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Wyszukujesz frazę "river levee" wg kryterium: Temat


Wyświetlanie 1-4 z 4
Tytuł:
Geodetic monitoring of earth-filled flood embankment subjected to variable loads
Autorzy:
Kuras, P.
Ortyl, Ł.
Owerko, T.
Borecka, A.
Tematy:
flood embankment
river levee
geodetic monitoring
control network
displacements
wał przeciwpowodziowy
monitoring geodezyjny
sieć sterowania
przemieszczenia
Pokaż więcej
Wydawca:
Politechnika Warszawska. Wydział Geodezji i Kartografii
Powiązania:
https://bibliotekanauki.pl/articles/106723.pdf  Link otwiera się w nowym oknie
Opis:
The article presents an example of supplementing geotechnical monitoring with geodetic observations. The experimental flood embankment built within the ISMOP project (Information Technology System of Levee Monitoring) was subjected to continuous monitoring based on built-in measuring sensors. The results of geodetic monitoring used for observation of earth-filled flood embankment subjected to external loads are presented in the paper. The tests were carried out on an experimental flood embankment forming a closed artificial water reservoir. The observations were carried out for two purposes. The first was long-term monitoring, which was aimed to determine the behaviour of the newly built embankment. The second purpose was to check the reaction of the levee to the simulated flood wave, caused by filling and draining the reservoir. In order to monitor the displacements of the earth-filled embankment, it was necessary to develop the proper methodology. For the needs of research works, an appropriate network of 5 reference points and 48 survey markers has been designed and established. The periodic measurements were carried out using precise robotic total station. The stability of the reference frame was each time checked and displacements of survey markers were determined based on it. The final results allow to reveal the reaction of levee to external loads. The displacement values were referred to the course of the filling and draining experiment to indicate the relationship between them. In the field of long-term monitoring the results clearly imply the dominance of displacements outside the reservoir for points located on the embankment, in contrast to points on the crest and foreground, which do not show significant movements. On the other hand, in the field of testing the embankment reaction to the flood wave, obtaining reliable results was possible thanks to high-accuracy geodetic measurements. Small displacement values, often at the level of their determination errors, were averaged for groups of points with the same height of foundation. A sizable number of points allows to perceive some tendencies and the relation between embankment soaking and its movement directions can be noticed. During periods when the levee was still saturated with water, slight movements outside the reservoir were revealed. On the other hand, the following period of drying caused movement in the opposite direction.
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zastosowanie metody konduktometrycznej do typowania stref o zmiennych parametrach filtracyjnych w obrębie podstawy wału przeciwpowodziowego
Application of the conductivity methods to select zones with variable filtration parameters around the base of river levee
Autorzy:
Cygal, A.
Stefaniuk, M.
Kret, A.
Klityński, W.
Tematy:
metody konduktometryczne
wał przeciwpowodziowy
przebicie hydrauliczne
geofizyka niesejsmiczna
conductivity methods
river levee
subsurface erosion
non-seismic geophysics
Pokaż więcej
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:
https://bibliotekanauki.pl/articles/2075405.pdf  Link otwiera się w nowym oknie
Opis:
The need to continuously monitor the flood embankment is necessary to introduce the measurement methods which give quick results in crisis situations. The protection of embankments as well as the prevention from floods are not only associated with the examination of the body river levee. Experience suggests that one of the problems involves the unknown geotechnical conditions of the levee base. Unfortunately, point geotechnical surveys carried out with a big measurement step were not able to fully identify the lithology variation over larger areas. This is caused by the high cost of drilling shallow wells. The application of non-invasive geophysical methods allows the completion of geotechnical research, and supplies additional information about the variability of geological medium. The structure in the area of the former river beds creates favorable conditions for carrying out geophysical surveys dependent on the variability of geoelectrical properties of rocks. This problem is solved by the use of conductivity method on the 100 m long part of the flood bank. This is recommended for quick and non-invasive measurements. A complex interpretation of geotechnical, hydrogeological and geophysical data provided information about the variability of geoelectrical parameters over this area and therefore made it possible to identify areas prone for greater filtration during high water levels.
