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Table 4 Rc values of Th–U decay series radionuclides

From: Water–rock interactions in the Bruchsal geothermal system by U–Th series radionuclides

Isotope

Rock activity (Bq kg−1)

Rc values

Half-life

238U

18.0

1.5 × 103

4.47 × 109 y

235U

0.8

> 2.1 × 102

7.04 × 108 y

234U

19.0

1.9 × 103

2.46 × 105 y

232Th

17.0

> 1.7 × 103

1.41 × 1010 y

230Th

19.0

> 2.4 × 102

7.54 × 104 y

228Th

19.0

> 9.5 × 102

1.91 years

226Ra

43.0

1.5

1600 years

228Ra

17.0

1.1

5.75 years

223Ra

0.8

1.8

11.43 days

224Ra

19.0

1.7

3.66 days

210Pb

37.0

1.4

22.30 years

212Pb

19.0

1.2

10.64 h

  1. Rc is defined as the ratio of rock activity relative to average fluid activity (cf. Table 3)