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Journal articles on the topic 'The Vistula and Odra rivers route'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

Woźny, Jacek. "Zabytki archeologiczne w otoczeniu drogi wodnej Wisła-Odra." GEOGRAPHY AND TOURISM 2, no. 2 (2014): 25–31. https://doi.org/10.5281/zenodo.19312.

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Archeological researches along the Vistula ond Odra rivers route, have been carrying out since the second half of the eighteenth century. At first the researches were done by an accident but since the twentieth century they have been done more systematically and professionally. Nowadays, there are 5000 archeological excavation sites along the Vistula ond Odra rivers route, which represent all the settlement phases from the declining years of the Ice Age till the Middle Ages. Most of them are distinctly seen in the landscape. Unfortunately, only a small numer of them have been signed for touris

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2

Czaja, Stanisław W., Robert Machowski, and Mariusz Rzętała. "Floods in the Upper Part of Vistula and Odra River Basins in the 19th and 20th Centuries / Powodzie W Górnej Części Dorzeczy Wisły I Odry W XIX I XX Wieku." Chemistry-Didactics-Ecology-Metrology 19, no. 1-2 (2014): 127–34. http://dx.doi.org/10.1515/cdem-2014-0012.

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Abstract The discussion of floods in this paper covers the section of the Odra River basin from its source down to the mouth of the Nysa Klodzka River and the section of the Vistula River basin down to the Krakow profile. The area of the upper part of Odra River basin is 13,455 km2 and the length of the river bed in this section is ca. 273.0 km. In the reach examined, the Vistula River is 184.8 km long and has a catchment area of approximately 8,101 km2. Geographical and environmental conditions in the upper part of the Vistula and Odra Rivers basins are conducive to floods both in the summer

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3

Suschka, J., S. Ryborz, and I. Leszczynska. "Surface Water and Sediment Contamination in an Old Industrial Region of Poland – Two Critical Examples." Water Science and Technology 29, no. 3 (1994): 107–14. http://dx.doi.org/10.2166/wst.1994.0075.

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The Upper Silesia Region, one of the most industrialized parts of Poland and also one of the oldest industrial regions in the world, has considerably contributed to the water pollution of the Vistula and Odra Rivers, the main watercourses in Poland. Wastewater from ferrous and non-ferrous metal industry, coal mines, coal-fired power and heat generation stations, chemical industry and large amounts of municipal sewage of the four million population have been discharged to the surface water for many years. Most rivers are highly polluted in spite of some remedial action which has been undertaken

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4

Andrulewicz, Eugeniusz, and Bogumila Kaczorek. "Effects of the 1997 flood of the Odra and Vistula rivers (summary)." Deutsche Hydrographische Zeitschrift 50, no. 2-3 (1998): 253. http://dx.doi.org/10.1007/bf02764491.

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5

Parczewski, Michał. "Origins of Early Slav Culture in Poland." Antiquity 65, no. 248 (1991): 676–83. http://dx.doi.org/10.1017/s0003598x00080303.

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The archaeological remains of the Early Slav Culture (ESC), which dates to the 6th and 7th centuries AD, cover a substantial area of Europe ranging from eastern Byelorussia and the Ukraine to central Germany and Lower Austria, and from the Baltic to the Adriatic and Aegean. The Polish area is crucial for the clarification of the extremely unclear origins of the Slav ethnic group and the circumstances of its expansion around the middle of the 1st millennium AD. Traditionally, Polish scholars have viewed the lands lying athwart the basins of the Odra and Vistula rivers as the cradle of Slavia. T

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6

NADŁONEK, W., and I. BOJAKOWSKA. "VARIABILITY OF CHEMICAL WEATHERING INDICES IN MODERN SEDIMENTS OF THE VISTULA AND ODRA RIVERS (POLAND)." Applied Ecology and Environmental Research 16, no. 3 (2018): 2453–73. http://dx.doi.org/10.15666/aeer/1603_24532473.

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7

Dziadziusko, Zbigniew, and Wlodzmierz Krzymiski. "Meteorological origin of the flood and its hydrological effects in the Odra and Vistula Rivers (summary)." Deutsche Hydrographische Zeitschrift 50, no. 2-3 (1998): 259–60. http://dx.doi.org/10.1007/bf02764494.

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8

Wrzesiński, Dariusz, Leszek Sobkowiak, Ileana Mares, Venera Dobrica, and Constantin Mares. "Variability of River Runoff in Poland and Its Connection to Solar Variability." Atmosphere 14, no. 7 (2023): 1184. http://dx.doi.org/10.3390/atmos14071184.

