Arte­sian waters are pres­sur­ized ground­wa­ter occur­ring at sig­nif­i­cant depths between two imper­me­able rock lay­ers.

Indus­tri­al waters nat­u­ral­ly con­tain dis­solved micro­com­po­nents and their salts.

Many res­i­dent enti­ties won­der what steps should be tak­en to legal­ize water well.

Water lab­o­ra­to­ry ana­lyzes are per­formed to obtain pre­lim­i­nary char­ac­ter­is­tics of the water qual­i­ta­tive com­po­si­tion with­in the study area.

Tran­scarpathi­an min­er­al waters con­tain var­i­ous trace ele­ments and their com­pounds.

In Ukraine, the ter­ri­to­ries which are char­ac­ter­ized by high geot­her­mal gra­di­ent are local­ized with­in young alpine fold­ing zones.

An essen­tial part of nitro­gen com­pounds that is brought in with fer­til­iz­ers, removes out from the soil by rain and gets into the ground­wa­ter.

The first records of the use of under­ground min­er­al ther­a­peu­tic waters in Ukraine date back to the peri­od of the Bosporus King­dom in Crimea.

In obe­di­ence to accu­mu­la­tion specifics trace ele­ments (microele­ments) in ground­wa­ter can be divid­ed into two groups.

The query of the ground­wa­ter ori­gin remained debat­able for a long time.

The ter­ri­to­ry of the Cherni­hiv region is locat­ed with­in the Dnipro-Donet­sk arte­sian basin.