Mathematical Modeling of the Processes Formations of Stocks in Low Water Period (on the example of the Kitab-Shahrisabz aquifer)
J. Х. Djumanov1, Н.N. Zaynidinov2, D. E. Eshmurodov3, X. S. Egamberdiev4
1Jamoljon Х. Djumanov*, Department of Computer Systems, Tashkent University of Information Technologies Named After Muhammad al-Khworezmi, Tashkent, Uzbekistan.
2Нakimjon N. Zaynidinov, Department of Information Technology, Tashkent University of Information Technologies Named After Muhammad al-Khworezmi, Tashkent, Uzbekistan.
3Eshmurodov Dilshod Elmurodovich – Associate Professor of the Department of Computer Systems of the Tashkent University of Information Technologies Named After Muhammad al-Khworezmi.
4Хojiakbar S. Egamberdiev, Department of Computer Systems, Tashkent University of Information Technologies Named After Muhammad al-Khworezmi, Tashkent, Uzbekistan.
Manuscript received on May 11, 2020. | Revised Manuscript received on May 24, 2020. | Manuscript published on June 10, 2020. | PP: 402-408 | Volume-9 Issue-8, June 2020. | Retrieval Number: 100.1/ijitee.H6351069820 | DOI: 10.35940/ijitee.H6351.069820
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© The Authors. Blue Eyes Intelligence Engineering and Sciences Publication (BEIESP). This is an open access article under the CC-BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/)
Abstract: In this study, we consider mathematical modeling of the dynamic state of groundwater aquifers, i.e., the process of groundwater formation in dry years under intensive (forced) groundwater intake withdrawal, i.e. operational selection exceeds the value of groundwater resources and depletion of capacitive reserves occurs) on the example of the Kitabo- Shakhrisabz groundwater deposits, of the Kashkadarya area of the Republic of Uzbekistan, which has a long period of regime observations and comparatively correct information on the groundwater level regime, groundwater intake withdrawal and interconnections within surface runoff. The data of hydrogeological area obtained as a result of analysis and schematization of hydrogeological conditions are generalized, and the hydrogeological parameters of the aquifer are calculated. The hydrogeological factors of groundwater formation are given and evaluated taking into account changes in water intake conditions, their current state is highlighted, and recommendations are given for substantiating the tasks of groundwater automations of monitoring in these territories.
Keywords: Mathematical modeling, Boundary conditions, Groundwater formation, Geofiltration process, Groundwater intake, Automations of monitoring water resource.
Scope of the Article: Water Resource.