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VUV Spectroscopy of VUV Spectroscopy of Astrophysical Ices Astrophysical Ices Michael Davis Michael Davis

VUV Spectroscopy of Astrophysical Ices Michael Davis

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Page 1: VUV Spectroscopy of Astrophysical Ices Michael Davis

VUV Spectroscopy of VUV Spectroscopy of Astrophysical IcesAstrophysical Ices

Michael DavisMichael Davis

Page 2: VUV Spectroscopy of Astrophysical Ices Michael Davis

IntroductionIntroduction

Experimental backgroundExperimental background Apparatus and techniquesApparatus and techniques Results and spectraResults and spectra DiscussionDiscussion

Page 3: VUV Spectroscopy of Astrophysical Ices Michael Davis

BackgroundBackground

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

Page 4: VUV Spectroscopy of Astrophysical Ices Michael Davis

BackgroundBackground

Ion irradiation Ion irradiation caused by Jupiter’s caused by Jupiter’s magnetospheremagnetosphere

Ices exist in bulkIces exist in bulk Higher temperatures Higher temperatures

(~100K) than ISM (~100K) than ISM (~10K)(~10K)

Page 5: VUV Spectroscopy of Astrophysical Ices Michael Davis

ApparatusApparatus

Page 6: VUV Spectroscopy of Astrophysical Ices Michael Davis

ApparatusApparatus

Designed to travel to Designed to travel to irradiation sourcesirradiation sources

CaF/MgFCaF/MgF22 substrate substrate

for IR/UV for IR/UV transmissiontransmission

Helium/nitrogen Helium/nitrogen cryogens, achieves cryogens, achieves temperatures <20Ktemperatures <20K

Reaches base Reaches base pressure 10pressure 10-8-8mbarmbar

Ion gauge

Rotary feed-through

Sample mount

Cryogen inlet

Page 7: VUV Spectroscopy of Astrophysical Ices Michael Davis

ApparatusApparatus

Sample deposition

Irradiation

Detection methods

FT

IR

SO

UR

CE

RF DEUTERIUM DISCHARGE

LAMP (UV)

DE

TE

CT

OR

FTIR Spectroscopy

VUV Spectroscopy

PMTSYNCHROTRON

SOURCE

ELECTRON GUN

ION

SO

UR

CE

SY

NC

HR

OT

RO

N

Page 8: VUV Spectroscopy of Astrophysical Ices Michael Davis

ExperimentsExperiments

VUV spectroscopy undertaken at:VUV spectroscopy undertaken at: ISA Storage Ring, University of AarhusISA Storage Ring, University of Aarhus SRS, Daresbury LaboratorySRS, Daresbury Laboratory

Most recent beam-times September 2004 Most recent beam-times September 2004 (ISA) and December 2004 (SRS)(ISA) and December 2004 (SRS)

Looking at simple ices (NHLooking at simple ices (NH33, CO, CO, CO, CO22) )

and mixtures with waterand mixtures with water Depositions at different speeds and Depositions at different speeds and

temperaturestemperatures

Page 9: VUV Spectroscopy of Astrophysical Ices Michael Davis

ExperimentsExperiments

Why use VUV spectroscopy?Why use VUV spectroscopy? Complements FTIR studiesComplements FTIR studies Highlight differences between gas and solid Highlight differences between gas and solid

phase VUV dataphase VUV data Knowing electronic transitions allows to Knowing electronic transitions allows to

know the effects of irradiation by UV know the effects of irradiation by UV discharge lamp discharge lamp

Page 10: VUV Spectroscopy of Astrophysical Ices Michael Davis

ExperimentsExperiments

Presenting NHPresenting NH33 and NH and NH33/H/H22O resultsO results

Depositing at 25K, 75K, 85K and 95KDepositing at 25K, 75K, 85K and 95K Annealing up to 120KAnnealing up to 120K Depositing ~0.2µm in <2 minutes and Depositing ~0.2µm in <2 minutes and

~30 minutes~30 minutes Mixtures at 9:1, 1:1 and 1:3 ratiosMixtures at 9:1, 1:1 and 1:3 ratios

Page 11: VUV Spectroscopy of Astrophysical Ices Michael Davis

Deposition speedDeposition speed

In ammonia, no In ammonia, no difference in curve difference in curve featuresfeatures

