Para melhor entender a relação entre os oceanos e as variações climáticas são necessários registros destes eventos. O presente trabalho tem por objetivo principal estudar as variações climáticas e oceanográficas utilizando os registros de conteúdo de carbonato em dois sedimentos coletados na Bacia de Campos. A cronologia dos testemunhos foi primeiramente estabelecida através do conteúdo de carbonato. Sua validação foi feita através das análises de radiocarbono em duas amostras próximas do topo de cada testemunho. Outros métodos usados para corroborar a cronologia foram o biozoneamento com base nos foraminíferos planctônicos Globorotalia menardii e Pulleniatina obliquiloculata, executadas em ambos os testemunhos; análises de isótopos de oxigênio em foraminíferos planctônicos Globigerinoides ruber em amostras do KF-13; e dados de susceptibilidade magnética para o KF-14. Com exceção de radiocarbono, os outros métodos não fornecem idades absolutas Foi então necessário compará-los com estratos de idade conhecida. Para isso utilizaram-se dados do SPECMAP, tornando possível a inferência dos estágios isotópicos marinhos para estes testemunhos. Estabelecida a estratigrafia para os testemunhos com base no conteúdo de carbonato, identificamos as diferentes condições climáticas nas quais os sedimentos foram depositados. As curvas de conteúdo de carbonato para ambos os testemunhos, junto com os dados de isótopos de oxigênio para o KF-13 e a de susceptibilidade magnética para o KF-14 foram comparados com a curva de isótopos de oxigênio do SPECMAP, inferindo assim idades aproximadas para algumas das feições apresentadas. Também foram utilizadas as biozonas de foraminíferos planctônicos identificadas para estimar as idades aproximadas em pontos ao longo do testemunho, além dos dados de radiocarbono. Estabelecida essa cronologia foi possível fazer o cálculo das taxas de sedimentação. Os resultados aqui apresentados mostram a importância que o conteúdo de carbonato nos sedimentos tem para estudos de variações climáticas. / Records of climatic variations are necessary for better understanding of the relationship between the oceans and these events. The main objective of this work is to study climate and ocean variations using carbonate records in two sediment cores collected from the Campos Basin. The chronology of the sediment cores was established through carbonate content. Validation was achieved through radiocarbon analysis in two samples from the top of each core. Other methods used to corroborate chronology were the establishment of biozones based on the planktonic foraminifera Globorotalia menardii and Pulleniatina obliquiloculata, used in both sediment cores; oxygen isotope analysis on the planktonic foraminifera Globigerinoides ruber in samples from KF-13; and magnetic susceptibility data for KF-14. With the exception of radiocarbon, other methods do not provide absolute ages, making it necessary therefore to compare with other stratum of known ages. Data from SPECMAP were used enabling inference of marine isotopic stages for this sediment cores. Once the stratigraphy was established based on the carbonate content, it was possible to identify the climate conditions in which the sediments were deposited. Carbonate content curves for both cores along with the oxygen isotope data for the KF-13 and KF-14 magnetic susceptibility data were compared with the oxygen isotope curve from SPECMAP, inferring approximate ages for some of the features presented. Identified foraminiferal biostratigraphic zones were used to estimate the approximate ages in certain points along the core, along with radiocarbon dating. Once this chronology was established, it was possible to calculate sedimentation rates along the sediment cores. The results here presented demonstrate the importance of carbonate content variations in sediment cores as a means to understanding climate variations.

