Uranium transfer phenomena in rock matrix: petrophysical and geochemical study of El Berrocal experimental site, Spain

The role played by the petrophysical characteristics of the rock matrix in the radioelement transfer phenomena through the geosphere is considered. The aim of this paper is to correlate information provided by the microcrack network, mineralogy and U-micromapping studies which can be used to quantify the extent of radioelement migration/retention in the granite. This study is part of an interdisciplinary research project on the El Berrocal site (Spain), which forms part of the R & D Programme “Management and Disposal of Radioactive Waste” of the Commission of the European Communities. The experimental procedure combines complementary microscopic techniques: polarizing light, fluorescence, confocal laser scanning, acoustic, scanning electron microscopy and uranium-induced fission-track micromapping. All of these techniques are applied for quantifying the rock matrix characteristics. Data on preferential fissure zones in relation to mineralogy, and the correlation between these data and uranium microdistribution are obtained. These results are discussed in terms of radionuclide mobility and can be used, with other information, for evaluating the retardation capacity of the crystalline rock matrix around a high-level radioactive waste repository.