PUBLISHED PAPERS #07.5

Tahir Gadjiev, Yasin Rustamov, Irada Dadashova, Mehrali Aliyev.
Mathematical Models of Mineral Waters of Azerbaijan
Abstract. Azerbaijan situated in the east of the Caucasian region of the Alpine folding beltisrich in not only great oil, gas and mineral reserves, but in unique mineral water deposits as well. Nonetheless, exploration of new potable, mineral and thermal water sources persists as one of the vital targets of geological services of the Republic. The issue of efficient use of available water resource assumes, at the same time, more and more significant attitude. This article is dedicated to ways solve this problem. In addition, we consider the inverse problem of determining the temperature of geothermal waters as sources of temperature dependence on the surface. We are talking about those tasks in which it is necessary to determine the causes if the results obtained because of observation are known. For example, to determine the location and power of an earthquake from the oscillations measured on the surface of the earth. Or by the structure on the surface of the earth’s minerals to determine the depth of their location underground, etc. When processing these experiments, a conclusion is drawn about the internal relationships of a phenomenon or process. When the mathematical model of the process under study is known, the problem of identifying the mathematical model is posed. In general, inverse problems are understood as tasks in which it is possible to draw conclusions in determining the parameters of this model from the available results of observations or other experimental information. The study is devoted to the inverse problem of determining the temperature of geothermal waters depending on the surface temperature for the efficient use of available water resources.
Keywords: geothermal, debit, mineral content, chemical, gradient, inverse problem, differential equations, mathematical model
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