VUV Spectroscopy of Astrophysical Ices Michael Davis
Introduction Experimental background Apparatus and techniques Results and spectra Discussion
Background Accretion of gas phase atoms and molecules A mantle of simple volatile molecules is formed, processed by UV/charged pratical irradiation An outer volatile mantle protects an inner organic mantle from irradiation Chemical explosions and other processes release molecules into the gas phase
Background Ion irradiation caused by Jupiter’s magnetosphere Ices exist in bulk Higher temperatures (~100K) than ISM (~10K)
Apparatus
Apparatus Designed to travel to irradiation sources CaF/MgF 2 substrate for IR/UV transmission Helium/nitrogen cryogens, achieves temperatures <20K Reaches base pressure mbar Ion gauge Rotary feed- through Sample mount Cryogen inlet
Apparatus Sample deposition Irradiation Detection methods FTIR SOURCE RF DEUTERIUM DISCHARGE LAMP (UV) DETECTOR FTIR Spectroscopy VUV Spectroscopy PMT SYNCHROTRON SOURCE ELECTRON GUN ION SOURCE SYNCHROTRON
Experiments VUV spectroscopy undertaken at: ISA Storage Ring, University of Aarhus SRS, Daresbury Laboratory Most recent beam-times September 2004 (ISA) and December 2004 (SRS) Looking at simple ices (NH 3, CO, CO 2 ) and mixtures with water Depositions at different speeds and temperatures
Experiments Why use VUV spectroscopy? Complements FTIR studies Highlight differences between gas and solid phase VUV data Knowing electronic transitions allows to know the effects of irradiation by UV discharge lamp
Experiments Presenting NH 3 and NH 3 /H 2 O results Depositing at 25K, 75K, 85K and 95K Annealing up to 120K Depositing ~0.2µm in <2 minutes and ~30 minutes Mixtures at 9:1, 1:1 and 1:3 ratios
Deposition speed In ammonia, no difference in curve features Absorbance is increased Other molecules show drastic changes
Temperature Effects Annealing from 20K to >75K shifts the main peak and adds another feature Depositing at 95K has a similar effect, but more pronounced 194nm
Temperature Effects Depositing at ~75K-85K causes major changes New features seen, existing features modified 194nm
Temperature Effects Some features enhanced or decreased No major changes to curve shape Completely different result than annealing the 20K sample
NH 3 :H 2 O Mixtures Adding small amounts of water to the ammonia does not change the spectra significantly No water features visible
NH 3 :H 2 O Mixtures Additional H 2 O suppresses the crystal structure Some H 2 O remains after NH 3 has been desorbed No significant annealing effects
Summary Outline of experimental techniques and apparatus Deposition speed has little effect in NH 3 Deposition temperature has a major effect in NH 3 Annealing has some effect on spectra Sample is not strongly affected by water “impurities”
Acknowledgements Prof. Nigel Mason Dr Anita Dawes Dr Robin Mukerji Philip Holtom Bhalamurugan Sivaraman Sarah Webb David Shaw (SRS) The Open University EPSRC PPARC