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River erosion is a complex process due to multiple factors, such as climate changes, discharge quantity, the type of transported sediments, and variations in the hydrological regime. This paper aims to analyse river erosion's impact on transport elements' stability (especially on bridges). To do so, a Geomorphic Change Detection analysis was used, which involves calculating the altitude differences between two successive digital models, as a basis for calculating surfaces and volumes of sediments displaced through the erosion process. This analysis was doubled by a series of cross-sections in the proximity of bridges to observe the current river bed configuration and identify the active processes. The variation of these processes is directly dependent on human interventions undertaken to reduce the erosion process and to protect the infrastructure elements. The bridges located in the studied area are in different stages of damage by lateral and depth erosion processes, depending on their intensity and the human interventions made to protect these bridges. The least affected are the bridges where complex measures have been taken (construction of bed sills) or the dynamic processes have a low intensity.
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Tom
Strony
137--145
Opis fizyczny
Bibliogr. 26 poz., rys.
Twórcy
autor
- Geomorphology-Pedology-Geomatics Department, Faculty of Geography, University of Bucharest, Romania
autor
- Geomorphology-Pedology-Geomatics Department, Faculty of Geography, University of Bucharest, Romania
autor
- Geomorphology-Pedology-Geomatics Department, Faculty of Geography, University of Bucharest, Romania
autor
- Geomorphology-Pedology-Geomatics Department, Faculty of Geography, University of Bucharest, Romania
autor
- Geomorphology-Pedology-Geomatics Department, Faculty of Geography, University of Bucharest, Romania
Bibliografia
- Abbe, T.B., Montgomery, D.R. (2003). Patterns and Processes of Wood Debris Accumulation in the Queets River Basin, Washington. Geomorphology, 51(1-3), 81-107. https://doi.org/10.1016/S0169-555X(02)00326-4
- Addiscott, T.M., Tuck, G. (2015). Sensitivity Analysis for Regional-Scale Solute Transport Modeling. Book Series: Soil Science Society of America, Inc. 153-62. https://doi.org/10.2136/sssaspecpub48.c8
- Camporeale, C., Perona, P., Porporato, A., Ridolfi, L. (2005). On the Long‐term Behavior of Meandering Rivers. Water Resources Research, 41(12). https://doi.org/10.1029/2005WR004109
- Coulthard, T.J., Van De Wiel, M.J. (2012). Modelling River History and Evolution. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 370(1966), 2123-42. https://doi.org/10.1098/rsta.2011.0597
- Dobre, R.R. (2016). Relația Dinamica Reliefului – Infrastructura de Transport. Bucharest: Editura Etnologică.
- Dobre, R.R. (2009). Pretabilitatea Reliefului Pentru Căi de Comunicație Și Transport În Culoarul Prahovei. Bucharest: University of Bucharest.
- Gurnell, A.M. (1997). Channel Change on the River Dee Meanders, 1946-1992, from the Analysis of Air Photo-graphs. Regulated Rivers: Research & Management, 13(1), 13-26.
- https://doi.org/10.1002/(SICI)1099-1646(199701)13:1<13::AID-RRR420>3.0.CO;2-W
- Gurnell, A.M., Walter, Bertoldi, Dov Corenblit. (2012). Changing River Channels: The Roles of Hydrological Processes, Plants and Pioneer Fluvial Landforms in Humid Temperate, Mixed Load, Gravel Bed Rivers. Earth-Science Reviews, 111(1-2), 129-41. https://doi.org/10.1016/j.earscirev.2011.11.005
- Ielenicz, M., Pătru, I., Ghincea, M. (2003). Subcarpații României. Bucharest: Editura Universitară.
- Kleinhans, M.G. (2010). Sorting out River Channel Patterns. Progress in Physical Geography: Earth and Environment, 34(3), 287-326. https://doi.org/10.1177/0309133310365300
- Lane, S.N., Richards, K.S. (1997). Linking River Channel Form and Process: Time, Space and Causality Revisited. Earth Surface Processes and Landforms, 22(3), 249-60.
