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    Tytuł:
    Rola krzemu w procesie eutrofizacji wód na przykładzie zbiorników Solina i Myczkowce
    The Role of Silicon in the Process of Eutrophication of the Waters – Solina and Myczkowce Reservoirs Case Study
    Autorzy:
    Koszelnik, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/1819150.pdf
    Data publikacji:
    2013
    Wydawca:
    Politechnika Koszalińska. Wydawnictwo Uczelniane
    Tematy:
    proces eutrofizacji wód
    rola krzemu
    nutrient limitation
    dissolved silicate
    retention
    nitrogen
    phosphorus
    lake
    transport
    sediments
    complex
    river
    Opis:
    This paper reports on studies conducted during 2005–2006 years in the ecosystem of the Solina-Myczkowce mountain complex of mesotrophic reservoirs on the San River, SE Poland. The goal of the present study has been to analyse the functioning of the reservoirs as a dissolved silicon sink especially whether silicon assumes a limiting role where the biological productivity of reservoirs waters is concerned. Silicon is one of the biosphere’s most abundant elements, and one that – in the form of dissolved silica – serves as a very important nutrient playing a major role in the functioning of marine, coastal and inland waters. Investigations indicate that reservoirs are major sinks for the dissolved silica in a river system and that unfavorable changes in water chemistry downstream may ensue where (as is usually the case), the water discharged from a reservoir is poorer in Si than that supplied to it. The noted Si depletion in both the analysed reservoirs influenced growth of non-siliceous algae expressed in terms of chl a. Siliceous algal growth is usually observed there during spring. I suppose that the first chl a maximum in the case of the Solina Reservoir, and the only maximum in the Myczkowce Reservoir, result from the growth of both siliceous and green algae. The next increase in chl a – observed only in the Solina Reservoir – may result from the presence of the cyanobacteria often observed in warm lakes at the end of summer. Their absence from Myczkowce reflects the low temperature of that reservoir’s water, this being supplied from the hypolimnion of the upper one. These observations are confirmed in relationships between mean measured concentrations of Si and mean concentrations of chl a in the euphotic zone of the two reservoirs. Observed summer depletion of the silicate accelerates the growth of phytoplankton exponentially, especially in the case of the upper reservoir.
    Źródło:
    Rocznik Ochrona Środowiska; 2013, Tom 15, cz. 3; 2218-2231
    1506-218X
    Pojawia się w:
    Rocznik Ochrona Środowiska
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Odtworzenie nieistniejących jezior jako element zwiększania retencji leśnej i pozaprodukcyjnych funkcji lasu
    Restoration of non-existing lakes as part of increasing forest retention and enhancing non-productive functions of forests
    Autorzy:
    Ptak, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/989832.pdf
    Data publikacji:
    2015
    Wydawca:
    Polskie Towarzystwo Leśne
    Tematy:
    lesnictwo
    lasy
    funkcje pozaprodukcyjne
    retencja wodna
    zasoby wodne
    jeziora srodlesne
    niecki jeziorne
    odtwarzanie
    lake disappearance
    water resources
    retention
    hydrotechnical works
    Opis:
    The aim of the work is to present the possibility of increase in water resources and creation of new non−productive forest functions by restoration of the non−existent forest lakes. Ten currently non−existent natural forest lakes were randomly selected in northern Poland and their extent and volume of the water deposited in their basins were determined. The analysis was performed in two stages. At first, based on the cartographic materials (1:25 000) from XIX and XX century, the location of the lakes before their complete disappearance was determined and their surface were calculated. Bathymetric plans were reconstructed based on the 1:10 000 topographic map. Obtained contour lines constituted the isobaths necessary to calculate the volume of the using Penck method. The results show a large−scale transformation of the natural environment in the forests. The total area of the analyzed lakes before their disappearance amounted to nearly 800 ha, and the total volume of water was estimated to 12 million m³. The main activities aimed at achieving the foregoing goal include damming of rivers and lakes, construction of artificial reservoirs, etc. At this point the possibility of restoring the natural hydrographic network elements to their original condition should be considered. Such an approach would certainly be less harmful to the environment than artificial structures, whose long−term impact on the environment is not always possible to determine. Yet another issue is the possibility of adaptation of the reconstructed forest lakes and their surroundings in order to achieve the objectives related to the non−productive forest functions. Based on the preliminary information on the location, area and volume of the lakes, more detailed analysis should be made taking into account natural needs (changing the species composition of the forest, increasing biodiversity, etc.) and economic aspects (e.g. leisure and recreational facilities).
