A correlation between the thermal neutron absorption cross section and the
clay volume for samples from the chosen geological region is discussed. A c
omparison of the calculated and measured absorption cross sections as a fun
ction of clay volume allows an estimate to be made on the presence of highl
y absorbing impurities in clays. From the example presented, it was deduced
that 105 ppm of B or 25 ppm of Gd in the clay minerals in the samples test
ed would be sufficient to explain the difference between the experimental a
nd calculated cross section and clay mineral sections. (C) 2000 Elsevier Sc
ience Ltd. All rights reserved.