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Geoinformation technologies and methods of mathematical modeling in hydrogeological research

Shavkat AkhralovTashkent University of Information Technologies named after Muhammad Al-Khwarizmi, Amir Temur str., 108, 100200, Scientific-Innovation Center of Information-Communication Technologies, Tashkent, Uzbekistan,Rustam YusupovTashkent University of Information Technologies named after Muhammad Al-Khwarizmi, Amir Temur str., 108, 100200, Tashkent, UzbekistanKhojakbar EgamberdievTashkent University of Information Technologies named after Muhammad Al-Khwarizmi, Amir Temur str., 108, 100200, Tashkent, UzbekistanJ.J. JumanovTashkent State Technical University named after Islam Karimov, Universitet str., 2, 100097, Tashkent, Uzbekistan
InterCarto InterGISjournal2020en
ABI

Аннотация

In the article the application issues of geographic information technologies and methods of mathematical modeling of geofiltration and geomigration processes of hydrogeological systems were discussed, as well as for information support of the groundwater monitoring system. The object of research is the Akhangaran aquifer, which is a large industrial area with intensification of agriculture, as well as densely populated, where industrial reproduction of water resources is established by designing water intake facilities using groundwater, also having huge data on regime, geological and hydrogeological aspects. The main goal of these researches is to learn the methodology for assessing groundwater resources by modeling to the GIS basis, theoretical and applied methods of mathematical analyses. The features are considered and the boundary and initial conditions are justified. The results are a research technique has been developed to simulate geofiltration and geomigration processes, to determine the balance of groundwater, and the hydrogeological parameters of the aquifer have been calculated from it. The calculated values of the natural resources of groundwater by the parameters of their level mode in the Akhangaran pool allowed establish the permissible convergence of resource estimates according to the amplitudes of fluctuations in the level of groundwater and according to geoinformation modeling.

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