MAGNITUDE AND RECURRENCE INTERVALS OF BANKFULL DISCHARGE IN RIVERS OF BASALTIC PLATEAU, PARANA STATE, SOUTHERN BRAZIL
DOI:
https://doi.org/10.14393/BGJ-v14n2-a2023-71238Keywords:
Planície aluvial; Dique marginal; Rio entalhado.Abstract
The objective of this work is to estimate the magnitudes of bankfull discharge (Qbf) and the respective recurrence interval (RI) in fluviometric stations located in the West and Southwest regions of Paraná state, southern Brazil. The study area is located in a homogeneous region with common physiographic characteristics (geological, geomorphological and climatic). The bankfull stage was defined in the field by topographic survey based on the average height of natural levees in shallow incised channels and aluvial break in deep incised channels. The corresponding Qbf was calculated using rating curve equation. RI was estimated by the Log-Pearson III distribution. The catchment area in 16 fluviometric stations analyzed ranged from 336 to 17,400 km2 and the estimated Qbf ranged from 77.7 to 2,580 m3/s respectively. The values of RI of bankfull ranged from 1.05 to 1.80 years with an average value of 1.34 years.
Downloads
References
AGÊNCIA NACIONAL DE ÁGUAS E SANEAMENTO BÁSICO (ANA) Dados de vazões e cotas. Disponível em: <http://hidroweb.ana.gov.br>. Acessado em dezembro de 2016.
AHILAN, S.; O’SULLIVAN, J.J.; BRUEN, M.; BRAUDERS, N.; HEALY, D. Bankfull discharge and recurrence intervals in Irish rivers. Proceedings of the Institution of Civil Engineers, Water Management, v. 166, n.7, p 381-393. 2013.
ALVARES, C.A.; STAPE, J.L.; SENTELHAS, P.C.; DE MORAES, G.; LEONARDO, J.; SPAROVEK, G. Köppen's Climate Classification Map for Brazil. Meteorologische Zeitschrift, v. 22, n. 6, p.711-728. 2013.
BEECHIE, T.J.; POLLOCK, M.M.; BAKER, S. Channel incision, evolution and potential recovery in the Walla Walla and Tucannon River basins, northwestern USA. Earth Surface Processes and Landforms, v. 33, p. 784–800. 2008.
BLANTON, K.; MOSSA, J.; KIEFER, J.; WISE, W. Bankfull indicators in Small Blackwater streams in Peninsular Florida reliability and relations with hydrology. Southeastern Geographer, v. 50, n. 4, p. 422-444. 2010.
BOBÉE, B.; CAVADIAS, G.; ASHKAR, F.; BERNIER, J.; RASMUSSEN, P. Towards a systematic approach to comparing distributions used in floods frequency analysis. Journal of Hydrology, v. 142, n 1-2, p.121-136. 1993,
CASTRO, J.M.; JACKSON, P.C. Bankfull discharge recurrence intervals and regional hydraulic geometry relationships: patterns in the Pacific Northwest, USA. Journal of the American Water Resources Association, v. 37, p. 1249-1262. 2001.
DUNNE, T.; LEOPOLD, L.B. Water in Environmental Planning. W.H. Freeman Co., San Francisco, CA. 1978.
DURY, G.H. Bankfull discharge: an example of its statistical relationship. Bulletin of the International Association of Scientific Hydrology, v. 6, n 3, p. 48–55. 1961.
DURY, G.H. Underfit streams: retrospect, perspect and prospect. In: River channels. (Ed. K.J. Gregory). Chichester, Willey, p. 281–293. 1977.
EMMETT, W.W.; WOLMAN, M.G. Effective discharge and gravel-bed rivers, Earth Surface Processes and Landforms, v. 26, p. 1369-1380. 2001.
FERNANDEZ, O.V.Q. Bankfull hydraulic geometry relationships for rivers and streams of the Western and Southwest regions of Paraná State, Brazil. Journal of Geography and Earth Sciences, v. 5, n.1, p. 50-63. 2017.
FRANCO-MAGALHÃES, A.O.B.; HACKSPACHER, P.C.; SAAD, A.R. Exumação tectônica e reativação de paleolineamentos no Arco de Ponta Grossa: termocronologia por traços de fissão em apatitas. Revista Brasileira de Geociências, v. 40, n.2, p. 184-195, 2010.