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Floodplain forms along the lowland Maros River, Hungary
Geographia Polonica Vol. 93 No. 1 (2020)
Autorzy:
Kiss, Tímea. Autor
Fiala, Károly. Autor
Fehérváry, István. Autor
Balogh, Márton. Autor
Wydawca:
IGiPZ PAN
Powiązania:
Urdea, P., Sipos, Gy., Kiss, T., Onaca, A. (2012). River Maros. In Sipos, Gy. (Ed.), A Maros folyó múltja, jelene, jövője (pp. 9-32). Szeged: SZTE.
Zwoliński, Z. (1992). Sedimentology and geomorphology of overbank flows on meandering river floodplains. Geomorphology, 4(6), 367-379. https://doi.org/10.1016/0169-555X(92)90032-J
Blanka, V., Sipos, Gy., Kiss, T. (2006). Spatial and temporal changes of meander formation on the Hungarian section of the River Maros. In Kertész, Á., Dövényi, Z., Kocsis, K., (Eds.), III. Magyar Földrajzi Konferencia (pp. 1-10), Budapest: MTA-FKI. [in Hungarian]
Brierley, G.J., Ferguson, R.J., Woolfe, K.J. (1997). What is a fluvial levee? Sedimentary Geology, 114(1-4), 1-9. https://doi.org/10.1016/S0037-0738(97)00114-0
Wolman, M.G., Leopold, L.B. (1957). River floodplains: Some observations on their formation. USGS Professional Papers, 282C, 87-107. https://doi.org/10.3133/pp282C
Gábris, Gy., Telbisz, T., Nagy, B., Belardinelli, E. (2002). Accumulation of the floodplain of the Tisza and its geomorphological background. Vízügyi Közlemények, 84, 305-318. [in Hungarian]
Wierzbicki, G., Ostrowski, P., Mazgajski, M., Bujakowski, F. (2013). Using VHR multispectral remote sensing and LIDAR data to determine the geomorphological effects of overbank flow on a floodplain (the Vistula River, Poland). Geomorphology, 183, 73-81. https://doi.org/10.1016/j.geomorph.2012.06.020
Schweitzer, F., Nagy, I., Alföldi, L. (2002). Recent point-bar formation and floodplain accumulation on the Middle-Tisza. Földrajzi Értesítő, 51(3-4), 257-278. [in Hungarian]
Fisk, H.N. (1947). Fine-grained alluvial deposits and their effects on Mississippi River activity. Vicksburg, Miss.: Waterways Experiment Station, Mississippi River Commission.
Ihrig, D. (1973). History of the river regulations in Hungary. Budapest: Országos Vízügyi Hivatal. [in Hungarian]
Cazanacli, D., Smith, N.D. (1998). A study of morphology and texture of natural levees, Cumberland Marshes, Saskatchewan, Canada. Geomorphology, 25, 43-55. https://doi.org/10.1016/S0169-555X(98)00032-4
Bogárdi, J. (1971). Sediment transport of rivers. Budapest, Hungary: Akadémiai Kiadó. [In Hungarian].
