Hidrológiai Közlöny 1933 (13. évfolyam)

Gedeon Tihamér: Szulfátos vizek képződése

102 Tihamér Gedeon Bitter water of Őrsöd: 7 Well walír of Töröli szentmiklós Al'" none 0.0023 grams pro liter Fe" 0.0036 0.0130 99 99 Ca" 0.4426 0.3306 >» 99 Mg" 2.8435 0.3515 99 99 Na' 7.3680 0.3812 99 99 K' 0.0539 0.0991 99 99 SO4" 26.4492 1.3481 99 99 er 0.6995 0.6163 99 99 HCOs' 0.4054 1.1565 99 99 CO3" none 0.0106 99 99 Ih-SiOs 0.0092 0.0169 99 99 The wel'l of the flower farm at Törö'kszentmiklós lies about 30 m far from the spot where the analysed bluish gray clay sample was taken. Its water is not concentrated enough to declare it as a mineral water (its dry remains equalling 4.6580 g pro 1) because the geological conditions are unfavourable for the concentration process

8. At Ciánt only a qualitative analysis was made of an alum water formed in a testing shaft and the presence of much Al was demonstrated. A well of alum water is already known found 'long ago in the vine-yards of Gánt at the western front of Mount Gránáshegy.

9 On examining chemically the salts of sulfate containing waters we find that their range is the following on base of their formation warmth values

1

0 (to make comparation easier, also the formation warmths of equivalent weights are shown). 7 Kunszí J.: A mai Magyarország ásványvizei, stb. 1928. page 128. (Mineral waters of the present Hungary, in Hungarian.) 8 Vendl A.: Hidrológiai Közi.. X. 41. 1930. • Schréter Z.: Földtani Közi., XL. 180. 1910. 1

0 Law of Berthelot: If several reactions may occur between stuffs, that will take place spontaneously, which forms the most heat.