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Tytuł artykułu

Development of Channel Processes and the Need to Forecast Deformations of the Stryi Riverbed

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Deformations of the channel are a consequence of the development of denudation processes in the basin area, increase in the volume of solid runoff and deposition of debris of the rock, its fractional redistribution in the channels, which especially increase during floods and flooding. They cause changes in the hydrological regime and structure of the river system, the destruction of residential and commercial buildings, as well as the infrastructure in the floodplain. Trends, magnitudes and intensity of deformations of riverbeds are formed by a complex of natural and man-made factors. Neglecting the planned and high-altitude displacements of riverbeds often leads to unpredictable consequences. Washing the shore can cause a gas or oil pipeline to rupture, leading to a strong explosion and fire, as well as oil pollution and environmental damage. Channel processes are associated with the washing of bridge piers, power lines, significant material losses and even human casualties during floods and flooding. The aim of the work is to analyze the development of channel processes in the basin of the river Stryi and forecast the deformation of its channel. The results of the analysis show that the riverbeds of Prykarpattia are very unstable and are characterized by intense erosion of the banks and bottom, which is caused by the influence of various factors. It is a man-made activity that includes the development of gravel quarries in floodplains and riverbeds and their straightening, runoff regulation, changes in forestry and land use. Natural factors, such as climate change and water runoff, etc., are also affected. It was found that the bed of the river Stryi does not have a stable shape, significantly changed the configuration, significantly reduced multi-sleeved and increased its straightness, and in some places the river changed its position by 60–80 meters. Restoration works carried out in some parts of the riverbed during this period were not effective enough. Water in different parts of the riverbed washes the shores, which causes dangerous landslides that occur directly near the riverbed. In these areas, it is necessary to more effectively carry out measures to regulate runoff and restore shore protection.
Rocznik
Strony
187--195
Opis fizyczny
Bibliogr. 22 poz., rys.
Twórcy
autor
  • 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
  • Institute of Civil Engineering and Building Systems, Lviv Polytechnic National University, Karpinsky str., 6, Lviv, 79013, Ukraine
  • John Paul II Catholic University of Lublin, Aleje Racławickie 14, 20-950 Lublin, Poland
  • 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
  • Department of Applied Hydroaeromechanics and Mechanotronics, National Technical University of Ukraine, Igor Sikorsky Kyiv Polytechnic Institute, Peremohy ave., 37, Kyiv, 03056, Ukraine
autor
  • Institute of Civil Engineering and Building Systems, Lviv Polytechnic National University, Karpinsky str., 6, Lviv, 79013, Ukraine
Bibliografia
  • 1. Allan J.D., Castillo M.M. 2007. Stream Ecology. Structure and function of running waters (Second Edi-tion). Springer; 436.
  • 2. Borutska Yu., Sakhnyuk I., Teleguz O., Medvid G., Kost M. 2015. Hydrogeochemical analysis of the Stryi river basin (ecological aspect). Geology and geochemistry of combustible minerals, 1–2, 108–117. (in Ukrainian)
  • 3. Buffington J.M., Montgomery D.R., Shroder J., Wohl E. 2013. Geomorphic classification of rivers. Treatise on Geomorphology. Fluvial Geomorphology, 9, 730–767.
  • 4. Burshtynska H.V., Babushka A.V., Bubnyak I.M., Babiy L.V., Tretyak S.K. 2019. Influence of geological structures on the nature of riverbed displacements in the upper part of the Dniester basin. Geodyna-mics, 2(27), 26–40. (in Ukrainian)
  • 5. Burshtynska K., Zayac I., Tretyak S., Halochkin M. 2017. Monitoring of the riverbed of river Dniester of the Сarpathian Region using GIS technologies. Archiwum Fotogrametrii, Kartografii i Teledetekcji, 29, 25–36.
