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New developments in Ion-Laser InterAction Mass Spectrometry

PN-3
23 Oct 2024, 08:30
40m
GRAND BALLROOM (宴会厅), 2nd Floor

GRAND BALLROOM (宴会厅), 2nd Floor

GULIN BRAVO HOTEL (桂林宾馆),14 Ronghu Road, Guilin, 541002, China
Oral Presentation RFQ Ion Cooler Techniques Plenary

Speaker

Martin Martschini (University of Vienna - Faculty of Physics)

Description

Interferences from isobars typically restrict the applicability of AMS to selected long-lived radionuclides. The novel Ion-Laser InterAction Mass Spectrometry (ILIAMS) technique at the Vienna Environmental Research Accelerator (VERA) can overcome this limitation in many cases by highly-efficient isobar removal at eV-energies in a gas-filled radiofrequency quadrupole. The virtually complete suppression of isobars serves two objectives: A great number of nuclides can be measured for the first time with AMS while others become accessible at environmental levels – even on low terminal voltage AMS-systems – with the benefit of unprecedented detection efficiencies and blank values. This opens exciting possibilities in environmental radioactivity ($^\text{90}$Sr, $^\text{99}$Tc, $^\text{135,137}$Cs), astrophysics ($^\text{44}$Ti, $^\text{53}$Mn, $^\text{182}$Hf), and Earth science ($^\text{26}$Al, $^\text{36}$Cl, $^\text{41}$Ca) research. [1] At AMS-15, we have reported on the excellent performance of ILIAMS for $^\text{26}$Al and $^\text{36}$Cl. Here we highlight the recent developments for the technique across the entire nuclear chart.
ILIAMS exploits differences in detachment energies (DE) within elemental or molecular isobaric systems by neutralizing anions with DEs smaller than the photon energy via laser photodetachment. In addition, molecular interactions with a buffer gas can further enhance isobar suppression, e.g., via breakup of $^\text{41}$KF$_{\text{3}}^-$ into $^\text{41}$KF$_{\text{2}}^−$ and F, or via O-pickup of $^\text{182}$WF$_{\text{5}}^−$ forming $^\text{182}$WF$_{\text{5}}$O$_{\text{x}}^-$.
With at least eleven orders of magnitude suppression of both Mg and K, ILIAMS-assisted AMS enables the detection of $^\text{26}$Al/$^\text{27}$Al (~10$^{-10}$, extraction of AlO$^-$) and $^\text{41}$Ca/$^\text{40}$Ca (10$^{-11}$−10$^{-13}$ extraction of CaF$_{\text{3}}^-$) directly from crushed stony meteorites containing intrinsic ~1% Al and Ca, respectively [2,3]. The presence of isobars originating from the natively abundant elements (13-20% Mg, ~1‰ K) does not cause any analysis problems making radiochemical separation redundant. Measurements of $^\text{41}$Ca in chemically untreated concrete from nuclear decommissioning and coral sand samples clearly demonstrate the huge potential of this newly-established instrumental AMS (IAMS) technique. It is opening routes to high-sample throughput analysis, reasonable and fast provenance checks for (extra-)terrestrial origin and nuclear clearance.
At the upper end of the nuclear chart, the laser-induced suppression of U during measurements of Np constitutes the first non-chemical isobar discrimination in AMS in the actinide region.
Finally, for $^{\text{90}}$Sr, highly efficient ILIAMS-suppression of the isobaric interference $^{\text{90}}$Zr enables a blank value of $^{\text{90}}$Sr/Sr < 5$\times$10$^{-16}$ at an overall Sr-detection efficiency of 4$\times$10$^{-4}$. This corresponds to a detection limit of <0.016$\,$mBq, i.e., 2$\times$10$^{\text{4}}$ atoms or 3$\,$ag of $^{\text{90}}$Sr in a sample of mg of stable Sr – at least a factor 100 better than any other known technique of measurement. Recently, we have successfully demonstrated the tremendous potential of this technique for $^{\text{90}}$Sr in the measurement of contemporary coral aragonite and seawater samples of less than 500$\,$ml, and the analysis of $^\text{90}$Sr concentration in small samples of soils and other environmental archives after adding Sr carrier.
Ackn.: This project received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement No 101008324 (ChETEC-INFRA) and No 824096 (RADIATE), and grants from the Austrian Science Fund (FWF): I 4803-N and P 31614-N28. (Extra-)terrestrial samples were kindly provided by A. Bischoff (U Muenster), A. Gaertner & K. Schniebs (Senckenberg Dresden), Forst- und Landwirtschaftsbetrieb der Stadt Wien, K. Pachnerová Brabcová (Czech Academy of Science, Prague).
References: [1] Martschini et al., Radiocarbon 64 (3) (2022) 555. [2] Bischoff et al., accepted for Meteorit. Planet. Sci.. [3] Bischoff et al., submitted to Meteorit. Planet. Sci..

Student Submission No

Primary authors

Martin Martschini (University of Vienna - Faculty of Physics) Dr Silke Merchel (University of Vienna – Faculty of Physics, Isotope Physics, Vienna, Austria) Prof. Karin Hain (University of Vienna – Faculty of Physics, Isotope Physics, Vienna, Austria) Dr Laura Frost (JEN Juelicher Entsorgungsgesellschaft für Nuklearanlagen mbH) Mr Oscar Marchhart (University of Vienna – Faculty of Physics, Isotope Physics, Vienna, Austria) Prof. Peter Steier (University of Vienna – Faculty of Physics, Isotope Physics, Vienna, Austria) Mr Alexander Wieser (University of Vienna – Faculty of Physics, Isotope Physics, Vienna, Austria) Mr Andreas Wiederin (University of Vienna – Faculty of Physics, Isotope Physics, Vienna, Austria) Stephan Winkler (Helmholtz-Zentrum Dresden-Rossendorf) Robin Golser (University of Vienna, Faculty of Physics, Isotope Physics, Vienna, Austria)

Presentation materials