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The aim of this research was to determine relationships between solar activity and variability of discharges of three Central European rivers: the Vistula, Odra and Warta in Poland in the multi-annual period of 1901–2020. Changes in precipitation and air temperature at Poznań meteorological station in the same period were also analyzed. The long-term variations in river runoff were investigated both from the point of view of temporal variability in relation to climate variations in the study area, and from the point of view of linear/non-linear links to solar activity, as described by the Wolf

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9

Piwowarczyk, Renata. "Orobanche purpurea (Orobanchaceae) in Poland: current distribution, taxonomy, plant communities, and preferred hosts." Biodiversity: Research and Conservation 26, no. 1 (2012): 73–81. http://dx.doi.org/10.2478/v10119-012-0006-5.

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Abstract The paper presents the current distribution of Orobanche purpurea s. str. (excl. O. bohemica) in Poland, based on a critical revision of herbarium and literature data as well as results of my field research. Most of the records date back to the 19th or early 20th century and are now historical. Most of them lack also herbarium documentation. Since the 1950s the species has been found in 10 new localities, only partly documented by herbarium specimens. Currently it is present in only 4 localities, in valleys of the Lower Vistula and the Lower Oder (Odra) rivers and in the Silesian-Krak

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10

Kubiak-Wójcicka, Katarzyna, and Sylwia Machula. "Influence of Climate Changes on the State of Water Resources in Poland and Their Usage." Geosciences 10, no. 8 (2020): 312. http://dx.doi.org/10.3390/geosciences10080312.

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The study aims to estimate the amount of available renewable water resources in Poland in the years 1999–2018 and the extent of their use by various sectors of the national economy at the national and regional levels. In the study period, the selected meteorological elements were found to have changed, resulting in a decrease in the flows of the two largest rivers in Poland: the Vistula and the Oder. The outflow of the Vistula and Odra basins determines the size of Poland’s water resources. Poland is classified as a country of low water resources, as evidenced by the per capita amount of surfa

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11

Siepak, J. "Total Organic Carbon (TOC) as a Sum Parameter of Water Pollution in Selected Polish Rivers (Vistula, Odra, and Warta)." Acta hydrochimica et hydrobiologica 27, no. 5 (1999): 282–85. http://dx.doi.org/10.1002/(sici)1521-401x(199911)27:5<282::aid-aheh282>3.0.co;2-2.

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12

Gądek, Wiesław, Tamara Tokarczyk, and Arkadiusz Środula. "Estimation of parametric flood hydrograph determined by means of Strupczewski method in the Vistula and Odra catchments." Journal of Water and Land Development 31, no. 1 (2016): 43–51. http://dx.doi.org/10.1515/jwld-2016-0035.

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AbstractWhile determining theoretical flood hydrographs, different methods of their construction are used depending on the needs of the problem or the scope of the project. It should be remembered that these methods differ mainly with the principle of the waveform averaging, which may be done either according to the flow or time. The hydrographs may be divided into nonparametric (determining on the basis of registered floods) and parametric (using mathematical description of the flood course). One of the analytical methods is Strupczewski method which has two parameters: responsible for the wa

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13

Olszewski, Henryk. "Czy potrzebna nam jeszcze jedna biografia Zygmunta Wojciechowskiego? Pożytek z klasyków." Themis Polska Nova 8, no. 1 (2015): 5–34. http://dx.doi.org/10.15804/tpn2015.1.01.

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Zygmunt Wojciechowski (1900–1955) was a historian of law at the University of Poznan. A student of one of the greatest Polish historians – Oswald Balzer – he was a medievalist, heavily involved in politics both in the times of Second Republic and the beginning of the Polish People’s Republic. His works comprised of content of cognitive qualities, but was always strongly coloured with politics. He was the creator of the theory of native Polish lands, located between Odra, Warta and Vistula Rivers. He is looking at history through the prism of Polish-German relations and he critically evaluates

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14

Piniewski, Mikołaj, Mateusz Szcześniak, Shaochun Huang, and Zbigniew W. Kundzewicz. "Projections of runoff in the Vistula and the Odra river basins with the help of the SWAT model." Hydrology Research 49, no. 2 (2017): 303–17. http://dx.doi.org/10.2166/nh.2017.280.