Absorbance is Absorbance is increasedincreased

Other molecules Other molecules show drastic show drastic changeschanges

0

0.5

1.0

1.5

2.0

2.5

140 160 180 200 220

NH3 deposited at 20K in 93s

NH3 deposited at 20K in 1760s

Wavelength (nm)

Ab

sorb

an

ce

Page 12: VUV Spectroscopy of Astrophysical Ices Michael Davis

Temperature EffectsTemperature Effects

Annealing from Annealing from 20K to >75K shifts 20K to >75K shifts the main peak and the main peak and adds another adds another featurefeature

Depositing at 95K Depositing at 95K has a similar has a similar effect, but more effect, but more pronouncedpronounced 0

1

2

3

140 160 180 200

NH3 dep. at 20K

NH3 ann. at 110K

NH3 dep. at 95K

Wavelength (nm)

Ab

sorb

an

ce

194nm

Page 13: VUV Spectroscopy of Astrophysical Ices Michael Davis

Temperature EffectsTemperature Effects

Depositing at Depositing at ~75K-85K causes ~75K-85K causes major changesmajor changes

New features New features seen, existing seen, existing features modifiedfeatures modified

0

1

2

3

140 160 180 200

NH3 dep. at 20K

NH3 dep. at 72.5K

NH3 dep. at 87K

NH3 dep. at 95K

Wavelength (nm)

Ab

sorb

an

ce

194nm

Page 14: VUV Spectroscopy of Astrophysical Ices Michael Davis

Temperature EffectsTemperature Effects

Some features Some features enhanced or enhanced or decreaseddecreased

No major changes No major changes to curve shapeto curve shape

Completely Completely different result different result than annealing the than annealing the 20K sample20K sample 0

0.5

1.0

1.5

2.0

2.5

140 160 180 200

NH3 dep. at 72.5K

NH3 ann. at 118K

Wavelength (nm)

Ab

sorb

an

ce

Page 15: VUV Spectroscopy of Astrophysical Ices Michael Davis

NHNH33:H:H22O MixturesO Mixtures

Adding small Adding small amounts of water amounts of water to the ammonia to the ammonia does not change does not change the spectra the spectra significantlysignificantly

No water features No water features visiblevisible

0

0.5

1.0

1.5

2.0

2.5

140 160 180 200

NH3 dep. at 20K

NH3:H

2O 10:1 dep. at 28K

NH3 dep. at 72.5K

NH3:H

2O 9:1 dep. at 72K

Wavelength (nm)

Ab

sorb

an

ce

Page 16: VUV Spectroscopy of Astrophysical Ices Michael Davis

NHNH33:H:H22O MixturesO Mixtures

Additional HAdditional H22O O

suppresses the suppresses the crystal structurecrystal structure

Some HSome H22O remains O remains

after NHafter NH33 has been has been

desorbeddesorbed No significant No significant

annealing effectsannealing effects0

1

2

3

140 160 180 200

NH3 dep. at 72.5K

NH3:H

2O 1:1 dep. at 72K

NH3:H

2O 1:3 dep. at 77K

NH3:H

2O 1:3 ann. at 150K

H2O dep.at 25K

Wavelength (nm)

Ab

sorb

an

ce

Page 17: VUV Spectroscopy of Astrophysical Ices Michael Davis

SummarySummary

Outline of experimental techniques and Outline of experimental techniques and apparatusapparatus

Deposition speed has little effect in NHDeposition speed has little effect in NH33

Deposition temperature has a major Deposition temperature has a major effect in NHeffect in NH33

Annealing has some effect on spectraAnnealing has some effect on spectra Sample is not strongly affected by water Sample is not strongly affected by water

“impurities”“impurities”

Page 18: VUV Spectroscopy of Astrophysical Ices Michael Davis

AcknowledgementsAcknowledgements

Prof. Nigel MasonProf. Nigel Mason Dr Anita DawesDr Anita Dawes Dr Robin MukerjiDr Robin Mukerji Philip HoltomPhilip Holtom Bhalamurugan SivaramanBhalamurugan Sivaraman Sarah WebbSarah Webb David Shaw (SRS)David Shaw (SRS) The Open UniversityThe Open University EPSRCEPSRC PPARCPPARC