1998 Volume 47 Issue 9 Pages 686-690
The radioactive disequilibrium between222Rnand its daughter nuclides214Pband214Biincluded in situ ground water has been investigated for three locations. Water samples collected carefully in 100mL Teflon vials were immediately transported to the laboratory and measured with a low-background Ge spectrometer. It has been shown that222Rnand its daughters214Pband214Biin ground water are not in radioactive equilibrium and deduced radioactivities of daughter nuclides are ranged from 0.5 to 38.5% of that of radon by fitting the growth decay curves.