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Abstract The objective of this paper is to assess climate change impacts on spatiotemporal changes in annual and seasonal runoff and its components in the basins of two large European rivers, the Vistula and the Odra, for future horizons. This study makes use of the Soil and Water Assessment Tool (SWAT) model, set up at high resolution, and driven by a multi-model ensemble (MME) of nine bias-corrected EURO-CORDEX simulations under two representative concentration pathways (RCPs), 4.5 and 8.5. This paper presents a wealth of illustrative material referring to the annual and seasonal runoff (R)

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15

Kalinowski, Marcin, and Rafał Koba. "Technical aspects of the International Waterway E40 – variants of the navigation channel route on the Vistula – Mukhavets section." Biuletyn Instytutu Morskiego 32, no. 1 (2017): 116–22. http://dx.doi.org/10.5604/01.3001.0010.6981.

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Along the international waterway E40, there are many barriers and restrictions that make it difficult or in some cases impossible to conduct regular passenger or freight traffic. The biggest problem is the connection between the Vistula and Mukhavets rivers, and in fact, lack of this connection. Currently, the MDW E40 course on this section on the AGN maps runs along the Bug River, which cannot be considered for revitalization of this waterway for environmental reasons. As a result, research has been undertaken to work out proposals for new alternatives. Three variants of the route have been c

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16

Bihałowicz, Jan Stefan, and Grzegorz Wierzbicki. "Rivers Try Harder. Reversed “Differential Erosion” as Geological Control of Flood in the Large Fluvial Systems in Poland." Water 13, no. 4 (2021): 424. http://dx.doi.org/10.3390/w13040424.

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We study cross-sections on the Detailed Geological Map of Poland (SMGP) to find a geologic and geomorphic pattern under river valleys in Poland. The pattern was found in 20 reaches of the largest Polish rivers (Odra, Warta, Vistula, Narew, and Bug) located in the European Lowland, in the landscape of old (Pleistocene, Saalian) glacial high plains extending between the Last Glacial Maximum (LGM) moraines on the North and the Upland on the South. The Upland was slightly folded and up-faulted during Alpine orogeny together with the thrust of Carpathian nappes and the uplift of Tatra Mts. and Sude

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17

Mańko, Robert, and Norbert Laskowski. "Comparative analysis of the effectiveness of the conceptual rainfall-runoff hydrological models on the selected rivers in Odra and Vistula basins." ITM Web of Conferences 23 (2018): 00025. http://dx.doi.org/10.1051/itmconf/20182300025.

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Identification of physical processes occurred in the watershed is one of the main tasks in hydrology. Currently the most efficient hydrological processes describing and forecasting tool are mathematical models. They can be defined as a mathematical description of relations between specified attributes of analysed object. It can be presented by: graphs, arrays, equations describing functioning of the object etc. With reference to watershed a mathematical model is commonly defined as a mathematical and logical relations, which evaluate quantitative dependencies between runoff characteristics and

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18

Szkoda, Józef, Jan Żmudzki, Agnieszka Nawrocka, and Mirosława Kmiecik. "Toxic elements in free-living freshwater fish, water and sediments in Poland." Bulletin of the Veterinary Institute in Pulawy 58, no. 4 (2014): 589–95. http://dx.doi.org/10.2478/bvip-2014-0091.

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Abstract Samples for analysis were collected from 10 areas, including the major Polish rivers and lakes, with different sources of environmental pollution (industrial, municipal, and farming). The materials was taken from the lakes of Mazury, located in a non-industrialised region, from the Brda River, an area impacted by pig farms, from the lakes of Lipczyno Wielkie/Pomerania, from the Wkra River, an area impacted by poultry farms, from the Dunajec River at the Roznowski Reservoir, from the Vistula River at Cracow and Warsaw, from the Odra River at Wroclaw and the Warta River estuary, and als

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19

Wrzesiński, Dariusz, Andrzej A. Marsz, Anna Styszyńska, Adam Edmund Perz, Wiktoria Brzezińska, and Leszek Sobkowiak. "Spatial Regularities of Changes in the Duration of Low River Flows in Poland Under Climate Warming Conditions." Water 17, no. 2 (2025): 243. https://doi.org/10.3390/w17020243.

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On the basis of daily discharges recorded in 140 water gauges located on 96 Polish rivers, the long-term changes of runoff and the number of days with low flows (NDLF) in relation to selected meteorological variables were studied. The analyses were performed for the entire multi-annual period 1951–2020 and two sub-periods: 1951–1988 and 1988–2020 that are before and after climate change. The average values of these hydro-meteorological variables in the two sub-periods were then compared. It was found that after 1988, a statistically significant (p < 0.001) increase in the average air temper

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20

Bij de Vaate, A., K. Jazdzewski, H. A. M. Ketelaars, S. Gollasch, and G. Van der Velde. "Geographical patterns in range extension of Ponto-Caspian macroinvertebrate species in Europe." Canadian Journal of Fisheries and Aquatic Sciences 59, no. 7 (2002): 1159–74. http://dx.doi.org/10.1139/f02-098.