- https://doi.org/10.1002/(SICI)1096-9837(199703)22:3<249::AID-ESP752>3.0.CO;2-7
- Latrubesse, E.M., Stevaux, J.C., Sinha, R. (2005). Tropical Rivers. Geomorphology, 70(3-4), 187-206. https://doi.org/10.1016/j.geomorph.2005.02.005
- Liébault, F., Piégay, H. (2002). Causes of 20th Century Channel Narrowing in Mountain and Piedmont Rivers of Southeastern France. Earth Surface Processes and Landforms, 27(4), 425-44. https://doi.org/10.1002/esp.328
- Paunescu, C., Dobre, R., Comănescu, L., Drăghici, T., Nedelea, A. (2021). GIS as a Support Tool for Sensitivity and Decision-Making Analysis for Transport Infrastructure Development. Rocznik Ochrona Środowiska, 23, 23-41. https://doi.org/10.54740/ros.2021.002
- Rădoane, M., Pandi, G., Rădoane, N. (2010). Contemporary Bed Elevation Changes from the Eastern Carpathians. Carpathian Journal of Earth and Environmental Sciences, 5(2), 49-60.
- Rinaldi, M. (2003). Recent Channel Adjustments in Alluvial Rivers of Tuscany, Central Italy. Earth Surface Pro-cesses and Landforms, 28(6), 587-608. https://doi.org/10.1002/esp.464
- Schumm, S.A. (1969). River Metamorphosis. Journal of the Hydraulics Division, 95(1), 255-74. https://doi.org/10.1061/JYCEAJ.0001938
- Surian, N., Cisotto, A. (2007). Channel Adjustments, Bedload Transport and Sediment Sources in a Gravel‐bed River, Brenta River, Italy. Earth Surface Processes and Landforms, 32(11), 1641-56. https://doi.org/10.1002/esp.1591
- Surian, N., Rinaldi, M. (2003). Morphological Response to River Engineering and Management in Alluvial Chan-nels in Italy. Geomorphology, 50(4), 307-26. https://doi.org/10.1016/S0169-555X(02)00219-2
- Swanson, B.J., Meyer, G.A., Coonrod, J.E. (2011). Historical Channel Narrowing along the Rio Grande near Albu-querque, New Mexico in Response to Peak Discharge Reductions and Engineering: Magnitude and Uncer-tainty of Change from Air Photo Measurements. Earth Surface Processes and Landforms, 36(7), 885-900. https://doi.org/10.1002/esp.2119
- Winterbottom, S.J. (2000). Medium and Short-Term Channel Planform Changes on the Rivers Tay and Tummel, Scotland. Geomorphology, 34(3-4), 195-208. https://doi.org/10.1016/S0169-555X(00)00007-6
- Wyżga, B. (2007). 20 A Review on Channel Incision in the Polish Carpathian Rivers during the 20th Century. In: Book series: Developments in Earth Surface Processes, 11, 525-53. https://doi.org/10.1016/S0928-2025(07)11142-1
- Zaharia, L., Grecu, F., Ioana-Toroimac, G., Neculau, G. (2011). Sediment Transport and River Channel Dynamics in Romania – Variability and Control Factors. Sediment Transport in Aquatic Environments, 293-316.
- Zawiejska, J., Wyżga, B. (2010). Twentieth-Century Channel Change on the Dunajec River, Southern Poland: Patterns, Causes and Controls. Geomorphology, 117(3-4), 234-46. https://doi.org/10.1016/j.geomorph.2009.01.014
- Ziliani, L., Surian, N. (2012). Evolutionary Trajectory of Channel Morphology and Controlling Factors in a Large Gravel-Bed River. Geomorphology, 173-174, 104-17. https://doi.org/10.1016/j.geomorph.2012.06.001
- * * *, Pedological Map of Romania, Sc. 1:200.000, ICPA, București, 1978
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-e79720b4-09e2-4460-84d8-7abbb8d3fe13
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