ELEMENTAL COMPOSITIONS OF TWO EXTRASOLAR ROCKY PLANETESIMALS

被引:116
作者
Xu, S. [1 ]
Jura, M. [1 ]
Koester, D. [2 ]
Klein, B. [1 ]
Zuckerman, B. [1 ]
机构
[1] Univ Calif Los Angeles, Dept Phys & Astron, Los Angeles, CA 90095 USA
[2] Univ Kiel, Inst Theoret Phys & Astrophys, D-24098 Kiel, Germany
基金
美国国家科学基金会;
关键词
planetary systems; stars: abundances; white dwarfs; LOCAL INTERSTELLAR-MEDIUM; DBZ WHITE-DWARF; PLANETARY SYSTEMS; ECHELLE SPECTROGRAPH; CHEMICAL-COMPOSITION; SPECTROSCOPIC SURVEY; DEBRIS DISKS; ACCRETION; RICH; WATER;
D O I
10.1088/0004-637X/783/2/79
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We report Keck/HIRES and Hubble Space Telescope/COS spectroscopic studies of extrasolar rocky planetesimals accreted onto two hydrogen atmosphere white dwarfs, G29-38 and GD 133. In G29-38, eight elements are detected, including C, O, Mg, Si, Ca, Ti, Cr, and Fe while in GD 133, O, Si, Ca, and marginally Mg are seen. These two extrasolar planetesimals show a pattern of refractory enhancement and volatile depletion. For G29-38, the observed composition can be best interpreted as a blend of a chondritic object with some refractory-rich material, a result from post-nebular processing. Water is very depleted in the parent body accreted onto G29-38, based on the derived oxygen abundance. The inferred total mass accretion rate in GD 133 is the lowest of all known dusty white dwarfs, possibly due to non-steady state accretion. We continue to find that a variety of extrasolar planetesimals all resemble to zeroth order the elemental composition of bulk Earth.
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页数:16
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