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Range extensions of aquatic Ponto-Caspian macroinvertebrate species in Europe have mainly been facilitated by the interconnection of river basins through man-made canals and intentional introductions. Three inland migration corridors can be distinguished: (i) a northern corridor: Volga [Formula: see text] Lake Beloye [Formula: see text] Lake Onega [Formula: see text] Lake Ladoga [Formula: see text] Neva [Formula: see text] Baltic Sea, (ii) a central corridor connecting the rivers Dnieper [Formula: see text] Vistula [Formula: see text] Oder [Formula: see text] Elbe [Formula: see text] Rhine, an

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21

Szymonik, Anna, Joanna Lach, and Krystyna Malińska. "Fate and Removal of Pharmaceuticals and Illegal Drugs Present in Drinking Water and Wastewater." Ecological Chemistry and Engineering S 24, no. 1 (2017): 65–85. http://dx.doi.org/10.1515/eces-2017-0006.

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Abstract Rapid development of pharmaceutical industry, and thus widespread availability of different types of therapeutical and increased intake of pharmaceuticals, results in elevated concentrations of pharmaceuticals in municipal wastewater subjected to treatment in wastewater treatment plants. Pharmaceuticals present in raw wastewater discharged from hospitals, households, veterinary and health care clinics eventually end up in wastewater treatment plants. Commonly applied methods for treating wastewater do not allow complete removal of these contaminants. As a consequence, pharmaceuticals

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22

Balcerek, Mariusz. "The Daugava River in the Early Modern Period. A Border, an Obstacle, and a Trade Route." Textus et Studia, no. 2(30) (October 5, 2022): 123–70. http://dx.doi.org/10.15633/tes.08202.

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The text aims to look at the three functions of the Daugava River: border, obstacle, and trade route. We will focus on the river in the Early Modern Period (from the 16th to the 18th century). We will go beyond the chronological framework, during which we will attempt to answer the following questions. Was the border on the Daugava shaped? To what extent was the dividing line permanent? What was the defensive value of the river? Due to the differences during the border and fighting conducted, the river has been divided into two sections: Livonian (today Latvian) and Ruthenian (today Belarussia

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23

Strzebońska, Magdalena, and Anna Kostka. "Geochemical State of Wilga River Environment in Kraków (Poland)—Historical Aspects and Existing Issues." Minerals 11, no. 8 (2021): 908. http://dx.doi.org/10.3390/min11080908.

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Aquatic systems are a very important part of the environment, which requires special attention due to the constant deterioration of the quality and quantity of water globally. Aquatic environments in Poland are mostly affected by the mining and smelting industry, which is especially visible in the south of the country, and one of such anthropogenically affected rivers is the Wilga—a small tributary of the Vistula River (the biggest river in Poland). For many years, the catchment area of the Wilga River accommodated a functioning industry that was based on the use of metals (fur, leather proces

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24

Wściślik, Wiktor, and Maciej K. Cichoń. "Selected problems of design and construction of the 19th century railway bridges by example of Ivangorod–Dąbrowa Railway." Archives of Civil Engineering, June 17, 2025, 83–98. https://doi.org/10.24425/ace.2025.154109.

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The present paper discusses selected issues related to the design, construction and operation of 19th century railway bridges in the Kingdom of Poland. Individual problems are discussed on the example of the Ivangorod–D˛abrowa Railway (IDR). The route as a whole is characterized, along with a discussion of statistical data regarding the bridges located along the line in question. The competences of private and then state institutions in the field of railway construction are discussed synthetically, taking into account the impact of military issues on the design of railway routes and bridges in

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25

Janiak, Radosław, and Joanna Słomska-Bolonek. "A fabric from the Hallstatt period yet unseen in Central Poland – some remarks on the find from Dąbrowa, Wieluń County." Praehistorische Zeitschrift, September 11, 2024. http://dx.doi.org/10.1515/pz-2024-2022.

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Abstract During excavations carried out in 2023 at the cemetery of the Lusatian culture in Dąbrowa, site 2, Wieluń County, an urnless cremation burial was discovered (Object 24), which is dated generally to the Hallstatt period. Burnt human bones were scattered throughout the object, which form a relatively compact cluster in the central part of the grave. Ceramic fragments from various vessels were found in the fill of the grave cavity. Metal objects, both bronze and iron, showed signs of being smoldered in the fire. This fosters the conclusion that they had been burned with the deceased on t

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