The long-lived radionuclide 182Hf (t1/2=9.0Ma [1]) is one of a number of candidates for the detection of a supernova isotope signature [2]. The most suitable site for detecting such a signature would be a deep-sea sediment of slow deposition rate. Both the expected amount of 182Hf and the 182Hf/Hf isotope ratio are very low, and hence the highest possible detection efficiency and effective separation from the stable isobar 182W are crucial requirements.
A suppression factor of ~6000 for 182W relative to 182Hf is achieved by injecting the HfF5- ion [3]. Even with optimum chemistry, however, the 182W counting rate limits the sensitivity to 182Hf/Hf ratios of ≥10-11 [3]. This detection limit is substantially above the value expected for the supernova signal. Hence, an isobar separation in the detector is required.
We have investigated techniques of isobar separation that can be used on the ANU 14UD tandem. The energies available do not allow for effective separation using either multiple energy-loss measurements in an ionization chamber or a gas-filled magnet. A number of other methods have been explored. Amongst these were projectile x-ray AMS (PXAMS) and the use of the differences in energy loss of 182Hf and 182W ions in a degrading foil measured via the residual energy in a subsequent ionization chamber. Data will be presented for both methods, and their potential and limitations for detecting a supernova signature in a typical deep sea sediment core will be discussed.
[1] C. Vockenhuber, F. Oberli, M. Bichler, I. Ahmad, G. Quitté, M. Meier, A. N. Halliday, D.-C. Lee, W. Kutschera, P. Steier, R. J. Gehrke, and R. G. Helmer. Phys. Rev. Lett. 93 (2004), 2501.
[2] J. Ellis, B.D. Fields, D.N. Schramm. ApJ 470 (1996), 1227.
[3] C. Vockenhuber, M. Bichler, R. Golser, W. Kutschera, V. Liechtenstein, A. Priller, P. Steier, S. Winkler. Nucl. Inst. And Meth. in Phys. Res. B 223-224 (2004), 823.
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