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Alkalien in Chondren - offenes oder geschlossenes System? / Alkalis in Chondrules - open or closed system?Kropf, Andreas 13 March 2009 (has links)
No description available.
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Porceliano ir olivino užpildų įtaka kaitrai atsparaus betono savybėms / The influence of fillers from porcelain and olivine on the properties of fireproof concreteSidorov, Andrej 04 July 2007 (has links)
Baigiamajame magistro darbe nagrinėjamos porceliano ir olivino užpildų įtakos kaitrai atsparaus betono savybėms problemos, jo gaminimas, tyrimas ir įdiegimas pramonėje. Išnagrinėti pagrindiniai užpildai, rišamosios medžiagos bei priedai, kuriuos naudojant buvo gaminamas kaitrai atsparus betonas. Šio darbo pagrindinis tikslas - sukurti plūkiamąjį, SiO2 mikrodulkėmis modifikuotą, kaitrai atsparų betoną, susidedantį iš aliuminatinio cemento, porceliano, olivino bei plastiklio, kuris būtų naudojamas šiluminių agregatų išklojų įrengimui, taip pat suirusių išklojų remontui. / In the master thesis are examined the problems of the influence of fillers from porcelain and olivine on the properties of fireproof concrete, its production, study and introduction in the industry; are examined basic fillers, binding agents and compounding material, on basis of which the fireproof concrete was made. The basic purpose of this work is to create packed fireproof concrete, modified by micro-specks of SiO2, which consists of the aluminates cement, porcelain, olivine and plastic, which would be used for the pavement of heat engine units, and also for repairing of the worn pavement.
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Abiotic Methane Formation at the Dun Mountain Ophiolite, New ZealandPawson, Joanna Frances January 2015 (has links)
The production of hydrogen (H2) and methane (CH4) related to olivine hydration (i.e. serpentinization) is considered a major contributor to abiotic hydrocarbon synthesis on Earth. Recent discoveries have highlighted the importance of low temperature (<100oC) serpentinization at continental peridotite outcrops. Such sites produce substantial fluxes of abiotic CH4 from gas seeps and/or springs. A limited number of studies in the southern hemisphere offer research on low temperature abiotic hydrocarbon synthesis in natural ultramafic environments, though large areas of exposed ophiolite are prevalent. This study assesses the origin and flux of CH4 and related water-rock interactions from a previously undiscovered site in the Dun Mountain Ophiolite Belt (DMOB), located at Red Hills, New Zealand. Methane emissions from a hyper-alkaline (pH >11.6) and reduced spring of calcium hydroxide (Ca2+-OH-) type waters near the Maitlands Fault were between 730 to 17,000 mg m 2day 1. The δ13C and δD values of CH4 emitting from this spring are consistent with CH4 of abiotic origin (δ13C: 32.7 ‰ VPDB, δD: 363 ‰ V SMOW). Hyper-alkaline fluids emitting from the spring are concentrated in dissolved CH4 (2.2 mg/L) and H2 (0.7 mg/L) and display δ13CCH4 signatures consistent with other sites worldwide. Extensive and localised carbonate precipitation occurs at the hyper-alkaline Ca-rich spring. Isotopic evaluation of carbonate nodules are kinetically fractionated with 13C and 18O depletions up to 30.8 ‰ and 9.3 ‰, respectively. This disequilibrium between the mineralogy and interacting fluids and gases represents a potential habitable environment for microorganisms. Porous, layered carbonates located on the outer edges of the hyper-alkaline spring are the result of atmospheric CO2 interaction with magnesium bicarbonate (Mg2+-HCO3) and Ca2+-OH- hyper-alkaline waters. The precipitation of these carbonates offers potential insight towards low temperature CO2 sequestration. Additionally, various forms of Fe-rich amorphous material precipitate in association with Mg2+-HCO3 type waters at the Red Hills. The identification of bacteria and diatoms within this material offers supporting information regarding microbial survival in metal-rich, reduced environments. This multidisciplinary study demonstrates the interconnected nature of geological, biological and atmospheric interactions in ultramafic environments at low temperature on Earth.
