No description available.

No description available.

The theory of the lamellar eutectoid reaction by volume diffusion has been extended to account for solute segregation within the product phases and the effect of dilute third element additions. It has been demonstrated for symmetric binary systems that the segregation can account for 10% or more of the free energy stored in the product phases and can lead correspondingly to a predicted lamellar spacings appreciably greater than those obtained when segregation is neglected. This segregation is relatively high in the systems Cu-In, Cu-Be and Ag-Cd and may account for the fact that a secondary coarse-grained pearlitic reaction follows the initial fine grained one in these systems. The binary theory has been-used to analyse the available data for the eutectoid reaction in the Cu-Al and Fe-C systems and satisfactory agreement is obtained. The theory for ternary systems, while complete in principle, proves to be. intractable in all but the simplest version of the solution thermodynamics. It is concluded that the effect of the third element on the binary eutectoid reaction is mainly through its effect on the phase diagram, the ternary cross effects in the diffusion matrix tending to cancel out. Any additional element which lowers the eutectoid temperature will retard the reaction. / Thesis / Doctor of Philosophy (PhD)

A model is developed to describe solute transport and retention in fractured rocks. It accounts for the fact that solutes not only can diffuse directly from the flowing channel into the adjacent rock matrix composed of different geological layers but can also at first diffuse into the stagnant water zone occupied in part of the fracture and then from there into the rock matrix adjacent to it. Moreover, the effect of radioactive decay-chain has also been studied in the presence of matrix comprising different geological layers. In spite of the complexities of the system, the analytical solution obtained for the Laplace-transformed concentration at the outlet of the flowing channel can conveniently be transformed back to the time domainby use of e.g. De Hoog algorithm. This allows one to readily include it into a fracture network modelorachannelnetwork model to predictnuclide transport through channels in heterogeneous fracturedmedia consisting of an arbitrary number of rock units withpiecewise constant properties. Simulations made in this study indicate that, in addition to the intact wall rock adjacent to the flowing channel, the stagnant water zone and the rock matrix adjacent to it may also lead to a considerable retardation of solute in cases with a narrow channel. The results further suggest that it is necessary to account for decay-chain and also rock matrix comprising at least two different geological layers in safety and performance assessment of the repositories for spent nuclear fuel. The altered zone may cause a great decrease of the nuclide concentration at the outlet of the flowing channel. The radionuclide decay, when accounted for, will drastically decrease the concentration of nuclides, while neglecting radioactive ingrowth would underestimate the concentration of daughter nuclides. / <p>QC 20140224</p>

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No description available.

No description available.

No description available.

<p>A self‐consistent model for non‐partitioning planar ferrite growth from alloyed austenite is developed. The model captures the evolution with time of interfacial contact conditions for substitutional and interstitial solutes. Substitutional element solute drag is evaluated in terms of the dissipation of free energy within the interface, and an estimate is provided for the rate of buildup of the alloying element ‘‘spike’’ in austenite. The transport of the alloying elements within the interface region is modeled using a discrete‐jump model, while the bulk diffusion of C is treated using a standard continuum treatment.</p> <p>The model is validated against ferrite precipitation and decarburization kinetics in the Fe‐Ni‐C, Fe‐Mn‐C, Fe‐Mo‐C, Fe‐Si‐C, Fe‐Cr‐C and Fe‐Cu‐C systems.</p> / Doctor of Philosophy (PhD)

Die Verschmutzung von Süßgewässern mit organischen Mikroschadstoffen ist ein Problem, das sich weltweit zunehmend verschärft. Die vorliegende Doktorarbeit soll zu einem besseren Verständnis des Verhaltens einzelner Mikroschadstoffe und deren Transformationsprodukten in Flüssen beitragen, sowie die Rolle relevanter Einflussfaktoren untersuchen. Verhalten verschiedener Stoffe wurde im Oberflächenwasser eines urbanen Flusses analysiert. Es zeigte sich, dass die Sonneneinstrahlung für einige Verbindungen der wichtigste Einflussfaktor ist, während andere eher biologisch abgebaut wurden. Die Mahd von Makrophyten hatte ebenfalls stoffspezifische Folgen auf den Abbau. Um langfristige Variabilität von Stofftransport besser zu verstehen wurde eine neue Methode zur Schätzung des Stofftransports anhand von Schwankungen der elektrischen Leitfähigkeit getestet. Einige Stofftransportparameter änderten sich über die Jahreszeiten hinweg und transiente Speicherung unterschied sich zwischen den Flussabschnitten. Um im Besonderen den Einfluss von mikrobieller Diversität und von hyporheischem Austausch zu bewerten, wurde ein Meskosmenexperiment mit 20 rezirkulierenden Fließrinnen entwickelt. Es konnte festgestellt werden, dass vor allem mikrobielle Diversität einen starken Einfluss hat. Der neue Versuchsaufbau kann zukünftig für die Untersuchung weiterer Variablen Verwendung finden. Schließlich wurden Mikroschadstoffe und Transformationsprodukte in der hyporheischen Zone der Fließrinnen analysiert. Das Verhalten war sowohl stoffspezifisch als auch fließwegspezifisch. Die Ergebnisse unterstreichen die Bedeutung des oberflächennahen, hyporheischen Austauschs auf den Stoffabbau. Im Allgemeinen konnte die hohe Variabilität des Abbaus von Mikroschadstoffen mit besonderer Relevanz der hyporheischen Zone und der mikrobiellen Diversität nachgewiesen werden. Diese Faktoren sollten in zukünftigen Forschungsvorhaben besonders berücksichtigt werden. / Contamination of freshwaters with organic micropollutants is a worldwide emerging problem. The present thesis aims to contribute to a better understanding of the variability of the behaviour of individual micropollutants, the formation of transformation products in rivers and the specific role of relevant influencing factors. The behaviour of several substances was investigated in the surface water of an urban river by accounting for spatial and temporal dynamics. Solar radiation was identified to be the major driver for some compounds, while others were more susceptible to biodegradation. The response to macrophyte removal was also compound-specific. To better understand long-term variability of solute transport on a reach-scale a new method to estimate solute transport by use of electrical conductivity fluctuations was proposed and tested. Some solute transport metrics changed over the seasons and transient storage differed between river sections. To specifically assess the influence of microbial diversity and hyporheic exchange, a mesocosm experiment with 20 recirculating flumes was developed. It was found that microbial diversity in particular had a strong impact and the novel setup was suggested to be a useful method to test other variables in the future. Finally, the behaviour of micropollutants and transformation products in the hyporheic zone of the flumes was investigated on a centimeter-scale. The behaviour was found to be compound-specific as well as flowpath-specific. But several compounds were degraded most on the shortest, most oxic flowpath. The findings highlight the importance of shallow, small-scale hyporheic exchange for turnover of micropollutants. Generally, the high variability of micropollutant degradation depending on relevant influencing factors, specifically hyporheic exchange and microbial diversity, has been demonstrated. These factors are of great importance and need to be addressed and considered in future research.