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Klasz, G., Reckendorfer, W., Gabriel, H., Baumgartner, C., Schmalfuss, R., Gutknecht, D. (2014). Natural levee formation along a large and regulated river: The Danube in the National Park Donau-Auen, Austria. Geomorphology, 215, 20-33. https://doi.org/10.1016/j.geomorph.2013.12.023
Wolfert, H.P., Hommel, P.W.F.M., Prins, A.H., Stam, M.H. (2002). The formation of natural levees as a disturbance process significant to the conservation of riverine pastures. Landscape Ecology, 17(1), 47-57. https://doi.org/10.1023/A:1015229710294
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Kiss, T. (2014). Alterations of fluvial processes due to anthropogenic impacts: Study on Equilibrium and sensitivity in fluvial environment. University of Szeged, Hungary. (Doctoral dissertation, in Hungarian
Kiss, T., Oroszi, V.G., Sipos, G., Fiala, K., Benyhe, B. (2011). Accelerated overbank accumulation after nineteenth century river regulation works: A case study on the Maros River, Hungary. Geomorphology 135, 191-202. https://doi.org/10.1016/j.geomorph.2011.08.017
Kiss, T., Balogh, M., Fiala, K., Sipos, Gy. (2018). Morphology of fluvial levee series along a river under human influence, Maros River, Hungary. Geomorphology, 303, 309-321. https://doi.org/10.1016/j.geomorph.2017.12.014
Kiss, T., Blanka, V. (2012). River channel response to climate- and human-induced hydrological changes: Case study on the meandering Hernád River, Hungary. Geomorphology, 175-176, 115-125. https://doi.org/10.1016/j.geomorph.2012.07.003
Chalov, R.S. (2004). Morphological expressions of river sediment transport and their role in channel processes. IAHS Publication, 288, 205-211.
Sipos, Gy. (2006). Review on the dynamic of the riverbed: case study on the Hungarian section of the River Maros. (PhD dissertation), Szeged: SZTE. (in Hungarian)
Branß, T., Dittrich, A., Núñez-González, F. (2016). River flow. In Constantinescu G., Garcia M., Hanes D. (Eds.), Reproducing natural levee formation in an experimental flume (pp. 1122-1128.), London: Taylor & Francis Group. https://doi.org/10.1201/9781315644479-178
Happ, S., Rittenhouse, G., Dobson, G. (1940). Some principles of accelerated stream and valley sedimentation. Technical Bulletin, 695, US Department of Agriculture.
Asselman, N.E.M., Middelkoop, H. (1998). Temporal variability of contemporary floodplain sedimentation in the Rhine-Meuse Delta, the Netherlands. Earth Surface Processes and Landforms, 23, 595-609. https://doi.org/10.1002/(sici)1096-9837(199807)23:7<595::aid-esp869>3.0.co;2-y
Steiger, J., Tabacchi, E., Dufour, S., Corenblit, D., Peiry, J.L. (2005). Hydrogeomorphic processes affecting riparian habitat within alluvial channel-floodplain river systems: A review for the temperate zone. River Research and Applications, 21, 719-737. https://doi.org/10.1002/rra.879
Nanson, G.C. (1986). Episodes of vertical accretion and catastrophic stripping: A model of disequilibrium flood-plain development. Geological Society of America Bulletin, 97, 1467-1475. https://doi.org/10.1130/0016-7606(1986)97<1467:eovaac>2.0.co;2
Łajczak, A., Plit, J., Soja, R., Starkel, L., Warowna, J. (2006). Changes of the Vistula River channel and floodplain in the last 200 Years. Geographia Polonica 79(2), 65-88.
Notebaert, B., Verstraeten, G., Govers, G., Poesen, J. (2009). Qualitative and quantitative applications of LiDAR imagery in fluvial geomorphology. Earth Surface Processes and Landforms, 34, 217-231. https://doi.org/10.1002/esp.1705
Blanka, V., Kiss, T. (2006). Case study on meander development of the downstream section of River Maros. Hidrológiai Közlöny 86(4), 19-22. [in Hungarian]
Gomez, B., Phillips, D., Magilligan, F.J., James, L.A. (1997). Floodplain sedimentation and sensitivity: Summer 1993 flood, Upper Mississippi Valley. Earth Surface Processes and Landforms, 22, 923-936. https://doi.org/10.1002/(sici)1096-9837(199710)22:10<923::aid-esp763>3.0.co;2-e
Smith, N.D., Pérez-Arlucea, M. (2008). Natural levee deposition during the 2005 flood of the Saskatchewan River. Geomorphology, 101, 583-594. https://doi.org/10.1016/j.geomorph.2008.02.009
Bridge, J.S. (2003). Rivers and floodplain: Form, processes, and sedimentary record. Oxford: Blackwell.