  • 6. Burshtynska Kh.V., Tretyak S.K., Shevchuk V.M. 2018. Monitoring of changes in the Stryi riverbed using GIS technologies. Modern achievements of geodetic science and production. 1 (35). P. 138–146. (in Ukrainian)
  • 7. Hajdukiewicz H., Wyżga B., Mikuś P., Zawiejska J., Radecki-Pawlik A. 2016. Impact of a large flood on mountain river habitats, channel morphology, and valley infrastructure. Geomorphology, 272, 55–67.
  • 8. Hooke J.M. 2006. Hydromorphological adjustment in meandering river systems and the role of flood events. Sediment Dynamics and the Hydromorphology of Fluvial Systems. In: Proceedings of a symposium held in Dundee, UK, July 2006), 306, 127–135.
  • 9. Hu Z., Wang L., Tang H., Qi X. 2017. Prediction of the future flood severity in plain river network region based on numerical model: A case study. Journal of Hydrology, 29(4), 586–595.
  • 10. Jacik A.V. 1991. Small rivers of Ukraine. (Eds.). Kyiv: Urozhay, 296. (in Ukrainian)
  • 11. Khilchevsky V.K., Gonchar O.M., Zabokrytska M.R., et al. 2013. Hydrochemical regime and surface water quality of the Dniester basin on the territory of Ukraine. Khilchevsky V.K., Stashuk V.A. (Eds.), K.: Nika-Center; 256. (in Ukrainian)
  • 12. Kovalchuk I., Mykhnovych A., Pylypovych O., Rud’ko G. 2013. Extreme Exogenous Processes in Ukrainian Carpathians. Book chapter in: Geomorphological impact of extreme weather: Case studies from central and eastern Europe. Loczy Denes. Series: Springer Geography, 1, 53–67.
  • 13. Kravchuk J.S. 1999. Geomorphology of Precarpathia. Lviv: Mercator; 188. (in Ukrainian)
  • 14. Kravchuk J.S. 2005. Geomorphology of the Skibo Carpathians. Lviv: Publishing center of Ivan Franko LNU. 232 p. (in Ukrainian)
  • 15. Matolych B., Kovalchuk I., Ivanov E. 2009. Natural resources of Lviv region. Lviv: PP Lukaschuk V.S. (Eds.); 120. (in Ukrainian)
  • 16. Mykhnovych A.V., Pylypovych O.V. 2017. Riverbed deformations in the upper Dnister catchment under gravel-pits exploitation. Problems of geomorphology and paleogeography of the Ukrainian Carpathians and adjacent territories, 1, 112–122.
  • 17. Nazaruk M.M. 2018. Lviv region: natural conditions and resources: monograph. Lviv: Staryi Lev Publishing House. 592. (in Ukrainian)
  • 18. Peggy A.J. 2006. Assessing Stream Channel Stability At Bridges in Physiographic Regions. Publication No. FHWA-HRT-05-072, July 2006. p. 147 [Access: https://www.fhwa.dot.gov/publications/research/infrastructure/hydraulics/05072]/
  • 19. Richards K., Brasington J., Hughes F. 2002. Geomorphic dynamics of floodplains: ecological implications and a potential modelling strategy. Freshwater Biology, 47, 559–579.
  • 20. Rudko G.I., Petryshyn V.Yu. 2014. Characteristics of boulder-gravel-sand deposits in Lviv region and their impact on the ecological state of the environment. Mineral resources of Ukraine, 1, 39–47. (in Ukrainian)
  • 21. Snitynskyi V., Khirivskyi P., Hnativ I., Yakhno O., Hnativ R. 2019. Changing aquatic ecological systems of the foothills of the Dniester river basin under anthropogenic loading. International Scientific Conference, Gabrovo 2019, 279–283.
  • 22. Watson A.J., Basher L.R. 2005. Stream bank erosion: a review of processes of bank failure, measurement and assessment techniques, and modelling approaches. Integrated Catchment Management Programme Report Series: Bank erosion review. Landcare ICM Report No. 2005–2006/01; 32.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-f2b8a1c5-bb72-4c8c-bbc0-71a2a170a4de
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