    Źródło:
    Sylwan; 2015, 159, 05; 427-434
    0039-7660
    Pojawia się w:
    Sylwan
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Próba oceny czynników hydrometeorologicznych wpływających na wielkość wydzielającego się posuszu na obszarze lasu łęgowego Uroczyska Warta
    Attempt of estimation of hydyometorological factors influencing on deadwood quantity on area the Uroczysko Warta floodplain forest
    Autorzy:
    Miler, A. T.
    Powiązania:
    https://bibliotekanauki.pl/articles/101572.pdf
    Data publikacji:
    2016
    Wydawca:
    Polska Akademia Nauk. Stowarzyszenie Infrastruktura i Ekologia Terenów Wiejskich PAN
    Tematy:
    las łęgowy
    posusz
    mała retencja wodna
    starorzecze
    Uroczysko Warta
    floodplain forest
    deadwood
    small water retention
    oxbow lake
    Opis:
    Uroczysko Warta stanowi jedno z najważniejszych skupisk lasów łęgowych w Polsce. Wybudowanie zbiornika Jeziorsko przyczyniło się do zmiany reżimu rzeki Warty (ograniczenie powierzchni zalewów i ich częstotliwości), co w konsekwencji wpływa destrukcyjnie na lasy łęgowe uroczyska. Lasy łęgowe należą do najbogatszych i bardzo urokliwych ekosystemów leśnych. Regulacja rzek i ochrona przeciwpowodziowa przyczynia się niestety do ich degradacji. W Polsce jedynie 0,2% całkowitej powierzchni zajmują lasy łęgowe. Uroczysko Warta stanowi jedno z najważniejszych skupisk tych siedlisk. Wybudowanie w środkowym biegu rzeki Warty zbiornika Jeziorsko przyczyniło się do zmiany reżimu rzeki (ograniczenie powierzchni zalewów i ich częstotliwości). Wydaje się, iż zastosowanie prostych systemów melioracyjnych – zastawek, progów, przepustów z klapami zwrotnymi, może spowodować odtworzenie korzystnych warunków hydrologicznych. Wystąpi wtedy zwiększenie pojemności retencyjnej starorzeczy, a wody gruntowe będą się utrzymywały na wyższym poziomie przez dłuższy okres. Planowana budowa licznych zastawek na ciekach oraz podpiętrzeń zbiorników wodnych to najtańsze metody zwiększania zasobów wodnych w zlewniach. Budowa tych urządzeń technicznych bez wątpienia przyczyni się też do ochrony bardzo wartościowych biotopów mokradłowych, pełniących głównie funkcje ochronną i rekreacyjną. W niniejszej pracy przedstawiono wpływ czynników klimatycznych oraz stanów wód powierzchniowych w starorzeczach i gruntowych na terenie uroczyska na wielkość wydzielającego się posuszu.
    The Uroczysko Warta is one of most important concentrations of floodplain forest in Poland. Building of the Jeziorsko reservoir contributed to change of the Warta River regime (limitation of surface overflows, their frequencies), what in consequence negatively influencing on floodplain forest areas. Flood plain forests are the richest and highly picturesque forest ecosystems. Unfortunately, river regulation and flood control contribute to their degradation. In Poland only 0.2% of total area is covered by flood plain forests. The Uroczysko Warta forest district constitutes one of the most important clusters of these sites. The construction of the Jeziorsko reservoir in the middle course of the Warta River has contributed to changes in the river regime (reduced flooding areas and decreased flooding frequency). It seems that the use of simple land improvement systems, i.e. gates, river bars and culverts with flap check valves, may result in the recreation of advantageous hydrological conditions. In such a case storage volume of oxbow lakes would be increased and ground water would be maintained at a higher level over longer periods of time. Planned building of numerous dams on water-courses and devices to dam up water on reservoirs are cheapest methods of enlarging of water supplies in catchments. Build of these technical devices no doubt will contribute also to protection very valuable marshland biotopes, fulfilling mostly functions protective and recreational. In paper a influences of climatic factors and levels of surface water in oxbow and ground water on deadwood quantity are presented.
