We report measurements of Al-26 and Be-10 activities in nine ordinary
chondrites and of the light noble gas concentrations and Cl-36 and Ca-
41 activities in subsets of those meteorites. All but Murray have low
Ne-21 concentrations (<1.0 x 10(-8) cm(3) STP/g) and have previously b
een used to estimate Ne-21 production rates. Ladder Creek, Murchison,
Sena, and Timochin have inventories of cosmogenic radionuclides that a
re compatible with a single stage of irradiation and give Ne-21 produc
tion rates that are consistent with the standard L-chondrite value of
similar to 0.33 x 10(-8) cm(3) STP/g/Ma. In contrast, Cullison, Guenie
, Shaw, and Tsarev experienced complex irradiation histories. They and
several other meteorites with low nominal exposure ages also have low
er He-3/Ne-21 ratios than expected based on their Ne-22/Ne-21 ratios.
A general association between low Ne-21 contents and He-3 losses sugge
sts that meteorites with short lifetimes often occupy orbits with smal
l perihelia. However, meteorites with low Ne-21 contents, one-stage ex
posure histories, and losses of cosmogenic He-3 are rare. Possible exp
lanations for the scarcity are (1) statistical, (2) that it is harder
for more deeply buried protometeoroids to lose gas in a liberating col
lision, and (3) that it is harder to insert more deeply buried protome
teoroids directly into orbits with small perihelia.