Fig. 6From: Original composition and formation process of slab-derived deep brine from Kashio mineral spring in central JapanNegative linear relationship between 3H and Cl concentrations in the Kashio A and B water samples. Assuming that KDE has no 3H, the Cl concentration of KDE was estimated to be 24,000 ± 2000 mg/L. [R2 correlation coefficient]Back to article page