In Kamienna River Valley the iron ore exploitation was done for a very long time. The intensification of the mining took place in XVIII and XIX century. For this region played an important role Stanisław Staszic. Kamienna River was supposed to be the source of energy and way of transport. Therefore, the river canalization and intensive training was undertaken, in consequence the river course was straighten and shorten, which resulted in the significant change in the river dynamics. Meander elimination and introduction of a uniform cross-section resulted in deterioration of habitat. To-day Kamienna River has deeply incised bed, which causes the drainage of surrounding grounds. After the analysis of the old maps and the river cross-sections it was found that it is impossible to restore the old river bed, because of the important erosion and cut off the sediment transport by dams on Świślina and Kamienna Rivers. Moreover the canalized river along some industrial vestiges is a part of technical patrimony. Therefore the only slight improvements could be proposed – introduction of slight meanders, more natural bed form and irregular banks. That could be obtained by an introduction of small hydraulic structures diverting the water stream. ...
This paper aims at sharing feedback about dry dams. These structures are efficient to mitigate floods, while little disruption of the continuity of the main channel and its flows outside the flood periods. Five sets of dams are presented here. They were selected so as encompass the diversity of the structures and of the problems. The oldest structures are presented first. These are dams built in the beginning of the twentieth century in Poland and in the USA, which are still in operation today. Then, recent realisations in France are presented. Large dams in Gard catchment and small dams upstream the nearby town of Nîmes are described, with analyses of behaviour during intense floods. Finally, small dams in Seine-Maritime allow to address the issue of an efficiency diagnostic at catchment's scale, when both dams and stakes are spread out. This article gives key references for further information about structures design. ...
The high precipitations, which appears now very frequently, are the main causes of damages in the infrastructure and the properties. Protection against flood should be still developed, but with the special attention on ecology and keep-ing the continuity of water and sediment flow throughout the river channel. Dry dam structure is efficient to mitigate floods, while little disruption of the continuity of the main channel and its flows outside the flood periods. In the paper we ana-lyse the efficiency of selected dry dams during the flood events. We have studied the dry dams located in southern France. In few cases the studies have shown, that dry dams had to be reconstructed in order to protect the area against the flood. ...
In order to protect the areas against the floods and droughts effect, we need to slow down the outflow in the scale of the whole catchment. The streams and rivers training are one of many possibilities of floods and droughts mitiga-tion. However, these activities often were done without any respect on the basic principle on keeping the ecological continuity of river corridor. In the paper, we propose improving the activities in the rivers and streams channels, in order to al-leviate effects of the technical training. ...
Dependly on the the land-use management, there are different technics of river training. The main aim of river training is floods mitigation. However, these activities often were done without any respect on the basic principle on keeping the ecological continuity of river corridor. In the current paper we present four types of trained river cross-sections, depend on their shapes, the material which forms them, and the condition for fauna and flora. There are also performed the patterns of the regulated channels, which are located in the different kind of urban area. For the selected trained river courses, which are located in the Upper Wisła catchment, the possibility of restoration has been analyzed.
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The Krzczonówka stream is left tributary of the Raba River. In 2014, during the period from April to September, the project related to the lowering of the existing debris dam was carried out. Heavy rainfall resulting in high flows occurred shortly after the start of work. In effect, large amount of debris was moved from the reach located upstream of debris dam to the reach downstream of it. This work aims to present the influence of flood discharges on the morphology of the stream channel under conditions of high sediment supply. Observations on the changing conditions of water flow and sediment transport will also be presented ...
Knowledge of properties of materials deposited in beds of small reservoirs is important, as it can be used for a range of analytic works, concerning river rehabilitation and river management and other similar undertakings. Usually the one property - the d50 value can be obtained using in-situ measurements using sieves but in most cases of preliminary, large scale research may not be feasible. In this paper the Osuch empirical formula for determination of standard sediment grain sizes of d50 is presented. Besides the original formula an improved method of assessing of the slope value for that formula is proposed, which may greatly improve the usefulness of the original, unmodified method. The calculation results are then compared with the in-situ measurements done on many samples taken from the Trzebuńka dam reservoir. The dam was recently partially removed and partially rebuilt, so there was an unique and easy access to wide strata of different layers of sediments, accumulated across many years of dam operation in the exposed bed of partially emptied reservoir. Additionally, the Ratomski formula for riverbed slope determination near dams was used as a reference. The mentioned methods taken together can be used for preliminary analysis before significant ...
The article presents an assessment of the variability of riverbed sediment throughout the Przemsza river course and its main tributaries in relation with the observed disturbances of grain size changes caused by hydro-engineering activity in the channel. Sediment grain size composition in the river channel depends on the hydrodynamic balance and the water flow. In the stable river channel sediment grain size decreases regularly with the river course from the source to the mouth. In the channel where there are sections of anthropogenically modifications, the variation of sediment grain size composition may be irregular in the river course. The article presents the results of measurements and calculations which were made in the following gauging stations: Łysa Góra, Będzin, Sosnowiec, Jęzor, Chełmek non Przemsza river, in Golczowice, Okradzionów, Sławków, Maczki, Niwka on Biała Przemsza river and in Brynica, Kozłowa Góra (above the back of the reservoir Kozłowa Góra and downstream the dam), Szambelnia on Brynica river. The results of studies showes that variability of characteristic diameter of d10 is minimal, while the diameters of d50 and d90 is characterized by significant differences in all the tested gauging stations of Przemsza river and its tributaries. In Brynica river where ...
The analysis of variability of riverbed elevation recorded at five selected gauging cross-sections of Nida River, and at three gauging stations of Czarna Nida is presented in the paper. The studies concern the period of 60 - 80 years of observation. The trends of riverbed changes during the study period at the selected gauging stations were calculated based on the variability of observed minimal annual water stages. The reasons for the observed changes in the river course and channel geometry are given. These changes were caused by river regulation consisted of the shortening and narrowing of the river channel. Moreover, grain size distribution analysis in the selected gauging stations of Nida River and characteristic diameter variability of sediments along the river course examination are presented. These analyses were to evaluate the variability of characteristic diameters along the river course in connection with observed changes in cross-sections' geometry. Additionally, to confirm the process of erosion or deposition recognized in the examined river channels, hydrodynamic equilibrium was determined. Three methods were proposed and used: the mean velocity and critical velocity in the main river channel comparison, the stream power value calculation which defines the character of the river channel, and the WWK ...
