By Paul Tomascak, Tomáš Magna, Ralf Dohmen
This paintings summarizes the old development of the sphere of lithium (Li) isotope reviews and offers a finished but succinct evaluation of the study functions towards which they've been directed. In synthesizing the old and present study, the quantity additionally indicates potential destiny instructions of analysis. no longer even an entire decade has handed because the book of a generally inclusive precis of Li isotope learn all over the world (Tomascak, 2004). during this couple of minutes, using this isotope process within the research of geo- and cosmochemical questions has elevated dramatically, due, partially, to the appearance of recent analytical expertise on the finish of the final millennium. Lithium, as a mild aspect that types low-charge, moderate-sized ions, manifests a couple of chemical houses that make its good isotope approach invaluable in a wide range of geo- and cosmochemical examine fields.
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Extra resources for Advances in Lithium Isotope Geochemistry
However, no further investigations were made that considered these meteorite classes. Given the low abundances of Li in metal, consistent with its lithophile character, the possible implications for histories of the respective parent bodies of iron meteorites may be rather limited. 3 Cosmochemistry of Lithium in Planetary Bodies Comparatively little has so far been done in order to improve our understanding of the behavior of Li and its isotopes in non-terrestrial materials despite at least three decades of successful measurements of Li isotopic compositions and despite the importance of Li in stellar processes.
7 Li/6Li * 104; Hammache et al. 2010; Nollett et al. 1997; Vangioni-Flam et al. 2000, 1999). Most 6Li is produced by much more efﬁcient spallation-induced energetic collisions of GCR through p, α + He and CNO → 6Li, 7Li, and fast nuclei (α, C, O) fragmenting on H and He in the ISM (Vangioni-Flam et al. 1999). We refer to a detailed review by Prantzos (2012) for the history and physical processes of Li evolution. It is generally accepted that the combined reactions of energetic cosmic ray C–N–O nuclei, and cosmic ray H–He interacting with ambient interstellar C, N and O species produce low-energy Li, Be and B nuclei.
2001; Tajitsu et al. 2015). Contrary to the clear variability in 7Li production owing to three different mechanisms (BBN, GCR, stellar nucleosynthesis), 6Li is nearly solely produced by spallative interactions of GCR with ISM. A very subordinate proportion of 6Li was probably synthesized during BBN. 1 Temperature (109 K) 22 3 H Abundance (Si=100) 106 He GCR abundances 104 C 102 O Ne Mg Si Fe S Ar Ni Cr 100 K Ti Zn F V -2 10 10-4 B Be Sc Ge As Kr Sr Y Li Fig. 4 Solar abundance of elements (in order of increasing Z, up to 39) normalized to Si, relative to Galactic Cosmic Ray abundance (dark grey line).
Advances in Lithium Isotope Geochemistry by Paul Tomascak, Tomáš Magna, Ralf Dohmen