2015
DOI: 10.1016/j.nimb.2014.09.023
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Nondestructive assay of fluorine in geological and other materials by instrumental photon activation analysis with a microtron

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Cited by 14 publications
(4 citation statements)
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“…The red color map represents the normalized activation rate obtained for laser-driven sources. The isolines correspond to the normalized activation rate that can be obtained with some existing conventional accelerators for PAA (reported electron energies and currents from literature 68,71 ). The value of the normalized activation rate for each isoline is reported on the right side of the plot.…”
Section: Resultsmentioning
confidence: 99%
“…The red color map represents the normalized activation rate obtained for laser-driven sources. The isolines correspond to the normalized activation rate that can be obtained with some existing conventional accelerators for PAA (reported electron energies and currents from literature 68,71 ). The value of the normalized activation rate for each isoline is reported on the right side of the plot.…”
Section: Resultsmentioning
confidence: 99%
“…Experimental details including the list of determinable elements and associated uncertainties have been described in Řanda et al (2007) or Mizera and Řanda (2010). Fluorine was determined using a non-destructive IPAA method described in Krausová et al (2015). For the quality control of analytical data, the USGS AGV-1 (andesite) and USGS GSP-2 (granodiorite) reference rock materials were simultaneously analysed.…”
Section: Methodsmentioning
confidence: 99%
“…The electron beam energy (i.e. the maximum photon energy) was set at 17 MeV based on optimization carried out for fluorine assay , which utilizes a reaction with a similar threshold energy (cf. in Table ).…”
Section: Methodsmentioning
confidence: 99%