Australian Facility For Noble-Gas Radio Isotope Measurements Using Atom Trap Trace Analysis Philip S. Light , Robert Sang, Axel Suckow, Pere Masque, Dioni Cendon, Bear McPhail, Mike Hotchkis, Stephen Eggins and Andre N. Luiten 16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS – INPC 2016 1 This facility is supported under Australian Research Council's Linkage Infrastructure, Equipment and Facilities scheme (project LE160100025)
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Australian Facility For Noble-Gas Radio Isotope ......16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS –INPC 2016 10 Yang, G.M. et al. Analysis of
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Australian Facility For Noble-Gas Radio Isotope Measurements Using Atom Trap Trace Analysis Philip S. Light, Robert Sang, Axel Suckow, Pere Masque, Dioni Cendon,Bear McPhail, Mike Hotchkis, Stephen Eggins and Andre N. Luiten
16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS – INPC 2016 1
This facility is supported under Australian Research Council'sLinkage Infrastructure, Equipment and Facilities scheme (project LE160100025)
Australian Facility For Noble-Gas Radio Isotope Measurements
A new facility for fast and accurate measurements of noble gas radio-nuclide ratios81Kr/Kr, 85Kr/Kr, 39Ar/Ar
16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS – INPC 2016 2
Noble Gas Radio-Isotope Tracers◦ Environmental markers to study ground and ocean water movement
1 10 100 1000 10000 100000 1000000
Groundwater Age / Years
4He (estimates)
40ArT/3He ratio
CFC/SF6
81Kr τ1/2 = 229,000 years85Kr τ1/2 = 10.8 years 39Ar τ1/2 = 269 years
14C τ1/2 = 5730 years
36ClD,18O
16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS – INPC 2016 3
Noble Gas Radio-Isotope Tracers◦ Application to water dating:◦ 39Ar, 81Kr, 85Kr† are cosmogenic nuclides
◦ Nearly ideal physical & chemical characteristics (e.g. unreactive)
◦ Well defined input function at water/atmosphere interface
†85Kr atmospheric concentration is primarily dueto nuclear fuel reprocessingPicture credit: Axel Suckow, CSIRO
16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS – INPC 2016 4
Noble Gas Radio-Isotope Tracers◦ Application to water dating:◦ 39Ar, 81Kr, 85Kr† are cosmogenic nuclides
◦ Nearly ideal physical & chemical characteristics (e.g. unreactive)
◦ Well defined input function at water/atmosphere interface
†85Kr atmospheric concentration is primarily dueto nuclear fuel reprocessingPicture credit: Axel Suckow, CSIRO
16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS – INPC 2016 5
Noble Gas Radio-Isotope Tracers◦ Application to water dating:◦ 39Ar, 81Kr, 85Kr† are cosmogenic nuclides
◦ Nearly ideal physical & chemical characteristics (e.g. unreactive)
◦ Well defined input function at water/atmosphere interface
◦ Rarely used due measurement difficulty
†85Kr atmospheric concentration is primarily dueto nuclear fuel reprocessingPicture credit: Axel Suckow, CSIRO
16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS – INPC 2016 6
Noble Gas Radio-Isotope Tracers◦ Environmental markers to study ground and ocean water movement
1 10 100 1000 10000 100000 1000000
Groundwater Age / Years
4He (estimates)
40ArT/3He ratio
CFC/SF6
81Kr τ1/2 = 229,000 years85Kr τ1/2 = 10.8 years 39Ar τ1/2 = 269 years
14C τ1/2 = 5730 years
36ClD,18O
Noble-gas mass spectrometry
Gas chromatography
Radiometry
Accelerator mass spectrometry
Atom trap trace analysis
16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS – INPC 2016 7
Radio-Isotope Measurements◦ Measurements difficult due to small atmospheric abundance:◦ 85Kr/Kr: 2x10-11 81Kr/Kr: 5.2x10-13 39Ar/Ar: 8x10-16
◦ 1L of surface water contains just ~9000 39Ar atoms & ~1500 81Kr atoms
◦ Need to measure ratio to ~1% of atmospheric abundance in water dating applications
◦ Low-level decay counting (LLC) is traditional measurement technique◦ Large water samples required (2000-5000 litres for 39Ar)
◦ Long measurement times (8-60 days for 39Ar)
◦ Performed where a low background count is present◦ e.g. University of Bern, 35m below ground
16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS – INPC 2016 8
Atom Trap Trace Analysis (ATTA)◦ Laser-based technique for measuring noble-gas radio-isotope ratios
◦ Atom-counting rather than decay-counting ➠ smaller samples, faster measurement
◦ Lasers used to cool specific isotope andhold in a magneto-optical trap
◦ Shifts in energy levels between isotopespermit selection of a single isotopeby tuning laser frequencies
16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS – INPC 2016 9
Rohan Glover, PhD Thesis, Griffith University
Atom Trap Trace Analysis◦ Based on established laser cooling and magneto-optical trapping
16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS – INPC 2016 10
Yang, G.M. et al. Analysis of 85Kr: a comparison at the 10-14 levelusing micro-liter samples. Sci. Rep. 3, 1596; DOI:10.1038/srep01596 (2013).
Atom Trap Trace Analysis◦ Current ATTA systems worldwide:◦ Argonne National Laboratory, IL, USA◦ Predominantly focussed on Kr measurements
◦ Only facility currently open for general samples
◦ Throughput ~100 samples / year
◦ University of Heidelberg, Germany◦ Initial 39Ar measurements demonstrated
◦ University of Science and Technology of China, Hefei, China◦ Developing Kr capability
16th September 2016 AUSTRALIAN FACILITY FOR NOBLE-GAS RADIO ISOTOPE MEASUREMENTS – INPC 2016 11
Performance
39Ar 81Kr Totalml-STP Water / L Time µl-STP Water / L Time Samples / yr