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Frequency Distribution Of Pyroxene Types And A Method To Separate The Composition Of Multiple Pyroxenes In A SampleDavis, Jimmy Allen 01 January 2007 (has links)
Determining mafic mineral composition of asteroid bodies is a topic reviewed by M.J. Gaffey et al. (2002). The iterative procedure discussed can be implemented as an algorithm, and such efforts revealed weaknesses that are examined in this work. We seek to illustrate the limits of this method and graphically determine its predictions. There are boundaries in the formulae given where the equations break down. In ranges where mafic mixtures are predicted, a method is illustrated that allows a decoupling of these mixtures into the constituents.
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Determination of Oxygen Fugacity using Olivine-Melt Equilibrium: Implications for the Redox States of Mid-Ocean Ridge Basalt and Ocean Island Basalt Mantle Source RegionsPeterman, Kenneth James January 2017 (has links)
No description available.
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Mineraliska material som reaktiva filter för avskiljning av tungmetaller från dagvattenLindquist, Anna January 2005 (has links)
<p>Highly polluted urban storm water from e.g. highways can contain large amounts of heavy metals that may cause harm if they are discharged into recipients. To remove the heavy metals a possible low-cost method that does not require much maintenance, could be the use of reactive filters with filter materials consisting of industrial residues or other cheap mineral based materials. Dissolved metal ions are removed by reactive filters through the processes of ions binding to active sites on the surface of the filter materials, or by formation of insoluble precipitates.</p><p>The ability of CaO-treated granulated blast-furnace slag, iron oxide coated sand, olivine and nepheline to remove seven heavy metals (Cr, Cd, Cu, Ni, Zn, Pb and Hg) from urban storm water was studied. Initially batch experiments were performed where the effect of pH, dissolved organic carbon (DOC) and dissolved ions on the adsorption efficiency was studied. The experiments were conducted with urban storm water and with a reference solution (10 mM NaNO3), both containing the same concentration of heavy metals (approx. 1 μM). The two materials with the best results were further investigated in a column study, where the capacity of the filter was tested. Chemical equilibrium calculations using the program Visual MINTEQ were performed in order to assess the role of precipitation as a mechanism for removal.</p><p>The results show that the blast-furnace slag was the most effective filter material and that it has great potential to be used as a heavy metal remover. Also the iron oxide coated sand worked satisfactory. The highest degree of removal was obtained for lead, cadmium and nickel, for which the removal efficiency exceeded 90% after a load of 300 times the water volume in the columns. For some metals, mainly copper, chromium and mercury the dissolved organic matter affected the removal negatively. The chemical mechanisms causing the removal are specific adsorption to the surfaces of the materials, and for the blast-furnace slag probably precipitation of insoluble metal sulfides.</p> / <p>Starkt förorenat dagvatten som rinner av från exempelvis motorvägar, kan innehålla betydliga mängder tungmetaller som kan orsaka skada om de kommer ut i omgivande vattendrag. En billig metod för tungmetallavskiljning, som inte kräver så mycket underhåll, skulle kunna vara att använda reaktiva filtermaterial bestående av restprodukter eller andra mineraliska lågkostnadsmaterial. Reaktiva filter fungerar som metallavskiljare genom att de lösta metalljonerna binder till ytgrupper på filtermaterialen eller att svårlösliga utfällningar bildas.</p><p>Förmågan att avskilja sju tungmetaller (Cr, Cd, Cu, Ni, Zn, Pb och Hg) ur dagvatten har undersökts för fyra mineraliska filtermaterial, kalciumoxiddopad masugnsslagg, järnoxidsand, olivin och nefelin. Studien inleddes med skakförsök där adsorptionens pH-beroende undersöktes. Försöken gjordes dels med dagvatten, dels med en referenslösning (10 mM NaNO3) med samma tungmetallkoncentration (ca 1μM). Detta gjordes för att studera effekter av löst organiskt material och andra ligander på adsorptionen. Därefter testades de material som uppvisat bäst resultat i skakförsöket i kolonnförsök, ett försök som mer efterliknar en praktisk tillämpning och där filtrets kapacitet kan studeras. Genom kemiska jämviktsberäkningar med programmet Visual MINTEQ var det möjligt att undersöka om bildningen av svårlösliga metallutfällningar bidrog till metallavskiljningen.</p><p>Resultaten visar att slaggen var det effektivaste filtermaterialet och att detta har stor potential att användas för avskiljning av tungmetaller. Även järnoxidsanden fungerade tillfredsställande. De metaller som avskiljdes bäst var bly, kadmium och nickel, för vilka avskiljningen var > 90 % i kolonnförsöket efter en belastning motsvarande 300 gånger vattenmängden i kolonnerna. För vissa metaller, främst koppar, krom och kvicksilver, försämrades avskiljningen betydligt när löst organiskt material fanns närvarande. Mekanismerna som står för avskiljningen är till störst del adsorption till grupper på filtermaterialens ytor, men bildning av svårlösliga metallsulfider är också tänkbar för slaggen.</p>