GRANT, G.E.; SWANSON F.J.; WOLMAN M.G. Pattern and origin of stepped-bed morphology in high-gradient streams, Western Cascades, Oregon. Geological Society of America Bulletin, v. 102, n. 3, p. 340–352. 1990.
HARRELSON, C.C.; RAWLINS, C.L.; POTYONDY, J.P. Stream channel reference sites: an illustrated guide to field technique. General Report No RM-245. U.S. Department of Agriculture. Forest Service, Fort Collins, Colorado, 61 p. 1994.
HARVEY, A.M. Channel capacity and the adjustment of streams to hydrologic regime. Journal of Hydrology, v. 8, p. 82-98. 1969.
IAPAR (Instituto Agronômico do Paraná) Cartas climáticas do Estado do Paraná. Londrina, Paraná. 2000.
IAT (Instituto Água e Terra) Bacias hidrográficas. Disponível em: https://www.iat.pr.gov.br/. Acessado em fevereiro de 2022.
KNIGHTON, D. Fluvial forms and processes: a new perspective. London. Arnold. 1998.
LEOPOLD, L.B. A view of the river. Cambridge, Massachusetts: Harvard University Press, 320 p. 1994.
LEOPOLD, L.B.; EMMETT, W.E.; SILVEY, H.L.; ROSGEN. D.L. A guide for field identification of bankfull stage in the Western United States (video). USDA Forest Service, Rocky Mountain Forest and Range Experiment Station, Stream Systems Technology Center. Fort Collins, Colorado. 1995.
LEOPOLD, L.B.; WOLMAN, M.G.; MILLER, J.P. Fluvial processes in geomorphology. New York, Dover Publications Inc., 544 p. 1964.
LINDROTH, E.M.; RHOADS, B.L.; CASTILLO, C.R.; CZUBA, J.A.; GÜNERALP, I.; EDMONDS, D. Spatial variability in bankfull stage and bank elevations of lowland meandering rivers: relation to rating curves and channel planform characteristics. Water Resources Research, v. 56. 2020.
MAACK, R. Geografia Física do Estado do Paraná. Curitiba, Codepar, 350 p. 1968.
McCANDLESS, T.L.; EVERETT, R.A. Maryland stream survey: Bankfull discharge and channel characteristics of streams in the Piedmont hydrologic region. U.S. Fish & Wildlife Service Chesapeake Bay Field Office. Annapolis, MD. 175 p., 2002.
MIDDLETON, B.A. Flood pulsing in Wetlands: restoring the Natural Hydrological Balance. Wiley, Chichester. 320 p. 2002.
MINEROPAR S. A. Atlas comentado da geologia e dos recursos minerais do estado do Paraná. Curitiba: Mineropar, 2001.
MOSLEY, M.P. Semi-determinate hydraulic geometry of river channels, South Island, New Zealand. Earth Surface Processes and Landforms, v. 6, p. 127-137. 1981.
NARDY, A.J.R.; OLIVEIRA, M.A.F.; BETANCOURT, R.H.S.; VERDUGO, D.R.H.; MACHADO, F.B. Geologia e Estratigrafia da Formação Serra Geral. Geociências, v. 21, n. ½, p. 15-32. 2002.
NAVRATIL, O.; ALBERT, M.B.; BREIL, P. Test of three methods to detect the overbank flow from water level time-series analysis. Hydrological Processes, v. 24, p. 2452-2464. 2010.
NERILO, N.; MEDEIROS, P.A.; CORDERO, A. Chuvas intensas no estado de Santa Catarina. UFSC, Florianópolis - SC, 156 p. 2002.
NRCS (Natural Resources Conservation Service) Log-pearson frequency analysis spreadsheet. Disponível em: <https://www.nrcs.usda.gov/wps/PA_NRCSConsumption/download?cid=stelprdb1256265&ext=xlsx>. Acessado em fevereiro de 2022.
PETIT, F.; PAUQUET, A. Bankfull discharge recurrence interval in gravel-bed rivers. Earth Surface Processes and Landforms, v. 22, n. 7, p. 685–693. 1997.
