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Titlebook: Dust-Gas Instabilities in Protoplanetary Disks; Toward Understanding Ryosuke Tominaga Book 2022 The Editor(s) (if applicable) and The Autho

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书目名称Dust-Gas Instabilities in Protoplanetary Disks
副标题Toward Understanding
编辑Ryosuke Tominaga
视频video
概述Highlights new instability triggered by dust-gas friction and turbulent viscosity.Presents a new instability driven by dust coagulation in protoplanetary disks.Offers a planetesimal formation scenario
丛书名称Springer Theses
图书封面Titlebook: Dust-Gas Instabilities in Protoplanetary Disks; Toward Understanding Ryosuke Tominaga Book 2022 The Editor(s) (if applicable) and The Autho
描述.How planets form is one of the long-standing questions in astrophysics. In particular, formation scenarios of planetesimals which are kilometer-sized bodies and a precursor of planets are still unclear and under debate although some promising mechanisms have been proposed..This book highlight disk instabilities that have the potential to explain the origin of planetesimals. Using linear analyses and numerical simulations, it addresses how a disk evolves through the development of instabilities, and also presents a new instability driven by dust coagulation. As a result, the simulation demonstrates a scenario of planetesimal formation: A successive development of multiple instabilities triggers planetesimal formation in resulting dusty rings..
出版日期Book 2022
关键词Disk Evoluation; Planet Formation in Protoplanetary Disks; Secular Gravitational Instability; Hydrodyna
版次1
doihttps://doi.org/10.1007/978-981-19-1765-3
isbn_softcover978-981-19-1767-7
isbn_ebook978-981-19-1765-3Series ISSN 2190-5053 Series E-ISSN 2190-5061
issn_series 2190-5053
copyrightThe Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Singapor
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Mariya Petrova,Seth J. Schwartzt radial drift. The contents of this chapter are based on our published paper: Tominaga et al. (2019), ApJ, 881, 53, DOI: 10.3847/1538-4357/ab25ea. Figures and some texts are reproduced in this thesis with permission from American Astronomical Society (©AAS)
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Introduction,ow in size through mutual sticking and form building blocks of planets called planetesimals. Further coalescence of planetesimals leads to formation of planets. However, it is known that there are some barriers against dust growth to planetesimals, and the formation process of planetesimals is still
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Numerical Simulations of Secular Instabilities,erstand subsequent planetesimal formation. Because of the slow growth of the instability, one has to use numerical methods that are less diffusive and avoid numerical errors as much as possible. Motivated by this, we first formulate Lagrange-cell method for long-term hydrodynamic simulations. Our me
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