Authors: P. Bochsler and R. Kallenbach,
Reference: Meteoritics 29 (1994) 653-658
Abstract:
Abstract: In a further step to assess processes leading to the complicated
secular trend of the isotopic composition of N implanted in lunar
regolith, we investigate mechanisms fractionating solar energetic particles
(SEPs). We conclude that such mechanisms are likely to occur, most probably
producing an enrichment of 15N over 14N in SEPs over the photospheric
abundance ratio. Simultaneously, 22Ne is enriched
over 20Ne but to a lesser extent. An enrichment of the heavy Ne isotope is
observed in the suprathermal solar particles, implanted in the
lunar regolith. Hence, the now well-established difference between the
isotopic composition of suprathermal Ne and solar wind Ne in the lunar
regolith might be taken as evidence for the validity of this model. The
present-day fluxes of energetic particles produced in impulsive flares
events, capable to produce such isotopic fractionations are, however, orders
of magnitude below the required amounts to explain the lunar
observations. The details of the secular variation of the N isotopic
composition remain an enigma.