Para melhor entender a relação entre os oceanos e as variações climáticas são necessários registros destes eventos. O presente trabalho tem por objetivo principal estudar as variações climáticas e oceanográficas utilizando os registros de conteúdo de carbonato em dois sedimentos coletados na Bacia de Campos. A cronologia dos testemunhos foi primeiramente estabelecida através do conteúdo de carbonato. Sua validação foi feita através das análises de radiocarbono em duas amostras próximas do topo de cada testemunho. Outros métodos usados para corroborar a cronologia foram o biozoneamento com base nos foraminíferos planctônicos Globorotalia menardii e Pulleniatina obliquiloculata, executadas em ambos os testemunhos; análises de isótopos de oxigênio em foraminíferos planctônicos Globigerinoides ruber em amostras do KF-13; e dados de susceptibilidade magnética para o KF-14. Com exceção de radiocarbono, os outros métodos não fornecem idades absolutas Foi então necessário compará-los com estratos de idade conhecida. Para isso utilizaram-se dados do SPECMAP, tornando possível a inferência dos estágios isotópicos marinhos para estes testemunhos. Estabelecida a estratigrafia para os testemunhos com base no conteúdo de carbonato, identificamos as diferentes condições climáticas nas quais os sedimentos foram depositados. As curvas de conteúdo de carbonato para ambos os testemunhos, junto com os dados de isótopos de oxigênio para o KF-13 e a de susceptibilidade magnética para o KF-14 foram comparados com a curva de isótopos de oxigênio do SPECMAP, inferindo assim idades aproximadas para algumas das feições apresentadas. Também foram utilizadas as biozonas de foraminíferos planctônicos identificadas para estimar as idades aproximadas em pontos ao longo do testemunho, além dos dados de radiocarbono. Estabelecida essa cronologia foi possível fazer o cálculo das taxas de sedimentação. Os resultados aqui apresentados mostram a importância que o conteúdo de carbonato nos sedimentos tem para estudos de variações climáticas. / Records of climatic variations are necessary for better understanding of the relationship between the oceans and these events. The main objective of this work is to study climate and ocean variations using carbonate records in two sediment cores collected from the Campos Basin. The chronology of the sediment cores was established through carbonate content. Validation was achieved through radiocarbon analysis in two samples from the top of each core. Other methods used to corroborate chronology were the establishment of biozones based on the planktonic foraminifera Globorotalia menardii and Pulleniatina obliquiloculata, used in both sediment cores; oxygen isotope analysis on the planktonic foraminifera Globigerinoides ruber in samples from KF-13; and magnetic susceptibility data for KF-14. With the exception of radiocarbon, other methods do not provide absolute ages, making it necessary therefore to compare with other stratum of known ages. Data from SPECMAP were used enabling inference of marine isotopic stages for this sediment cores. Once the stratigraphy was established based on the carbonate content, it was possible to identify the climate conditions in which the sediments were deposited. Carbonate content curves for both cores along with the oxygen isotope data for the KF-13 and KF-14 magnetic susceptibility data were compared with the oxygen isotope curve from SPECMAP, inferring approximate ages for some of the features presented. Identified foraminiferal biostratigraphic zones were used to estimate the approximate ages in certain points along the core, along with radiocarbon dating. Once this chronology was established, it was possible to calculate sedimentation rates along the sediment cores. The results here presented demonstrate the importance of carbonate content variations in sediment cores as a means to understanding climate variations.

In the region of Bohemian Cretaceous Basin can be found some springs with specific yield over 100 l/s. The doyen of Czech hydrogeology Prof. Hynie described some of those springs to be of karst origin and as the most permeable area he described the so-called transitional facies between shallow-water sandstones and deep-water marlstones. Possibilities of karstification have not yet been studied for rocks in the BCB, so the origin of well-permeable pathways in the BCB is a subject of speculations. This thesis deals with the question of which sedimentary rocks potentially allow the generation of karst permeability in the BCB. To do so, rock samples drilled from outcrops in the BCB were subjected to a fast dissolution simulation by leaching in hydrochloric acid. Carbonate content is measured by a standard and one's own method. Mineral composition, grain size and microscopic structure of rocks are studied with SEM. As is shown, the border of rock karstification is not defined just by the carbonate content, but also the grain size, rock structure and by the occurrence of fine secondary silicate content. Concerning the amount of dissolvable compounds, the border of total disintegration can be at 30 % of carbonate content for some rocks, but the most resistant rocks (mostly fine rocks with SiO2 matrix) stay intact...

Graduation date: 2003

No description available.