    Źródło:
    Infrastruktura i Ekologia Terenów Wiejskich; 2016, II/2; 491-500
    1732-5587
    Pojawia się w:
    Infrastruktura i Ekologia Terenów Wiejskich
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Role of geophysical surveys in the identification of water escape zones from retention lakes: a case study on a selected object in Upper Silesia
    Autorzy:
    Mieszkowski, Radosław
    Wójcik, Emilia
    Kozłowski, Mikołaj
    Popielski, Paweł
    Powiązania:
    https://bibliotekanauki.pl/articles/2025248.pdf
    Data publikacji:
    2018
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    Ground penetrating radar (GPR) method
    electrical resistivity tomography (ERT) method
    retention lake
    water reservoir
    Opis:
    The main scientific goal of this work is the presentation of the role of selected geophysical methods (Ground-Penetrating Radar GPR and Electrical Resistivity Tomography ERT) to identify water escape zones from retention reservoirs. The paper proposes a methodology of geophysical investigations for the identification of water escape zones from a retention fresh water lake (low mineralised water). The study was performed in a lake reservoir in Upper Silesia. Since a number of years the administrators of the lake have observed a decreasing water level, a phenomenon that is not related to the exploitation of the object. The analysed retention lake has a maximal depth between 6 and 10 m, depending on the season. It is located on Triassic carbonate rocks of the Muschelkalk facies. Geophysical surveys included measurements on the water surface using ground penetration radar (GPR) and electrical resistivity tomography (ERT) methods. The measurements were performed from watercrafts made of non-metal materials. The prospection reached a depth of about 1 to 5 m below the reservoir bottom. Due to large difficulties of conducting investigations in the lake, a fragment with an area of about 5,300 m2, where service activities and sealing works were already commenced, was selected for the geophysical survey. The scope of this work was: (1) field geophysical research (Ground-Penetrating Radar GPR and Electrical Resistivity Tomography ERT with geodesic service), (2) processing of the obtained geophysical research results, (3) modelling of GPR and ERT anomalies on a fractured water reservoir bottom, and (4) interpretation of the obtained results based on the modelled geophysical anomalies. The geophysical surveys allowed for distinguishing a zone with anomalous physical parameters in the area of the analysed part of the retention lake. ERT surveys have shown that the water escape zone from the reservoir was characterised by significantly decreased electrical resistivities. Diffraction hyperboles and a zone of wave attenuation were observed on the GPR images in the lake bottom within the water escape zone indicating cracks in the bottom of the water reservoir. The proposed methodology of geophysical surveys seems effective in solving untypical issues such as measurements on the water surface.
    Źródło:
    Studia Quaternaria; 2018, 35; 121-129
    1641-5558
    2300-0384
    Pojawia się w:
    Studia Quaternaria
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Results of floodplain forests protection in the Uroczysko Warta, the Wielkopolska Region, Poland
    Autorzy:
    Miler, Antoni T.
    Dobraczyński, Marek
    Powiązania:
    https://bibliotekanauki.pl/articles/100899.pdf
    Data publikacji:
    2019
    Wydawca:
    Polska Akademia Nauk. Stowarzyszenie Infrastruktura i Ekologia Terenów Wiejskich PAN
    Tematy:
    floodplain forest
    deadwood
    small water retention
    oxbow lake
    Uroczysko Warta
    Opis:
    The Uroczysko Warta is one of the most important riparian forest areas in Poland. The construction of the Jeziorsko reservoir resulted in changes in the Warta river hydrological regimes. This in turn led to a reduction in the floodplain area and flooding frequency, which as a consequence has had a dramatically detrimental effect on the floodplain forests in that wilderness. Riparian forests are among the richest and most beautiful forest ecosystems. Unfortunately, river regulation and flood control measures result in their degradation. In Poland only 0.2% total area is covered by riparian forests. The Uroczysko Warta is one of the most important groups of these habitats not only in Poland, but also on the European scale. It was assumed that the implementation of simple land and water system restoration systems - gates, barrages, culverts with backwater valve gates - may promote recreation of advantageous hydrological relations. This study presents results of water monitoring in the Uroczysko Warta Wilderness and the volume of deadwood formed as a consequence of hydrometeorological conditions. The paper provides a detailed description of climate characteristics (air temperature and precipitation) in the 30-year period of 1988-2017, i.e. after the commissioning of the Jeziorsko reservoir along with the hydrological characteristic of the wilderness area in the years 2009-2017 (water stages in the Warta river and in the Lutynia river, water stages in oxbow lakes and groundwater tables) and the volume of deadwood formed in the years 2006-2014. Water stages in the Warta and the Lutynia as well as water levels in oxbow lakes and groundwater tables show considerable mutual correlations. This indicates efficient operation of constructed land reclamation systems. The volume of formed deadwood shows no evident trends, only a close relationship with climatic conditions. Thus it may be hypothesised that the concept for the protection of floodplain forests in the Uroczysko Warta, consisting in the buffer supply of oxbow lakes at high water stages in the Warta and the Lutynia is appropriate, particularly since waters supplying the wilderness area do not stagnate, but they move within the ground.
    Źródło:
    Infrastruktura i Ekologia Terenów Wiejskich; 2019, II/1; 7-24
    1732-5587
    Pojawia się w:
    Infrastruktura i Ekologia Terenów Wiejskich
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-5 z 5

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