La réactivité pouzzolanique de la métakaolinite, silico-aluminate désordonné obtenu par deshydroxylation de la kaolinite, était corrélée jusqu'à présent, à des variables structurales comme le niveau de cristallinité de la kaolinite et le niveau de désordre de la métakaolinite. Nous avons examiné l'influence d'un nouveau type de variables sur cette réactivité: Les variables dimensionnelles. Six kaolinites possédant une large diversité de caractéristiques dimensionnelles et structurales ont été retenues. Ces kaolinites se présentent sous la forme d'agglomérats poreux de plaquettes que l'on peut caractériser par leur surface externe et leur indice d'agglomération (rapport de la surface interne des agglomérats sur la surface totale des agglomérats). Les métakaolinites ont été obtenues par un traitement thermique de cinq heures à 735°C. Ce traitement thermique s'accompagne d'un phénomène d'agglomération des plaquettes de kaolinite et conduit a la formation d'agglomérats poreux de plaquettes de métakaolinite. Un traitement de désagglomération est nécessaire si l'on désire restituer tout ou partie de la surface externe des grains de kaolinites. L'étude minéralogique à 20°C et à 100°C des produits de la réaction pouzzolanique dans des milieux en excès de chaux nous a permis de définir le taux d'avancement de la réaction qui est le pourcentage de métakaolinite réactive. Ce taux d'avancement ne se corrèle pas aux caractéristiques structurales des kaolinites et des métakaolinites. Par contre le taux d'avancement à long terme est une fonction linéaire décroissante de l'indice d'agglomération des métakaolinites alors que le taux d'avancement à court terme est une fonction croissante de la surface externe des métakaolinites.

Mineral treatment processes generally produce wastewaters containing ultrafine and colloidal particles that cause pollution upon their discharge into environment. It is essential that they should be removed from the wastewater before discharge. This study was undertaken by using synthetic turbid systems containing kaolinite and quartz particles in water with the amount of 0.20 g/L and 0.32 g/L, respectively. Removal of the turbidity was tried in two ways / electrocoagulation with aluminum anode and conventional coagulation with aluminum sulfate. Several key parameters affecting the efficiency of electrocoagulation and coagulation were investigated with laboratory scale experiments in search of optimal parameter values. Optimal values of the parameters were determined on the basis of the efficiency of turbidity removal from ultrafine suspensions. The parameters investigated in the study were suspension pH, electrical potential, current density, electrocoagulation time, and aluminum dosage. This study was also performed to compare electrocoagulation and conventional coagulation regarding the pH ranges under investigation and coagulant dosages applied. A comparison between electrocoagulation and coagulation was made on the basis of total dissolved aluminum, revealing that electrocoagulation and coagulation were equally effective at the same aluminum dosage for the removal of ultrafine particles from suspensions. Coagulation was more effective in a wider pH range (pH 5-8) than electrocoagulation, which yielded optimum effectiveness in a relatively narrower pH range around 9. In both methods, these pH values corresponded to near-zero zeta potentials of coagulated kaolinite and quartz particles. The mechanism for both coagulation methods was aggregation through charge neutralization and/or enmeshment in aluminum hydroxide precipitates. Furthermore, the experimental results confirmed that electrocoagulation could display some pH buffering capacity. The kinetics of electrocoagulation was very fast (&lt / 10 min) in approaching a residual turbidity, which could be modeled with a second-order rate equation.

Thesis (Ph. D.)--Institute of Paper Chemistry, 1959. / Includes bibliographical references (p. 142-143).