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Layer Formation on Bed Particles during Fluidized Bed Combustion and Gasification of Woody BiomassHe, Hanbing January 2017 (has links)
Although more than a hundred papers dealing with the agglomeration problem in combustion and gasification of biomass can be found in the literature, very few studies focusing on the bed particle layer formation process in fluidized bed combustion (FBC) and fluidized bed gasification (FBG) can be found. With increased knowledge of the bed particle layer formation process — i.e. the main route behind bed agglomeration and bed material deposition in wood combustion/gasification — suitable combinations of fuel/bed material and/or bed material management measures can be suggested. This would not only aim to reduce the risk of ash related operational problems but also to enhance the catalytic activity of the bed material (e.g. for tar removal in gasification). The present investigation was therefore undertaken to determine the layer formation process on and within typical bed materials (i.e. quartz and olivine) and for a potentially interesting new bed material, K-feldspar. Bed material samples were collected from four different combustion and two different gasification appliances: two bubbling fluidized beds (BFB) (5 kWth/30 MWth), two full-scale circulating fluidized beds (CFB) (90/122 MWth), and two dual fluidized bed gasifiers (DFB) (8/15 MWth). Scanning electron microscopy/energy-dispersive spectroscopy (SEM/EDS) and X-ray diffraction (XRD) were used to explore layer morphology and elemental composition and to gain information about crystalline phases of the layers. Phase diagrams and thermodynamic equilibrium calculations (TECs) were used to interpret the melting behavior of the layers and the melt fragments in deposits. In addition, a diffusion model was used to interpret the layer growth process. For quartz bed particles taken from BFB, the younger particles (< around 1 day) had only one thin layer, but for particles older than 3 days, the layer consisted of inner and outer layers. In addition to the inner and outer layers, a K-rich inner-inner layer was found for bed particles taken from CFB and DFB. No outer layers were found for quartz bed particles taken from DFB. The thin/absence of an outer layer could have resulted from the more significant attrition between particles in CFB and DFB. Reduced availability of Ca and a risk of layer breakage from the particle lead to the formation of the inner-inner layer. Similar elemental compositions of the layers upon the quartz bed particles taken from different fluidized bed techniques were found. The inner-inner layers are dominated by Si, K and Ca (excluding O), and the outer layers are rich in Ca, Si and Mg, which seem to resemble more closely the fuel ash composition. The inner layers, mainly consisted of Si and Ca, were found to have higher concentrations of Ca for older particles. The layer thickness increases with particle age, but the growth rate decreases. Melt was estimated to exist in the inner layer for younger particles (< around 1 day) and in the inner-inner layer. The existence of partially melted inner-inner layers, in particles from CFB and DFB, points towards higher risk of bed agglomeration in these techniques compared to BFB. Based on the experimental results, thermodynamic equilibrium calculations, and diffusion model analyses, a layer formation process on quartz bed particle was suggested: the layer formation is initiated by reaction of gaseous K compounds with quartz to form K-rich silicate melt, which prompts the diffusion of Ca2+. The gradual incorporation of Ca into the melt followed by the precipitation of Ca-silicates, e.g. Ca2SiO4, will result in the continuous inner layer growth. However, because of increasing concentration of Ca and release of K from the inner layer, the melt disappears in the inner layer and the layer formation process gradually becomes Ca diffusion controlled. The diffusion resistance increases with increasing thickness of a more Ca-rich layer, resulting in a decreasing layer growth rate. Crack layers with similar compositions dominated by Si, K and Ca were observed in relatively old quartz bed particles. A melt was predicted to exist in the crack layer according to thermodynamic equilibrium calculations. The crack layers found in quartz particles from BFB and CFB connect with the cracks in the inner layer, whereas for bed samples collected from DFB, the crack layers were found along existing cracks in the quartz particle. The different morphologies may indicate different routes of formation for crack layers in bed particles from different fluidized bed technologies. For quartz particles from BFB and CFB, crack formation through the inner layer down to the interface between the inner layer and the core of quartz bed particle initiates the cracks in the quartz bed particle. This allows for diffusion of gaseous alkali compounds to react with quartz in the bed particle core, thereby