7Be, 10Be, and 36Cl in precipitation
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Cited by (42)
Atmospheric deposition of <sup>10</sup>Be in Altzomoni rainfall
2023, Nuclear Instruments and Methods in Physics Research, Section B: Beam Interactions with Materials and AtomsEarly Pleistocene uplift of the northeastern Tibetan Plateau: Evidence from the Dunhuang Basin, NW China
2020, Journal of Asian Earth SciencesMonthly record of the Cl and <sup>36</sup>Cl fallout rates in a deciduous forest ecosystem in NE France in 2012 and 2013
2016, Quaternary GeochronologyCitation Excerpt :Several studies have been dedicated to the spatial distribution of 36Cl in rainwaters at the scale of a country (Herut et al., 1992), and of a continent (USA: Bentley et al., 1986 and Europe: Johnston and McDermott, 2008) and even at the global scale (Scheffel et al., 1999). Only a few studies focused on 36Cl fallout rate monthly variations (USA: Hainsworth et al., 1994; Knies et al., 1994; Japan: Tosaki et al., 2012; and Spain: Santos et al., 2004). These studies highlighted 1- a latitudinal dependence of the 36Cl fallout rate, essentially linked to the stratosphere–troposphere mixing zone which is maximal at mid latitudes (between 30° and 60°) (Lal and Peters, 1967; Keywood et al., 1998) and 2- a seasonal variation of the 36Cl fallout rate due to an annual variation in the tropopause height.
Plutonium isotope measurements from across continental Australia
2013, Nuclear Instruments and Methods in Physics Research, Section B: Beam Interactions with Materials and AtomsCitation Excerpt :It is plausible that the more consistent rainfall in the south-east of Australia removes more of the fallout isotopes from the atmosphere because it falls year round, whereas in the north there is essentially no rainfall for 4 months of the year during the dry season, while the intense rains of the wet season rapidly remove any fallout isotopes that are present in the atmosphere at the time leaving little for subsequent rainfall. Such an effect has been reported by Knies et al. [25] who measured 10Be and 36Cl in the course of individual rainfall events and found significantly more isotope near the beginning of an event than at the end. In order to investigate this further, we are currently measuring other fallout nuclides in the samples, and making a more detailed assessment of regional fallout at the sites using annual fallout and rainfall records for each region.