Contaminated sites are found all around the world. In order to contain these contaminants, engineers propose capping the contaminated sediments with a sand cap. When capping these contaminants, the sand causes consolidation to occur and could cause a slope failure if the contaminants were on a slope. Investigating the properties of these contaminated sediments allows for proper analysis of a slope failure. The primary objective of this research was to determine the shear strength of contaminated sediments. Since soil samples from actual contaminated sites are highly variable and difficult to explain, the soil used in this research project was mixed and controlled in the lab. A mixture of Kaolinite, water and mineral oil (NAPL, non-aqueous phase liquid) was used for the specimens. Different oil amounts were placed into the specimens to create different scenarios. The different oil combinations included: 100% water, 100% oil, 90% oil, 70% oil, and 50% oil. All of the specimens were fully saturated, and the specimens that had less than 100% oil contained water in the remaining percentage. Consolidated Undrained and Consolidated Drained triaxial tests were performed on the specimens. The constructed specimens were subjected to consolidation stages ranging from 0.6psi to 29psi in confining pressure. The main focus of the study was on low confining pressures. After consolidation the specimens were sheared either undrained or drained. Both tests were utilized in order to see the difference in the pore pressures generated. Failure envelopes were developed for the different oil contents that contained three dimensions included the shear strength, the effective stress, and the pore pressure difference between the pore oil pressures and the pore water pressures. Also, the behavior of oil-dominated versus water-dominated was determined. Results from the 100% water specimens were comparable to previous data. The shear strength for the 100% oil specimens was higher than the 100% water specimens, but lower than the 90% oil and 70% oil specimens. The 50% oil specimens resulted in a great deal of variability on whether the specimen was water-dominated or oil-dominated. The main conclusion was that the Kaolinite had an increase in strength with the introduction of mineral oil. / text

No description available.

The technique of Inverse Gas Chromatography (IGC) was employed for the study of the interactions between various organic solvents with various types of the major inorganic materials (clay minerals and sand) found in Albertas oil sands. Heat of adsorption (-H) was measured for each solvent with respect to each of the four studied inorganic materials. The calculation we used was based on the Infinite Dilution Thermodynamics approach used by Katsanos et. al. [Journal of Chromatography A. 795, 133-184 (1998)]. Retention time data is converted into Retention Volume; H is then obtained by a plot vs. 1/T. The solvents studied were straight chain, branched and cyclic alkanes, alkenes, aromatics, and ketones. The inorganic materials studied were kaolinite, illite, illite-smectite mixed layer, and sand. Our results show that solvents had significantly less affinity for sand when compared to the three types of clay studied. Additionally, solvent affinity to illite had appreciable difference when compared to kaolinite and the mixed layer of illite-smectite. Furthermore, increase in carbon number leads to increased adsorption to the clay. Branched or cyclic alkanes have slightly lower adsorption to clay when compared to straight chain alkane of the same carbon number. Double bonds significantly increase solvent affinity to clay, but have no effect on sand. Lastly, alcohols and ketones have very high affinity to clay that no elution occurred when either solvent was injected into the GC and only ketone eluted when sand was the stationary phase in the GC column. / Chemical Engineering

The focus of this doctoral thesis is the atomic level design of photocatalysts and gas sensing materials. The band gap narrowing in the metal oxides for the visible-light driven photocatalyst as well as the interaction of water and gas molecules on the reactive surfaces of metal oxides and the electronic structure of kaolinite has been studied by the state-of-art calculations. Present thesis is organized into three sections. The first section discusses the possibility of converting UV active photocatalysts (such as Sr2Nb2O7, NaTaO3, SrTiO3, BiTaO4 and BiNbO4) into a visible active photocatalysts by their band gap engineering. Foreign elements doping in wide band gap semiconductors is an important strategy to reduce their band gap. Therefore, we have investigated the importance of mono- and co-anionic/cationic doping on UV active photocatalysts. The semiconductor's band edge position is calculated with respect to the water oxidation/reduction potential for various doping. Moreover, the tuning of valence and conduction band edge position is discussed on the basis of dopant's p/d orbital energy. In the second section of thesis the energetic, electronic and optical properties of TiO2, NiO and β-Si3N4 have been discussed to describe the adsorption mechanism of gas molecules at the surfaces. The dissociation of water into H+ or OH- occurs on the O-vacancy site of the (001)-surface of rutile TiO2 nanowire, which is due to the charge transfer from Ti atom to water molecule. The dissociation of water into OH- and imino (NH) groups is also observed on the β-Si3N4 (0001)-surface due to the dangling bonds of the lower coordinated N and Si surface atoms. Fixation of the SO2 molecules on the anatase TiO2 surfaces with O-deficiency have been investigated by Density Functional Theory (DFT) simulation and Fourier Transform Infrared (FTIR) spectroscopy. DFT calculations have been employed to explore the gas-sensing mechanism of NiO (100)-surface on the basis of energetic and electronic properties. In the final section the focus is to describe the optical band gap of pristine kaolinite using the hybrid functional method and GW approach. Different possible intrinsic defects in the kaolinite (001) basal surface have been studied and their effect on the electronic structure has been explained. The detailed electronic structure of natural kaolinite has been determined by the combined efforts of first principles calculations and Near Edge X-ray Absorption Fine Structure (NEXAFS).

