Fig. 7From: Water–rock interactions in the Bruchsal geothermal system by U–Th series radionuclidesComparison of MIN3P and CAS model for one-dimensional transport of 224Ra along a flow line, calculated at different half-lives (t1 = 0.5 t1/2; t2 = 2 t1/2; t3 = 45 t1/2)Back to article page