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Webb and Spitzer spectra split 21 extreme debris disks into silica-rich and silica-poor groups

Kate Su's team combined Webb and Spitzer spectra to sort 21 extreme debris disks around young stars into silica-rich and silica-poor groups. NASA says the minerals encode how violent each dust-making collision was, a possible check on Moon-formation ideas.

The Scientist · Science desk

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Illustration accompanying Webb and Spitzer spectra split 21 extreme debris disks into silica-rich and silica-poor groups
Generated illustration

What happened

  • Webb observed 16 of the disks, 12 for the first time and four as follow-ups of Spitzer targets, while the other five came from archival Spitzer data.
  • Mid-infrared spectra confirmed three defining traits: grains smaller than in other disks, unusually high amounts of warm dust, and irregular changes in brightness.
  • Extreme debris disks, first picked out by the now-retired Spitzer telescope, hold large amounts of warm dust roughly where rocky planets orbit in our own solar system.
  • The study, led by Kate Su of the Space Science Institute in Boulder, Colorado, was published on October 1 in The Astrophysical Journal.

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Why it matters

  • capability If silica content does track impact violence, one mid-infrared spectrum could rank collisions in young systems against each other and give Moon-formation models present-day cases to compare with.
  • constraint With 21 disks divided between two mineral groups, any scale tying silica to impact energy will rest on few systems per group until more extreme disks turn up.
  • contradiction Models expect the extreme-debris phase to be relatively common while observations find it around about 1% of young stars, and any claim that the solar system went through it inherits that mismatch.

The sorting depends on mineralogy read from mid-infrared spectra [3][4]. On Earth, volcanic glass such as obsidian is silica-rich. Forsterite, the silica-poor mineral, turns up as green sand on some Hawaiian beaches [5]. "To just see their mid-infrared emission and beautiful spectral features with Webb, which allowed us to identify their compositions, was the most exciting thing for me," said Agnes Kospal of Konkoly Observatory in Budapest, a coauthor [14].

According to NASA's release, whether a disk is rich or poor in silica "can reveal important information about the collision that created its debris." The release adds that the difference may help explain why some disks swing more widely in infrared brightness than others [6]. It also says researchers can use these systems to estimate how energetic the collisions were [16]. The available text of the release does not say which group marks the harder impacts, or how the team arrived at the "Mars-sized worlds" in NASA's headline [15].

A Moon test would depend on exactly that step. The leading account of the Moon's origin has a Mars-sized body called Theia hitting the young Earth. That impact likely vaporized huge quantities of rock, and some of the debris later came together as the Moon [10]. Our own solar system may have passed through an extreme-debris phase too [9]. In my view, a young disk tells us something about Theia-style impacts only once its silica content has been tied to an impact energy and an impactor size. What the paper delivers, as NASA describes it, is the sorted sample that such a calibration would start from [1][4].

The work is the first sizeable sample of this class, and Su compares it with the familiar cold debris disks. "This is the first time we have gathered enough systems to truly understand this subclass that we call extreme debris disks," said Su, the paper's lead author [12]. "Before Webb, we had limited information," she said. "We knew that they are weird and very different from the typical cold debris disks that we know, like Vega and Fomalhaut. Now that we have more data, we can pin down what these disks represent for planet formation and evolution." [13]

What to watch

  • Whether the full Astrophysical Journal paper says which mineral group marks the more energetic impacts and puts impactor sizes on individual systems.
  • Repeat Webb observations of the most variable disks, to see whether silica content tracks how strongly their infrared brightness fluctuates.
  • New surveys of young stars that test whether the roughly 1% occurrence rate holds or rises toward what models predict.
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