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Physical and mechanical properties of Carboniferous arkoses from Březín natural stone deposit
Čada, Martin ; Přikryl, Richard (advisor) ; Krutilová, Kateřina (referee)
The aim of the thesis is to determine the levels of the physical and mechanical properties of chosen sedimentary (siliciclastic) rocks and also to describe their microstructural nature. With respect to the intended use of the studied material (building stone raw material) the laboratory testing methods are presented. The samples were taken from the drill cores and also from the surface blocks in locality "Zlatý lom" Březín situated in western Bohemia. The microstructural phenomena in the samples were studied using optical microscopy and digital image analyses. According to Folk's classification (1980) the name of the rock was lithic arkose. The strength testing methods were represented by unconfined compressive strength and the Brazilian test. The rest of the mechanical parameters were determined in form of Young's modulus, shear modulus and Poisson's ratio. Special emphasis was given to the hydric expansion (after full immersion) test. The other physical methods were used in order to describe the pore space and real density of samples. For this purposes the absorption test, mercury intrusion porosimetry and helium pycnometry were performed. Besides the porosity value, the pore-size distribution histograms were obtained. In order to calculate the theoretical density of the rock MINLITH and MODES...
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Estimation of Raman spectrometric instruments (785 nm excitation) for detection of dark minerals
Šimon, Jan ; Jehlička, Jan (advisor) ; Machovič, Vladimír (referee)
Summary: Raman spectroscopy is a widely used method in geoscience fields. Using a portable Raman spectrometer is possible to identify different materials, Raman spectrometer will participate in the survey the Martian surface. Its use is widely applied in mineralogy. There was measured a set of dark, green and some bright minerals of different mineralogical system groups that have been assessed the applicability of the chosen detector excitation at 785 nm mainly off-road equipment. The obtained spectra were measured off-road equipment ahura at excitation 785 nm and laboratory equipment InVia Renishaw and there were used lasers at excitaion of 785 nm and 514 nm. It was set of these minerals: Prehnite, Sulphur, Tyrkenit (howlit), Pyroxene (diopside), Libethenite, Toutmaline (verdelite), Dioptas, Klinoklas, Langit, Jadeit, Pseudomalachit (ehlit), Actinolite, Epidote, Augite. Results are composed of field measurement device Ahura, with excitation 785 nm and laboratory apparatus Invite Renishaw excitations with 785 nm and 514 nm. Measured values are arranged in tables, where the measurements are compared with each other, including literature and reference graphically demonstrated in the form of spectra. Subsequently evaluated their measurability. Keywords: Raman spektroscopy, portable Raman spectrometer,...
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Sulphidic mineralization in the vicinity of the Bílina fault
Markes, Jan ; Zachariáš, Jiří (advisor) ; Goliáš, Viktor (referee)
The neoidic sulphide mineralization located in tertiary sediments of Lom Bílina in Bílina's fault is of hydrothermal origin. The sulphidic mineralization is associated with fault systems of Eger rift and temperature of fluid crystallization was about 50řC. The mineralization of Bílina's fault is rather monotonous, the marcasite and pyrite is mostly found without a trace elements. In the crystals were also registered zones with the contents of trace elements, especially As and Ni. The contents of As enriched precipitation zones were fluctuating from 0,2 to 5,4 wt. %, Ni enriched zones were ranged from 1,6 to 5,9 wt. %. The precipitation zones with increased As and Ni content were very thin, there were very short time intervals of As and Ni enriched fluids precipitation. In the marcasite crystals were also found the porous zones of clay mineral microinclusions. These zones showed higher content of Al and Si. There is high abundance of Fe-disulfides at Bílina's fault-dispersed in coal bed, or bonded to tectonic zone of the Bílina's fault. Pyrite and marcasite are dispersed in the coal bed and genetially aren't related to sulphides bonded to Bílina's fault.
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Picritic rocks of the České Střredohoří Mts.
Šnellerová, Zuzana ; Jelínek, Emil (advisor) ; Ulrych, Jaromír (referee)
The first part of the thesis represents a summary of background knowledge about the geology of the České středohoří Mnt. In the second part, picritic rocks were investigated in detail. General aspects of the chemical and mineralogical compositions of this rock type and classification of picrites are discussed. In addition, macro and microscopic characteristics of rocks are included. The results of macroscopic and microscopic investigations indicate that the studied subvulcanic rocks from the České středohoří Mnt. can be characterised as picritic. However, chemical analyses of the rocks did not confirm this conclusion. Only the samples S-39 and S-40 can be disignated as picrites. Although the other samples show similar mineralogical composition, they need to be classified as basic subvulcanites of picritic type due to higher alkali content.
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Mineralogy in the School curricula
Kálalová, Anna ; Matějka, Dobroslav (advisor) ; Ziegler, Václav (referee)
This bachelor thesis is focused on teaching geology and mainly mineralogy on grammar schools. Questionnaire was made for purposes of this bachelor thesis. Objective of this questionnaire was to ascertain information about organization teaching geology and mineralogy on these types of schools and their inclusion in the school curricula. The questionnaire results showed that each school is very different in organization of teaching geology. Mineralogy is most often taught in first classes of four-year, or an equivalent multi-year study. Mineralogy is at some schools taught only in classes corresponding to an elementary school. Optional subject in which is the geology taught students may choose only to nearly forty percent of surveyed schools. Schools use a lot of sorts of material - textbooks for elementary and secondary schools, university textbooks, professional books and Internet resources. The most common tools used in the teaching of geology are collections of samples. Very frequent are also models of crystals and the geological maps. Fewer common are paintings, photographs and films with a geological theme. Uncommon are tools for microscopy and geological compass. 48 % of grammar schools incorporate to education laboratory work and geological or mineralogical excursion, 4 % only laboratory...
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Obnova krajiny postižené dlouhodobou těžbou nerostů a intenzivním osidlováním: Nerostné suroviny
Janeček, O. ; Malý, T. ; Dvořák, Z. ; Rückl, Pavel
IV. část hodnotící zprávy tvoří tyto dílčí studie: IV.B.1 - Doprovodné suroviny severovýchodní části hnědouhelné pánve, IV.B.2 - Sběratelsky zajímavé lokality pánve a okolí (stav mineralogických nálezů SHP, významné paleontologické lokality SHP, mineralogické lokality Krušných hor, DNT, Údlice), IV.B.3 - Poddolovaná území - přehled, IV.B.4 - Sesuvy v pánvi - přehled.
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