A method for making artificial mineralized drinking water of the spring-autumn purpose provides for correcting ionic composition of source water and the following addition of K2SO4 and a magnesium salt up to the preset content of the cations K+, Mg2+ and the anions SO42-, Cl-. The demineralized water, the pH of which is set in the ranges of 6.5-6.9, is used as the source water, the salts MgSO4, K2SO4, ZnSO4, Cr2(SO4)3, NaCl, CaCl2 and KI are added into the demineralized water with the specified pH value in the amount providing the following content of the cations: K+ = 9-11 mg/l, Na+ = 9-11 mg/l, Mg2+ = 26-30 mg/l, Ca2+ = 14-18 mg/l, Zn2+ = 0.5-0.7 mg/l, Cr3 + = 0.03-0,035 mg/l and the anions I- = 0.03-0.035 mg/l, SO42- = 116-134 mg/l, Cl- = 48-59 mg/l.
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