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Water Retention Problem in the Mountain Areas: a Case of Sola River Flows, Polish Carpathians

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Języki publikacji
EN
Abstrakty
EN
The paper considers mountain rivers, which usually feature high dynamics of hydrological phenomena. The variability of the Sola river flows in the Polish Carpathians is presented based on water-gauge measurements from the hydrological long-period of 1956-2015. The flows for the upper section of the river, where no storage reservoirs are found, were analysed. A broad range of flows was shown – from 0.59 to 1250 m3/s at a mean flow of 15.5 m3/s. It was also shown that within a year, the flows grow in the spring (thaw freshets) and summer periods (rainwater freshets). Mainly the summer freshets are dangerous, consisting in a sudden rise of the flow due to rains. This is shown by the high values of maximum flows in June and July. In the case of mountain rivers, such as the Sola river, it is necessary to undertake the actions stabilising the flows, which on the one hand have flood-prevention importance, and on the other hand protect the water resources in long dry periods. The actions should be concentrated on the proper arrangement of the catchment area, slowing down the rainwater outflow. Appropriate land use is especially important (distribution of forests, of arable and developed areas) depending on the land elevation above the sea level and inclination, as well as creation of small storage facilities.
Rocznik
Strony
167--177
Opis fizyczny
Bibliogr. 26 poz., rys., tab.
Twórcy
  • University of Bielsko-Biala, Willowa 2, 43-309 Bielsko-Biała, Poland
Bibliografia
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  • 6. Jagus A. 2018. Economic and social importance of dam reservoirs – a study of the Sola River cascade. Inzynieria Ekologiczna, 19(1), 25–35 (in Polish).
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  • 8. Klima K. 1997. A protective aspect of mountain crop rotation. Acta Academiae Agriculturae ac Technicae Olstenensis – Agricultura, 64, 261–266 (in Polish).
  • 9. Kurek S. 1990. Land use in water protection. Materialy Seminaryjne IMUZ, 27, 83–94 (in Polish).
  • 10. Kusmierski E. 1991. Water balance of the Sola catchment for the river gauge Rajcza (methodological remarks). In: Jankowski A.T. (Ed.) Przeobrazenia stosunkow wodnych na obszarach silnej antropopresji. Published by PTG, Sosnowiec, 108–130 (in Polish).
  • 11. Lipski C., Kostuch R. 2005. Soil erosion processes in the Carpathian mountain regions. Infrastruktura i Ekologia Terenow Wiejskich, 3, 95–105 (in Polish).
  • 12. Malata T. 2008. Development of Polish Flysch Carpathians revealed in outcrops and landscape. Przeglad Geologiczny, 56(8/1), 688–691.
  • 13. Mathison C., Wiltshire A.J., Falloon P., Challinor A.J. 2015. South Asia river-flow projections and their implications for water resources. Hydrology and Earth System Sciences, 19(12), 4783–4810.
  • 14. Mioduszewski W. 1999. Protection and shaping of water resources in the agricultural landscape. Published by IMUZ, Falenty (in Polish).
  • 15. Oszczypko N., Chowaniec J., Koncewicz A. 1981. Water pressure tests of the Magura sandstones. Rocznik Polskiego Towarzystwa Geologicznego, 51(1/2), 273–302 (in Polish).
  • 16. Querner E.P., Tallaksen L.M., Kasparek L., Van Lanen H.A.J. 1997. Impact of land use, dimate change and groundwater abstraction on stream flow droughts, using physically based-models. IAHS Publication, 246, 171–179.
  • 17. Ryffel A.N., Rid W., Gret-Regamey A. 2014. Land use trade-offs for flood protection: A choice experiment with visualizations. Ecosystem Services, 10, 111–123.
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  • 22. Twardy S., Kuzniar A., Kopacz M. 2001. The characterization of agriculture in the Polish Carpathians. In: Twardy S. (Ed.) Trwala okrywa roslinna jako podstawa zrownowazonego rozwoju rolnictwa w zlewniach karpackich. Published by IMUZ, Falenty, 230–237 (in Polish).
  • 23. Walega A., Mlynski D. 2017. Seasonality of median monthly discharge in selected Carpathian rivers of the Upper Vistula basin. Carpathian Journal of Earth and Environmental Sciences, 12, 617–628.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-dd9bb023-9e5d-4490-a817-609842b763e8
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