We study the effects of self-shielding in the X-wind model of protosolar co
smic-ray irradiation of early solar-system rocks. We adopt a two-component
picture of protoCAIs consisting of cores with the elemental abundances of t
ype B1 CAIs (calcium-aluminum-rich inclusions) and mantles of less refracto
ry material. The cores have a power-law distribution of sizes between R-min
and R-max. The mantles have a uniform thickness, whose value is chosen to
bring the total inventory of elements at least as refractory as sulfur to c
osmic abundances for the entire population of protoCAIs. Each object is irr
adiated with a fluence consistent with the product of their residence time
in the reconnection ring and the flux of solar cosmic rays obtained by a sc
aling of impulsive flares from the hard X-rays observed from low-mass proto
stars. For R-min in the 50 mum regime and R-max in the few centimeter regim
e, which corresponds to the range of sizes of observed CAIs in micrometeori
tes and chondrites, we recover approximately the canonical values quoted fo
r the ratios Al-26/Al-27, Mn-53/Mn-55, and Ca-41/Ca-40 in CV3 meteorites. M
oreover, the excess La-138 (denoted as La-138*) produced by proton bombardm
ent of Ba-138 lies within the CAI range obtained in the experiments of Shen
et al. When we include fragmentation reactions that produce Be-10 from the
impact of protons, alphas, and He-3 on the O-16 that is bound up in rocks,
we further obtain a level of Be-10/Be-9 that agrees approximately with the
report of McKeegan et al. for a CAI from the Allende meteorite. Similar ca
lculations for the expected anomalies in the stable isotopes of lithium sho
w rough consistency with the measured values and further support our interp
retation. The value for Be-10/Be-9 is particularly difficult to produce by
any other astrophysical mechanism. Thus, the Be-10 discovery greatly streng
thens the case for an origin in early solar-system irradiation, rather than
external stellar seeding, for the shortest-lived radionuclides inferred fr
om CAIs in chondritic meteorites.