The concentration of hydroxyl ion in natural waters is one of the main parameters governing most natural hydrogeochemical systems; therefore, there is a natural interest in ultraalkaline waters, in which the pH reaches a maximum.
How to cite:
Korotkov A.I., Salman A.F. Hydrogeochemistry of ultra-alkaline waters // Journal of Mining Institute. 1985. Vol. 103. p. 96-102.
