SIMBAD references

The neutron star ocean is a plasma of ions and electrons that extends from the base of the neutron star's envelope to a depth where the plasma crystallizes into a solid crust. During an accretion outburst in an X-ray transient, material accumulates in the envelope of the neutron star primary. This accumulation compresses the neutron star's outer layers and induces nuclear reactions in the ocean and crust. Accretion-driven heating raises the ocean's temperature and increases the frequencies of g-modes in the ocean; when accretion halts, the ocean cools and ocean g-mode frequencies decrease. If the observed low-frequency quasi-periodic oscillations on accreting neutron stars are g-modes in the ocean, the observed quasi-periodic oscillation frequencies will increase during the outburst-reaching a maximum when the ocean temperature reaches steady state-and subsequently decrease during quiescence. For time-averaged accretion rates during outbursts between <\dotM>=0.1–1.0 \dotM_Edd the predicted g-mode fundamental n = 1 l = 2 frequency is between ≃3-7 Hz for slowly rotating neutron stars. Accreting neutron stars that require extra shallow heating, such as the Z-sources MAXI J0556-332, MXB 1659-29, and XTE J1701-462, have predicted g-mode fundamental frequencies between ≃3-16 HZ. Therefore, observations of low-frequency quasi-periodic oscillations between ~8–16 Hz in these sources, or in other transients that require shallow heating, will support a g-mode origin for the observed quasi-periodic oscillations.