Article

Article title MATHEMATICAL OF KISLOVODSK DEPOSIT CARBON MINERAL WATER
Authors А.V. Malkov, I.M. Pershin, I.S. Pomelyayko
Section SECTION III. MODELING AND DESIGN
Month, Year 07, 2015 @en
Index UDC 28,50, 519.876.5
DOI
Abstract It is known that the study of gidrolitosfernyh processes used different models: hydraulic, flat, flat-spatial and spatial. Each of the original study fields, Mathematical models of the structure may be similar, but the parameters, used in mathematical models for each field original. Determination of these parameters for the given field area is very time-consuming and important task. The problem of constructing a mathematical model of the processes gidrolitosfernyh Kislovodsk mineral water. The hydrodynamic and hydrogeochemical regimes aquifers are characterized by highly dynamic, and depend on the natural and man-made factors. The subject field is studied for about a century, but the answers have not received, largely due to the complexity of the geological structure of the deposit. A mathematical model of the deposit described by partial differential equations, reflecting flat-spatial filtering process and mass transfer. On the basis of geological and hydrogeological characteristics of the structure, is a three-layer flat-spatial model geofiltration, including top – pressure-unconfined aquifer subhorizon verhnevalanzhinsky and two pressure: nizhnevalanzhinsky subhorizon and tithonian horizon. Capacity and filtration properties of the aquifer were determined by the results of experimental-filtration works with existing production wells. This work is considered to deposit, done for the first time by the authors. The filtration area is taken piecewise smooth. The possibility of such an assumption is confirmed by geophysical surveys. Verification results of a mathematical model of Kislovodsk field are given in the article. Purpose - to develop a mathematical model of Kislovodsk me-deposits is mineral water. Despite the high complexity of the geological and hydrogeological structure model fairly accurately reflects the processes gidrogeodinamiki and migration, which is confirmed by the analysis of retrospective ion data for 11-year period (2002–2013 gg.). The resulting mathematical model not only has scientific importance (to evaluate the relationship of various aquifers and their development in the near and distant perspective), but also of great practical importance. Using the model can be organized and long-term operational management system hydromineral base of deposits, to predict the situation with feed forward periods up to 10–20 years.

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Keywords Hydrolithosphere; mathematical model; filtration reservoir parameters; mineral waters; verification.
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