Dietrich, W.E., Wilson, C.J., Reneau, S.L. (1986). Hollows, colluvium, and landslides in soil-mantled landscapes. In Abrahams, A.D. (Ed.), Hillslope processes (pp. 361-388). Boston: Allen and Unwin.
Nanson, G.C., Croke, J.C. (1992). A genetic classification of floodplains. Geomorphology, 4, 459-486. https://doi.org/10.1016/0169-555x(92)90039-q
Sándor, A. (2011). Review on the process of floodplain accumulation: case study on the Middle- and Lower-Tisza. (PhD dissertation), Szeged: SZTE. [in Hungarian]
Lane, S.N., Westaway, R.M., Hicks, D.M. (2003). Estimation of erosion and deposition volumes in a large gravel-bed, braided river using synoptic remote sensing. Earth Surface Processes and Landforms 28, 249-271. https://doi.org/10.1002/esp.483
Taylor, C. (2002). Recognising channel and floodplain forms. Water & Rivers Commision, Report No. RR17. Perth, Australia.
Hudson, P.F., Heitmuller, F.T. (2003). Local and watershed-scale controls on the spatial variability of natural levee deposits in a large fine-grained floodplain: lower Pánuco Basin, Mexico. Geomorphology, 56, 255-269. https://doi.org/10.1016/s0169-555x(03)00155-7
Brown, A.G. (1983). An analysis of overbank deposits of a flood at Blandford-Forum, Dorset, England. Revue Geomorphologie Dynamique, 32(3), 95-99.
Kiss, T., Sándor, A., Gresó, Zs. (2004). Investigations on the rate of floodplain sediment accumulation in the Mártély embayment of the Lower Tisza. Acta Universitatis Szegediensis Acta Geographica, 38, 15-26.
Allen, J.R.L. (1965). A review of the origin and characteristics of recent alluvial sediments. Sedimentology, 5, 89-191. https://doi.org/10.1111/j.1365-3091.1965.tb01561.x
Gregory, K.J. (2004). Human activity transforming and designing river landscapes: A review perspective. Geographia Polonica, 77(2), 5-20.
Laczay, I. (1975). River system of the Maros. In Vízrajzi Atlasz, 19 (pp. 4-23). Budapest: VITUKI. [in Hungarian]
Sagar, S.D. (2013). Improved Floodplain Delineation Method Using High-Density LiDAR Data. ComputerAided Civil and Infrastructure Engineering, 28(1), 68-79. https://doi.org/10.1111/j.1467-8667.2012.00774.x
Sorrells, R.M. (2012). Hydrogeomorphology of alluvial benches in an anabranching reach of the upper Yadkin River, North Carolina. (PhD dissertation), Greensboro: University of North Carolina.
Bown, T.M., Kraus, M.J. (1987). Integration of channel and floodplain suites, I. Developmental sequence and lateral relations of alluvial paleosols. Journal of Sedimentary Petrology, 57, 587-601. https://doi.org/10.1306/212f8bb1-2b24-11d7-8648000102c1865d
Keen-Zebert, A., Tooth, S., Rodnight, H., Duller, G.A.T., Roberts, H.M., Grenfell, M. (2013). Late Quaternary floodplain reworking and the preservation of alluvial sedimentary archives in unconfined and confined valleys in the eastern interior of South Africa. Geomorphology, 185, 54-66. https://doi.org/10.1016/j.geomorph.2012.12.004
Kiss, T., Nagy, Z., Balogh, M. (2017). Floodplain level development induced by human activity - case study in the Lower Maros/Mures River, Romania and Hungary. Carpathian Journal of Earth and Environmental Sciences, 12 (1), 83-93.
