抄録
Migration data of 90Sr, 237Np and 238Pu in natural aquifer were collected by a field test, which was performed in an aquifer at 30m under ground surface of the field test site. Migration parameters for analysis of the results obtained from the field test were measured by laboratory column tests and batch tests.
The large retardation effects of the soil for the radionuclides were confirmed in the natural aquifer. Dispersion coefficient corresponding to water velocity was determined from the relationship between water velocity and dispersivity, which obtained from the column tests. Distribution coefficient was determined by considering reliability of data, test conditions, and environmental conditions. One dimensional migration behavior of the radionuclides in aquifer, calculated by using the migration parameters obtained from the batch and column tests, agreed with the results obtained from the field test. It was confirmed that the migration behavior of α-nuclides could be evaluated by applying the conventional equation for evaluating the radionuclide migration and the migration parameters obtained from laboratory tests.
