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Geomorphological effects of the catastrophic drainage of artificial reservoir in the Młynówka valley at Górowo Iławeckie, Poland

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The problem concerns the catastrophic flood flow caused by the breaking of the dam of the artificial reservoir in the valley of the small river Młynówka Górowska. Extensive studies were focused on the section just below the broken dam, were the geomorphological effects of that event were most noticeable. A number of erosional and accumulative forms have been distinguished. The structure and grain size of the flood deposits have been studied. The occurrence of deposit sequences characteristic of slurry-flows has been found. The rapid fall of the flood wave was associated with the deposition of the coarser deposit fractions on the sides of the valley and of the finer ones on its floor.
Czasopismo
Rocznik
Tom
Strony
75--82
Opis fizyczny
Bibliogr. 19 poz., rys.
Twórcy
autor
  • Polish Academy of Sciences, Institute of Geography and Spatial Organization Department of Geomorphology and Hydrology of Lowlands ul. Kopernika 19, 87-100 Toruń
  • Polish Academy of Sciences, Institute of Geography and Spatial Organization Department of Geomorphology and Hydrology of Lowlands ul. Kopernika 19, 87-100 Toruń
autor
  • Polish Academy of Sciences Institute of Geography and Spatial Organization Department of Geomorphology and Hydrology of Mountains and Uplands ul. Św. Jana 22, 31-018 Kraków
Bibliografia
  • Baker, V.R. & Nummedal, D., 1978: The Channeled Scabland. A Guide to the Gcomorphology of the Columbia Basin, Washington, pre¬pared for the Comparative Planetary Geology Field Conference held in the Columbia Basin, June 5-8, 1978: 186 pp.
  • Bellos, C. & Hrissanthou. V., 1998: Numerical simulation of sediment transport following a dam break. Water Resources Management 12 (6): 397-407.
  • Chen, Y.H. & Simons, D.B., 1979: An Experimental Study of Hydraulic and Geomorphic Changes in an Alluvial Channel Induced by Failure of a Dam. Water Resources Research 15 (5): 1183-1188.
  • Costa, J.E., 1988a: Floods from dam failures. In: V.R. Baker, R.C. Kochel & C.P Patton (Eds.) Flood Geomorphology. John Wiley & Sons, New York: 439-463.
  • Costa. J.E., 1988b: Rheologic, geomorphic, and sedimentologic differentiation of water floods, hyperconcentrated flows, and debris flows. In: V.R. Baker, R.C. Kochel & C.P. Patton (Eds.) Flood Geomorphology. John Wiley & Sons, New York: 113-122..
  • Dynowska, I., 1972: Typy reżimów rzecznych w Polsce. Zeszyty Naukowe UJ. Prace Geograficzne 28: 155 pp.
  • Froehlich, D.C., 1995: Peak outflow from breached embankment dam. Journal of Water Resources Planning and Management, ASCE 121 (1): 90-97.
  • Gębica, P. & Sokołowski, T., 1999: Catastrophic geomorphic processes and sedimentation in the Vistula valley between the Dunajec and Wisłoka mouths during the 1997 flood, Southern Poland. Quatern. St. in Poland. Special Issue: 253-261.
  • Graham, W., 1998: Channel and Valley Changes Resulting from Dam Failure. CADAM Proceedings, Munich Meeting 8-9 October 1998. (Online) http://www.hrwallingford.co.uk/projects CADAM/.
  • Jarrett, R.D. & Costa. J.E., 1986: Hydrology, geomorphology, and dambreak modeling of the July 15, 1982 Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado. U. S. Geological Survey Professional Paper 1369: 78 pp.
  • Kondracki, J., 1972: Polska północno-wschodnia. PWN. Warszawa: 272 pp.
  • Kubrak, J. & Ordyniec, Z., 1999: Parametry fali spiętrzenia w dolinie Warty powstałej po hipo-tetycznym uszkodzeniu zapory czołowej zbiornika Jeziorsko. In: Eksploatacja i oddziaływanie dużych zbiorników nizinnych (na przykładzie zbiornika wodnego Jeziorsko), Konf. Nauk.-Tech., Uniejów, 20-21 maja 1999, Wyd. Akad. Roln. w Poznaniu: 67-77.
  • McKee, E.D., Crosby, EJ. & Berryhill, H.L., JR.. 1967: Flood deposits. Bijou Creek. Colorado. June 1965. J. Sedim. Petrol. 37: 829-851.
  • Pierson, T.C. & Costa, J.E., 1987: Archeologie classification of subaerial sediment-water flows. In: J.E. Costa & G.F. Wieczorek (Eds.) Debris flows/avalanches, processes, recognition, and mitigation. Geological Society of America Reviews in Engineering Geology 7: 1-12.
  • Scott, K.M. & Gravlee, G.C., 1968: Flood Surge on the Rubicon River, California - Hydrology, Hydraulics, and Boulder Transport. U. S. Geological Survey Professional Paper 422-M: 40 pp.
  • Singh, V.P & Quiroga, A.C., 1988: Dimensionless analytical solutions for dam-break erosion. J. Hydraulics Res. 26 (2): 179-197.
  • Teisseyre, A.K., 1988: Recent overbank deposits of the Sudetic valleys, SW Poland. Part III: Subacrially and subaqueously deposited over¬bank sediments in the light of field experiment (1977-1979). Geol. Sudetica 23 (2): 1-52.
  • Walder, J.S. & O’Connor, J.E., 1997: Methods for predicting peak discharge of floods caused by failure of natural and constructed earthen dams. Water Resources Research 33 (10): 2337-2348.
  • Zwoliński, Z., 1992: Sedimentology and geomorphology of overbank flows of meandering river floodplains. Geomorphology 4: 367-379.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-c11e804f-fc0e-483b-a785-0b4dc15fac69
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