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Posouzení kvality půdy zpracované klasickým způsobem ve vybrané lokalitě v Olomouckém kraji / Assessment of soil quality processed with conventional tillage in the selected site in the Olomouc regionDrlíková, Barbora January 2017 (has links)
Diploma thesis documents the problems of soil quality, which is assessed on the basis of physical, chemical or biological indicators of soil quality. The paper describes the various indicators, its methodology and evaluation. In the practical part evaluates the quality of soil cultivated with the traditional way - using plowing. The experimental area, where the samples were taken from the soil, lies in the Olomouc region in the municipality Šumvald. Evaluated were selected physical, chemical and physico-chemical properties of soil, e.g. particle size distribution, bulk density, porosity, air capacity, hydrolimits, pH, carbonates, humus content and salinity of the soil.
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Geology of the Palo Verde Ranch Area, Owl Head Mining District, Pinal County, ArizonaApplebaum, Steven January 1975 (has links)
A quartz diorite intrusion of probable early Tertiary age that crops out over at least 6 square miles in the Palo Verde Ranch area in Pinal County, Arizona was mapped as a distinct intrusion. The quartz diorite intrudes an area comprising Pinal Schist, Oracle granite, andesitic flows, granoaplite, and dike rocks including both pegmatite and diabase. Two major physical features, the Owl Head Buttes and Chief Buttes volcanic areas, both remnants of an extensive early Tertiary series of flows of intermediate composition that covered the area, now remain as lava-capped buttes above the pediment. Weak but persistent fracture-controlled copper mineralization is found in the quartz diorite and the Pinal Schist at or near their mutual contacts in the form of chrysocolla, malachite, black copper oxides, chalcocite, chalcopyrite, and bornite, in decreasing order. Pyrite is rare. Alteration related to northeast and northwest-trending fractures increases in intensity from the common propylitic to argillic to the northeast toward the San Juan claims area. A barely discernible increase in copper sulfides mirrors the alteration zoning, although geochemical sampling showed background copper in the quartz diorite to be more uniform away from fractures.
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Geobiology of bituminous carbonates from the Ediacaran Shibantan Member (Dengying Formation, South China)Duda, Jan-Peter 20 August 2014 (has links)
No description available.
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Datation et caractérisation de processus minéralisateurs à l'Archéen : Application à l'Antimony Line, Ceinture de Roches Vertes de Murchison, Afrique du SudJaguin, Justine 07 December 2012 (has links) (PDF)
Les circulations de fluides dans la croûte sont les vecteurs de mobilités élémentaires dont une des conséquences est la concentration de métaux et la genèse de gisements. Ces fluides circulent dans les zones de déformation où ils modifient la composition des roches encaissantes. Dans la ceinture archéenne de roches vertes de Murchison (Afrique du Sud), l'Antimony Line est une zone déformée qui a été le siège de circulations de fluides minéralisateurs en Sb-Au. Pour caractériser les processus minéralisateurs, des données pétro-géochimiques, en particulier en isotopes stables et inclusions fluides, ont été associées à la datation multi-méthode (U-Th-Pb, Pb-Pb et Ar-Ar) des corps minéralisés et de leur encaissant au cœur et autour de l'Antimony Line. L'étude structurale de la région souligne le caractère distribué de la déformation. La ceinture a ainsi subi une phase majeure de collision d'arc, associée à un magmatisme important vers 2.97 Ga, contemporain d'une minéralisation en Au (±Sb) qui pourrait être responsable d'une phase de pré-enrichissement en Sb. La minéralisation principale en Sb est la conséquence de la circulation d'un fluide métamorphique à H2O-CO2, à 2-3 kbar et 350-450°C. L'albitisation de granitoïdes intrusifs dans l'Antimony Line, datée à 2.8 Ga, est génétiquement liée à cette circulation, laquelle s'inscrit donc dans l'histoire tectono-métamorphique tardive de la ceinture et est contemporaine de la mise en place de leucogranites sur la bordure sud. Ces résultats illustrent la pertinence du couplage pétro-géochimie/géochronologie pour la compréhension globale d'un système métallogénique.
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Hodnocení kvality/zdraví půdy v blízkosti obce Bohaté Málkovice / Assessment health/quality of the soil near the village Bohaté MálkoviceSuchá, Kateřina January 2019 (has links)
Diploma thesis evaluates quality and healthiness of the soil health located close to Bohate Malkovice focusing on changes in both physical and chemical characteristics of the soil in time. The theoretical part describes physical, chemical, and biological parameters of the soil. Selected physical parameters are structure, texture, determination of measured weight, bulk density of the soil, porosity, actual volumetric water content of the soil, aeration, saturated and unsaturated hydraulic conductivity, infiltration, and colour. Chosen chemical parameters are pH, carbonates, soil electrical conductivity, and humus content. Picked biological parameters are microbial biomass, respiration, nitrogen content, and weed infestation. The practical part analyses selected indicators of quality of the soil from the location of the experiment close to Bohate Malkovice. The area under evaluation has been treated using reduced tillage for long term. The practical part is based on the laboratory examination of disturbed and undisturbed soil samples taken between years 2016 and 2018. Based on outcome results we can evaluate the quality of the soil considering plants growth, development, and soil fertility.
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Postglazialer Anstieg des Meeresspiegels, Paläoklima und Hydrographie, aufgezeichnet in Sedimenten der Bermuda inshore waters / Postglacial rise of sea level, palaeoclimate and hydrography, recorded in sediments of the Bermuda inshore watersVollbrecht, Rüdiger Dr. 13 January 1997 (has links)
No description available.
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