An internal monostandard method for PGAA is proposed for completely non-des
tructive analysis of elements in bulky samples by the use of a neutron beam
guided out from the reactor. The method is essentially the same as the k(0
) method except that it corrects for the change of relative gamma-ray count
ing efficiencies caused by the absorption and scattering of neutrons and ab
sorption of gamma-rays within the sample. Some examples of applications to
archaeological samples of earthen wares, bronze mirrors, and to voluminous
meteorite samples are demonstrated, and its future application to the in-si
tu studies of distribution and metabolism of a certain elements in animals
is also explained.