Features typical for karst, such as fast groundwater flow and existence of open conduits were observed in various parts of Bohemian Cretaceous Basin (BCB). So far, vertical and areal extent of karst rocks is not known. In case of concerning conduits in quartz sandstones the observation of their evolution in profiles perpendicular to flow is missing. The thesis deals with above mentioned issues. Concerning potential to karstification it is limited to Jizera facial area of BCB. For this purpose, leaching of samples in hydrochloric acid were carried out. The hydrochloric acid was used as an accelerated simulation of natural processes of dissolution of rock by acidic solutions. The reaction of samples on leaching in acid, disintegration and content of the CaCO3 component were evaluated. CaCO3 content was determined also by calcimetry. Rocks which disintegrated can be a suitable for the evolution of karst conduits. According to the lithostratigraphic sections, the examined profiles belong to the TUR5 and TUR6 units - thus these units contain rocks suitable for the evolution of karst conduits. In Předměřice site about 23 % of samples disintegrated, in Kosmonosy site 8 % and in Turnov site 36 % disintegrated. Thus about 1/10 to 1/3 of tested profiles is prone to karstification and evolution of karst...

Submitted by Johnny Rodrigues (johnnyrodrigues@ufcg.edu.br) on 2018-11-05T22:28:11Z No. of bitstreams: 1 ROSEMARY RIBEIRO RAMOS - DISSERTAÇÃO PPGEQ 1985..pdf: 46832957 bytes, checksum: 99eea8bc7664b29c95a76c9107593a6f (MD5) / Made available in DSpace on 2018-11-05T22:28:11Z (GMT). No. of bitstreams: 1 ROSEMARY RIBEIRO RAMOS - DISSERTAÇÃO PPGEQ 1985..pdf: 46832957 bytes, checksum: 99eea8bc7664b29c95a76c9107593a6f (MD5) Previous issue date: 1985-12-27 / CNPq / Este trabalho de laboratório procurou dar continuidade a uma serie de pesquisas que, com o decorrer do tempo,vem se desenvolvendo com as argilas esmectíticas de cores verde-clara, vermelha e do tipo sortida da localidade de Bravo,Distrito de Boa Vista, Município de Campina Grande, Paraíba, visando o estudo dos efeitos de tratamento de cura* cm algumas propriedades reológicas dessas argilas para uso como fluidos tixotrópicos na perfuração de poços de Petróleo. De início foram feitos os ensaios de caracterização mineralógica. Posteriormente foi feita uma analise das propriedades tecnológjcas verificadas através da determinação das viscosidades aparente e plástica e do volume do filtrado nas argilas em sua forma natural. Em seguida, foram observadas as propriedadesreologicas nas argilas tratadas com carbonato de sódio na proporção de 100meq por 100g de argila seca sem tratamento de cura. Os processos de tratamento de cura foram realizados com o auxílio de uma câmara úmida e autoclave , mantendo-se constante a concentração de carbonato de sódio e umidade relativa, e, variando-se a temperatura e o tempo. Em todas as condições estudadas foi verificado o efeito da diálise e o efeito da diálise com uso de COj. 0 uso da diálise, visa eliminar os compostos solúveis ou parcialmente solúveis de cálcio e magnésio, formados pela reação química de dupla trocapor ocasião de tratamento com o composto de sódio (montmorilonita (Mg ,Ca ,Na ,K ,11) + Na2C03 -> montmori 1 onita (Na) + MgCO^ + CaCO., + CO +llO0 + K? CO ) (|ne se pode dissolver na dispersão aquosa da argila, prejudicando as propriedades coloidais da montmorilonita , principalmente a viscosidade plástica. O uso do CO2 tem a finalidade de observar ate que ponto sua ação prejudica as propriedades reológicas das argilas em estudo. Foram determinados, igualmente, teores de carbonatos e bicarbonatos, existentes na suspensão a 6% de sólidos. Estes valores foram utilizados para explorar possíveis correlações com as viscosidades aparentes, plásticas e volume do filtrado, através da análise de regressões lineares simples e múltipla. Os resultados obtidos dos ensaios tecnológicos mostraram que as argilas de cores verde-clara, vermelha e do tipo sortida após tratamento conveniente, apresentaram excelentes propriedades reológicas, possibilitando, assim, o uso dessas argilas como agentes tixotrópicos em fluidos para a perfuração rotativa de poços de Petróleo. 