Oral fluid is an important biological environment that provides a normal functional state of organs and tissues of the oral cavi-ty, due to its multi-component biochemical composition, the vio-lation of which leads to the development of dental pathology. The composition and properties of oral fluid are closely related to metabolic processes in the body, as well as the level of oral hygiene and dental diseases.Purpose of research. To study changes in the mineral composi-tion of oral fluid in patients with type 1 diabetes.Material and methods of research. The collection of non-stimulated mixed saliva (4 ml) in the morning on an empty stomach in graduated tubes in 34 patients with type 1 diabetes aged 18 to 34 years. The control group consisted of 33 people of the appropriate age without General somatic pathology. A col-orimetric method was investigated, the concentration of total calcium with arsenazo III, the concentration of magnesium with silidianin blue. The concentration of inorganic phosphorus was determined by direct reaction with phosphomolybdate. The de-termination was carried out on an automatic biochemical ana-lyzer. The content of ionized calcium, potassium, sodium, pH of the oral fluid was studied on an ion-selective electrolyte analyz-er.Research result. In patients with type 1 diabetes mellitus, signif-icant violations of the mineral composition of the oral fluid were revealed. It is established that in the oral fluid of patients sig-nificantly reduced the content of total and ionized calcium in comparison with indicators of control group patients and the physiological norm, in that time, as the content of inorganic phosphorus in the patients was at the level of individuals of the control group and in the normal range, resulting in the calcium-phosphorus ratio in patients with diabetes mellitus of the 1st type was 2 times lower. The pH value of oral fluid in patients with diabetes mellitus and in the control group did not differ.Summary Thus, in the examined persons with type 1 diabetes mellitus, significant changes in the main mineral components of the oral fluid were revealed, first of all, a reduced content of to-tal and ionized calcium, as a result of which the calcium-phosphorus coefficient decreases, which, of course, worsens the mineralizing function of the oral fluid and reduces the possibil-ity of mineralization of tooth enamel and its restitution in the event of acid demineralization.