forming crack layers. The reaction is accelerated with bridge formation between crack layers. This may later lead to the breakdown of the bed particle into smaller alkali-silicate-rich fragments. For K-feldspar bed particles from BFB and CFB, only one layer was found for particles with an age of 1 day. For bed particles with ages older than 3 days, two layers including a homogenous inner layer containing cracks and a more particle-rich outer layer can be distinguished. Compared to bed particles from BFB with similar ages, the outer layer is thinner for bed particles from CFB. The inner layer is dominated by Ca, Si and Al (excluding O), whereas the outer layer is dominated by Ca, Si and Mg. The average concentration of Ca in the inner layer increases with bed particle age. Increasing layer thickness with decreasing growth rate was found, similar to that on quartz particles. For particles from DFB, the inner layer is also mainly consisted of Ca and Si, but cracks in the inner layer were not found. For all the particles, the Ca/Si molar ratio in the layer decreases towards the bed particle core and the change of concentration is more significant at the bed particle core/layer interface. The overall inner layer growth is resultant from the gradual incorporation of Ca into the layer. For olivine bed particles from DFB, the younger bed particles (< around 24 h) have only one layer, but after 24 h, an inner layer and an outer layer appear. Furthermore, for bed particles older than 180 h, the inner layer is separated into a distinguishable Ca-rich and Mg-rich zone. Two kinds of cracks in the inner layer either perpendicular or parallel to the particle surface were observed. Compared to the younger bed particles, the Ca concentration in the layer of older particles is much higher. A detailed mechanism for layer formation on olivine particles in fluidized bed gasification (most likely also applicable to combustion) based on the interaction between woody biomass ash and olivine has been proposed. The proposed mechanism is based on a solid-solid substitution reaction. However, a possible enabling step in the form of a Ca2+ transport via melts may occur. Ca2+ is incorporated into the crystal structure of olivine by replacing either Fe2+ or Mg2+. This substitution occurs via intermediate states where Ca-Mg silicates, such as CaMgSiO4, are formed. Mg2+ released from the crystal structure most likely forms MgO, which can be found in a distinguishable zone between the main particle layers. Due to a difference in the bond lengths between Mg/Fe and incorporated Ca2+ with their respective neighboring oxygen atoms, the crystal structure shifts, resulting in formation of cracks. The dominating elements in the inner layers are similar for each kind of bed material from BFB, CFB, and DFB, indicating limited effects of atmosphere on the inner layer formation. The initiation of layer formation differs depending on the bed material, but increasing Ca concentration in the inner layer with time for all bed materials indicates that the layer growth resulted from the incorporation of Ca into the layer. Compared to quartz, K-feldspar and olivine are more promising bed materials in wood combustion/gasification, especially in CFB and DFB techniques, from the perspective of mitigating bed agglomeration and bed material deposit build-up.
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Solubilité du sodium dans les liquides silicatésMathieu, Romain 04 September 2009 (has links) (PDF)
Les alcalins, généralement lithophiles à basse température, deviennent volatils à haute température et/ou sous des conditions réductrices. Il existe peu de données expérimentales sur les relations activité-composition dans les silicates fondus et aucun modèle thermodynamique ne permet de prédire leur comportement dans les liquides silicatés. Pour acquérir une base de données cohérente sur ces relations, nous avons développé un nouveau système expérimental permettant d'imposer et de contrôler, à haute température, une pression partielle de sodium sous des conditions d'oxydoréduction fixées. Une cellule thermochimique originale, simple de mise en œuvre et efficace a été conçue pour contraindre l'ensemble de ces paramètres thermodynamiques. Les résultats de cette étude montrent que les processus de condensation et de volatilisation du sodium dans les liquides silicatés du système CaO-MgO-Al2O3-SiO2 peuvent être décrits par une équation simple de type : Na(gaz) +1/2 O2(gaz) = Na2O(liq). Les données obtenues à l'équilibre sur des liquides de compositions différentes ont permis de dériver un modèle permettant de prédire la solubilité et les coefficients d'activité (aNa2O et γNa2O) dans un liquide silicaté du système CaO-MgO-Al2O3-SiO2, à différentes températures et différentes PNa, en fonction de la composition de ce dernier. Ce modèle est basé sur la détermination de la basicité optique du liquide sans sodium, c'est-à-dire suivant l'état de polymérisation du liquide et suivant ses interactions acide-base entre oxydes. Par ailleurs, ces travaux ont permis la détermination d'un nouveau type de diagramme de phase à isoPNa. Enfin cette étude a de nombreuses applications en cosmochimie, sidérurgie et magmatologie.
