[en] In many cases simple hydrogeochemical evaluations are sufficient to distinguish different source of the waters in the hydrogeological studies. In this study how hydrochemical data can be used to understand mixing mechanism is explained. Mixing ratios determined by using physically or chemically nonreactive component in hydrogeological studies. For mixing quantity calculations, quantity of the end members that cause to mixing, need to be known. Electrical conductivity is another parameter may be used when lack of hydrochemical data is present or more practical and fast solution is required. Isotope techniques are widely used to describe the hydrogeological conditions, where the conventional methods is not sufficient to understand. Since ¹⁸O ve D are conservative isotopes and do not effected by the hydrochemical processes in the aquifer, they are used to explain recharge quantities of the aquifer, determination of the recharge areas, groundwater-surface water relations, determination of mixing quantities and understanding of recharge-discharge relations in the fractured aquifers. By using stable isotope data, sources of the mixing portions, dissolution of salts, evaporation and isotopic enrichment or fresh water-salt water/fresh water- sea water mixing can be identified easily