Three-dimensional Simulations of the Magnetorotational Instability in Eccentric Disks

被引:4
作者
Chan, Chi-Ho [1 ,2 ]
Piran, Tsvi [3 ]
Krolik, Julian H. [4 ]
机构
[1] Georgia Inst Technol, Ctr Relativist Astrophys, Atlanta, GA 30332 USA
[2] Georgia Inst Technol, Sch Phys, Atlanta, GA 30332 USA
[3] Hebrew Univ Jerusalem, Racah Inst Phys, Jerusalem, Israel
[4] Johns Hopkins Univ, Dept Phys & Astron, Baltimore, MD 21218 USA
基金
美国国家科学基金会; 欧洲研究理事会;
关键词
DIFFERENTIALLY ROTATING-DISKS; WEAKLY MAGNETIZED DISKS; LOCAL SHEAR INSTABILITY; TIDAL DISRUPTION EVENT; ACCRETION DISKS; MAGNETOHYDRODYNAMIC SIMULATIONS; NUMERICAL SIMULATIONS; VERTICAL STRUCTURE; DISCS; SHOCKS;
D O I
10.3847/1538-4357/ad5d5a
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Previously we demonstrated that the magnetorotational instability (MRI) grows vigorously in eccentric disks, much as it does in circular disks, and we investigated the nonlinear development of the eccentric MRI without vertical gravity. Here we explore how vertical gravity influences the magnetohydrodynamic (MHD) turbulence stirred by the eccentric MRI. Similar to eccentric disks without vertical gravity, the ratio of Maxwell stress to pressure, or the Shakura-Sunyaev alpha parameter, remains similar to 10-2, and the local sign flip in the Maxwell stress persists. Vertical gravity also introduces two new effects. Strong vertical compression near pericenter amplifies reconnection and dissipation, weakening the magnetic field. Angular momentum transport by MHD stresses broadens the mass distribution over eccentricity at much faster rates than without vertical gravity; as a result, spatial distributions of mass and eccentricity can be substantially modified in just similar to 5 to 10 orbits. MHD stresses in the eccentric debris of tidal disruption events may power emission greater than or similar to 1 yr after disruption.
引用
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页数:15
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