0 efeito da diálise, por sua vez, tem grande influência na melhoria das propriedades reológicas para o tratamento das argilas sem processo de cura e, após o processo de cura em câmara úmida e autoclavagem ,onde as argilas são tratadas com solução de carbonato de sódio na proporção adequada após a autoclavagem; o uso do CO2 por sua vez, influencia bastante as propriedades reológicas, que por serem solúveis, mostram tendência de flocular o sistema e consequentemente prejudicar as propriedades reológicas. Com relação as correlações obtidas de validade Limitada, tendo em vista o reduzido numero de observações realiza das, foram obtidos coeficientes próximos de 1, mostrando que existe relação linear entre os teores de carbonatos, bicarbonatos e carbonatos mais bicarbonatos com as viscosidades aparentes e plásticas e volume do filtrado em algumas condições de cura. / This work of laboratory aims continue a series of research work, which has been developing, using the smectites clays light green, red and mixed couloured from Bravo, District of Boa Vista,Campina Grande, Paraîra, with purpose to study the effects of treatment of cure in some rheological properties of these clays, keeping in mind its applicability as tixotropic fluids for perfuration of oil well. Inicially, the analysis of the rheological properties was done investing from the determination of the apparent plastic viscosités and filtrate volume in the clays under it natural form. The rheological properties of the clays were observed by the treatment of sodium carbonate at the proportion of lOOmeq per 100g of dry clay without treatment of cure. The processes of cure treatment were done in a humid chamber and autoclave keeping the concentration of sodium carbonate and relative humidity constant and changing the temperature and time. The dialysis effect was investigated with the use of C02 at all conditions studied. The use of dialysis process has the purpose to eliminate either soluble compounds or parcially soluble of calcium and magnesium compounds or parcially soluble of calcium and magnesium compounds formed by double exchange chemical reaction by the • 2 + 2-1- + treatment with sodium compounds (montmorilonite, Mg ,Ca ,Na , K+, H30+)+ Na2C03 - montmorilonite (Na + ) + MgC03 + CC>2 compounds (montmorilonite, Mg ,Ca ,Na , K+, H30+)+ Na2C03 - montmorilonite (Na + ) + MgC03 + CC>2 + H20 + K2C03) that are able to be dissolved into clays aqueous dirpèrsion so this will spoil the colloid properties of the montmorilonite, mainly the plastic viscosité. The use of CC>2 has the objective to observe the maximun point that its action will damage rheological properties of the clays in this study. Carbonates and Bicarbonates existing in the 6% solids suspension were determined. These values were used to find correlation in filtrate volume and apparent and plastic viscosites by simple and multiple linear regression analysis. results obtained from technological tests showed that light green, red and mixed coloured clays, after the treatment, presented rheological properties adequated to be used in the perforation of oil wells. However, the effects,of dialysis has considerable influence in the improvement of the rheological properties to the treatment of the clays without the cure process and after the cure process in chamber and autoclave where the clay are treated with sodium carbonate to adequade to proportion after autoclave process.; The use of CC^,however , has considerable influence on the rheological properties, once it being soluble, presented the tendency to floculate the system and consequently to damage the rheological properties. With relation to correlations obtained showing to be of limited validity, even to the rcdused number of observations taken; so were obtained correlations coeficients approximately one taking that there exists linear relation between amounts of carbonates and carbonates plus bicarbonates with apparent and plastic viscosites and the filtrate volume in some of the cure conditions.

This diploma thesis is focused on influence of reduced tillage technology of soil processing on it´s near-surface soil layer (0 to 10 cm). The research was carried out on agricultural land near Šardičky village, where company ZEMO spol. s r.o. provides long-term use of reduced tillage technology. In 2016 the soil quality in this site was evaluated by using physical and hydrophysical parameters, results are presented in the previous bachelor thesis "Selected hydrophysical parameters as indicators of soil quality.". In diploma thesis in addition chemical and other hydrophysical properties have been evaluated to provide a comprehensive assessment of soil quality. In 2016, poppy seed was grown on this site and spring barley was grown in 2017 and 2018. Grab samples and intact soil cores were taken during the vegetation period of the crop. After three years of experimental research, in which I participated, it is possible to assess the development of individual parameters and the influence of reduced tillage technology on near-surface soil layer. The theoretical part of the diploma thesis deals with the description of the reduced tillage technology and problematics of the determination of soil parameters, which are used for evaluation of the quality of the near-surface layer. The practical part deals with evaluation of these parameters according to various authors and describes the development of soil quality during years 2016, 2017 and 2018.

No description available.