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The scenery was spectacular, the climate healthy and thermal spring waters available.
Thanks to private research, scientific literature is now available for some thermal spring waters which justify their widespread therapeutic use in the 21st century.
However, also thermal spring waters often have a near-surface water component (Fig. 14, e.g. Badenweiler, Bürchau).
Analysis of Cl levels in thermal springs sampled in the 15 years following the crisis has attributed the cause to shallow magma intrusion (Villemant et al. 2005; Boichu et al. 2011), and the chlorine isotope signature of thermal spring waters is markedly magmatic (Li et al. 2012).
Thermal spring waters have been used widely in the treatment of inflammatory skin diseases for a long time, but their use has been largely empirical.
They are used in 12 therapeutic orientations, but the curative use of thermal spring waters has been totally empirical, and for years physicians generally have doubted their medical value.
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The plots clearly indicate that the thermal spring water is Na-HCO3 type.
Study was undertaken to measure physical and chemical characterization of the thermal spring water from Dholera hot springs.
There is no indication of an interaction of seawater with the thermal spring water as is the case of other west coast springs.
The mineral content of thermal spring water contributes to the skin comfort provided.
The Zavarzin thermal spring water temperature is 56-58°C 56-58°C pH is 6.6, which is andthe boundary between neutral and acidic water (Table 1).
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