|
|
Runoff from a mainly peat bog basin
Vlček, Lukáš ; Falátková, Kristýna
This research focuses on the basin's hydrological regime, where peatlands make up approximately half of the area. Hydrological processes in the peat bog and the surrounding forest were evaluated using the HBV model. The results show that the peatlands significantly increase the water regime fluctuation of local streams. Moreover, water balance shows a lower cooling effect of tree-less peat bogs than forests on organo-mineral soils. Except for a positive ecological aspect, peatland restoration can have a negative hydrological impact on the surrounding landscape and local streams.
|
|
| |
|
|
Dářská rašeliniště nature trail - the use in primary science education
PÓLOVÁ, Monika
The Bachelor thesis deals with the possibilities of interconnecting the nature trail Velké Dářko with natural history lessons at elementary school. The theoretical part defines the educational goals of the Framework Educational Program of basic education in the area of human and nature. The practical part contains excursions - walking routes with activities that lead to the fulfilment of the above mentioned objectives.
|
|
|
Predikace druhového složení těžeben na základě biotopového mapování okolní krajiny: využití charakteristických druhů vyšších rostlin
SLABA, Michal
The surrounding habitats play an important role in the spontaneous vegetation succession in disturbed sites. They serve as donor sites for species colonizing various post-mining sites from the close surrounding. This diploma thesis deals with the species composition in post-mining sites and the surrounding habitats up to the 1 km distance from the locality. The results indicate, that basalt quarries share the largest amount of species with their surrounding habitats. The studied methods have got limited capability to predict the species composition of post-mining sites using only the knowledge about habitat types occurred in the surrounding. On the other hand, species composition of the surrounding habitats, defined by a selection of the representative relevés of the Czech National Phytosociological Database (CNFD), seems to be more promising approach. It could provide more precise results applied in ecological restoration of post-mining sites in the Czech Republic.
|
|
|
Distribution of sulfur isotopes in peat bogs
Haluzová, Eva ; Mihaljevič, Martin (advisor) ; Zachariáš, Jiří (referee)
The goal of this barchelor thesis is to describe the influence of human activity to sulphur cycle and monitoring processes and changes in this cycle with the assistance of specific sulphur isotopes. The first part describes sulphur and its compounds, then appearence in environment and its total cycle. The next part is focused on specific sulphur isotopes and thein application in studies of soils and peats. The final part summarizes total results and informations of human activity and it's influence on the sulphur cycle.
|
|
|
Hydrological drought in headwater areas of the Ore Mountains
Vlach, Vojtěch
Changes in the hydrological cycle are one of the expected impacts of climate change. Until recently, Central European mountain ranges have not been considered to be affected by water scarcity. Nevertheless, recent years have suggested an increasing risk of drought occurrence also in these regions, which have a major impact on the water supply to rivers that drain them. The master thesis deals with the evaluation of hydrological drought in the headwater areas of three catchments in the Ore Mountains for the period from 1967 to 2018. The main aim is to compare the of hydrological drought characteristics in the catchment areas of upper Svatava River, upper Rolava River and Načetínský brook based on available hydrological and climatic data. In connection with this, the work aims to detect the long-term trends of drought occurrence in selected basins. Furthermore, the emphasis is given on the evaluation of natural conditions, especially the historical and current land cover changes in the study catchments. The results point to a significant change in the seasonality of the occurrence of hydrological drought in the second half of the studied period, when the streamflow deficits concentrate between August and October. Furthermore, increasing trends in deficit volumes were found in the catchment areas of...
|
|
| |
|
|
Impacts of hydrological extremes on surface water quality in headwater areas. Application in the model study area of the upper Rolava catchment.
Šajnarová, Lucie ; Matoušková, Milada (advisor) ; Havlíková, Petra (referee)
Precipitation-runoff extremes in the source areas have a significant effect on changes in the geochemism of surface waters, which also affect peatlands in the basin. The main goals of this theses include research literature on the topic of changes in the geochemism of surface waters in spring areas with peat bogs in the basin in response to precipitation-runoff extremes. Furthermore, an analysis of runoff and precipitation conditions in the hydrological years 2018, 2019 and 2020 and an analysis of changes in water quality parameters depending on precipitation-runoff extremes for the period from 2013 to 2020 were performed. The relationship between conductivity and flow was monitored using hysteresis loops. The work used data from the experimental profile of KFGG PřF UK on the Slatinný potok and data on flows for the profile Chaloupky in the Rolava from ČHMÚ. The results show that the relationship between conductivity and flow can be analyzed using hysteresis loops, especially in the period with a rapid increase in flow and their shape changes depending on the reconditioning of the basin. Flow dependence was also observed for other parameters, such as iron. Keywords: hydrological drought, flood, surface water quality, peat bog, electrical conductivity, hysteresis loop
|
|
|
Hydrological function of peat bogs and peat water properties of the Vydra River headwaters
Doležal, Tomáš
The retention potential of landscapes, along with the water regime of spring areas, are important hydrological topics of research, particularly in the current context of increasing extreme drought frequencies. The present work is focused on monitoring the mountain peat bogs, which, due to their overall frequency of occurrence in the spring area of the Vydra river, represent a significant constituent of the rainfall-runoff process of the area of interest. The specific hydropedological features of the organogenous soils (Histosol type soil) provide the high retention potential of the area, however, the influence of these soils on the runoff process is determined by complex physicogeographical factors. The general opinion on the hydrological function of the peat bogs has changed in recent years and the most important factor in the runoff formation in the mountain area of the Šumava Mts. is now thought to be the actual saturation of the headwater, which is predominantly composed of hydromorphic and organogenous soils. The organogenous soils are significant water reservoirs and have an important impact on the landscape. However, they may also intensify the extreme values of the watercourses during extreme precipitation events. The fundamental part of this work focuses on detailed observations of the...
|
|
|
Hydrological function of peat bogs and peat water properties of the Vydra River headwaters
Doležal, Tomáš
The retention potential of landscapes, along with the water regime of spring areas, are important hydrological topics of research, particularly in the current context of increasing extreme drought frequencies. The present work is focused on monitoring the mountain peat bogs, which, due to their overall frequency of occurrence in the spring area of the Vydra river, represent a significant constituent of the rainfall-runoff process of the area of interest. The specific hydropedological features of the organogenous soils (Histosol type soil) provide the high retention potential of the area, however, the influence of these soils on the runoff process is determined by complex physicogeographical factors. The general opinion on the hydrological function of the peat bogs has changed in recent years and the most important factor in the runoff formation in the mountain area of the Šumava Mts. is now thought to be the actual saturation of the headwater, which is predominantly composed of hydromorphic and organogenous soils. The organogenous soils are significant water reservoirs and have an important impact on the landscape. However, they may also intensify the extreme values of the watercourses during extreme precipitation events. The fundamental part of this work focuses on detailed observations of the...
|
guest ::
