Takeout and Delivery: Erasing the Dusty Signature of Late-stage Terrestrial Planet Formation

被引:2
|
作者
Najita, Joan R. [1 ]
Kenyon, Scott J. [2 ]
机构
[1] NSFs NOIRLab, 950 N Cherry Ave, Tucson, AZ 85719 USA
[2] Smithsonian Astrophys Observ, 60 Garden St, Cambridge, MA 02138 USA
来源
ASTROPHYSICAL JOURNAL | 2023年 / 944卷 / 02期
关键词
WARM DEBRIS DISKS; POWERED MASS-LOSS; T-TAURI STARS; RADIATION HYDRODYNAMICS SIMULATIONS; SPECTRAL ENERGY-DISTRIBUTIONS; INNER SOLAR-SYSTEM; GIANT IMPACTS; CIRCUMSTELLAR DISKS; RADIUS DISTRIBUTION; SIZE DISTRIBUTIONS;
D O I
10.3847/1538-4357/acac8f
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The formation of planets like Earth is expected to conclude with a series of late-stage giant impacts that generate warm dusty debris, the most anticipated visible signpost of terrestrial planet formation in progress. While there is now evidence that Earth-sized terrestrial planets orbit a significant fraction of solar-type stars, the anticipated dusty debris signature of their formation is rarely detected. Here we discuss several ways in which our current ideas about terrestrial planet formation imply transport mechanisms capable of erasing the anticipated debris signature. A tenuous gas disk may be regenerated via takeout (i.e., the liberation of planetary atmospheres in giant impacts) or delivery (i.e., by asteroids and comets flung into the terrestrial planet region) at a level sufficient to remove the warm debris. The powerful stellar wind from a young star can also act, its delivered wind momentum producing a drag that removes warm debris. If such processes are efficient, terrestrial planets may assemble inconspicuously, with little publicity and hoopla accompanying their birth. Alternatively, the rarity of warm excesses may imply that terrestrial planets typically form very early, emerging fully formed from the nebular phase without undergoing late-stage giant impacts. In either case, the observable signposts of terrestrial planet formation appear more challenging to detect than previously assumed. We discuss observational tests of these ideas.
引用
收藏
页数:13
相关论文
共 50 条
  • [41] Late-stage intrusive activity at Olympus Mons, Mars: Summit inflation and giant dike formation
    Mouginis-Mark, Peter J.
    Wilson, Lionel
    ICARUS, 2019, 319 : 459 - 469
  • [42] Transition-Metal-Free Amine Oxidation: A Chemoselective Strategy for the Late-Stage Formation of Lactams
    Griffiths, Robert J.
    Burley, Glenn A.
    Talbot, Eric P. A.
    ORGANIC LETTERS, 2017, 19 (04) : 870 - 873
  • [43] Diversity of planetary systems in low-mass disks Terrestrial-type planet formation and water delivery
    Ronco, M. P.
    de Elia, G. C.
    ASTRONOMY & ASTROPHYSICS, 2014, 567
  • [45] AN IMPROVED METHOD FOR MICRORNA-SEQUENCING ANALYSIS IDENTIFIES A SIGNATURE OF CIRCULATING MICRORNAS IN LATE-STAGE RADIOGRAPHIC KNEE OSTEOARTHRITIS
    Ali, S. A.
    Loveless, I.
    Datta, I.
    Potla, P.
    OSTEOARTHRITIS AND CARTILAGE, 2021, 29 : S311 - S312
  • [46] Radiomic signature accurately predicts the risk of metastatic dissemination in late-stage non-small cell lung cancer
    Wilk, Agata Malgorzata
    Kozlowska, Emilia
    Borys, Damian
    D'Amico, Andrea
    Fujarewicz, Krzysztof
    Gorczewska, Izabela
    Debosz-Suwinska, Iwona
    Suwinski, Rafal
    Smieja, Jaroslaw
    Swierniak, Andrzej
    TRANSLATIONAL LUNG CANCER RESEARCH, 2023, 12 (07) : 1372 - 1383
  • [47] Selective Late-Stage Sulfonyl Chloride Formation from Sulfonamides Enabled by Pyry-BF4
    Gomez-Palomino, Alejandro
    Cornella, Josep
    ANGEWANDTE CHEMIE-INTERNATIONAL EDITION, 2019, 58 (50) : 18235 - 18239
  • [48] Direct formation of aromatics from biopolymers during late-stage, high-severity pyrolysis.
    Evans, RJ
    Looker, MJ
    Nimlos, MN
    ABSTRACTS OF PAPERS OF THE AMERICAN CHEMICAL SOCIETY, 2002, 223 : U588 - U588
  • [49] Formation of K-feldspar megacrysts in granodioritic plutons by thermal cycling and late-stage textural coarsening
    Johnson, Breck R.
    Glazner, Allen F.
    CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 2010, 159 (05) : 599 - 619
  • [50] Formation of K-feldspar megacrysts in granodioritic plutons by thermal cycling and late-stage textural coarsening
    Breck R. Johnson
    Allen F. Glazner
    Contributions to Mineralogy and Petrology, 2010, 159 : 599 - 619