3D Radiation-hydrodynamical Simulations of Shadows on Transition Disks

被引:2
|
作者
Zhang, Shangjia [1 ,2 ,3 ]
Zhu, Zhaohuan [1 ,2 ]
机构
[1] Univ Nevada, Dept Phys & Astron, 4505 S Maryland Pkwy, Las Vegas, NV 89154 USA
[2] Univ Nevada, Nevada Ctr Astrophys, Las Vegas, NV 89154 USA
[3] Columbia Univ, Dept Astron, 538 W 120th St,Pupin Hall, New York, NY 10027 USA
关键词
VERTICAL SHEAR INSTABILITY; DRIVEN SPIRAL ARMS; PROTOPLANETARY DISK; SCATTERED-LIGHT; HD; 142527; DUST FILTRATION; PLANET; ACCRETION; EVOLUTION; PROJECT;
D O I
10.3847/2041-8213/ad815f
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Shadows are often observed in transition disks, which can result from obscuring by materials closer to the star, such as a misaligned inner disk. While shadows leave apparent darkened emission as observational signatures, they have significant dynamical impact on the disk. We carry out 3D radiation-hydrodynamical simulations to study shadows in transition disks and find that the temperature drop due to the shadow acts as an asymmetric driving force, leading to spirals in the cavity. These spirals have zero pattern speed following the fixed shadow. The pitch angle is given by tan-1(c s /v phi ) (6 degrees if h/r = 0.1). These spirals transport mass through the cavity efficiently, with alpha similar to 10-2 in our simulation. Besides spirals, the cavity edge can also form vortices and flocculent streamers. When present, these features could disturb the shadow-induced spirals. By carrying out Monte Carlo radiative transfer simulations, we show that these features resemble those observed in near-infrared scattered light images. In the vertical direction, the vertical gravity is no longer balanced by the pressure gradient alone. Instead, an azimuthal convective acceleration term balances the gravity-pressure difference, leading to azimuthally periodic upward and downward gas motion reaching 10% of the sound speed, which can be probed by Atacama Large Millimeter/submillimeter Array line observations.
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页数:9
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