Development of Components for the Angular Framework

Cílem práce je vytvoření skupiny komponent pro framework Angular, které se zaměřují na práci s mapou. Komponenty budou umožňovat práci s geografickými daty, které budou využity při vizualizaci výškového profilu, plánování tras či správě vrstev. Tyto komponenty budou následně použity ve vzorové aplikaci testující jejich funkcionalitu. Součástí práce je také seznámení s frameworkem Angular a jeho porovnání s ostatními frameworky pro vývoj jednostránkových webových aplikací.The aim of this thesis is to create a group of components for the Angular framework that focus on working with the map. The components will allow working with geographic data, which will be used for elevation profile vizualization, planning routes or managing map layers. These components will be used in a sample application testing their functionality. This thesis also includes an introduction to the Angular framework and its comparison with other frameworks for developing single-page web applications.460 - Katedra informatikyvýborn

PILOTNÍ STUDIUM FLUIDNÍCH INKLUZÍ V SÁDROVCÍCH ZE SEDIMENTŮ MIOCENNÍHO STÁŘÍ U KOBEŘIC

Fluid inclusions found in gypsum from Kobeřice told us lot of information about forming conditions during crystallization of crystals of gypsum and confirmed a prognosis of migration of fluids into the sedimentary basin. All microthermometric measurements performed on microthermometric stage mounted on microscope have been done on 0.05 mm thin plates. All measured temperatures including eutectic temperature and temperature of melting of last solid phase (ice) led us to very small salinity of fluids closed inside the inclusions. The salinity was calculated between 0.9 and 2.6 wt. % NaCl eq., which is very small compared to nowadays and Miocene seawater (3.5 wt. %). Parent fluids which are responsible for crystalization of gypsum crystals could be interpreted most likely as mixing sea water with a more diluted fluid (meteoric water?)

HYDROTERMÁLNÍ ASOCIACE NA ŽILÁCH V KLASTICKÝCH HORNINÁCH SPODNÍHO KARBONU DRAHANSKÉ A ZÁBŘEŽSKÉ VRCHOVINY: GENETICKÉ ASPEKTY

Hydrothermal veins occurred in the Lower Carboniferous siliciclastics of the Drahany and Zábřeh Upland and have been investigated by several methods: optic, structural and petrography, geochemistry and microthermometry. The principal aim of the study was to reveal the main precipitation conditions and to distinguish different generations of veins. The attention was concentrated on post-Variscan veins and their gangue minerals, especially on carbonates (calcites). Their optical and chemical characteristics, stable isotope signature and fluid inclusions have been studied. Only few samples contained hydrothermal sulphides. The older vein system, most likely late Variscan, has mineral assemblage: quartz ± calcite ± chlorite ± sulphides (pyrite). Minerals display a severe deformation and calcites are fine grained with a low intensity of cathodoluminescence. Post-Variscan generations of veins have the mineral assemblage with calcite - barite - sulphides (sphalerite, galena, chalcopyrite, pyrite-markazite) ± quartz ± fluorite ± siderite. Hydrothermal phases are coarser grained and the vein direction coincide with regional faults (NW-SE, NNE-SSW, NE-SW). The main post-Variscan population of calcites precipitated from solutions of H2O - NaCl ± CaCl2 ± KCl ± MgCl2 ± FeCl2 type under low temperatures within a range of 60-90°C. One of the younger aqueous hydrothermal systems contain also higher liquid hydrocarbons displaying light blue fluorescence. Isotopic composition of parent fluids were about values of d18O from 0 to ­10  SMOW, what is indicative for transformed basinal brines originated from sea or partly meteoric waters

Biosensors for unattended cost-effective and continuous monitoring of environmental pollution: Automated water analyser computer supported system (AWACSS) and river analyser (RIANA)

This work describes our recent progress and achievements in the field of fully automated biosensors (Automated Water Analyser Computer Supported System (AWACSS) and River Analyser (RIANA)) for unattended, cost-effective and continuous monitoring of environmental pollution. We report on ultra-sensitive immunoassays for the hormones progesterone, testosterone and estrone and the pesticides propanil and isoproturon as examples of the outstanding progress made on biosensors in the field of environmental monitoring and water analysis. Most of the bio-active organic pollutants (estrone, progesterone, propanil and isoproturon) were detected at levels as low as 1.0pgm/L or even below. In fact, the reported limits of detection (LOD) were between 0.2 and 6.0pgm/L. For the first time, commercially available derivatives and antibodies were incorporated into immunoassays (progesterone and testosterone) for fully automated biosensors. To verify the assay performance for quantifying testosterone, progesterone, and isoproturon in real-world samples using our immunosensors, we spiked river and drinking water at six different levels from 0.9pgm/L to 90ngm/L. Nearly all recovery rates could be obtained between 70 and 120% as the AOAC International recommends it chiefly for water analysis