Lóczy, D. (2013). Geomorphological classifications of floodplains in international scientific papers. Földrajzi Közlemények, 137, 105-120. (in Hungarian)
Sipos, Gy., Kiss, T., Fiala, K. (2007). Morphological alterations due to channelization along the Lower Tisza and Maros Rivers (Hungary). Geografia Fisica e Dinamica Quarternaria, 30, 239-247.
Geographia Polonica
Brierley, G.J., Hickin, E.J. (1992). Floodplain development based on selective preservation of sediments, Squamish River, British Columbia. Geomorphology 4, 381-391. https://doi.org/10.1016/0169-555X(92)90033-K
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Radecki-Pawlik, A., Wyżga, B., Czech, W., Mikuś, P., Zawiejska, J., & Ruiz-Villanueva, V. (2016). Modelling hydraulic parameters of flood flows for a Polish Carpathian river subjected to variable human impacts. In Kundzewicz Z., Stoffel M., Niedźwiedź T., Wyżga B. (Eds.), Flood Risk in the Upper Vistula Basin. GeoPlanet: Earth and Planetary Sciences. Springer, Cham GeoPlanet: Earth and Planetary Sciences (pp. 127-151). Cham: Springer. https://doi.org/10.1007/978-3-319-41923-7_7
Opis:
24 cm
The floodplain forms of lowland rivers act as fluvial archives, as their morphology, material and spatial characteristics refer to the hydromorphological changes of the river and (dis)connectivity of the alluvial system. The aims of the research are (1) to identify natural levees, crevasses, and point-bars on the Hungarian floodplain section of the Maros River, (2) to measure their morphometric parameters, and (3) to analyse their spatial and temporal variations in connection with various human impacts. Six genetic types of natural levees and pointbar systems developed as the result of various human impacts, thus the development of the forms terminated or became laterally limited.
Dostawca treści:
RCIN - Repozytorium Cyfrowe Instytutów Naukowych
Książka
Tytuł:
Men at a construction of the bridge] [An iconographic document
Mężczyźni przy budowie mostu] [Dokument ikonograficzny
Opis:
Według właścicielki zdjęcia przedstawia ono pracę przy budowie mostu oraz przy utrwalaniu wałów ochronnych wzdłuż rzeki Prosna w Robakowie w 1930 r., gdzie zatrudnił się jej teść. Po powrocie z wojska zamieszkał wspólnie z żoną w Racendowie pracując u Niemca Janinga, za co otrzymywał 1 zł dziennie. Ponieważ na świat przychodziły kolejne dzieci, teść musiał dorabiać. Wyruszył do Robakowa pieszo (około 30 km od Racendowa) by tam znaleźć pracę. Pracował w jednej z dwóch grup: każda pracowała przez miesiąc a następnie zmieniała ją druga
Zdjęcie przesłane na konkurs "Fotografia polskiej wsi" do 1948 roku, organizowany w 1983 r. przez kwartalnik "Fotografia" i tygodnik "Nowa Wieś". Odbitka zdjęcia przechowywana w Instytucie Archeologii i Etnologii PAN (dawniej Instytut Historii Kultury Materialnej)
1930 rok, Robakowo
Fotografia przedstawia kilkunastu mężczyzn stojących przy drewnianej konstrukcji i zajętych pracą. Ubrani są w odzież roboczą. Po ich prawej stronie, osobno stoi mężczyzna w kurtce i kapeluszu. Po lewej stronie wśród robotników wyróżnia się starannym ubiorem (elegancka skórzana kurtka, koszula z krawatem, maciejówka) mężczyzna, być może nadzorca robót
The photo sent to the contest named “Photography of the Polish village pre-1948” organized in 1983 by the quarterly “Fotografia” (Photography) and the weekly “Nowa Wieś” (New village). Copy of the photo kept at the Institute of Archaeology and Ethnology of the Polish Academy of Sciences (former Institute for the History of Material Culture)
Dostawca treści:
RCIN - Repozytorium Cyfrowe Instytutów Naukowych
Inne
    Wyświetlanie 1-4 z 4

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