The inner structure and thermodynamics of thin accretion discs

ABSTRACT Using three-dimensional general relativistic magnetohydrodynamic simulations with electron and proton thermodynamics and an electron cooling function, we probe the inner radial and vertical structure of weakly magnetized geometrically thin accretion discs around rapidly spinning black holes. We find that the thin, cold disc transitions to a thick, hot accretion flow at a radius dependent on the mass accretion rate due to proton–electron Coulomb decoupling. At high accretion rates, the disc truncates close to the innermost stable circular orbit $r\approx 2r_g$, demonstrating that even in the canonical thin disc model, the plunging region should be treated with two-temperature physics. At intermediate accretion rates, the transition radius moves outwards by a factor of 2 to $r\approx 5r_g$, forming a radiatively inefficient inner flow. The simulations also reveal extended cooling along the surface of the disc out to $\sim 10r_g$, with 40 per cent of the total cooling at intermediate accretion rates occurring above the disc body. Two-temperature effects also impact the emission from within the plunging region of the black hole, leading to less thermal emission than predicted by single-temperature models. These results have implications for X-ray binary state transitions, the physical origin of the X-ray corona, and spin measurements that rely on determining the location of the innermost stable circular orbit.

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Publication Details

Journal
Monthly Notices of the Royal Astronomical Society
Published
2025-07-16
DOI
https://doi.org/10.1093/mnras/staf1169
Citations
4
Primary Topic
High-pressure geophysics and materials
Type
article
Field-Weighted Citation Impact
7.47

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article

The inner structure and thermodynamics of thin accretion discs

Amelia Hankla, Jason Dexter, Nicolas Scepi
4 citations
Monthly Notices of the Royal Astronomical Society
High-pressure geophysics and materials
7.47
article

The inner structure and thermodynamics of thin accretion discs

Amelia Hankla, Jason Dexter, Nicolas Scepi
article en
4 citations

Abstract

ABSTRACT Using three-dimensional general relativistic magnetohydrodynamic simulations with electron and proton thermodynamics and an electron cooling function, we probe the inner radial and vertical structure of weakly magnetized geometrically thin accretion discs around rapidly spinning black holes. We find that the thin, cold disc transitions to a thick, hot accretion flow at a radius dependent on the mass accretion rate due to proton–electron Coulomb decoupling. At high accretion rates, the disc truncates close to the innermost stable circular orbit $r\approx 2r_g$, demonstrating that even in the canonical thin disc model, the plunging region should be treated with two-temperature physics. At intermediate accretion rates, the transition radius moves outwards by a factor of 2 to $r\approx 5r_g$, forming a radiatively inefficient inner flow. The simulations also reveal extended cooling along the surface of the disc out to $\sim 10r_g$, with 40 per cent of the total cooling at intermediate accretion rates occurring above the disc body. Two-temperature effects also impact the emission from within the plunging region of the black hole, leading to less thermal emission than predicted by single-temperature models. These results have implications for X-ray binary state transitions, the physical origin of the X-ray corona, and spin measurements that rely on determining the location of the innermost stable circular orbit.

Monthly Notices of the Royal Astronomical SocietyVol. 541(4)
Centre National de la Recherche Scientifique (FR), Planetary Science Institute (US), National Institute of Standards and Technology (US), Joint Institute for Laboratory Astrophysics (US), University of Maryland, College Park (US), Université Grenoble Alpes (FR)
National Science Foundation, National Aeronautics and Space Administration, Space Telescope Science Institute, Nuclear Safety and Security Commission, Astrophysics Division
Openalex Percentile: Top 3%
High-pressure geophysics and materials
7.47
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