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Visualization of River Water Flow in Hydrodynamically Active Areas under Different Flow Regimes

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
It was established that in the territory of the Stryi river basin, the natural landscapes are maximally preserved in comparison with other regions of Western Ukraine, but under modern conditions an increase of negative anthropogenic impact on the quality of natural waters is observed. The hydrodynamic barriers or hydrodynamically active areas (HAA) of mountain rivers, characterized by a significant oxygen saturation of the water flow, which activates the processes of biochemical and biological self-purification of surface waters, are important for the efficiency of self-purification processes. In order to verify the results of theoretical and field research, an existing experimental setup was designed and improved. It provided the conditions for modeling the flow of mountain rivers in accordance with the laws of similarity theory and the principles of hydrodynamic modeling. On the basis of the results of field observations in the foothills of rivers, as well as regulatory and design documentation, the limits of the main operating factors were determined, namely the Freud number, flow depth and flow rate, which are decisive in studying the impact of HAA on flow self-cleaning processes. By changing the length of the tray section, the gullies and the waterfall niche of the real hydrodynamically active section were simulated, on which field experiments on the Tyshivnytsia River were conducted. In the studies, measurements were performed at different flow regimes, which simulated different hydrological parameters. In order to analyze the impact of HAA on self-cleaning processes, the flow was visualized using photography. The change in the structure of a stream of natural waters at passage of HAA was established. The high oxygen saturation of the river waters of the Stryi river basin is caused by the influence of HAA, which contribute to the purification of polluted waters from biological pollutants and other man-made pollutants and form the high quality of water resources in the region. A method of modeling and visualization of mountain rivers in the laboratory was developed.
Rocznik
Strony
129--135
Opis fizyczny
Bibliogr. 14 poz., rys.
Twórcy
  • Department of Ecology, Lviv National Agrarian University, Volodymyra Velykoho str., 1, Dublyany, Lviv region, 30831, Ukraine
  • Department of Ecology, Lviv National Agrarian University, Volodymyra Velykoho str., 1, Dublyany, Lviv region, 30831, Ukraine
autor
  • Department of Ecology, Lviv National Agrarian University, Volodymyra Velykoho str., 1, Dublyany, Lviv region, 30831, Ukraine
autor
  • Institute of Mechanical Engineering, National Technical University of Ukraine, Igor Sikorsky Kyiv Polytechnic Institute, Peremohy ave., 37, Kyiv, 03056, Ukraine
autor
  • Department of Forest Machines, National Forestry University of Ukraine, General Tchuprynka str., 103, Lviv, 29057, Ukraine
autor
  • Institute of Civil Engineering and Building Systems, Lviv Polytechnic National University, Karpinsky str., 6, Lviv, 79013, Ukraine
Bibliografia
  • 1. Borutska Yu Z. 2015. Cavitation and aeration impact of hydrodynamic barriers on the quality of natural waters of the Stryi river basin. Scientific notes of TNPU. Series: Biology., 3–4(64), 66-69. (in Ukrainian).
  • 2. Ecology of erosion-channel systems of Russia / [ed. R.S. Chalov]. M: Geogr. 2002. MSU. 163.
  • 3. Snitynskyi V.V., Yakhno O.M., Khirivskyi P.R., Hnativ I.R., Hnativ R.M. 2020. Changes in the quality of natural waters in hydrodynamically active areas of mountain rivers. Proceedings of the XXV International Scientific and Technical Conference “Hydroaeromechanics in Engineering Practice”, Kyiv, 256-259. (in Ukrainian).
  • 4. Reid D.E., Hickin E.J. 2008. Flow resistance in steep mountain streams. Earth Surface Processes and Landforms, 33, 2211–2240.
  • 5. Chiari M. & Rickenmann D. 2011. Back-calculation of bedload transport in steep channels with a numerical model. Earth Surface Processes and Landforms, 36, 805–815.
  • 6. Comiti F., Mao L., Wilcox A., Wohl E.E., Lenzi M.A. 2007. Field-derived relationships for flow velocity and resistance in high-gradient streams. Journal of Hydrology, 340, 48–62.
  • 7. Radecki-Pawlik A., Pagliara S., Hradecky J. 2018. Open Channel Hydraulics, River Hydraulic Structures and Fluvial Geomorphology. Publisher: CRC, Taylor & Francis, 516.
  • 8. Young F.R. 1999. Cavitation. London, U.K.: Imperial College Press, 418.
  • 9. Cain P. & Wood I.R. 1981. Measurements of selfaerated flow on a spillway. Jl. Hyd. Div., ASCE, 107(HY11), 1425–1444.
  • 10. Wood I.R. 1991. Air Entrainment in Free-Surface Flows. IAHR Hydraulic Structures Design Manual No. 4, Hydraulic Design Considerations, (Balkema Publication: Rotterdam, The Netherlands), 149.
  • 11. Chanson Hubert. 2004. Environmental Hydraulics for Open Channel Flows. U.K., Elsevier Butterworth-Heinemann, 488.
  • 12. Voznyak О., Korbut V., Davydenko B., Sukholova І. 2019. Air distribution efficiency in a room by a twoflow device. Springer, Proceedings of CEE 2019, Advances in Resourse-saving Technologies and Materials in Civil and Environmental Engineering, 47, 526–533.
  • 13. Krutov V.I., Grushko I.M., Popov V.V., et al. 1989. Fundamentals of Scientific Research: Textbook. tech. universities / V.I. Krutov, / / edited by V.I. Krutova, V.V. Popov. M .: Higher. sch. 400. (in Russian).
  • 14. Determination of the calculated hydrological characteristics: СНиП 2.01.14-83 [Electronic resource]. – [Valid from 1984-07-01; BST amendments №6, 1985 р.]. – M .: Stroyizdat, 1985. 36 p. (National standard of Ukraine). Access mode: http://document.ua/opredelenie-raschyotnyh-gidrologicheskihharakteristik-nor616.html. (In Russian).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-c8d8b5e4-641c-4143-b87c-5ab250dff933
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