron star MAXI J0556-332, revealing it exceeds known nuclear sources and likely originates from stored mechanical energy, affecting the star's cooling behavior.

Contribution

It identifies a significantly larger shallow heating component in MAXI J0556-332 than in other neutron stars, suggesting a novel energy source beyond nuclear reactions.

Findings

Shallow heating is approximately 6-16 MeV per accreted nucleon.

High crust temperature makes cooling largely independent of composition.

Urca cooling pairs are disfavored in the crust.

Abstract

An accretion outburst in an X-ray transient deposits material onto the neutron star primary; this accumulation of matter induces reactions in the neutron star's crust. During the accretion outburst these reactions heat the crust out of thermal equilibrium with the core. When accretion halts, the crust cools to its long-term equilibrium temperature on observable timescales. Here we examine the accreting neutron star transient MAXI J0556-332, which is the hottest transient, at the start of quiescence, observed to date. Models of the quiescent light curve require a large deposition of heat in the shallow outer crust from an unknown source. The additional heat injected is $\approx 4\textrm{-}10\,\mathrm{MeV}$ per accreted nucleon; when the observed decline in accretion rate at the end of the outburst is accounted for, the required heating increases to $\approx 6\textrm{-}16\,\mathrm{MeV}$. This shallow heating is still required to fit the lightcurve even after taking into account a second accretion episode, uncertainties in distance, and different surface gravities. The amount of shallow heating is larger than that inferred for other neutron star transients and is larger than can be supplied by nuclear reactions or compositionally driven convection; but it is consistent with stored mechanical energy in the accretion disk. The high crust temperature ($T_b \gtrsim 10^{9} \, {\rm K}$) makes its cooling behavior in quiescence largely independent of the crust composition and envelope properties, so that future observations will probe the gravity of the source. Fits to the lightcurve disfavor the presence of Urca cooling pairs in the crust.