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The influence of precipitation on shallow mineral water abstraction
Hlaváčová, Michaela ; Hrkal, Zbyněk (advisor) ; Procházka, Vladimír (referee)
This study focuses on the influence of precipitation on shallow catchments of mineral springs in the special area of Františkovy Lázně. The thesis was made on the basis of the data provided by the company Spa Františkovy Lázně a.s.. The interdependent relations between yield springs, precipitations, atmospheric pressure and the content of free CO2 were studied. These relations were observed onto six springs - František, Luční, Nový, Solný, Železnatý and Žofie. The precipitations were compared with the yield of individual springs. The season was proved by three springs (František, Železnatý and Žofie). Retention of the precipitation was determined for springs František, Solný, Železnatý and Žofie. Considering more than half a year delay, we cannot claim that the precipitations should have a major influence on the dotation of mineral springs. The downtrend was founded for the free CO2 in all researched resources. Significant indirect relation was found using the correlation coefficient between atmospheric pressure and free CO2.
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Artificial recharge of watewater in small catchments
Pleskotová, Nikola ; Hrkal, Zbyněk (advisor) ; Datel, Josef (referee)
The main objective of the thesis is to study artificial wastewater recharge in the area of Řevničov and reassessment of related problems such as groundwater chemical changes, colmatage, and unfavorable legislation in the Czech Republic. Individual chapters describe the experience with the above mentioned topic in the Czech Republic, but classifies it into the global context. The major part of the thesis focuses on the assessment of the qualitative and quantitative impacts of wastewater artificial recharge in the geological environment. These conclusions are drawn from monitoring changes of groundwater quality, which are controlled on the network of monitoring boreholes in the Řevničov experimental catchment. The natural attenuation of geological environment has considerable impact to final composition of contaminated water, which is compared to legal limits of underground and potable water in Czech Republic. In the research area several tracing tests were also applied, with the aim of proving the expected flow of wastewater into monitoring borehole. The obtained data specify the situation in the area of interest, or may serve as a source of information for future studies dealing with similar topics. Powered by TCPDF (www.tcpdf.org)
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Artificial recharge of surface water to aquifer
Čechová, Tereza ; Hrkal, Zbyněk (advisor) ; Bruthans, Jiří (referee)
Artificial recharge of surface water to aquifer Tereza Čechová, Geotechnologie Abstract: The bachelor thesis is devoted to groundwater recharge. The source of groundwater is infiltration of atmospheric precipitation. The study deals with the use of controlled artificial recharge in the Czech Republic and the other countries in the Word.
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Artificial recharge of surface water to aquifer
Čechová, Tereza ; Hrkal, Zbyněk (advisor) ; Bruthans, Jiří (referee)
Artificial recharge of surface water to aquifer Tereza Čechová, Geotechnologie Abstract: The bachelor thesis is devoted to groundwater recharge. The source of groundwater is infiltration of atmospheric precipitation. The study deals with the use of controlled artificial recharge in the Czech Republic and the other countries in the Word.
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The issue of drugs in surface and ground waters
Šrot, Martin ; Hrkal, Zbyněk (advisor) ; Datel, Josef (referee)
The presented work deals with the state of research of medicinal substances in water formations of Czech Republic and in smaller ammount it deals with this issue abroad. It provides an overview of the most frequently occurring medicinal substances and methods for their detection and also describes the possible sources of pollution and impact of these substances on the environment. Keywords: ground water, surface water, drugs, contamination
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Flooding of the Hamr I mine and evaluation of the geological structure impact on the hydrogeological conditions in the northeastern part of Stráž block
Rozman, David ; Datel, Josef (advisor) ; Hrkal, Zbyněk (referee)
The main objective of diploma thesis is to evaluate the impact of the geological structure on the hydrogeological conditions in the northeastern part of Stráž block. The study area in northern Bohemia is characterised by Cenomanian and Turonian sandstone aquifers, which are horizontally divided by Lower Turonian aquitard. The thesis focuses groundwater level analysis and study hydrogeological impacts of faults, neovolcanic veins and disturbances of rock environment caused by uranium mining. First part of the study presents description of general geological and hydrogeological conditions in the area with summary of previous investigations and reports. Various hydraulic interventions during mining, which have great impact on the groundwater level situation are described. Based on the data from collected boreholes, contour maps of groundwater level are prepared to study its shape and temporal changes. Hydraulic communication through aquitard and through Stráž fault zone have been examined by correlations of groundwater levels. The results of the study confirm sealing effect of Stráž fault zone in the examined section. Barrier effect of the neovolcanic veins has been confirmed on several locations and examples of increased hydraulic conductivity as the result of fault disturbances have been located....
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Interaction of surface water and groundwater og Luznice River
Slabá, Zdenka ; Hrkal, Zbyněk (advisor) ; Datel, Josef (referee)
This thesis is a part of a project run by The Department of Geography, Faculty of Science in Charles University in Prague. This project deals with processes in floodplains of the Lužnice, the Stropnice and the Blanice rivers. The research in the floodplain of the Lužnice started in the year 2008 and is focused on the interaction between groundwater and surface water. The monitored territory it is situated to the south of a locality called Halámky and its area is 0,6 km2. In this thesis mainly the outputs of the research were elaborated. The highlighted points were the interpretation of the groundwater level behaviour, the groundwater streaming orientation in the area and interaction between groundwater and surface water. The outputs of this thesis can be used in the next stages of the project.
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Mineral waters of Františkovy Spa region
Veselá, Michaela ; Hrkal, Zbyněk (advisor) ; Datel, Josef (referee)
The thesis deal with mineral water of Františkovy Spa region and NPR SOOS. Its aim is to provide information about the history of the explotation of mineral water in Františkovy Spa and its surroundings, in the locality of SOOS. It is divided into several chapters. The first chapter introduce Františkovy Spa and its geological and hydrogeological conditions. The history of exploitation of mineral water is also mentioned there. The next chapters are about mineral springs, their genesis and quality. The last chapter summarizes the protection of natural resources. It is focused on exceptional nature reserve SOOS and it refers to general information about the geological and hydrogeological position and ecosystems found there.
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Grounwater regime of the Cheb Basin
Walter, Dominik ; Datel, Josef (advisor) ; Hrkal, Zbyněk (referee)
This study summarizes some general findings of geological, hydrogeological, hydrological, structural and other conditions of the Cheb tertiary basin and descrides how these conditions are connected with circulation of graoundwaters and with appearance of mineral waters of different chemical composition and appearance of discharge of dry CO2. The final chapter shows information of changes of groundwater level at specific locations and periods of time by analyzing data gathered from borehole monitoring site of Czech Hydrometeorological Institute. Measuring of groundwater level was taken every day or every week, also average data of every month were taken. These data show variant changes of groundwater level which can be associated with definite events and this study shows if it is possible to associate some changes of groundwater level with exact events.
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