Diss. (sammanfattning) Uppsala : Sveriges lantbruksuniv., 2002. / Härtill 4 uppsatser.

Thesis (Ph. D.)--Université de Nantes, L'U.E.R. des Sciences de la Nature, 1979. / Accompanying map: "Carte des points de prélèvements éffectués dans l'estuaire de la Loire." Includes bibliographical references (p. 213-227).

Resumo: Os atributos mineralógicos e físicos possuem dependência espacial e a distribuição espacial destes atributos possui relação com as formas do relevo. O objeto deste trabalho foi avaliar os atributos mineralógicos da fração argila e os atributos físicos de um argissolo em curvaturas do relevo, assim como avaliar a correlação entre esses atributos. Uma malha de dimensão 100 x 100 m foi delimitada em uma área caracterizada pela forma convexa e outra pela fôrma côncava. As malhas possuem espaçamento regular de 10 x 10 m e os pontos de cruzamento deste espaçamento determinaram os pontos de coleta das amostras, num total de 121 pontos amostrais georreferenciados em cada malha. Os atributos físicos foram avaliados nas profundidades 0,0- 0,2 e 0,2-0,4 m e os atributos mineralógicos na profundidade 0,0- 0,2 m. Os atributos físicos analisados foram diâmetro médio ponderado, diâmetro médio geométrico, agregados maiores que 2 mm, agregados entre 2 e 1 mm , agregados menores que 1 mm, microporos, macroporos, volume total de poros, densidade do solo, resistência do solo à penetração e teor de água no solo, já os atributos mineralógicos da fração argila foram largura a meia altura, diâmetro médio do cristal dos óxidos de ferro, da caulinita e gibbsita, substituição isomórfica e área de superfície específica da hematita e goethita. Os teores da goethita e hematita e razão goethita/(goethita+hematita) e razão caulinita/(caulinita+gibbsita) também foram calculados. Os dados foram submetidos às análises estatísticas e geoestatísticas para avaliação da variabilidade espacial e influência das curvaturas nestes atributos. Para avaliação da relação entre os atributos da mineralogia e físicos realizaram-se as análises de correlação simples e espacial. Os atributos físicos e mineralógicos apresentaram-se dependentes das curvaturas do relevo... (Resumo completo, clicar acesso eletrônico abaixo) / Abstract: The mineralogicals and physical attributes have spatial dependence and the distribution of these attributes has relation with the forms of relief. The object of this study was to evaluate the attributes of clay mineralogy and the physical attributes of an argissol in curvatures of relief, as well as assess the correlation between these attributes. A grid size of 100 x 100 meters was defined in an area characterized by the convex shape and another in an area characterized by the concave shape. The grids have regular spacing of 10 x 10 m and the spacing of the points of intersection determine the points of collection of samples, a total of 121 georeferenced sample points in each grid. The physical attributes were evaluated in depth from 0.0 - 0.2 and 0.2 -0.4 m and the mineralogical attributes in depth 0,00-0,20 m. The physical attributes were analyzed: mean weight diameter, mean geometric diameter, aggregates larger than 2 mm, aggregates between 2 and 1 mm, aggregates smaller than 1 mm, microporosity, macroporosity, total porosity, bulk density, penetration resistance and water content in soil. The attributes of minerals were: width at half height, average diameter of crystals of iron oxides and kaolinite and gibbsite and isomorphic substitution and specific surface area of hematite and goethite. The contents of goethite and hematite and ratio goethite / (goethite + hematite) [Gt / (Gt + Hm)] and ratio kaolinite / (kaolinite + gibbsite) [Ct / (Ct + Gb)] were also calculated. Data were subjected to statistical and geostatistical analysis to evaluate the spatial variability and influence of these curvatures on these attributes. To assess the relation between mineralogy and physical attributes simple and spation correlation analysis where made. The physical and mineralogical attributes and depend on the curvature of the relief. There was also the influence of crystallinity of goethite and gibbsite in soil physical. / Orientador: José Marques Júnior / Coorientador: Gener Tadeu Pereira / Banca: Marcílio Vieira Martins Filho / Banca: Zigomar Menezes de Souza / Mestre