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The analysis of time variability of riverbed elevation recorded at eight cross-sections of the Upper Vistula River is presented in the paper. The variability is analyzed on the base on the observed low annual water stages and the cross-sectional geometry variation observed over decades. Furthermore, the analysis of riverbed changes in the years 2001 – 2011 was done in 16 cross-sections located between the Koło and Zawichost gauging stations. Based on the analyzed changes in the riverbed elevation of the eight tested gauging stations it should be noted that since the beginning of the observation period, that is from about the beginning of the 20th century to the mid 1960’s, in the Upper Vistula River riverbed erosion can be observed with a slight tendency for accumulation. As a result of technical regulations of the river channel of the Vistula River from km 247 +000 to 295 +000 carried out in the years 1975 to 1982, intensive processes of riverbed erosion has occured. In most of the 16 profiles it was found that in the years 2001-2011 the river channel was deepened. The occurrence of local riverbed deepening at the river banks was also observed.
According to the results of many studies construction of dams, their decommissioning, and sediment flushing from the reservoir have been associated with vegetation dynamics. However, factors governing the spatial changes of forestation in the floodplain below the dams have not been explored extensively. This study examined the interacting effects of dam, inflow and land-use patterns of catchment areas and other factors on downstream vegetation patterns along the downstream reaches of Southern African Rivers. A total of 105 segments of 15 rivers (16 dams) located in seven Southern African countries were studied. Areas of herbaceous and forest vegetation of river channels below a dam and land-use catchment area patterns were obtained by the Google area calculator and aerial image analysis. Forest development was the highest just below the dams, and the ratio of forest cover decreased with distance from the dam toward the river mouth. Forest coverage ratio was found to decrease with an increase in dyke distance, number as well as of inflows (r = −0.66, P <0.01) and water coverage ratio, and bare land in the river flood plain. However, a principal component analysis (PCA) showed that the proportion of bare land in the catchment area, the dyke distance of the river and the number of inflows or tributaries are the factors most associated with forestation among the studied parameters. Forestation progressively decreased following the entrance of free following tributaries below dams, which appeared to reduce the effects produced by dams on vegetation forestation by causing local deviation. The impact of different land use types, such as agriculture on forestation, was insignificant though in some cases, land use areas cause the forest area reduction.
In the period 2007-2009, floristic, habitat and physico- chemical analysis was made of the hydraulically improved surrounding ditch of Lake Bikcze in the Łęczna-Włodawa Lakeland. Hemicryptophytes, with a large proportion of geophytes as well as hydrophytes and helophytes, were the main component of the flora of the studied section of the transformed Piwonia River channel. In terms of historical-geographical classification, spontaneophytes were predominant, and apophytes among them, whereas anthropophytes were poorly represented, which was confirmed by the correspondingly high values of the synanthropization and apophytization indices (> 50%) as well as the low value of the anthropophytization index (approx. 2%). In the aspect of the range of occurrence, Euro-Siberian and cosmopolitan species were predominant, which are classified in terms of the indicator values as hygrophilous plants, neutral to continentality, living in moderately cool or moderately warm climatic conditions, characterized by a wide range of tolerance to the trophic state index and to soil acidity. An analysis of the values of the basic physico-chemical factors of the stagnant water in the surrounding ditch showed variations in the value of pH, electrolytic conductivity and the value of the concentration of organic and ammonium nitrogen as well as of organic phosphorus and phosphates. In spite of the anthropogenic nature of the studied watercourse, the qualitative and quantitative proportions of the flora species indicated the natural state of the flora based on the native vegetation, characteristic of the study area.
The relationship between the river channel parameters – morphological, hydraulic and substrate – and the composition and distribution of macrozoobenthos communities was studied on the 75 m channel reach of the stream (Teplička brook, Strážovské vrchy Mts., Slovakia) located at the altitude of 256 m; with average width 4 m, depth 0.25m, average current velocity 0.32 m s⁻¹ and discharge in sampling season 0.2 m³s⁻¹. Following the River Morphology Hierarchical Classification (RMHC), the fluvial geomorphological research was realised on the selected channel reach – taxon defined in accordance to RMHC. The plane bed and a riffle-pool channel types have been identified in the investigated channel reach. At the habitat level morphological and hydraulic features represent an alternative approach of habitat assessment in order to gain representative macroinvertebrate sample in stream assessment according to the Water Framework Directive (WFD). The morphological units defined in terms of Froude (Fr) and Reynolds (Re) numbers differed in the extent of the shear stress and turbulence of the water environment. Also Fr and Re values rose in the row of flow types: standing water (SW) – scarcely perceptible flow (SP), smooth flow (S) – rippled (R) – unbroken standing waves (USW) – broken standing waves (BSW) – chute (CH). Different taxa and feeding groups preferred different morphological units and flow types. In terms of morphological units, runs, bars, edgewaters and scours were generally inhabited by the lowest abundance of all invertebrate groups; only Gastropoda reached the higher abundance in these habitats. Glides, pools and backwaters were inhabited by somewhat higher numbers of invertebrates, Oligochaeta and Bivalvia dominated here. Units with organic substrate (moss on boulder clusters and roots) together with rapids and riffles were characterised by high abundance mainly of Gammaridae and Simuliidae. Regarding flow types, standing water separated from others by its low abundances of taxa group but Gastropoda and Bivalvia. SP, S and R types were preferred by Oligochaeta and Chironomidae, while Gammaridae and Simuliidae dominated in standing waves (USW, BSW) and chutes. Also distribution of feeding groups followed the gradient of local environmental conditions. Significant correlations of feeding groups and flow types, current velocity, Fr, Re and depth were observed. Organic substrates played an important role in distribution and abundance of the macrozoobenthos. Overall abundance and also abundance of Ephemeroptera, Trichoptera, Coleoptera and Diptera was significantly higher in the moss or roots compared to other habitats.. Benthos communities of these habitats showed similarities with habitats in the highly turbulent environment (riffles, rapids).
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