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Caractérisation de nanomatériaux C-LiFePO4 optimisés pour matériaux d'électrode positive pour batteries lithium – ion. Détermination du mécanisme de désintercalation / intercalation du lithium à partir de ces<br />matériaux.Maccario, Magalie 30 November 2007 (has links) (PDF)
Des nanomatériaux C-LiFePO4 d'électrode positive pour batteries lithium-ion ont été synthétisés dans différentes conditions de synthèse (rapport Li/Fe, température, traitement thermique), après mécano-activation du mélange des précurseurs. Une étude des propriétés physico-chimiques et structurales de différents matériaux C-LiFePO4 a été réalisée par les techniques classiques de la Chimie du Solide et de la Science des Matériaux : diffraction (X, neutrons et électrons), spectroscopies (Mössbauer, IR, Raman, ...) et microscopie (MEB et MET-HR) de façon à essayer de déterminer le (les) facteur(s) clé(s) à de bonnes performances électrochimiques en batteries au lithium. La combinaison des analyses des matériaux désintercalés par DRX et MET-HR nous a permis de proposer le mécanisme dit "dominocascade" pour expliquer la désintercalation / intercalation rapide du lithium dans ces matériaux « LixFePO4 » et donc leurs bonnes performances électrochimiques en batteries lithium-ion. L'effet des cyclages longue durée à différentes températures a également été étudié.
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Interaction entre déformation et percolation de magma ou de fluide dans le manteau à l'aplomb des zones de subductionSoustelle, Vincent 02 December 2010 (has links) (PDF)
Ce travail apporte de nouvelles contraintes sur les interactions entre déformation et processus d'hydratation et de percolation de magma ou de fluides dans le manteau à l'aplomb d'une zone de subduction et leurs implications sur les propriétés sismiques dans le coin mantellique. Il se base sur l'analyse de péridotites à spinelle provenant du massif de Ronda (Espagne) et deux séries de xénolites issues de zones de subduction actives (Kamchatka, Papouasie-Nouvelle-Guinée). L'étude structurale, pétrologique et géochimique de ces échantillons montrent qu'ils ont subit une percolation réactive de magma ou de fluide synchrone d'une déformation de haute température basse contrainte cohérente avec les condition PT de la base de la lithosphère ou de l'asthénosphère. Cette percolation réactive est responsable d'un enrichissement en pyroxènes, qui est souvent localisé dans des bandes parallèles à la foliation. Cet enrichissement est associé à une dispersion de l'orientation cristallographique de l'olivine. Les systèmes de glissement dominant dans l'olivine sont dans tous les cas {0kl}[100], ce qui implique que la direction de polarisation rapide des ondes S dans la partie supérieure du coin mantellique est parallèle à la direction d'écoulement dans le manteau. La décroissance de l'intensité des OPR de l'olivine associée à l'enrichissement en pyroxènes a pour conséquence une réduction non négligeable de l'anisotropie sismique qui peut induire jusqu'à 33% d'erreur sur l'interprétation de l'épaisseur de la couche anisotrope. Un enrichissement en orthopyroxène peut aussi entraîner une baisse du rapport Vp/Vs, mais ne peut expliquer les rapports Vp/Vs <1,7 cartés dans certains avant-arcs. Cependant de telles valeurs peuvent être expliquées si l'anisotropie des péridotites du coin mantellique est prise en compte. Les analyses par spectroscopie infra-rouge montrent que les olivines des deux séries de xénolites étudiées contiennent moins d'eau que la saturation théorique calculée pour leurs températures d'équilibre dans le domaine du spinelle. Ces faibles concentrations en eau sont similaires à celles observées dans les olivines des péridotites à spinelle des autres zones de subduction. Elles enregistrent probablement la faible solubilité de l'eau dans l'olivine à des pressions relativement basses et la déshydratation au cours de l'exhumation des xénolites. Ces teneurs en eau mesurées ainsi que les estimations de la saturation théorique ne sont pas suffisantes pour changer la direction de glissement dominante dans l'olivine de [100] à [001].
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