Real-Life Death Stars: Measuring Rocks on Alien Planets by Tearing Them Apart JJ Hermes Hubble Fellow University of North Carolina at Chapel Hill jjhermes.web.unc.edu
My History: The University of Texas at Austin • Undergrad in Physics & Astronomy, 2002-2007 • Ph.D. in Astronomy, 2008-2013 • I have spent >220 nights at McDonald Observatory
My History: The University of Warwick • I did my first Postdoctoral Research Fellowship in England – There I learned to include a ‘u’ in words like colour • Astronomers tend to have postdoc appointments for 2-7(!) years before settling in at a faculty job teaching at a university William Herschel Telescope, Canary Islands, Spain
My History: The University of North Carolina • Currently I am a Hubble Fellow at the University of North Carolina at Chapel Hill, another postdoctoral research job
Under Gravity, Heaviest Elements Sink Sharyn Morrow A ‘Typical’ White Dwarf Carbon/Oxygen Core (r = 8500 km) Helium Layer (260 km) Outer Hydrogen Layer (30 km)
1. Take a solar system. There are likely billions in our Galaxy. 2. As the host star evolves, the orbits of planets expand. Some may scatter and collide. 3. Ancient solar systems have leftover debris. We can see it if it gets close to a white dwarf.
Oxygen Excess: Water-Rich Material! Rocks = MgO, Al2 O3 , SiO2 , CaO, TiO2 , Cr2 O3 , MnO, FeO, Fe2 O3 , ... Anything Else = CO2 , H2 O Farihi et al. 2013; Raddi et al. 2015 Very little Carbon, so excess Oxygen likely H2 O! White Dwarf GD 61 Two specific white dwarfs have rocks, maybe worlds, that are roughly 25-40% water!
Billions of planets likely exist in the Galaxy “The Search for Life Beyond Earth…” Many of these planets are rocky, like Earth Using ancient stars, we can learn that these alien rocks are composed of the same material as Earth… including water!