A quadrupole-based mass spectrometer used in static mode has been empl
oyed to determine noble gas concentrations of water samples by isotope
dilution. Water samples are degassed and spiked with minor isotopes o
f each noble gas. After separation of the various gas components, the
isotopic ratios are measured in the mass spectrometer. Because a spike
is added to each sample, the recovery of each gas component does not
have to be quantitative. Equilibration temperatures are calculated fro
m the gas concentrations, based on noble gas solubility data. An accur
acy of +/-1 degrees C, from the air equilibration temperature, is atta
inable for air-saturated water samples prepared under controlled condi
tions in the laboratory. The method has been applied to groundwaters f
rom the London Basin Chalk aquifer. The noble-gas-derived temperatures
are consistent with climatic conditions prevailing at the periods of
recharge. (C) 1997 Elsevier Science Ltd. All rights reserved.