2005
DOI: 10.1039/b509726f
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Preparation and certification of synthetic uranium isotope mixtures with 236U/238U ratios of 10–6, 10–7, 10–8

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Cited by 15 publications
(15 citation statements)
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“…A similar spread was also detected in the CCQM-P48, a pilot study organised by IRMM on behalf of the Comité Consultatif pour la Quantité de Matière (CCQM) [26]. On the other hand, measurements performed with TIMS in synthetic isotope mixtures in the ratios of 10 −4 to 10 −8 showed excellent agreement with the prepared values [27]. This shows that reliable measurements can be carried out even at these low values.…”
Section: Measurement Of Uranium Minor Isotope Amount Ratiossupporting
confidence: 73%
“…A similar spread was also detected in the CCQM-P48, a pilot study organised by IRMM on behalf of the Comité Consultatif pour la Quantité de Matière (CCQM) [26]. On the other hand, measurements performed with TIMS in synthetic isotope mixtures in the ratios of 10 −4 to 10 −8 showed excellent agreement with the prepared values [27]. This shows that reliable measurements can be carried out even at these low values.…”
Section: Measurement Of Uranium Minor Isotope Amount Ratiossupporting
confidence: 73%
“…For isotope ratio measurements, systematic biases due to matrix effects are well documented in literature [2]. TIMS measurements are less susceptible to such biases and therefore have been more widely applied to certification measurements of isotopic CRMs [3][4][5][6][7][8]. Most commonly used TIMS analytical methods are total evaporation (TE), modified total evaporation (MTE), and conventional analyses.…”
Section: Introductionmentioning
confidence: 99%
“…Les TIMS atteignent des valeurs de rapport de masse 236 U/ 238 U de l'ordre de 10 -8 (Richter et al, 2005) et jusqu'à 2 × 10 -10 , sous certaines conditions (Boulyga et Heumann, 2006 (Boulyga et Heumann, 2006 ;Steier et al, 2008). C'est actuellement la seule technique de spectrométrie de masse qui permet de mesurer les rapports 236 U/ 238 U au niveau du bruit de fond naturel (Quinto et al, 2009 Bien que les concentrations en uranium varient fortement dans les roches, terme source de l'uranium présent naturellement dans la biosphère (Gascoyne, 1992), on considère les roches suffisamment anciennes (> 1 Ma) comme des systèmes « clos » c'est-à-dire que 238 U (tête de chaîne) présente une activité égale à celle de ses descendants (notamment 234 U) (Fig.…”
Section: Les Techniques De Mesure Des Isotopes De L'uraniumunclassified