A well-logging system containing a high-purity germanium (HPGe) detect
or provides quantitative assessment of gamma-ray-emitting contaminants
and natural radionuclides in the subsurface. The system is in operati
on at the Hanford Site of the U.S. Department of Energy where radionuc
lide-laden effluent from the production of nuclear materials in the pa
st has contaminated the soil. The system is calibrated by using standa
rd formations that have known concentrations of K, U and Th. This prod
uces calibration constants for K, U and Th, and a detector inverse eff
iciency function for the energy range 0.1-3 MeV. The inverse efficienc
y function, along with a knowledge of the energies and gamma-ray produ
ction coefficients for artificial radionuclides, allows the system to
be calibrated for these artificial gamma-ray sources, even though they
are not contained in the calibration standards. Corrections for a ste
el borehole casing and the diameter of a water-filled borehole are als
o derived from measurements with the calibration standards. The boreho
le logging measurements provide concentrations (activity per gram of e
arth material) of the following isotopes: K-40, Ra-226 (via Bi-214), U
-238 (via Pa-234m), U-235, Th-232 (via Tl-208), Co-60, Sb-125, Cs-137,
Eu-152, Eu-154, Np-237 (via Pa-233), Pu-239, Pu-240 and Am-241.