PICKUP, G.; WARNER, R.F. Effects of hydrologic regime on magnitude and frequency of dominant discharge. Journal of Hydrology, v. 29, p. 51-75. 1976.
RADECKI-PAWLIK, A. Bankfull discharge in mountain streams: theory and practice. Earth Surface Processes and Landforms, v. 27, p. 115-123. 2002.
RADECKI-PAWLIK, A.; SKALSKI, T. Bankfull discharge determination using the new Invertebrate Bankfull Assessment Method. Journal of Water and Land Development, v. 12, p. 145–153. 2008.
RAZAVI, T; COULIBALY, P. Streamflow prediction in ungauged basins: review of regionalization methods. Journal of Hydrologic Engineering, v. 18, n. 8, p. 958-975. 2013.
RICHARDS, K. Rivers, Form and Process in Alluvial Channels. Methuen, 358 p. 1982.
ROSGEN, D.L. A classification of natural rivers. Catena, v. 22, p. 169-199. 1994.
ROSGEN, D.L. Applied river morphology. Pagosa Springs, Colorado, Wildland Hydrology, 388 p. 1996.
SANTOS, L.J.C.; OKA FIORI, C.; CANALI, N.E.; FIORI, A.P.; SILVEIRA, C.T.; SILVA, J.; ROSS, J.L.S. Mapeamento geomorfológico do estado do Paraná. Revista Brasileira de Geomorfologia, v. 7, p. 3-12. 2006.
SILVA, E.S.; TRINCA, L.A.; NERY, J.T. Áreas espacialmente homogêneas de níveis de precipitação nas regiões Sudeste e Sul do Brasil. Revista Energia na Agricultura, V. 24, n. 3, p. 34-59. 2009.
TURNER, S.; REGELOUS, M.; KELLEY, S.; HAWKESWORTH, C.J.; MANTOVANI, M. S.M. Magmatism and continental break-up in the South Atlantic: high precision 40Ar-39Ar geochronology. Earth and Planetary Science Letters, v. 121, p. 333-348. 1994.
Van CAMPENHOUT, J.; HOUBRECHTS, G.; PEETERS, A.; PETIT, F. Return period of characteristic discharges from the comparison between partial duration and annual series, application to the Walloon Rivers (Belgium). Water, v. 12, 792. 2020.
VERRY, E.S. A guide to identification of bankfull stage in the Northeastern United States (video). USDA Forest Service, Stream Systems Technology Center. Fort Collins, Colorado. 2005.
WILKERSON, G.V. Improved bankfull discharge prediction using 2-year recurrence-period discharge. Journal of the American Water Resources Association, v. 44, n. 1, p. 244-258. 2008.
WILLIAMS, G.P. Bank-full discharge of rivers. Water Resources Research, v. 14, p. 1141-1153. 1978.
WMO (World Meteorological Organization) Guide to climatological practices, Geneva. 153 p. 2018.
WOHL, E.E. Mountain rivers revisited. American Geophysical Union. Washington. 2010.
WOHL, E.E.; WILCOX, A. Channel geometry of mountain streams in New Zealand. Journal of Hydrology, v. 300, p. 252-266. 2005.
WOLMAN, M.G.; EMMETT, W.E.; VERRY, E.S.; MARION, D.A.; SWIFT, L.W.; KAPPESSER, G.B. Identifying bankfull stage in forested streams in the Eastern United States (video). USDA Forest Service, Stream Systems Technology Center. Fort Collins, Colorado. 2003.
WOLMAN, M.G.; LEOPOLD, L.B. River flood plains: some observations on their formation. Profissional Paper, United States Geological Survey, 282C, 87-107. 1957.
WOODYER, K.D. Bankfull frequency in rivers. Journal of Hydrology, v. 6, p. 114-142. 1968.
XIA, J.; WU, B.; WANG, G.; WANG, Y. Estimation of bankfull discharge in the Lower Yellow River using different approaches. Geomorphology, v. 117, n. 1–2, p. 66–77. 2009.
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 2023 Oscar Vicente Quinonez Fernandez
This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.
All copyrights are reserved to authors. Reproductions of any part of this journal, including the non-commercial use of figures, maps and other illustrations, are allowed provided that the original source of publication be assigned.
