Thermal water, Vichy, France (N = 1) |
25 |
– |
Bardet (1914) |
Thermal water, Senami, Japan (N = 1) |
30 |
– |
Kuroda (1939) |
Thermal water, Beppu, Japan (N = 24) |
< 2–150 |
– |
Kawakami et al. (1956) |
Thermal spring waters, USA and Iceland (N = 7) |
< 10–40 |
– |
El Wardani (1957) |
Thermal waters, Hokkaido and Honshu islands, Japan (N = 84) |
0.4–43.3 |
7.8 |
Uzumasa et al. (1959) |
Thermal waters, New Zealand (N = 38) |
1–128 |
52.5 |
Koga (1967) |
Carbonate thermal waters, Pamir and Caucasus mountains (N = 16) |
12–140 |
32.5 |
Kraynov (1967) |
Groundwaters of ore deposits, USSR (N = 26) |
0.5–48 |
3.0 |
Goleva and Vorobjeva (1967) |
Mineral (Na-HCO3-Cl) waters and Na-Cl saline waters, oil deposits, USSR (N = 36) |
0.3–8.5 |
3.25 |
Nuriev et al. (1968) |
Thermal waters, Vosges, France (N = 8) |
< 0.5–15.4 |
– |
Gijbels et al. (1983) |
Thermal waters, Iceland (N = 132) |
0.5–52.5 |
6.1 |
Arnórsson (1984) |
Thermal waters, Vals Les Bains and Vichy, Massif Central, France (N = 35) |
0.5–47.9 |
13.1 |
Criaud and Fouillac (1986) |
Mineral waters, deep gold mines, South Africa (N = 12) |
< 0.05–276 |
– |
Duane et al. (1997) |
Thermal spring waters, Baikal area (N = 4) |
0.98–9.81 |
– |
Kenison Falkner et al. (1997) |
Groundwater (fresh) in crystalline bedrocks, Norway (N = 476) |
< 0.002–1.5 |
0.017 |
Frengstad et al. (2000) |
Thermal waters, Iceland (N = 88) |
0.001–23.6 |
2.66 |
Elmi (2009) |
European bottled waters (only waters with Ge concentration ≥ DL) (N = 882) |
0.03–110 |
0.09 |
Reimann and Birke (2010) |
Thermal spring waters, Lesvos Island, Greece (N = 6) |
< DL–13 |
– |
Tziritis and Kelepertzis (2011) |
Fresh and mineral groundwaters, Bieszczady Mountains, Poland (N = 23) |
0.08–35.8 |
7.5 |
Dobrzyński et al. (2011) |
CO2-rich and thermal curative waters, the Sudetes Mountains, Poland (N = 33) |
0.025–10.62 |
1.01 |
This study |